Thursday, May 5, 2022

Uranus Planet

 Astronomy

         Uranus

         Planet


 

         How long did Uranus last?

         Is Uranus a dreamy distance from the sun?

         What is the average temperature in the atmosphere of Uranus?

         How many moons and rings does Uranus have?

         What is so unusual about the axis of Uranus?

         Uranus, the seventh planet at a distance from the Sun and the four giants of the solar system, or Jupiter, the largest of the planets, including Jupiter, Saturn and Neptune.  At its brightest level, Uranus appears as a blue-green dot of light without assistance.



         Two views of the southern hemisphere of Uranus, created from images obtained by Voyager 2 on January 17, 1986.  In the colors of the human eye without any help, Uranus is a light, almost non-existent sphere (left).  Uranus shows a shared band-cloud structure for four large planets (right), in a color-changing scene for low-contrast front-to-front processing.  At this point, from Voyager's polar point of view, the bands are centered around the planet's orbital axis, which is almost pointing towards the sun.  The small features of the ring shape in the picture on the right are the patterns created by the dust in the spacecraft.

         Jet Propulsion Laboratory / National Aeronautics and Space Administration


         Uranus is named in Greek mythology for the figure of the sky and the child and husband of Gaia.  It was found by a bean in 1781. It was the first planetary epoch. It was not recognized in the prehistoric period.  Uranus was seen by many barbinians in the last century, but was rejected as another star.  Its average distance from the sun is about 2.9 billion kilometers (1.8 billion miles), which is 19 times longer than the earth, and it never gets closer to 2.7 billion kilometers (1.7 billion miles) from the earth.  Its relatively low density (only 1.3 times that of water) and its large size (four times the radius of the Earth) make it a high cement that, like other large crusts, Uranus is mainly composed of hydrogen, helium, water,  And other non-authentic compounds.  Like its brethren, Uranus has no solid surface.  In the uranium atmosphere, methane absorbs red wavelengths of sunlight, giving North Korea its blue-green color.




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         Planetary data for Uranus

         * It takes time for the planet to return to the same position in the solar system as seen from Earth.

         ** Used for heights for which results count 1 time.

         Average distance from the sun 2,870,658,000 km (19.2 AU)

         The eccentricity of the orbit is 0.0472

         The tilt of the orbit is 0.77 طرف towards the lunar eclipse

         Uranium year (by revolution) 84.02 Earth years

         Visual Speed ​​Average Update to 5.5

         Meaning synodic period * 369.6 Earth days

         Meaning orbital speed 6.80 km per second

         Equatorial radius ** 25,559 km

         Polar radius ** 24,973 km

         Mass 8.681 × 1025 kg

         Average density 1.27 g / cm3

         Gravity ** 887 cm / sec 2

         Escape speed ** 21.3 km / s

         Duration of rotation (magnetic field) 17 hours 14 minutes (retreat)

         Tilt the equator to 97.8

         The power of the logical field at the equator is 0.23 gauss

         The angle of inclination of the axis is 58.6

         The power axis of the radius of Uranus offset 0.31

         Number of known moons 27

         Planetary ring system 13 known circles


         Hubble Space Telescope: Uranus

         Hubble Space Telescope, Uranus image taken after 1998.  Showing its four large circles and its 10 satellites.

         Erich Karkoska, University of Arizona and NASA


         Most planets revolve around an axis that is more or less straight in the orbit of the orbit around the sun.  But the axis of Uranus is almost parallel to that of the orbital plane, which means that as the planet rotates, its poles turn towards the sun as it travels in its orbit.  In addition, the axis of the planet's logical field is significantly tipped over the axis of rotation and offset from the center of the planet.  Uranus has more than two dozen moons (natural planets), five of which are relatively large, and a system of narrow circles.


         Uranus has only sailed once - 1986 US Voyager 2 probe.  Before that, astronomers knew very little about it.  .  Different values ​​are generated to increase the rotation period of the planets on Earth from 24 to 13 hours to try to use the feature primarily, while Voyager 2 has a rotation period of 17.24 hours for the Uranium inner size.  Told  Establishment After the Voyager collision, advances in ground-based observation technology increased knowledge of the uranium system.


  

         From the sun to the atmosphere of Uranus, the planet completes one orbit for 84 Earth years, basically during the entire human life.  The eccentricity of its orbit is low - that is, its orbit deviates very far from a perfect circle - and the tilt of the orbit is a lunar eclipse - the plane of the Earth's orbit and the approximate plane of the solar system - less than 1.  ° Low orbital eccentricity and inclination of the solar system's planets, with Mercury and Pluto notable.  Scientists believe that collisions and gaseous drag removed energy from orbits when the planets were forming, thus reducing their eccentricity and inclination toward existing values.  Thus, about 4.6 billion years ago, immediately after the Sun's birth, Uranus formed with other planets (see Solar System: Origin of the Solar System).



         Uranus and its neighbor Neptune, the next extraterrestrial planet, are almost twin in size.  Once there is a boundary of space (equal to Earth's sea level), the equatorial radius of Uranus is 25,559 km (15,882 miles).  Is.  The difference in their bulk density - 1.285 and 1.64 grams per cubic centimeter, respectively - shows the basic difference in structure and internal structure.  Although Uranus and Neptune are significantly larger than the terrestrial planets, their pulses are less than half that of the largest planets and Saturn.  For additional orbital and physical data about Uranus, see Table.


         For this one pole is above the lunar eclipse and the other below it.  (The terms above and below refer to the sides of the eclipse that occur above the Earth's North and South Poles, respectively, regardless of the direction in which the planet is orbiting. By this definition, Uranus is at its North Pole.  In the direction of rotation, or retreat, which is the opposite of the progressive spin of most of the Earth and other planets. When Voyager 2 flew from Uranus in 1986, the North Pole was in darkness, and the Sun was almost  Right at the South Pole. 42 In North Korea, or in a year and a half a year, the sun will move almost to the top of the pole.  One evening after the event you collided with Uranus, which crashed into your country. An alternative theory is that it was a Mars-sized moon, orbiting Uranus in the opposite direction to the planet's danger, eventually colliding with the planet.  Went and dropped it on his country.


         The orbital period of Uranus was 17.24 hours when Wake 2 detected the emission of waves starting from charged particles trapped in the logical field of the planet.  A straight path later in the field shows that it is tilted at an angle of 58.6 شدت to the intensity of the axis of rotation and turns with the same duration of 17.24 hours.  These fields are thought to be the planet's electrically ascendant, for which a period of 17.24 hours is assumed to be an internal size.  Relatively fast rotation causes the poles of the planet to become thicker, or flatter, as the polar radius is about 2.3% less than the equator radius.  Clouds revolve around the planet on the visible surface as it moves through the atmosphere, during which time it can be anywhere from 18 hours near the equator to more than 14 hours at high altitudes.


         Space


         Molecular hydrogen and atom helium are two important components of the uranium atmosphere.  Hydrogen can be detected from the earth in the spectrum of sunlight scattered from the planet's clouds.  The balance of helium-hydrogen and the disturbance of the radio signal (Mo) of Voyager 2 in the atmosphere was determined as it passed behind spacecraft C.  Helium contains 15% of the total number of hydrogen molecules and helium atoms, which is equivalent to 26% of the total number of hydrogen and helium.  These values ​​are higher than the values ​​estimated for the Sun and higher than the values ​​estimated for Jupiter and Saturn.  It is assumed that the four major planets had a hydrogen-helium relationship like the Sun during their formation, but in the case of the joint and Saturn, some helium settles towards its center (see joint: ؛ Saturn:  ).  The processes that lead to this settlement in theoretical studies do not work on large planets such as Uranus and Neptune.


         Man is strongly attracted to near and long wavelengths and is exposed to the light of the reflected spectrum as the number of molecules is only 2.3%.  Astronomers have estimated that the abundance of methane uses Voyager 2 radio signals that examine the depths of the atmosphere where the hydrogen connection with methane is part of a permanent routine.  If this consistency is characteristic of the planet as a whole, then Uranus' carbon-hydrogen ratio is 24 times that of the Sun.  (Methane [CH4]] contains one atom of carbon and four hydrogen atoms.  As can be seen below. Director Observations on Earth A strange decrease in ammonia molecules appears in the atmosphere, probably due to the high concentration of hydrogen sulfide and all ammonia together to form cloud particles of ammonium hydro sulfide.  Ultraviolet spectrometers rarely detect traces of acetylene and ethane, gases of methane, which are separated when the sun's ultraviolet light hits the upper atmosphere.



         On average, Uranus releases an amount of energy at 59.1 K (K ؛ 3 353 ° F, 14214 ° C) as an ideal, absorbing surface.  This radiation temperature is about 0.4 times the equivalent of ambient temperature.  With the compounder the temperature decreases - that is, with increasing altitude - in this observation of the atmosphere this level reaches the level of millibars, where Uranus is about 52 K (−36 ° F, −221 ° C).  Cold temperatures in the atmosphere.  From this point the temperature rises again until it reaches 750 K (890 ° F, 480 C) in the outer sphere - 1.1 Uranus from the center of the planets.  Above - where the point is in order.  One trillionth.  High temperatures remain to be fixed, but may include ultraviolet absorption, electron bombardment, and failure to emit gas at weapon wavelengths.


         Voyager 2 measures the horizontal temperature of the atmosphere in the range of twice the height, measuring 60-200 mm bar and 500-1000 mm bar.  The pole-to-pole difference in both ranges is eliminated - less than 1 K (1.8 ° F, 1 ° C) - due to the fact that one pole faces the sun during the fly-by.  This reduction in global change is thought to be related to the efficient horizontal temperature transfer and greater capacity to store heat in the home.


         Although not particularly significant for comparison to Uranus, the Vail 2 contrasting fine images and recent observations of the Earth show bands of fading clouds parallel to the equator.  This type of zonal flow is common and dominates the rotation of Saturn's atmosphere, whose axis of rotation is slightly tilted from the axis of Uranus, as well as those whose climatic changes in solar light are very different.  Apparently, the rotation of the planet itself controls the distribution patterns of absorbed sunlight, not the pattern itself.  Rotation shows you through your Coriolis force, an effect that causes a rotating object to turn to the right or to the left.  In terms of the pattern being, because, Uranus looks like the tip and version of Jupiter or Saturn.



         Orbiting planets move.  At high altitude over Uranus, this nation-state moves in the direction of the planet's orbit.  The movement of women in the equator is in the opposite direction.  Uranus is like the earth in his experiments.  On Earth, these directions are called East and West, respectively, but the more common terms are development and retreat.  Many times more than the land on Uranus.  The wind blows at 200 meters per second (720 kilometers [450 miles] per hour) at 55 ° S latitude and 110 meters per second (400 kilometers [250 miles] per hour) at the equator.  Neptune's equator also retreats to the equator, but is moving towards the joint and Saturn.  There is no satisfactory theory to explain these statements.


         Jupiter's long stay in Uranus is not as big a spot as the Great Red Dot or the Great Dark spot (Neptune: see the atmosphere) seen on the Voyager 2 video Neptune in 1989.  On Uranus, there were only four small spots around Voyager whose visual contrast was not 2 or 3% higher than in the surrounding environment.  There is no solid surface, so the consensus of hurricanes to the spots is not clear because of them, it seems that Uranus also has the lowest number of hurricanes of any major planet.


         Destination field and field field

         Like the other major planets, Uranus has a dissertation field generated by convection currents in an electrically charged internal structure.  Doppol Field, which is centered on a small but time-lapse field, has a force of 0.23 gas in its equatorial plane on a field of uranium equatorial radius from the center.  The polarity of the field is based on the same direction as the current field of the earth - that is, the counterclockwise of a general article report will point to the rotating pole, which is the north pole for the earth (see: geographic field and cross field  ).  The Doppler axis rotates at an angle of 58.6 سے with a glimpse of the planet's orbital axis, which is too much for Earth 11.5 °) Jupiter (9.6 °) and Saturn (less than 1).  The nearest center is 31% (approximately 8,000 kilometers [5,000 miles]) of Uranus's radius from the center of the planet.  Migration occurs mainly along the axis of rotation towards the North Pole.



         The logical field is not only due to its unusual inclination and offset but also due to its large size in terms of small components.  This "roughness" indicates that it grows at shallow depths within the field C, as small-scale components rapidly disappear from the electrically conductive area.  Thus the common portion of Uranus, electronically closer to Saturn and Earth, is thought to be due to the fact that the internal structure of Uranus is known for its ammonia, which contains more water, methane and more than the average density of C.  Methane must be present.  Water and ammonia are separated into positive and positive ions at relatively low temperatures - which move electrically.  That together, on Saturn and Earth, this field is formed by fluid movements in the convex layers, but the layers on Uranus are not two-sided.



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         On the other hand, the path of the planets which have the field of dissertation, the field of Uranus repels the solar, the stream of charged particles which is very far from the sun.  Planetary segmentation - a large region of space in which charged particles emerge from the required field - surround the planet and view it from below.  Upstairs, the meeting of the Sun, the magnetopias; the airspace between the magnetic sphere and the sun, from the center of the planet to the hotel at 18 Uranine Place (460,000 km [286,000 miles]).


         The particles trapped inside the uranium magnetosphere contain protons and electrons, which indicates that the planet's upper atmosphere is providing most of the material.  There is no evidence of helium, which originated from the sun, or of heavy ions, which could come from the uranium moons.  The largest uranium circulates inside the silver sphere, they make some sense in trapped particles.  As they are connected to the dissertation field lines, so that the moon in the orbit that the particles trapped in the exposure lines compared to the neighboring field lines.


         Partition that is common to Saturn, particles charged from the uranium magnetosphere collide in the upper atmosphere and form auroras.  The high temperatures of the outer sphere of Uranus can hardly be (see atmosphere above).  One of the effects of high temperatures is that the atmosphere is outward, which includes rings and limits their life span by increasing the drag.  It looks like a sack that encloses with a drawstring.


         Inside out


         Although Uranus has a slightly lower density than Jupiter, it has a higher proportion of heavier elements than hydrogen and helium.  The greater mass of Jupiter (from the element of 22) leads to greater gravity and thus compresses itself against Uranus.  This extra compression adds to the bulk density of Jupiter.  If Uranus is equal to the common, it is much less.


         The various rocks (silicate and metals) recommended for Uranus, ice (water, methane, and ammonia), and gases (mainly hydrogen and helium) have different ratios.  At high temperatures and locations within the giant planets, f "actually" in the past "to keep up with the bulk density data and statistics, the chrysanthemum of ice except chit should be about 80% of the total mass.  10% for Jupiter and 2% for the composition of the Sun. All in one liquid planet, in which the gaseous light enters U in a high atmosphere. About five mega bars at the center of the planet.


         Scientists have responded to the response of fugal forces arising from the planet's rotation by obtaining information about them, along with the actual planetary response measured by Voyager 2.  By combining the force of the flattening force at the poles with the speed of rotation, the distribution of density within the dream planet can be estimated.  For two planets of the same mass and bulk density, the mass near the center is less flat than the rotation.  Before the Voyager mission, they had to choose between the three components, hard rock, ice and gas, and the ones that got along well with ice and gas.  Combining the great altitude and relatively cheap rotation for Uranus on the Voyager scale, it appears that ice and gas are well mixed and that a rocky portion is small or non-existent.



         The fact is that those who mix Uranus prefer better observations to information about the formation of the planet.  This process is made up of the center of a rock ice in changing the situation after which gas has been extracted from the solar molecule, it seems to have been incorporated into it, in favor of which, a solid budget is continuously a.  Was imprisoned on a large planet that already had a large amount.  Gas component.


         Unlike the other three major planets, Uranus does not emit much heat.  The total heat output is determined by the measurement and emission of C, while the heat input absorbs this vacuum of sunlight.  ۔  For Uranus, the ratio of the two is between 1.00 and 1.14, which means that it provides more energy to the planet than its internal energy, 14% more energy from the sun.  (For other giant planets, the equivalent relationship is greater than 1.7. For example, the heat flow from the inner part of the earth is only one tenth of the heat of the sun.)


         It is not clear why Uranus produces less heat than other living organisms.  All the planets should be warm, because the energy of gravity has not changed during this time.  Over the age of the solar system, Earth and other small companies have lost most of the heat of their formation.  Due to the massive investment in cool surfaces, however, the giant planets store heat well and deteriorate.  Therefore, the massive heat of its structure must change it, and it must escape today.  A small event (such as some planets experiencing collisions with large objects but others have not formed them and suggested a difference between the resulting giant planets)  One explanation is that Uranus produces extraordinary heat.


         Moon and rings of Uranus

         With 27 known moons of Uranus, each of the countless particles forming at least 10 circles can be considered as one moon in its orbit.  Generally, all are located close to the circle, some small moons orbiting outside the circle, the largest moon is out of orbit, and other smaller moons are farther away in orbit.  The orbits of the outermost group of moons are eccentric (long) and very inclined towards the equator of Uranus.  Other moons and rings are mainly along the equator with coplanar.



         Video of Uranus' hemisphere, orbital system, and Voyager K2 came out with images of eight of the ten tiny moons, which were shown on July 28, 199, in the 90-minute atmosphere of the Hubble Space Telescope.  The movement appears.  The rotation of the moon with the equator of Uranus and the clockwise rotation of the cloud in the planetary atmosphere.

         Erich Karkoska, University of Arizona, Takin, and NASA

         The moon of Uranus

         The five largest moons of Uranus are about 240 to 800 kilometers (150 to 500 miles) in radius.  People were grounded through binoculars, four of them before the 20th president (see observations from the ground below).  The ten smaller moons Voyager 2 highlighted in 1985-86 were estimated to be between about 10 and 80 kilometers (6 and 50 miles) in radius, and they hovered between 49,800 and 86,000 kilometers (31,000 and 53,500 miles).  But they revolve around the planet.  To reach the innermost moon, Cordelia, the outermost circles, Lambda and Epsilon.  The 11th, like the moon, was photographed by Voyager near the orbit of Belanda with a picture of Predata.  All 18 of the above people who participated in the Earth observations in 2003 are progressives from planetary divisions, with less inclination, and less eccentric orbits.



         The moon of Uranus

         Composite image of Uranus with its five large moons, mounted on Voyager 2 at one time.  From the smallest to the largest moon, Ariel, Miranda, Titania, Oberon, and Umbrella are here.

 


         Nine outer moons of about the same size met Earth in 1997 that Voyager observed.  These are irregular planets with extremely elliptical orbits which are inclined at great angles towards the planet's equator.  In the direction of all orbits except one.  Their average distance from the planet is between 4 4 and ڈالر 21 kilometers (2.5 2.5 and ڈالر 13 miles), which is 7-36 times more than the outermost powerful moon, Oberon.  Immediately after the formation of the planet, the irregular moon was caught in orbit around Uranus.  Question: The moon is probably in the orbit of its equator at the same time as the planets.  The characteristics of known Uranium moons are summarized in the table.  The names and orbital and physical characteristics are listed separately for the mass and the 10 smaller moons that Voyager actually saw the moon.


         The moon of Uranus

         The name means distance from the center of Uranus (radius of volume 3 km) Orbital distance (cedril period; day of the earth) * Tilt of the orbit of the planet's equator (degrees)  ** Radius (km) Mass (1020 kg) Average density (g / cm3)

         * Following the amount of R does not lead to a receding orbit.

         ** Values ​​of tilt in parentheses related to lunar eclipse.

         *** Scene rotation and orbital periods such as.

         Cordelia 49,800 0.335 0.085 0.0003 20

         Ophelia 53,800 0.376 0.104 0.0099 21

         Statement 59,200 0.435 0.193 0.0009 26

         Cressida 61,800 0.464 0.006 0.0004 40

         Desdemona 62,700 0.474 0.113 0.0001 32

         Juliet 64,400 0.493 0.065 0.0007 47

         $ 66,100 0.513 0.059 0.0001 68

         Rosalind 69,900 0.558 0.279 0.0001 36

         Cupid 74,392 0.613 0.099 0.0013 5

         Belanda 75,300 0.624 0.031 0.0001 40

         Perdita 76,417 0.638 0.47 0.0116 10

         86,000 0.762 0.319 0.0001 81.

         Mab 97,736 0.923 0.134 0.0025 5

         Miranda 129,900 1.413 4.338 0.0013 Scenario 235.7 0.66 1.2

         Ariel 190,900 2.52 0.041 0.0012 Imagine.  578.9 13.5 1.67

         Umbriel 266,000 4.144 0.128 0.0039 sync.  584.7 11.7 1.4

         Titania 436,300 8.706 0.079 0.0011 Concept.  788.9 35.2 1.71

         O'Brien 583,500 13.46 0.068 0.0014 Map.  761.4 30.1 1.63

         Francisco 4,276,000 266.56R (145.22) 0.1459 11

         Caliban 7,231,000 579.73R (140.881) 0.1587 36

         Stephano 8,004,000 677.36R (144.113) 0.2292 16

         Trinculo 8,504,000 749.24R (167.053) 0.22 9

         Sycorax 12,179,000 1288.3R (159.404) 0.5224 75

         Margaret 14,345,000 1687.01 (56.63) 0.6608 10

         Prospero 16,256,000 1978.29R (151.966) 0.4448 25

         Setbus 17,418,000 2225.21R (158.202) 0.5914 24

         Ferdinand 20,901,000 2887.21R (169.84) 0.3682 10

         The density of the four largest Titania, Oberon, Umbrella and Ariel - the equivalent of a reinforced moon - is 1.4–1.7 grams per cubic centimeter.  This limit is higher than the density of a hypothetical object which is to cool the solar compound and remove all gaseous substances and run it.  All that's left is 60 percent ice and 40 percent rock compared to the four Miranda, the fifth largest moon in Uranium, but only half the size of Ariel or Umbrella.  Like Saturn's small moons, Miranda's density (1.2 grams per cubic centimeter) is slightly below the solar system, due to the high ratio of ice to rock.



         Moon of Uranus: Ariel

         Ariel (White Doctor) and his shadow (Black Doctor) cross the middle of Uranus in a widely patterned image from the Hubble Space Telescope.



         Water Snow Show the Spectra of the Surface of the Five Great Moons The surface of the lunar moon is less than that of pure ice, which clearly means that they contain ice water.  The composition of the dark component is not known, but at wavelengths other than water, the surface tectonics appears to be darker, which speaks of a non-free gray color and thus rejects materials such as iron ore.  Which produces a reddish hue, a fraction of carbon, which emanates from under the moons or from the rings of Uranus, emitting methane gas, which is then bombarded by charged particles and solar ultraviolet light to produce solid carbon.  There are flowers for.  ۔



         Titania, the largest moon of Uranus, in a collection of images taken by Voyager 2 when it formed the closest approach to the uranium system on January 24, 1986.  The shape of the upper right side of the lunar disk near the terminator (night range).  The non-selective gray color of Titania represents the planet's five largest moons as a whole.

 

         Two observations show that the surface of large moons is insecure and highly insulated.  First, when the observer is within 2 سور of the sun being seen from the planet, the reflection is dramatically created.  Such so-called opposition surges are characteristic of loose-fitting particles that shadow each other, except for the special geometry in which the observer corresponds to the light source and reflects the light directly from the spaces between the particles.  Can see  Second, changes in surface temperature appear to follow the sun during the day, with no significant intervals due to thermal inertia.  Again, such behavior is characteristic of unsafe surfaces that block the internal flow of heat.



         Auburn, the largest of Uranus' five largest moons, as recorded by Voyager 2 on January 24, 1986.  This image, taken from the best of the moon, shows several large impact pits surrounded by bright rays of ejaculation.  The most notable crater, located just below Oberon's disc, has a bright central peak and a floor partially covered with black material.  Rising on the lower left limb against a dark background is a mountain approximately 6 km (4 miles) high.

         NASA / Caltech / JPL

         Practically all that is known about the specific superficial characters of Uranus's giant moons comes from Voyager 2, which passed through them in a matter of hours and photographed only their sunlit southern hemisphere.  O'Brien, and Umbrella in particular, represent the dense population of large-impact citadels, similar to the highlands of the Earth's moon and many of the oldest regions in the solar system.  In contrast, Titania and Ariel have very few large craters (50–100 km [30–60 mi] in diameter) but their numbers are comparable in smaller sizes.  Larger craters are thought to be four billion years older than the early history of the solar system, when large planets still existed, while smaller craters reflect recent events, including, perhaps, the effects of knocked objects.  Are  Loose than other moons in the uranium system.  Thus, the surfaces of Titania and Ariel should be smaller than the surfaces of Auburn and Umbrella.  These differences, which do not follow any clear pattern regarding the distance of the moon from Uranus or their size, are largely obscure.



         Umbrella, the third closest and darkest of the five largest moons of Uranus, in an image created by Voyager 2 on January 24, 1986.  Umbrella is also the heaviest and evenly crater in the large Uranine moons, indicating that very little work has been done on its surface.  Through tectonic activity in the past.  This view shows the southern hemisphere in Umbrella sunlight.  The bright ring near the moon's equator (at the top of the picture), called Wanda, is a mysterious feature that appears to line the floor of the impacting pit.

         NASA / JPL


         Volcanic deposits seen on large moons are usually flat, with shoreline and surface waves characteristic of fluid flow.  Some deposits are bright, while others are dark.  Due to the extremely low temperatures expected for the outer solar system, the erupting fluid was probably a mixture of water and ammonia, the melting point of which is below the ice of pure water.  Differences in brightness can indicate differences in the structure or surface history of the erupting fluid.



         Ariel, one of the five largest moons of Uranus, in a mosaic of photographs taken on January 24, 1986 by Voyager 2 during a flight through the Uranus system.  Small impact pits - close to the resolution limit in this image - most of the moon's surface.  The most notable features are the spots and valleys that traverse the rugged terrain.  Some valleys are partially filled with material that may have risen from the interior of the moon.

         Jet Propulsion Laboratory / National Aeronautics and Space Administration

         The raft-like valley visible on the big moons means the expansion and rupture of their surfaces.  The Miranda valleys are the most spectacular, some 80 kilometers (50 miles) wide and 15 kilometers (9 miles) deep.  The eruption of the crust was caused by an increase in the size of the moon, which is estimated to be in the range of 1-2%, except for Miranda, for which this expansion is considered to be 6%.  The spread of Miranda can be explained by the fact that all the water forming its interior is once liquid and then freezes after the formation of crust.  By freezing at low pressure, the water would expand and thus spread and disperse the surface.  Liquid water is unlikely to be present on the surface at any stage of the moon's history.



         Miranda, the innermost of the large moons of Uranus and the most diverse in terms of topography, in a mosaic of images obtained by Voyager 2 on January 24, 1986.  In this South Pole landscape, the old, heavily pitted region is connected to the great currents of youth.  , Light-pitted areas characterized by parallel bright and deep bands, spots and peaks.  The patches, called coronae, are unique to Miranda in all parts of the solar system.

         US Geological Survey / NASA / JPL

         Miranda has a mess of something made up of separate pieces that didn't fit together completely.  The base surface is very deep, but is disturbed by three light-pitted regions, which astronomers have named Coroni (but which are not geologically related to the surface features of Venus of the same name).  They are quite square in shape, approximately the length of a Miranda radius on one side, and are surrounded by parallel bands that revolve around the edges.  The boundaries where the corona meets the crater are sharp.  Corona is the opposite of the features found elsewhere in the solar system.  Whether they reflect a different origin for the moon, a larger effect that shattered it, or a unique pattern of eruption from its interior is not known.


         Ring system

         The orbits of Uranus were the first to be found around a planet other than Saturn.  Nine years before the collision of Voyager 2 in 1977, American astronomer James L. Elliott and his colleagues performed a stellar spell by Uranus, meaning that when the planet passed between a star and the Earth, the starlight  Stopping, he discovered the color system from the ground.  .  Unexpectedly, they saw the star fade briefly five times before and after landing on the planet's star at some considerable distance above the atmosphere of Uranus.  The decrease in brightness indicates that the planet is surrounded by five narrow circles.  Later ground-based observations revealed four additional circles.  Voyager 2 detected the 10th ring and found clues from others.  Outside of Uranus, 10 is named 6, 5, 4, Alpha, Beta, Eta, Gamma, Delta, Lambda and Epsilon.  This cumbersome name arose because new rings were found in places that did not match the original name.  The characteristics of the rings are given in the table.


         Rings of Uranus

         Name distance from the center of the planet (km) Observed width (km) * Equal width (km) **

         * Value range reflects real variations in latitude and measurement error.

         ** Equal width is the product of the observed width and the dimming part of the light and is given for visible light.

         6 41,837 1–2 0.66

         5 42,235 2–7 1.23

         4 42,571 1–6 1.06

         Alpha 44,718 4–11 3.86

         Beta 45,661 4–13 3.16

         Eta 47,176 1–4 0.64

         Gamma 47,627 2–8 3.13

         Delta 48,300 3–8 2.69

         Lambda 50,026 2–3 0.3

         Epsilon 51,149 20–95 42.8


         Circles are narrow and quite vague.  Observed widths are only the radial distances between the beginning and end of individual fading events.  Product of equal width radial distance (more precisely, integral) and part of the starlight is blocked.  The fact that the equivalent widths are generally less than the observed widths indicates that the circles are not completely obscure.  Combining the brightness of the circles seen in the Voyager images with the width equal to the magic shows that the colored particles reflect less than 5% of the sunlight.  Their almost flat reflection spectrum means that the particles are mainly gray in color.  Ordinary mascara, which is mostly carbon, is the closest ground analogue.  It is unknown at this time what he will do after leaving the post.


         The scattering effects on Voyager's radio signals were spread through circles on Earth, which are mostly composed of large particles, more than 140 centimeters (4.6 feet) long.  The scattering of sunlight when Voyager was far away from the circles and its camera was back towards the sun, also revealed small particles of dust in the micrometer size range.  Only a small amount of dust was found in the central circles.  Instead, most of the microscope particles were distributed in the spaces between the central circles, indicating that the circles were losing mass as a result of the collision.  The life span of dust in orbit around Uranus is limited by the planet's diffuse atmosphere and the radiation pressure of sunlight.  Dust particles move to the lower orbit and eventually fall into the uranium atmosphere.  Mathematical orbital life is so short - 1,000 years - that dust must be created quickly and continuously.  Dragging Uranus into space seems so large that current circles themselves could be short-lived.  If so, the rings did not form with Uranus, and their origin and date are unknown.


         The collision between the particles of the tightly filled ring will naturally increase the radial width of the circles.  Moons larger than rings can stop its spread in a process called shepherding.  Specific orbits that occur inside or outside the orbit of a given circle are at a suitable radius for the moon in such an orbit so that a stable dynamic resonance is established with the particles in the circle.  The condition for resonance is that the orbital periods of the moon and the particles of the circle are related to each other in the ratio of small whole numbers.  In this type of relationship, as the moon and particles pass through each other from time to time, they interact with gravity in a way that maintains the regularity of competition.  The moon applies pure torque to the ring, and as the moon and the ring exchange angular momentum, energy is dispersed by collision between the particles in the ring.  The result is that the moon and the ring particles repel each other.  Every body in the outer orbit moves outwards, while the body in the inner orbit moves inwards.  Because the moon is much larger than the ring, it prevents the ring from spreading in the radius at which it resonates.  A pair of shepherd's moons, on either side of a ring, can maintain its narrow width.


         Voyager 2 found that the innermost two moons, Cordelia and Ophelia, were needed for the shepherd to orbit on the far right in either orbit of the Epsilon ring.  Shepherds have not been observed for other circles, perhaps because the moons are too small to be seen in Voyager images.  Small moons can also be deposits that leave the color system and provide dust.



         The part of the ring system of Uranus that contains the Epsilon ring lit by its two shepherds, Cordelia and Ophelia, in a photograph obtained by Voyager 2 on January 21, 1986, of the spacecraft's Urine.  Three days before the closest approach to the system.  Many other rings of Uranus can be seen on the inside of the Epsilon ring.

         Jet Propulsion Laboratory / National Aeronautics and Space Administration

         Observations from the ground

         Uranus was discovered by the English astronomer William Herschel, who surveyed all the stars below the eighth magnitude - the stars that are five times weaker than the stars visible to the naked eye.  On March 13, 1781, he discovered "a curious star, or perhaps a comet," distinguishing it from a disk clearly visible to the stars.  With no trace of its tail and its slow movement, it came to the conclusion within months that the object was a planet, rather than a comet, orbiting Saturn in an almost circular orbit.  Observations of the new planet over the next 65 years revealed discrepancies in its orbital motion - evidence of the forces of gravity on Uranus that were not due to any other known planet, which eventually led to the discovery of Neptune in 1846.  Made



         Herschel suggested the name of his new discovery Georgium Siddus (Latin: "Georgian Star"), but Herschel and others called it the "Georgian Planet" - in honor of their patron, King George III of England, while the French named Herschel's  Name supported.  The planet was eventually named after the Greek and Roman mythological deities.  Uranus is the father of Saturn, who in turn is the father of Jupiter.


         The orbit of Uranus seems to fulfill a simple experimental principle, the prediction of Baude's law, which was formulated in 1766 and became popular in 1772 to measure the Earth's orbital distance from the Sun and the five planets known to the ancients.  To be explained.  In addition, where the law predicted another planet between Mars and Jupiter, the planets appeared to be filling the gap, beginning in 1801 with the discovery of the largest planet, Ceres.  For almost three-quarters of a century, these achievements overcame doubts.  From the fact that the law had no ideological basis and that it provided only an approximate fit for the orbits of the planets.  Neptune did not fit this pattern at all (approximately 21% closer to the Sun as predicted by the law), nor did Pluto, and now Bod's law is only historically significant.


         After the discovery of Uranus, Herschel continued to observe it with larger and better telescopes, and finally in 1787 discovered his two largest moons, Titania and Oberon.  The absence of these moons was not realized until the middle of the 19th century, despite an almost complete lack of confirmation from other astronomers.  Did  The Four Moons comes from English literature, taken from the characters of William Shakespeare and Alexander Pope, and was suggested by Herschel's son John.  (The names of the children of Uranus, the Titans, have already been assigned to the moons of Saturn.)  The works of Shakespeare and the Pope continued to apply to later discoveries.


         Search for the spacecraft


         In this computer animation of the Voyager 2 space probe, discover Uranus' nightside and ring system as it emerges from the planet's solar system.

         This computer animation shows the Voyager 2 space probe with the planet Uranus on January 24, 1986.  As the spacecraft moves toward the planet's night shore, Uranus's system of thin circles becomes increasingly visible.  Near the end of the sequence, the distant sun passes behind Uranus, while Voyager 2 begins to move away from the solar system at its own speed.

         NASA

         Watch all the videos for this article

         Although the twin Voyager 1 and 2 spacecraft missions originally required only the fly-bikes of Jupiter and Saturn, the launch time of the Voyager 2 allowed it to change its speed to allow Uranus and Neptune to launch an expansion mission.  But could be targeted again.  Was finally done.  After more than eight years in space, Voyager 2 passed through the uranium system on January 24, 1986.  His instruments accurately determined the size and radiology of the planet and its large moons, detected the magnetic field of Uranus and determined its strength and direction.  , And measured the rate of internal rotation of the planet.  Images of the Uranium system, numbering more than 8,000, show for the first time the weather patterns in the planet's atmosphere and the surface features of the moon.  In addition to Voyager's discovery of the new moon, a ring, and the dust band between the rings, he provided details of the structure of the ring on a non-ground scale.  Yet, despite these successes, Voyager has left many unanswered questions that only one other spacecraft could solve with a major breakthrough in mission or ground-based observation technology.  No future missions are planned for Uranus.

Wednesday, May 4, 2022

Earth's magnetic field

 Earth's magnetic field


 , Geographic magnetism, terrestrial magnetism

  


 

  Geographical field, the magnetic field attached to the earth.  It is basically bipolar at the surface of the earth (that is, it has two poles, the geographic north and south).  Dupole distorts off the surface.




  The magnetic field of a bar magnet



 

   Polar polar orbital magnetic storm electro jet chapman ferro current system

 


  Understand the geographical area of ​​the earth through the principle of dynamo effect.

  The currents in the center of the earth create a magnetic field according to a principle called the dynamo effect.

 

  In the 1830's, the German mathematician and astronomer Carl Friedrich Gass studied the Earth's magnetic field and concluded that the principal Doppler component is inside the Earth rather than outside.  It showed that the doppler component was a decreasing function inversely proportional to the square of the Earth's radius, a result that led scientists to speculate on the origin of the Earth's magnetic field in terms of ferromagnetism (such as a huge bar).  In the magnet), different rotation theories, and different dynamo theories.  Theories of ferromagnetism and rotation are generally discredited - ferromagnetism because the curry point (the temperature at which ferromagnetism is destroyed) reaches only 20 kilometers or more (approximately 12 miles) below the surface.  There is, and is, a theory of rotation because there seems to be no fundamental relationship between mass.  Movement and its associated magnetic field.  Most geomagnetists find themselves dealing with various dynamo theories, according to which a source of energy in the center of the earth causes a self-sustaining magnetic field.



  Earth's stable magnetic field is created by sources both above and below the surface of the planet.  Outside the cover, these include geomagnetic dynamos, crystal magnetization, ion spherical dynamos, ring currents, magnetopaz currents, tail currents, field-connected currents, and orbital or connective electro jets.  Geomagnetic dynamo is the most important resource because, without this field, there would be no other resource.  The effect of other sources, not more than the surface of the earth, is just as strong or stronger than that of a geomagnetic dynamo.  In the ensuing discussion, each of these sources is considered and the reasons given are explained.


  Earth's magnetic field is subject to change at all times.  Each of the major sources of the so-called stable field undergoes changes that cause temporary variations, or disruptions.  There are two major obstacles in the main field: cosperiodic reversals and secular transformation.  The ionospheric dynamo is concerned with seasonal and solar cycle changes, as well as solar and lunar marine effects.  The current of the ring responds to the solar wind (the ionized atmosphere of the sun which spreads outwards in space and carries with it the solar magnetic field), the strength increases when the proper conditions of the solar wind are present.  There is another phenomenon associated with the development of ring current, the magnetospheric substorm, which is most clearly seen in the aurora borealis.  A very different type of magnetic variation is caused by magnetic hydrodynamic (MHD) waves.  These waves are sinusoidal changes in the electrical and magnetic fields that are associated with changes in particle density.  These are the means by which information about changes in electromagnetism is transmitted, both inside the earth and in the atmosphere around charged particles.  Each of these sources of change is also discussed separately below.



  The position of the Earth's geographic North Pole

  A map of the Earth's Arctic region marks the known geographical locations and times of the North Pole since 1900.

  Encyclopædia Britannica, Inc./Kenny Chmielewski

  Observation of the Earth's magnetic field

  Field representation


  The electric and magnetic fields are created by the electric charge, a basic property of matter.  Electric fields are created by charges more comfortable than an observer, while magnetic fields are created by moving charges.  The two fields are different aspects of the electromagnetic field, this is the force that causes the electric charges to interact with each other.  The electric field, E, is defined as the force per unit charge at any point around the distribution of charge when a positive test charge is placed at that point.  For point charges, the electric field refers to a positive charge radically far and a negative charge.


  A magnetic field is created by moving charges.  Magnetic induction, B, can be defined as E. The force per unit is proportional to the strength of the pole when the test magnetic pole is brought close to the source of the magnet.  However, it is more common to define it with the Lorentz-force equation.  This equation states that the force felt by a charge q, moving with velocity v, is given by it.

  F = q (vxB).


  In this equation, bold letters indicate vectors (quantities that have both intensity and direction) and non-bold letters indicate scalar quantities such as B, length of vector B.  x represents a cross product (ie, a vector at right angles to both v and B, along the length vB ​​sin θ).  Theta vectors is the angle between v and b.  (B is commonly referred to as a magnetic field despite the fact that the name H is specific to quantities, which is also used in the study of magnetic fields.) For a simple line current, the field is cylindrical around the current.  The sense of field depends on the direction of current, which is defined as the direction of movement of positive charges.  The principle of the right hand defines the direction of B by stating that when the thumb points in the direction of the current, it points in the direction of the fingers of the right hand.



  In the International System of Units (SI), the electric field is measured in terms of potential conversion rate, volts per meter (V / m).  Magnetic fields are measured in Tesla (T) units.  Tesla is a large unit for geophysical observations, and a smaller unit, nanotesla (nT; one nanotesla equals 10−9 Tesla), is commonly used.  A nanotisella is the equivalent of a gamma, a unit originally defined as 10−5 gas, which is a unit of magnetic field in a centimeter second system.  Both Goss and Gamma are still widely used in the literature on geo-magnetism, although they are no longer standard units.


  Both the electric and magnetic fields are represented by vectors, which can be represented in different coordinate systems, such as Cartesian, polar, and spherical.  In the Cartesian system the vector is divided into three components which are approximated by the vector on three mutual orthogonal axes which are usually labeled x, y, z.  The vector at polar points is usually expressed by the length of the vector in the x-y plane, its angle of inclination in the plane relative to the x-axis, and the third Cartesian z component.  In spherical points, the field is defined as the total field vector length, the polar angle of the vector from the z axis, and the azimuth angle of the projection of the vector in the x-y plane.  All three systems are widely used in the study of the Earth's magnetic field.


  The names used in the study of geomagnetism for the various components of the vector field are summarized as follows.  B is the vector magnetic field, and F is the intensity or length of B.  X, Y, and Z are the three Cartesian components of the field, usually measured with reference to the geographical coordinate system.  X is to the north, Y is to the east, and, completing the right-hand system, Z is to the center of the earth vertically.  The magnitude of the field presented in the horizontal plane is called H.  This projection forms an angle D (for fall) from north to east.  Dip angle, I (for tilt) is the angle formed by the total field vector with respect to the horizontal plane and is positive for the vector below the plane.  This completes the normal polar angle of spherical points.  (Geographic and magnetic north meet the "Egonic Line".)



  Components of magnetic induction vectors

  The components of the magnetic induction vector, B, are shown in three integrated systems: Cartesian, Polar, and Spherical.

  Encyclopedia Britannica, Inc.

  Field measurement

  Magnetic fields can be measured in different ways.  The simplest measurement technique still used today involves the use of a compass, a device consisting of a permanent magnetic needle that is balanced to the axis in a horizontal plane.  In the presence of a magnetic field and in the absence of gravity, a magnetic needle aligns itself perfectly with the magnetic field vector.  When it is balanced on the axis in the presence of gravity, it attaches to a component of the field.  In the traditional compass, it is a horizontal component.  A magnetic needle can also be axial and balanced on a horizontal axis.  If this instrument, called a deep meter, is first pointed in the direction of a magnetic meridian by a compass, then the needle lines up with the total field vector and measures the angle of inclination I.  Finally, it is possible to measure the intensity.  Horizontal field through the doubles of the compass needle.  It can be shown that the duration of such oscillation depends on the characteristics of the needle and the strength of the field.



  Magnetic observatories constantly measure and record the Earth's magnetic field at various locations.  In such an observatory, magnetic needles are suspended by quartz fibers with a reflecting mirror.  Photographs mounted on the drum are photographed negatively as the rays of light reflected from the mirror rotate.  Variations in the field cause a relative deviation from the negative.  Typical scale factors for such observatories are 2–10 nanotypes per millimeter vertically and 20 millimeters per hour horizontally.  The printed negative print is called a magnetogram.


  Magnetic observatories have recorded data in this way for over 100 years.  Their magnetograms are photographed on microfilm and submitted to global data centers, where they are available for scientific or practical use.  Such applications include the creation of magnetic maps of the world for navigation and surveys.  Correction of data obtained from air, land and sea surveys for mineral and oil reserves;  And the scientific study of the sun's interaction with the earth.


  Other methods of measuring magnetic fields have become more convenient in recent years, and older instruments are slowly being replaced.  One such method involves a proton-precision magnetometer, which utilizes the magnetic and gyroscopic properties of protons in liquids such as gasoline.  In this method, the magnetic moment of the proton is first connected to a strong magnetic field produced by the outer coil.  Then the magnetic field suddenly stops, and the protons try to align themselves with the earth's field.  However, since protons are magnetic as well as rotating, they move with a frequency around the Earth's field, depending on the intensity of the latter.  The outer coil senses the weak voltage generated by this gear.  The duration of gyration is determined electronically with sufficient accuracy to produce sensitivity between 0.1 and 1.0 nanotesla.



  One device that complements the proton-precision magnetometer is the Flexgate magnetometer.  Unlike a proton-precision magnetometer, the FluxGate device measures the three components of a field vector rather than its amplitude.  It has three sensors, each connected to one of the three components of a field vector.  Each sensor is made of a high permeability material (e.g., mu-metal) wound from a transformer wound around the core.  The main winding of the transformer is excited with a high frequency (approximately 5 kHz) sine wave.  In the absence of any field along the axis of the transformer, the output signal in the secondary winding consists of only odd harmonics (component frequencies) of the drive frequency.  If, however, a field exists, it biases the hysteresis loop in one direction to the core.  As a result, one half of the drive cycle covers more quickly than the other.  As a result, the secondary voltage incorporates all the coordinates as well as the oddity.  The amplitude and phase of the avon harmonics are linearly proportional to the field component along the axis of the transformer.


  Most modern magnetic observatories have both proton-precision magnetometers and flux gate magnetometers mounted on granite columns in non-magnetic, temperature-controlled rooms.  The output from the devices is electrical signals, and they are digitized and recorded on magnetic media.  Many observatories also transfer their data to central facilities immediately after acquisition, where they are stored in a large computer database with data from other locations.


  Magnetic measurements are often made at locations far from designated observatories.  Such measurements are usually part of a survey designed to better describe the Earth's central field or to detect anomalies in it.  Such surveys are usually carried out on foot, by plane, by air and by space.  The proton-precision magnetometer is almost always used for surveys near the surface of the earth because it does not need to be attached.  The central field above ground level is rapidly declining, and the need for precise alignment is less acute.  Thus, flex gate magnetometers are typically mounted on a spacecraft.  Knowledge of the location and direction of a spacecraft is required to calculate the components of a vector field in a ground coordinate system.


  Characteristics of Earth's Magnetic Field

  The magnetic field observed on the surface of the earth is like a magnet attached to the planet's rotating axis.  Statistics show such a field for a bar magnet located in the center of a sphere.  If the Earth is taken along the North Geographic Pole at the top of the diagram, then the direction of the magnet along its North Magnetic Pole should be downwards towards the South Geographic Pole.  Then, as shown in the diagram, the lines of the magnetic field leave the north pole of the magnet and rotate until they cross the Earth's equator, pointing north geographically.  ۔  They orbit the earth further in the northern latitudes, eventually returning to the south pole of the magnet.  At present, the North Pole equals the bar equal to the South Pole of the magnet.  This has not always been the case.  Many times in the history of the earth the direction of the equivalent magnet has been pointed in the opposite direction

Tuesday, May 3, 2022

NEPTUNE PLANET

 Neptune


 

  What does Neptune look like?

  Neptune's moon

 

  Neptune is the eighth planet from the Sun in our solar system.  According to NASA, this blue gas giant is much larger than Earth, 17 times the mass of Earth and about 58 times the volume of Earth.  The rocky portion of Neptune is surrounded by a muddy liquid mixture of water, ammonia, and methane ice.


 

  Astronomer Galileo Galilei was one of the first to identify Neptune as a space object, but he assumed it was a star based on its slow motion.  Nearly two hundred years later, in 1846, the French astronomer Erbine Jean-Joseph Le Warrier estimated the location of Neptune by studying the gravitational disturbances in the movements of Uranus, according to researchers at the University of St Andrews in Scotland.  According to a summary.  .


  

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  At the same time, Le Warrier was calculating the existence of Neptune, as was the English astronomer John Couch Adams.  The two scholars independently made almost identical mathematical predictions about the existence of Neptune.  Le Warrier then reported his calculations to his colleague, the German astronomer Johann Gottfried Gale, and Gale and his assistant Henrik de Aristt, after seeing Neptune through binoculars at his observatory in Berlin, identified it.  Confirmed Le Warrier's predictions.


  According to all the other planets in the sky, and as Le Warrier suggested, this new world was given a name from Greek and Roman mythology - Neptune, the Roman god of the sea.


  Related: The Biggest Mystery About Neptune


 

  The only mission Neptune flew was Voyager 2 in 1989.  Even today, many mysteries remain about the cold, blue planet, such as why its winds are so strong and why its magnetic field is moving.  Although Neptune is of interest because it is in our own solar system, astronomers are also interested in learning more about the planet to help study the exoplanet.  In particular, astronomers are interested in learning about the habitation of a world larger than Earth.


  Like Earth, Neptune has a rocky center, but its atmosphere is so thick that it forbids the existence of life as we know it.  Astronomers are still trying to figure out where the planet is so large that a large amount of gas could accumulate in its area, making life difficult or impossible.


  What does Neptune look like?

  The result of the absorption of red light by methane into the still unknown compound and most of the planet's hydrogen helium atmosphere.


  Despite Neptune's distance from the sun, which means it receives very little sunlight to help warm and run its atmosphere, Neptune's winds can reach 1,500 miles per hour (2,400 kilometers per hour).  Is the fastest ever in the solar system.  The winds were linked to a major black storm that Voyager 2 tracked in the southern hemisphere of Neptune in 1989.  This elliptical, clockwise "Great Dark Spot" was large enough to envelop the entire earth, and moved westward at a speed of about 750 miles per hour (1,200 kilometers per hour).  The storm disappeared when the Hubble Space Telescope searched for it in later history, and since then, Hubble has seen the appearance and reappearance of other great black spots on Neptune over the past decade.


  Due to the high temperature and pressure on Neptune and Uranus, scientists believe that compressed carbon in the form of diamonds causes a "diamond rain" phenomenon on these icy giants.  In 2017, researchers were able to mimic the conditions that lead to the formation of diamonds in the lab, supporting the hypothesis that diamonds rain down on Neptune and Uranus.


 


  Ultrasonic Neptune is photographed using a ground-based telescope.

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  Neptune is surrounded by unusual circles, which are not uniform, but have bright thick clumps of dust called arcs.  Rings are thought to be relatively young and short-lived.  According to an article in the journal Icarus, ground-based observations announced in 2005 found that Neptune's rings were apparently more unstable than previously thought, with some rapidly declining.


  Neptune's magnetic poles are pointed at about 47 degrees relative to the poles with which it rotates.  Thus, the planet's magnetic field, which is about 27 times stronger than the Earth's, passes through wild swings during each rotation.


  By studying the formation of clouds on the gas giant, scientists have been able to calculate that a day on Neptune is less than 16 hours.  Neptune's elliptical, elliptical orbit keeps the planet approximately 2.8 billion miles (4.5 billion kilometers) or about 30 times farther from the Earth, which makes it invisible to the naked eye.  Neptune orbits the Sun about once every 165 Earth years, and completes its first orbit since its discovery in 2011.


  Every 248 years, Pluto orbits Neptune for 20 years or more, during which time it is closer to the Sun than Neptune.  Nevertheless, Neptune is the farthest planet from the Sun, as Pluto was reclassified as a dwarf planet in 2006.


  Neptune's moon

  Neptune has 14 well-known moons, named after lesser sea gods and nymphs than Greek mythology.  The largest Triton to date, discovered indirectly through beer on October 10, 1846 - amateur astronomer William Lasell, who discovered Triton, a wine maker to finance his telescopes.  Used funds created as


  Quick facts about Neptune

  - Atmosphere composition (by volume): 80% hydrogen, 19% helium, 1.5% methane


  - Magnetic field: about 27 times more powerful than the earth


  - Mass Composition: 25% rock, 60-70% ice, 5-15% hydrogen and helium


  - Internal structure: mantle mantle of water, ammonia and methane ice;  Iron and magnesium silicate core


  - Average distance from the sun: 2,795,084,800 miles (4,498,252,900 kilometers) (30,069 times higher than Earth)


  - Pierre Helen (closest view to the Sun): 2,771,087,000 miles (4,459,630,000 km) (29.820 times the Earth)


  - Ophelon (longest distance from the Sun): 2,819,080,000 miles (4,536,870,000 km) (30,326 times the Earth)


  (Source: NASA)


  Triton is Neptune's only spherical moon.  The other 13 moons of the planet are randomly shaped.  Triton is also unique as being the only large moon in the solar system to orbit its planet in the opposite direction of its planet's rotation - this "backward orbit" suggests that Triton may have been a dwarf planet someday.  Which was captured by Neptune instead of being in place.  According to NASA.  Neptune's gravity is bringing Triton closer to the planet, meaning that millions of years from now, Triton will be so close to the forces of gravity that it will tear it apart.


  Triton is extremely cold, with its surface temperature reaching about minus 391 degrees F (minus 235 degrees Celsius), making it one of the coldest places in the solar system.  Nevertheless, Voyager 2 detected a geyser spewing more than 5 miles (8 km) of icy matter, indicating that its interior appears warm.  Scientists are investigating the possibility of an underground ocean on an icy moon.  In 2010, scientists discovered seasons on Triton.


  Related: What would it be like to live on Neptune's moon Triton?


  In 2020, NASA announced the possibility of a new space mission to visit Triton, called Trident.  "Triton has always been one of the most intriguing and intriguing bodies in the solar system," said Louise Proctor, director of the Lunar and Planetary Institute at the Universities Space Research Association in Houston.


  In 2013, scientists working with SETI used data from the Hubble Space Telescope to observe Neptune's "lost" moon.  The 62-mile-wide (100 km) moon has been missing since Voyager 2 was discovered in 1989.


  Also in 2013, scientists using the Hubble Space Telescope discovered the 14th moon, called S / 2004 N 1.  It is the smallest moon in Neptune and is only 11 miles (18 kilometers) wide.  It got its temporary name because it is the first satellite (S) of Neptune (N) to be found in photographs taken in 2004.

PLOTO PLANE

 Astronomy

   Pluto

   Dwarf planet


 


 

   Is Pluto a planet?

   Who Discovered Pluto?

   How far is Pluto from the sun?

   Is Pluto's orbit circular or eccentric?

   Does Pluto have a moon?

   Pluto, the largest, most distant member of the solar system, was previously thought to be the outermost and smallest planet.  It was also considered to be the most recently discovered planet, discovered in 1930.  In August 2006, the International Astronomical Union (IAU), which has been accused by the scientific community of classifying astronomical objects, voted to remove Pluto from the list of planets.  This is a new classification of dwarf planets.  This change reflects astronomers' realization that Pluto is a major member of the Kuiper Belt, a collection of ice and rock debris left over from the formation of the solar system and is now orbiting the sun outside Neptune's orbit.  ۔  (For further discussion of the IAU difference between a planet and a dwarf planet and the change in Pluto's classification, see Planet.)



   Pluto

   Pluto as observed by the New Horizons spacecraft, July 13, 2015.

   NASA / Johns Hopkins University Applied Physics Laboratory / Southwest Research Institute


   Pluto cannot be seen in the night sky without the aid of the eye.  Its largest moon, Charon, is so close in size to Pluto that it has become common for two bodies to be called double systems.  Pluto is designated by the symbol.



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   Pluto is named in Roman mythology for the god of the underworld (the Greek equivalent of heads).  It is so far away that sunlight, which travels at about 300,000 kilometers (186,000 miles) per second, takes more than five hours to reach it.  An observer standing on the surface of Pluto will see the sun as a very bright star in the dark sky, giving Pluto an average of 1 / 1,600 of the sunlight reaching the earth.  Pluto's surface temperature is so cold that ordinary gases such as nitrogen and carbon monoxide are present there as ice.


   Due to Pluto's remoteness and small size, even the best binoculars on Earth and in Earth's orbit can handle very little detail of its surface.  In fact, for decades, it has been difficult to determine basic information such as its radius and mass.  Pluto was not visited in July 2015 by the New Horizons, a US spacecraft that flew via Pluto and its four satellites, which answered many important questions about it and its environment.


   Basic astronomical data


   Pluto's average distance from the Sun, about 5.9 billion kilometers (3.7 billion miles or 39.5 astronomical units), gives it a larger orbit than the outermost planet, Neptune.  (An astronomical unit [AU] is the average distance of the Sun from the Earth; about 150 million kilometers [93 million miles].) Its orbit, in comparison to the planets, is unusual in many ways.  It is longer than any of the orbits of the planets, or eccentric, and more inclined towards the lunar eclipse (at 17.1)), the plane of the Earth's orbit, near which the orbits of most of the planets are located.  Traveling on its eccentric path around the Sun, Pluto differs from 29.7 AU, at its closest perihelion, to 49.5 AU, at its farthest aphelion.  Because Neptune rotates in an almost circular path at 30.1 AU, Pluto is for a small fraction of each revolution that is actually closer to the Sun than Neptune.  However, the two bodies will never collide, as Pluto is locked in a 3: 2 stabilization echo with Neptune.  That is, it completes two revolutions around the sun at exactly the same time that Neptune takes to complete three.  This interaction of gravity affects their orbit in such a way that they can never pass close to 17 AU.  Pluto last reached Perry Helen in 1989.  For about 10 years before and after that time, Neptune was farther from the sun than Pluto.


   Earth observations have shown that Pluto's luminosity varies with the duration of 6.3873 Earth days, which is now well established as the period of its rotation (cidral day).  Of the planets, only Mercury, which has a rotation period of about 59 days, and Venus, with 243 days, rotate more slowly.  Pluto's axis of rotation is at an angle of 120 ول to the length of its orbit, so that its north pole actually points 30 ° down from the plane.  (According to the convention, the top of the plane is taken in the direction of the Earth and the North Pole of the Sun; below, in the opposite direction.  Tilted.) This way Pluto rotates almost in a reverse direction (opposite the direction of rotation of the sun and most of the planets);  On its surface an observer would see the sun rising in the west and setting in the east.


   Compared to the planets, Pluto is also unique in its physical properties.  Pluto's radius is less than half that of Mercury.  It is only two-thirds the size of the Earth's moon.  Next to the outer planets - Jupiter, Saturn, Uranus and Neptune - it is surprisingly small.  When these properties are combined with what is known about its density and structure, Pluto seems to have more in common with the large icy moons of outer planets than with any other planet itself.  Its nearest twin is Neptune's moon Triton, which represents the same origin for both bodies (see Origin of Pluto and its moon below).  For additional orbital and physical data about Pluto, see Table.


   Basic data for Pluto

   * Pluto needs time to return to the same position in the sky as the sun, as seen from Earth.

   ** The smallness of deviation from the cedral day is due to the very large orbit of Pluto.

   Average distance from the sun 5,910,000,000 km (39.5 AU)

   The eccentricity of the orbit is 0.251

   The inclination of the orbit towards the lunar eclipse is 17.1

   Plutonian Year (Revolutionary Period) 247.69 Earth years

   Visual Intensity on Average Opposition 15.1

   Mean synodic period * 366.74 Earth days

   The average orbital speed is 4.72 km / s

   Radius 1,185 km

   Mass 1.2 x 1022 kg

   The average density is about 2 g / cm

   The average surface gravity is 58 centimeters per second

   Escape speed 1.1 km per second

   Circulation duration (Plutonin ciderl day) 6.3873 Earth days (retreat)

   Plutonin ie solar day ** 6.3874 Earth days

   Tilt of the equator towards the orbit (slant) 120

   The average surface temperature is about 40 K (8387 ° F, −233 ° C).

   Surface pressure (near paraffin) about 10−5 bar

   Number of known moons 5


   Pluto and Charon

   A mix of fine color images of Pluto (right) and Charon (left) taken by the New Horizons spacecraft.

   NASA / JHUAPL / SwRI

   Pluto's atmosphere

   Although the discovery of methane ice on the surface of Pluto in the 1970s (see surface and interior below) convinced scientists that the body has an atmosphere, it will have to wait until the next decade for direct observation.  Its atmosphere was discovered in 1988 when Pluto passed in front of a star as observed from Earth.  Before Pluto's disappearance, the star's light gradually dimmed, indicating the presence of a thin, very diffused atmosphere.  Since Pluto's atmosphere must contain vapor in balance with its ice, small changes in temperature must have a large effect on the amount of gas in the atmosphere.  During the years around Pluto's Peri Helen in 1989, when Pluto was a little colder than average, most of its frozen gases evaporated.  At that time the atmosphere was at or near its densest, which made it a good time to study the body.  In the year 2000, astronomers estimated the surface pressure in the range of a few to tens of microbars (one microbar is one millionth of the surface pressure of the earth).  In aphelion, when Pluto is receiving minimal sunlight, its atmosphere cannot be identified at all.



   A layer of fog over Pluto

   A layer of fog over Pluto, as observed by New Horizons.

   NASA / JHUAPL / SwRI

   Observations made during the magic show that nitrogen was the basic gas in the plutonium atmosphere, which also contained small amounts of methane, carbon monoxide and hydrogen cyanide.  (Nitrogen is an important component of Triton and Saturn's largest satellite, Titan, as well as the Earth's atmosphere.) During their flight, New Horizons determined the surface pressure to be 10 microbars, including acetylene, ethylene and ethane.  Found  Space.  The temperature near the surface is 45 K (−228 ° C, or 7379 ° F).  Fog layers can be seen up to 200 km (120 miles) high.  The upper atmosphere is quite expansive, moving 1,800 kilometers (1,100 miles) above the surface, and is quite cold, which prevents nitrogen from entering space.



   New Horizons near Pluto

   Artist offering New Horizons spacecraft approaching Pluto and its three moons.

   NASA / Johns Hopkins University Applied Physics Laboratory / Southwest Research Institute

   Surface and interior


   New Horizons observed only one hemisphere of Pluto.  This hemisphere is dominated by the Tombaugh Regio, a white heart-shaped field.  The western half of the Tombaugh Regio is Sputnik Planitia, a flat area of ​​nitrogen ice that has no effect.  The lack of craters suggests that Sputnik Planetia is a very young feature and thus Pluto may have some geological activity.  The Tombaugh Regio is surrounded by low-lying areas with some mountain ranges.  These mountains are made of water ice, which is probably floating in the surrounding nitrogen ice.  The upper northern latitudes are covered by deep plains.  Tombaugh is the darkest region of Pluto, west of the Regio.  Originally nicknamed the "Whale" because of its shape and later called the Chattulho Reggio, the region has a diverse topography with plains, spots, mountains and strongholds.  The darker color of this region is formed by organic compounds called tholan.



   Mountains on Pluto

   A close-up view of the mountains and plains on Pluto via the New Horizons spacecraft.

   NASA / JHUAPL / SwRI

   Pluto's average reflection, or albedo, is 0.72 (that is, it returns 55% of the light that falls on it), compared to 0.1 for the moon and 0.8 for Triton.  However, it covers a wide range of average albedo reflections, ranging from 0.1 to 0.2 for the Chattulho Regio and 0.8 to 1 for the Tombao Regio.


   The first crude infrared spectroscopic measurements (see Spectroscopy), performed in 1976, revealed the presence of solid methane on the surface of Pluto.  Using new ground equipment available in the early 1990's, observers discovered ice of water, carbon monoxide, and molecular nitrogen.  Although the spectral signature of nitrogen is very weak internally, it is now clear that this substance must be part of the dominant surface.  Methane is present in pure methane ice patches and in nitrogen ice as a frozen "solution" of methane.



   Sputnik Planetia on Pluto

   High resolution image of Pluto taken by New Horizons spacecraft, combined with blue, red and infrared images taken by Ralph / Multispectral Visual Imaging Camera.  The bright spread is the western lobe of the "heart" called Sputnik Planetia, which has been found to be rich in nitrogen, carbon monoxide and methane ice.

   NASA / Johns Hopkins University Applied Physics Laboratory / Southwest Research Institute

   Pluto has a density of 1.85 grams per cubic centimeter, and Charon has a density of 1.7 grams per cubic centimeter.  These values ​​indicate that both bodies contain a significant portion of the material, such as silicate rock and organic compounds, denser than water ice (at 1 gram per cubic centimeter).  The low density of charon may be due to its being more insecure or being a smaller part of the rock.  Like the icy moons of Pluto, Jupiter and Saturn, there is probably an inner rocky mass surrounded by a thick sheet of water ice.  The frozen nitrogen, carbon monoxide and methane visible on its surface are in the form of a relatively thin layer, similar to the water layer on the surface of the earth.  Sputnik Planitia is a deep basin that may have formed as a result of an impact.  It is located on the ocean axis of Pluto.  That is, it is in the opposite direction of the four dwarf planets.  The location of Sputnik Planitia requires extra mass beneath it, and this extra mass can be from the ocean floor above the rock cover and below the mantle of water ice.



   Pluto sunset scene

   Pluto's New Horizons image shows icy mountains, flat plains, and layers of fog in the air.

   NASA / JHUAPL / SwRI

   Pluto's moon

   Pluto has five well-known moons.  Charon, the largest ever, is about half the size of Pluto.  It revolves around Pluto - more precisely, the two objects revolve around a common center - at a distance of about 19,640 kilometers (12,200 miles), approximately equal to eight Pluto diameters.  (In contrast, the Earth's moon is slightly more than a quarter of the size of the Earth and later about 30 times the diameter of the Earth.)  In other words, Charon is in orbit around Pluto.  As a result, Charon is visible from only one hemisphere of Pluto.  It stays in the same position on the surface of Pluto, never rises or sets (as communications satellites do in geostationary orbit above the earth; see space flight: Earth's orbit).  Also, like most moons in the solar system, Charon is in a state of harmonious rotation.  That is, it always presents the same face to Pluto.



   Pluto  Four

   Pluto and its largest moon, Charon (left), as seen by the New Horizons spacecraft.  They revolve around their center of gravity, and the four always face the same hemisphere as Pluto.  Charon also always represents the same hemisphere because it is in a state of synchronous rotation.  That is, it rotates on its axis at the same time as it orbits Pluto.

   NASA / Johns Hopkins University Applied Physics Laboratory / Southwest Research Institute


   Charon is slightly less reflective than Pluto (less albedo - about 0.25) and more neutral in color.  Its spectrum reflects the presence of water ice, which is the dominant component of the surface.  There is no indication of solid methane that is so obvious to its larger neighbor.  There are also ammonia spots in some of its influential pits on the surface of Charon.  As discussed above on the surface and in the interior, the density of four means that the moon contains substances such as silicates and organic compounds that are denser than water ice.  For additional data about Charon, see Table.



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   Pluto's moon

   The name means distance from the center of Pluto (radius 3 km) orbital distance (cedril period; day of the earth) Tilt of the orbit Towards the equator of the planet (degree) Eccentricity of the orbit

   Four 17,536 6.387 0 0.0022

   Styx 42,000 20.2

   Nix 48,708 24.86 0.195 0.003

   Kerberos 59,000 32.1

   Hydra 64,749 38.2 0.212 0.0051

   Name Rotation Length (Earth Day) * Radius or Radial Dimension (km) Mass (1020 kg) Average Density (g / cm3)

   * Synchronization = synchronous rotation;  Rotation and orbital periods are the same.

   Charon Sync.  604 15 1.63

   Styx 10-25

   Knox 44 0.0058

   Kerberos 13–34

   Hydra 36 0.0032


   Four

   Charon, Pluto's largest moon, in a photo taken by the New Horizons spacecraft on July 11, 2015.  This picture shows the ditch, impact craters and deep North Pole.

   NASA / Johns Hopkins University Applied Physics Laboratory / Southwest Research Institute


   Pluto's other four moons - Hydra, Nix, Kerberos and Styx - are much smaller than the four.  All four are tall.  They revolve around Pluto in almost circular orbits outside of Charon's path (such as Charon) and in the same orbital plane as Charon.  Hydra's orbital radius is approximately 64,721 kilometers (40,216 miles).  Kerberos has 57,750 kilometers (35,884 miles);  Knicks has 48,690 kilometers (30,254 miles);  And Styx has 42,413 kilometers (26,354 miles).  Styx, Nix, and Kerberos are reflective like Charon, while Hydra is more reflective.


   For each orbit completed by Charon, Hydra completes about one-sixth of the orbit, Kerberos about one-fifth, Nix about one-fourth, and Styx about one-third.  This means that the orbital periods of Hydra, Kerberos, Nix, and Styx are in the ratio 6: 5: 4: 3.  These relations of orbital periods, which are in proportion to almost small whole numbers, suggest that Hydra, Nix, Kerbrus, and Styx are all four and in stable dynamic resonance with each other.  That is, the five bodies pass through each other from time to time, communicating through gravity in a way that maintains the regularity of their competition.  Due to the ever-changing gravitational field of Pluto and Charon (which revolve around each other), the Knicks and Hydra sometimes rotate their poles in rotation.  Unlike other satellites in the solar system, Pluto's four small moons are not in rotation with the planet.  That is, the duration of their rotation is not equal to their orbital period.  The rotation period ranges from 0.4295 days for Hydra to 5.31 days for Kerberos.



   Pluto  Charon Knox;  Hydra

   Pluto and its three moons; Charon, Nix and Hydra - as observed by the Hubble Space Telescope.

   HST Pluto Companion Search / ESA / NASA

   Discovery of Pluto and its moon


   When Pluto was discovered, it was thought to be the third planet discovered after Uranus and Neptune, in contrast to the six planets that have been visible in the sky with the naked eye since ancient times.  The existence of the ninth planet was assumed based on the apparent turbulence of Uranus' orbital motion in the late 19th century, which suggested that a distant body was disturbing it by gravity.  Astronomers later found the disturbances to be ridiculous - the small-scale gravitational pull of Pluto was not strong enough to cause a suspected disturbance.  Thus the discovery of Pluto was an extraordinary coincidence that was attributed to careful observations rather than accurate predictions of the existence of a fictitious planet.


   The search for the anticipated planet was most actively supported in the early 20th century at the Lowell Observatory in Flagstaff, Arizona, USA.  It was started by the founder of the observatory, Percival Lowell, an American astronomer who gained notoriety for his famous claims of canal view on Mars.  After two failed attempts to find the planet before Lewell's death in 1916, an astronomical camera specially designed for this purpose, capable of collecting light from a vast expanse of sky, was put into service in 1929.  Was introduced, and a young amateur astronomer, Clyde Tombo, was placed to search.  On February 18, 1930, less than a year after his work began, Tombao found Pluto in the Gemini Bridge.  The object appeared as a faint "star" of the 15th magnitude, which gradually changed its position against the fixed background stars, following its 248-year orbit around the Sun.  Although Lowell and other astronomers predicted that the unknown planet would be much larger and brighter than the object found in Tombaugh, Pluto was soon accepted as the expected ninth planet.  The symbol he invented for this is ♇, for the first two letters of Pluto and for both the beginnings of Percival Lowell.


   Charon was discovered in 1978 on photographs of Pluto, less than 6 kilometers (3.7 miles) from the site of Pluto's discovery, recorded by the Flag Staff at the US Naval Observatory Station.  These images were recorded by James W. Christie and Robert S. Herrington in an attempt to obtain a more accurate measurement of Pluto's orbit.  The new satellite is named after the boatman in Greek mythology who takes dead souls to the realm of Hades in the underworld.



   One of Pluto's four moon discoveries, taken in 1978 at the US Naval Observatory Station in Flagstaff, Arizona.  Charon appears only as a bulge in the upper right of Pluto's slate.

   Official photo of the US Navy


   Prior to Charon's discovery, Pluto was thought to be larger and larger than reality.  There was no way to determine the quantity directly.  Even in the discovered images, Charon appears as an unresolved collision on the edge of Pluto, due to the relative proximity of the two bodies, their extreme distance from Earth, and the distorting effects of the Earth's atmosphere.  Indicates observation difficulties that arise.  Only near the end of the 20th century, with the availability of the Hubble Space Telescope (HST) and ground-based instruments to compensate for the environmental turbulence, equipped with optical optics, astronomers first discovered Pluto and four.  Solved in separate bodies.



   Pluto  Four

   Pluto (center) and quadrupeds (bottom left), as observed by the European Space Agency's Fant object camera mounted on the Hubble Space Telescope.

   From the National Aeronautics and Space Administration / European Space Agency

   A team of neo-astronomers working in the United States discovered two small moons, Hydra and Nix, in short images taken with the Hubble Space Telescope in 2005, which traveled a short distance of 25 km (16 miles) around Pluto.  Searching for items to do.  To confirm the orbits, astronomers examined Hubble images of Pluto and Charon made in 2002 to study surface mapping, and two faint but definite objects moving along orbital paths calculated from 2005 images.  Get hints


   In 2011, six astronomers discovered the small moon Kerberos in images taken with HST.  As with the discovery of Nix and Hydra, astronomers examined early Hubble images and found faint traces of Kerberos in images from 2006 and 2010.  HST was re-used in 2012 to search for Styx.

Thursday, April 7, 2022

BLACK HOLE


   black holes

  By their very nature, black holes are black.  This is the first image of a black hole since April 2019.  Light forms a bright circle that rotates around a black hole under intense gravity, which is 6.5 billion times wider than our Sun.  This black hole is at the center of the galaxy M87, 55 million light years from Earth.  Photo courtesy of Event Horizon Telescope.

  What are black holes?

  Black holes have such strong gravity that nothing, not even light, can escape them.  That's why black holes are black.  We cannot see them directly.  But we can see how black holes affect the space around them.  Black holes can be as large as millions or billions of stars.  Or they could be as small as a few stellar masses that are crushed at high densities during supernova explosions.  And last year we learned that there are intermediate mass black holes.  In addition, there may be micro-black holes.


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  From theory to reality

  In his general theory of relativity since 1915, Albert Einstein was the first to suggest that our universe consists of such strange, dense, massive objects.  As a natural consequence of massive star deaths and falls, black holes emerge from Einstein's general relativity equation.  In 1916, German mathematician Carl Schwarzschild was the first to mathematically create black holes.  Theoretical physicist John Wheeler first named the black hole many years later, in 1967.


  Until the 1970s, black holes were only mathematical curiosity.  Then, in 1971, scientists discovered the first physical black hole, the Cygnux X-1.


  Stellar massive black holes

  We know of three types of black holes.  The first is the so-called stellar mass black hole.  These are the remnants of huge stars.  When, at the end of its life, a star about five times the mass of our Sun explodes as a supernova, gravity suddenly and violently compresses its center.


  Depending on the mass of the star, it could stop falling and become a neutron star.  But if its mass is sufficient, the core will continue to break, forming a black hole.  Stellar mass black holes range from at least five times the mass of our Sun to about 60 times the mass of the Sun.  They are usually between 10 and 30 miles (16-48 km) in diameter.



  Artist's concept of Science X-1.  Astronomers believe that Cygnus X-1 is a typical stellar black hole in the binary star system.  Cygnus X-1 was once a star before falling into a black hole.  The reason we can detect a black hole is that it is its companion, a blue supergiant variable star named HDE 226868.  Image via ESA / Wikimedia Commons.

  Medium black holes

  Scientists have announced the discovery of a medium-sized black hole in 2021.  This type of black hole bridges the gap between small, large star-shaped black holes and supermassive black holes hidden in the center of galaxies.  The newly discovered "Gold Locks" black hole has a volume of 55,000 suns.  Astronomers have discovered the middle black hole by locating something far behind it: a gamma-ray signal.  The gravitational lens of the burst emission sent scientists into a medium-sized black hole.




  Intermediate mass black holes, larger than those formed by individual stars - but smaller than the supermassive at the centers of galaxies - should theoretically exist.  Astronomers say they have discovered a gamma-ray burst that has been lensed by a black hole in terms of gravity.  In this diagram, the gamma ray burst is shown on the right.  At the center, a large black hole is acting as a beam of light emitted by gamma rays.  Photo by Carl Knox / Oz Grow / University of Melbourne.

  Massive black holes

  The third type of black hole is the supermassive black hole.  They can contain billions of suns.  Astronomers believe that most galaxies have large black holes at their centers.  At the center of our own Milky Way galaxy, Sagittarius A *, is about 4 million times the mass of our Sun and has a diameter of about 37 million miles.


  Another example of a supermassive black hole is in the center of the quasar called TON 618.  Its central black hole is estimated to be 66 billion solar masses.  Huge black holes could have formed from large collapsing clouds of interstellar hydrogen in the early history of the universe, although their origins are not clear and this is an area of ​​very active research.  They may also have accumulated extra mass on Evans by merging with other black holes.



  The artist's imagination represents the atmosphere of a large black hole in the heart of many galaxies.  The black hole is surrounded by a magnificent action disc of very hot, falling material and dusty torus (donut-shaped ring).  Black hole poles often carry high-speed jets of material that can travel very long distances in space.  Image via ESO / Wikimedia Commons.

  The fourth type of black hole

  There could be another type of black hole, a micro black hole.  These stars will be smaller in size than black holes.  So far, they are still fictitious, and no one's existence has been proven.


  What's inside a black hole?

  By definition, we cannot observe what is inside a black hole, because no light - no information of any kind - can escape.  But astronomical theories suggest that, at the center of a black hole, the mass of all black holes is concentrated in a small point of infinite density.  This point is known as unity.


  This is the point - this uniformity - that creates the incredibly strong gravitational field of the black hole.  Note, however, that uniformity does not exist.  This is because all known physics breaks down in extreme conditions at the center of a black hole, where quantum effects undoubtedly play a large part.  Since we do not yet have a quantum theory of gravity, it is impossible to say what is actually at the center of the black hole.


  Black hole boundaries

  The extent of the black hole is its event horizon.  This is not a physical edge.  It is just a point in space beyond which it is impossible to escape the gravity of the black hole.  Once anything falling into a black hole passes through the horizon of the event, it can never leave the black hole again.  It inevitably and inevitably pulls towards the center of the black hole.  Within the event horizon, any solid object explodes under intense gravity and its component is reduced to subatomic particles.  On the horizon of the event, the speed of escape of the black hole reaches the speed of light.


  Observation of black holes

  Without emissions from black holes, scientists can only observe the effects of their gravity on nearby objects in space.  If there are stars or gases near the black hole, it is actively "feeding" them.  That is, a black hole can pull material from nearby objects.  In that case, there would be an action disk in the black hole.  This is where the matter moves inward before the black hole eats it, like water in a drain.  The action disk can rotate at a significant percentage of the speed of light: friction between the particles colliding in the disk raises its temperature to millions of degrees, which produces large amounts of X-rays which can be detected by special binoculars.  Is.


  In April 2019, the Event Horizon Telescope Project revealed for the first time a live image of a black hole, the supermassive black hole at the center of the giant elliptical galaxy M87.  A global array of radio telescopes captured the image.  This undoubtedly shows that there are black holes.  Scientists were able to directly test the general relativity models of the black hole's behavior and found that the M87's black hole is very accurate.



  Picture of the Hubble Space Telescope, a jet-powered jet from the center of the Galaxy M87.  The jet consists of electrons and other subatomic particles that travel at approximately the speed of light.  Photo by Hubble Heritage Team (STScI / AURA) / NASA / ESA / esahubble.org.

   A black hole is an area of ​​space in which the field of gravity is so strong that nothing, even light, can escape it.  Black holes come in three sizes, possibly four.

FOOD

 Food is any substance that is used to nourish an organism.  Food is usually made from plants, animals, or fungi, and contains essential nutrients, such as carbohydrates, fats, proteins, vitamins, or minerals.  Matter is eaten by an organism and is absorbed by the cells of the organism to provide energy, sustain life, or stimulate growth.  Different species of animals have different eating behaviors that meet their unique metabolism requirements, which are often designed to fill a specific ecological space within a specific geographical context.



     Display of different foods

     Omnivorous humans are highly adaptable and have adapted to food in many different ecosystems.  Historically, humans have received food in two main ways: hunting and gathering, and agriculture.  As agricultural technology progressed, humans adopted an agricultural lifestyle with food according to the geographical opportunities in their geography.  Geographical and cultural differences have led to the creation of many foods and cuisines, including a wide range of ingredients, herbs, spices, techniques and dishes.  As cultures have merged through forces such as international trade and globalization, ingredients have become more widely available than their geographical and cultural origins, leading to a cosmopolitan exchange of different food traditions and practices.


     Today, much of the food energy needed by the world's ever-growing population is supplied through the industrial food industry, which produces food with extreme agriculture and distributes it through complex food processing and food distribution systems.  ۔  This conventional agricultural system relies heavily on fossil fuels, which means that food and agricultural systems are one of the major contributors to climate change, accounting for 37% of total greenhouse gas emissions.  [1] The carbon footprint of the food system and food waste are important measures to mitigate the global response to climate change.


     The food system has significant effects on a wide range of other social and political issues, including: sustainability, biodiversity, economics, population growth, water supply, and access to food.  The right to food is a human right derived from the International Covenant on Economic, Social and Cultural Rights (ICESCR), which includes "the right to a decent standard of living, including adequate food" as well as the "fundamental right to liberty".  Has been recognized.  "Because of these fundamental rights to hunger, food security is often a priority international policy activity. For example, Sustainable Development Goal 2" Zero Hunger "aims to end hunger by 2030. Food Safety and Food Security  Supervised by international agencies such as the International Association for Food Protection, the World Resource Institute, the World Food Program, the Food and Agriculture Organization, and the International Food Information Council.  And Drug Administration.


     Definition and rating

     Food sources

     Classification and food types

     Taste perception

     Original article: Taste

     Animals, especially humans, have five different tastes: sweet, sour, salty, bitter and imami.  As animals have evolved, the flavors that provide the most energy (sugar and fat) are most pleasant to eat while others, such as bitter ones, do not enjoy. [84]  It is important for survival, it has no taste.  On the other hand, fats, especially saturated fats, are thick and rich and are therefore considered more palatable.


     sweet


     Structure of sucrose

     Commonly known as the sweetest taste, sweetness is almost always caused by a type of simple sugar such as glucose or fructose, or disaccharides such as sucrose, a molecule that combines glucose and fructose. [86]  Complex carbohydrates are long chains and thus do not taste sweet.  Artificial sweeteners such as sucrose are used to mimic sugar molecules, creating a sweet feeling without calories.  Other types of sugar include raw sugar, which is known for its amber color because it is unprocessed.  As sugar is essential for energy and survival, sugar tastes good.


     The stevia plant contains a compound called steviol which, when extracted, is 300 times sweeter than sugar and has a minimal effect on blood sugar. [87]


     Sour

     Sourness is caused by the taste of acid, such as vinegar in alcoholic beverages.  Sour foods include lemons, especially lemons, lime and, to a lesser extent, oranges.  Sour is important for evolution because it symbolizes a food that can be spoiled by bacteria. [88] However, many foods are slightly acidic, and help stimulate taste buds and enhance flavor.  Do


     Salty


     Salt dunes in Bolivia

     Salinity is the taste of alkali metal ions such as sodium and potassium.  It is found in almost every food in moderate amounts to enhance the taste, although eating pure salt is considered extremely unpleasant.  There are many different types of salt, each with varying degrees of salinity, including sea salt, fluoride salt, kosher salt, mining salt, and gray salt.  In addition to enhancing the taste, it is important that the body needs and maintains a delicate electrolyte balance, which is the function of the kidneys.  Salt can be iodized, meaning it contains iodine, an essential nutrient that promotes thyroid function.  Some canned foods, especially soups or packaged soups, have high salt content to keep food safe for longer.  Historically, salt has long been used as a preservative for meat, as it promotes water excretion.  Similarly, dry foods also promote food safety.


     Bitter

     Bitterness is a feeling that is often considered unpleasant, characterized by a sharp, pungent taste.  Without sweet chocolate, caffeine, lemon peel and some fruits are bitter.


     امامی

     This section is an excerpt from Imami.

     امامی




     Soy sauce, ripe tomatoes, and muesli are examples of foods rich in ingredients.

     Imami (/ uːˈmɑːmi / from Japanese: Japanese pronunciation: [ɯmami]), or flavor, is one of the five basic flavors.  It has been described as delicious and is characteristic of broths and cooked meats


     People taste amaranth through taste receptors that typically respond to glutamate and nucleotides, which are abundant in meat broths and fermented products.  Glutamate is usually added to some foods in the form of monosodium glutamate (MSG), and nucleotides are usually added in the form of inosine monophosphate (IMP) or guanosine monophosphate (GMP).  Because imams have their own receptors, rather than originating from a combination of traditionally recognized flavors, scientists now consider imams to be a distinct flavor.


     Foods with strong amami flavors include meat, shellfish, fish (including fish sauce and preserved fish such as Maldivian fish, sardines and anchovies), tomatoes, mushrooms, hydrolyzed vegetable protein, meat liqueur, yeast liqueur, cheese  And soy sauce.  .

Sunday, April 3, 2022

HUMAN EYE

 Human eye


  The human eye, in humans, is the specialized sensory organ capable of receiving visual images, which are then transmitted to the brain.


  Cross section of human eye


  The eye is protected from mechanical injury by being enclosed in a socket, or orbit, which forms a four-sided pyramid with several bone parts of the skull, the top of which points to the head.  Thus, the floor of the orbit is made up of parts of the maxilla, zygomatic and palatine bones, while the roof is made of the orbital plate of the frontal bone and behind it, the short arm of the sphenoid.  The optic pharynx, the hole through which the optic nerve goes back to the brain and enters the orbit of the large eye, is towards the nostril.  The superior orbital fissure is a large hole through which large veins and nerves pass.  These nerves can carry non-visual sensory messages - such as pain - or they can be motor nerves that control the eye muscles.  There are other cracks and canals that carry nerves and blood vessels.  The eyeball and its active muscles are surrounded by a layer of orbital fat that acts like a cushion, allowing the eyeball to rotate smoothly around a fixed point, the center of rotation.  ۔  Protosis of the eyeballs is caused by the accumulation of fluid in the orbital fatty tissue in the exophthalmic goiter.



  Britannica Quiz

  Human organs

  How much energy does the brain use in the human body?  On average, how many times does the human heart beat per minute?  Take this quiz to strengthen your brain and speed up your pulse rate.

  Eyelids

  It is important that the front surface of the eye hair, the cornea, remains moist.  This is achieved through the lashes, which regularly wipe the surface of the tear glands and other glandular secretions during waking hours and which cover the eyes during sleep and prevent evaporation.  The reflex action of the eyelids in the lids has the added function of preventing injuries from foreign bodies.  The lids are basically layers of tissue that cover the front of the orbit and leave an almond-shaped aperture when the eye is opened.  Almond points are called canthi.  Near the nose is the inner canthus, and the other is the outer canthus.  The lid can be divided into four layers: (1) the skin, which contains glands that open at the marginal surface of the lid, and the eyelids;  (2) A layer of muscle consisting primarily of the orbicularis oculi muscle, which is responsible for closing the lid.  (3) A fibrous layer that gives the lid mechanical stability, its main parts are the tarsal plates, which are directly attached to the opening between the lids, called palpebral aperture.  And (4) the innermost layer of the lid, a part of the conjunctiva.  The conjunctiva is a viscous membrane that connects the eyeball to the orbit and the lids, but allows the eyeball to rotate considerably in orbit.



  Eyelash

  Upper and lower eyelids.

  Isra SU

  conjunctiva

  Conjunctivitis lines the lids and then bends back to the surface of the hair follicles, forming an outer covering on the front of it and ending at the transparent area of ​​the eye, the cornea.  The part that lines the lids is called the palpebral part of the conjunctiva.  The part that covers the whites of the eye's hair is called the bulbar conjunctiva.  Between the bulbar and the palpebral conjunctiva are two loose, spare parts that return to the equator of the world.  These holidays are called upper and lower forensics, or conjunctival sacs.  It is the looseness of the conjunctiva in these places that makes the movement of the lids and eyeballs possible.


  Fibrous layer

  The fibrous layer, which gives the lid mechanical stability, is made up of thick, and relatively stiff, tarsal plates, which appear directly on the palpebral aperture, and a thinner palpebral fascia, or sheet of connective tissue;  Together they are called septum orbitals.  When the lids are closed, the entire septum is covered by this septum.  The two ligaments, the medial and lateral palpebral ligaments, connected to the orbit of the orbit and the septum, strengthen the position of the lids in relation to the globe.  The medial ligament is still strong.


  The muscles of the lids

  Closure of the lids is achieved by contraction of the orbicularis muscle, a single elliptical sheet of muscle extending from the forehead and facial areas and into the lids around the orbit.  It is divided into orbital and palpebral parts, and it is mainly the palpebral part, inside the lid, which causes the lid to close.  The palpebral portion passes through the lids through a ligament called the medial palpebral ligament and forms a band of fibers in a series of hemispheres to the neighboring bone of the orbit that meet outside the outer corner of the eye, the lateral kineths.  raphe.  The extra parts of the orbicularis are given different names - Horner's muscle and Revlon's muscle;  They come in close contact with the tear gas and help to drain the tears.  Revolving muscles, lying close to the edge of the lid, help keep the lids close.  The orbital part of the orbicularis is not usually associated with the eyelid, which can be done entirely through the palpebral part.  However, it has to do with closing the eyes tightly.  The skin of the forehead, temples and cheeks is then pulled towards the middle of the orbit (nose), and the rays produced by this process of the orbital part, eventually lead to the so-called well feet of the elderly.  .  It should be noted that both parts can be activated freely.  In this way, the orbital part can shrink, causing wrinkles in the eyebrows, which reduces the amount of light coming from above, while the palpebral part is relaxed and the eyes are left open.


  Opening of the eye is not only the result of inactive relaxation of the muscles of the orbicularis but also the effect of contraction of the levator palpebrae superioris muscles of the upper lid.  This muscle begins with the extravascular muscle at the top of the orbit as a narrow tendon and progresses to the upper lid as a wide tendon, the levator aponeurosis, which attaches to the anterior surface of the tarsus and covers the upper.  Skin  Lid.  Muscle contraction causes elevation of the upper eyelid.  The nerve connections to this muscle are closely related to the extracular muscles needed to lift the eye, so when the eye looks upwards, the upper eyelid converges and rises.


  The orbicularis and levator are striped muscles in voluntary control.  The lids also contain smooth (involuntary) muscle fibers that are activated by the sympathetic distribution of the autonomic system and widen the pelvic fissure (opening of the eye) by the height of the upper and the depression of the lower lid.


  In addition to the muscles described earlier, other facial muscles often assist in the process of closing or opening the lid.  Thus, the muscles of the corrugator supercilii pull the eyebrows towards the bridge of the nose, creating a characteristic trench in the forehead, forming a "roof" at the middle angle of the eye.  The roof is mainly used to protect the eye from sunlight.  The pyramid, or processor, muscles occupy the bridge of the nose.  They originate in the lower part of the nasal bones and are attached to the skin of the lower part of the forehead on either side of the midline.  They pull the skin into translucent skins.  When the lid is opened, the frontalis muscle rises high on the forehead, between the coronal sutures, a suture in the upper part of the skull, and the orbital border is attached to the skin of the eyebrows.  The contraction therefore causes the eyebrows to be raised and resists the action of the orbital part of the orbicularis.  Muscles are used especially when one looks upwards.  It is also practiced when vision is presented with difficulty either due to distance or lack of sufficient light.


  Quick

  The outermost layer of the lid is the skin, the characteristics of which are not very different from the skin of the rest of the body, with the possible exception of the large pigment cells, which, although found elsewhere, are very much in the skin of the lid.  Are  Cells can wander, and these are the movements of pigment cells that determine color changes in some people as health changes.  The skin contains sweat glands and hair.  As the connection between the skin and the conjunctiva develops, the hair changes its character and becomes mahram.


  Glandular device


  Moisture from the tear glands (tear glands) keeps the eye moist.  These almond-shaped glands extend inward from the outer corner of each eye under the upper lid.  Each gland has two parts.  One part of the eye socket is in a shallow depression formed by the frontal bone.  The second part projects into the back of the upper lid.  The ducts that come out of each gland, in numbers three to 12, open into the superior conjunctival pharynx, or sac.  From the pharynx, tears flow across the eye and into the pancreatic lacrimal, with small holes in the margins of each eyelid near the inner corner.  Pentacles have holes in the tear ducts.  They carry tears to the sacs, the wide upper end of the nasolabial ducts, which carry the tears to the nose.


  When tears vapor flow into the eye, the secretion of oil and mucus through other glands is largely prevented.  Thus, the meibomian, or tarsal gland, consists of a series of long glands that spread through the tarsal plates.  They release an oil that rises to the surface of the margin of the lid and acts as a barrier to tear fluid, which accumulates in the ducts between the eye hair and the lid barrier.

BENIGN TUMOR

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