The Sun is the Most Prominent Feature in Our Solar System
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Transcript of The Sun is the Most Prominent Feature in Our Solar System
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The Sun is the most prominent feature in our solar system. It is the largest object and contains
approximately 98% of the total solar system mass. One hundred and nine Earths would be required to fit
across the Sun's disk, and its interior could hold over 1.3 million Earths. The Sun's outer visible layer is
called the photosphere and has a temperature of 6,000C (11,000F). This layer has a mottled
appearance due to the turbulent eruptions of energy at the surface.
The Sun appears to have been active for 4.6 billion years and has enough fuel to go on for
another five billion years or so. At the end of its life, the Sun will start to fuse helium into heavier
elements and begin to swell up, ultimately growing so large that it will swallow the Earth. After a billion
years as a red giant, it will suddenly collapse into a white dwarf-- the final end product of a star like
ours. It may take a trillion years to cool off completely.
Sun Statistics
Mass (kg)1.989e+30
Mass (Earth = 1)332,830
Equatorial radius (km)695,000
Equatorial radius (Earth = 1)108.97
Mean density (gm/cm^3)1.410
Rotational period (days)25-36*
Escape velocity (km/sec)618.02
Luminosity (ergs/sec)3.827e33
Magnitude (Vo)-26.8
Mean surface temperature6,000C
Age (billion years)4.5
Mercury
Mercury was named by the Romans after the fleet-footed messenger of the gods because it seemed to
move more quickly than any other planet. It is the closest planet to the Sun, and second smallest planet
in the solar system. Its diameter is 40% smaller than Earth and 40% larger than the Moon. It is even
smaller than Jupiter's moon Ganymede and Saturn's moon Titan.
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Mercury could not support water in any form. It has very little atmosphere and is blazing hot during the
day, but in 1991 scientists at Caltech bounced radio waves offMercury and found an unusual bright
return from the north pole. The apparent brightening at the north pole could be explained by ice on or
just under the surface. But is it possible forMercury to have ice? BecauseMercury's rotation is almost
perpendicular to its orbital plain, the north pole always sees the sun just above the horizon. The insides
of craters would never be exposed to the Sun and scientists suspect that they would remain colder than
-161 C. These freezing temperatures could trap water outgassed from the planet, or ices brought to the
planet from cometary impacts. These ice deposits might be covered with a layer of dust and would still
show bright radar returns.
Mercury Statistics
Mass (kg)3.303e+23
Mass (Earth = 1)5.5271e-02
Equatorial radius (km)2,439.7
Equatorial radius (Earth = 1)3.8252e-01
Mean density (gm/cm^3)5.42
Mean distance from the Sun (km)57,910,000
Mean distance from the Sun (Earth = 1)0.3871
Rotational period (days)58.6462
Orbital period (days)87.969
Mean orbital velocity (km/sec)47.88
Orbital eccentricity0.2056
Tilt of axis (degrees)0.00
Orbital inclination (degrees)7.004
Equatorial surface gravity (m/sec^2)2.78
Equatorial escape velocity (km/sec)4.25
Visual geometric albedo0.10
Magnitude (Vo)-1.9
Mean surface temperature179C
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Maximum surface temperature427C
Minimum surface temperature-173C
Venus
Venus, thejewel of thesky, was once know by ancient astronomers as
the morningstar and eveningstar. Early astronomers once thought Venus to be two separate bodies.
Venus, which is named after the Roman goddess of love and beauty, is veiled by thick swirling cloud
cover. Astronomers refer to Venus as Earth's sister planet. Both are similar in size, mass, density and
volume. Both formed about the same time and condensed out of the same nebula. Venus is scorched
with a surface temperature of about 482 C (900 F). This high temperature is primarily due to a
runaway greenhouse effect caused by the heavy atmosphere of carbon dioxide. Sunlight passes through
the atmosphere to heat the surface of the planet. Heat is radiated out, but is trapped by the dense
atmosphere and not allowed to escape into space. This makes Venus hotter thanMercury.
Venus Statistics
Mass (kg)4.869e+24
Mass (Earth = 1).81476
Equatorial radius (km)6,051.8
Equatorial radius (Earth = 1).94886
Mean density (gm/cm^3)5.25
Mean distance from the Sun (km)108,200,000
Mean distance from the Sun (Earth = 1)0.7233
Rotational period (days)-243.0187
Orbital period (days)224.701
Mean orbital velocity (km/sec)35.02
Orbital eccentricity0.0068
Tilt of axis (degrees)177.36
Orbital inclination (degrees)3.394
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Equatorial surface gravity (m/sec^2)8.87
Equatorial escape velocity (km/sec)10.36
Visual geometric albedo0.65
Magnitude (Vo)-4.4
Mean surface temperature482C
Atmospheric pressure (bars)92
Earth
Earth is the 3rd planet from the Sun at a distance of about 150
million kilometers (93.2 million miles). It takes 365.256 days for the Earth to travel around the Sun and
23.9345 hours for the Earth rotate a complete revolution. It has a diameter of 12,756 kilometers (7,973
miles), only a few hundred kilometers larger than that of Venus. Our atmosphere is composed of 78
percent nitrogen, 21 percent oxygen and 1 percent other constituents.
Besides affecting Earth's weather, solar activity gives rise to a dramatic
visual phenomenon in our atmosphere. When charged particles from the solar wind become trapped in
Earth's magnetic field, they collide with air molecules above our planet's magnetic poles. These air
molecules then begin to glow and are known as the auroras or the northern and southern lights.
Earth Statistics
Mass (kg)5.976e+24
Mass (Earth = 1)1.0000e+00
Equatorial radius (km)6,378.14
Equatorial radius (Earth = 1)1.0000e+00
Mean density (gm/cm^3)5.515
Mean distance from the Sun (km)149,600,000
Mean distance from the Sun (Earth = 1)1.0000
Rotational period (days)0.99727
Rotational period (hours)23.9345
Orbital period (days)365.256
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Mean orbital velocity (km/sec)29.79
Orbital eccentricity0.0167
Tilt of axis (degrees)23.45
Orbital inclination (degrees)0.000
Equatorial escape velocity (km/sec)11.18
Equatorial surface gravity (m/sec^2)9.78
Visual geometric albedo0.37
Mean surface temperature15C
Atmospheric pressure (bars)1.013
Mars
Mars is the fourth planet from the Sun and is commonly
referred to as the Red Planet. The rocks, soil and sky have a red or pink hue. The distinct red color was
observed by stargazers throughout history. It was given its name by the Romans in honor of their god of
war. Other civilizations have had similar names. The ancient Egyptians named the planet Her Descher
meaning the red one.
Before space exploration, Mars was considered the best candidate for harboring
extraterrestrial life. Astronomers thought they saw straight lines crisscrossing its surface. Thisled to the popular belief that irrigation canals on the planet had been constructed by intelligent
beings. In 1938, when Orson Welles broadcasted a radio drama based on the science fictionclassic War of the Worlds by H.G. Wells, enough people believed in the tale of invading
Martians to cause a near panic.
Another reason for scientists to expect life on Mars had to do with the apparent seasonal color
changes on the planet's surface. This phenomenon led to speculation that conditions mightsupport a bloom of Martian vegetation during the warmer months and cause plant life to become
dormant during colder periods.
Mars Statistics
Mass (kg)6.421e+23
Mass (Earth = 1)1.0745e-01
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Equatorial radius (km)3,397.2
Equatorial radius (Earth = 1)5.3264e-01
Mean density (gm/cm^3)3.94
Mean distance from the Sun (km)227,940,000
Mean distance from the Sun (Earth = 1)1.5237
Rotational period (hours)24.6229
Rotational period (days)1.025957
Orbital period (days)686.98
Mean orbital velocity (km/sec)24.13
Orbital eccentricity0.0934
Tilt of axis (degrees)25.19
Orbital inclination (degrees)1.850
Equatorial surface gravity (m/sec^2)3.72
Equatorial escape velocity (km/sec)5.02
Visual geometric albedo0.15
Magnitude (Vo)-2.01
Minimum surface temperature-140C
Mean surface temperature-63C
Maximum surface temperature20C
Atmospheric pressure (bars)0.007
Jupiter
Jupiter is the fifth planet from the Sun and is the largest planet in the solar system. If Jupiter were
hollow, more than one thousand Earths could fit inside. It also contains two and a half times the mass of
all the other planets combined. It has a mass of 1.9 x 1027
kg and is 142,800 kilometers (88,736 miles)
across the equator. Jupiter possesses 62 known satellites. The four largest are Callisto, Europa,
Ganymede and Io, and were named after Galileo Galilei who observed them as long ago as 1610. The
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German astronomer SimonMarius claimed to have seen the moons around the same time, but he did
not publish his observations and so Galileo is given the credit for their discovery.
Jupiter has a very faint ring system, but is totally invisible from the Earth. (The
rings were discovered in 1979 by Voyager 1.) The atmosphere is very deep, perhaps comprising the
whole planet, and is somewhat like the Sun. It is composed mainly of hydrogen and helium, with smallamounts of methane, ammonia, water vapor and other compounds. At great depths within Jupiter, the
pressure is so great that the hydrogen atoms are broken up and the electrons are freed so that the
resulting atoms consist of bare protons. This produces a state in which the hydrogen becomes metallic.
Jupiter Statistics
Mass (kg)1.900e+27
Mass (Earth = 1)3.1794e+02
Equatorial radius (km)71,492
Equatorial radius (Earth = 1)1.1209e+01
Mean density (gm/cm^3)1.33
Mean distance from the Sun (km)778,330,000
Mean distance from the Sun (Earth = 1)5.2028
Rotational period (days)0.41354
Orbital period (days)4332.71
Mean orbital velocity (km/sec)13.07
Orbital eccentricity0.0483
Tilt of axis (degrees)3.13
Orbital inclination (degrees)1.308
Equatorial surface gravity (m/sec^2)22.88
Equatorial escape velocity (km/sec)59.56
Visual geometric albedo0.52
Magnitude (Vo)-2.70
Mean cloud temperature-121C
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Atmospheric pressure (bars)0.7
Saturn
Saturn is the sixth planet from the Sun and is the second largest in the solar system with an equatorial
diameter of 119,300 kilometers (74,130 miles).Much of what is known about the planet is due to the
Voyager explorations in 1980-81. Saturn is visibly flattened at the poles, a result of the very fast rotation
of the planet on its axis. Its day is 10 hours, 39 minutes long, and it takes 29.5 Earth years to revolve
about the Sun. The atmosphere is primarily composed of hydrogen with small amounts of helium and
methane. Saturn is the only planet less dense than water (about 30 percent less). In the unlikely event
that a large enough ocean could be found, Saturn would float in it. Saturn's hazy yellow hue is marked
by broad atmospheric banding similar to, but fainter than, that found on Jupiter.
Saturn Statistics
Mass (kg)5.688e+26
Mass (Earth = 1)9.5181e+01
Equatorial radius (km)60,268
Equatorial radius (Earth = 1)9.4494e+00
Mean density (gm/cm^3)0.69
Mean distance from the Sun (km)1,429,400,000
Mean distance from the Sun (Earth = 1)9.5388
Rotational period (hours)10.233
Orbital period (years)29.458
Mean orbital velocity (km/sec)9.67
Orbital eccentricity0.0560
Tilt of axis (degrees)25.33
Orbital inclination (degrees)2.488
Equatorial surface gravity (m/sec^2)9.05
Equatorial escape velocity (km/sec)35.49
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Visual geometric albedo0.47
Magnitude (Vo)0.67
Mean cloud temperature-125C
Atmospheric pressure (bars)1.4
Uranus
Uranus is the seventh planet from the Sun and is the third largest in the solar system. It
was discovered by William Herschel in 1781. It has an equatorial diameter of 51,800 kilometers (32,190
miles) and orbits the Sun once every 84.01 Earth years. It has a mean distance from the Sun of 2.87
billion kilometers (1.78 billion miles). It rotates about its axis once every 17 hours 14 minutes. Uranus
has at least 22 moons. The two largest moons, Titania and Oberon, were discovered by William Herschel
in 1787.
The atmosphere ofUranus is composed of 83% hydrogen, 15% helium, 2% methane and
small amounts of acetylene and other hydrocarbons.Methane in the upper atmosphere absorbs red
light, giving Uranus its blue-green color.
Uranus Statistics
Discovered byWilliam Herschel
Date of discovery1781
Mass (kg)8.686e+25
Mass (Earth = 1)1.4535e+01
Equatorial radius (km)25,559
Equatorial radius (Earth = 1)4.0074
Mean density (gm/cm^3)1.29
Mean distance from the Sun (km)2,870,990,000
Mean distance from the Sun (Earth = 1)19.1914
Rotational period (hours)-17.9
Orbital period (years)84.01
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Mean orbital velocity (km/sec)6.81
Orbital eccentricity0.0461
Tilt of axis (degrees)97.86
Orbital inclination (degrees)0.774
Equatorial surface gravity (m/sec^2)7.77
Equatorial escape velocity (km/sec)21.30
Visual geometric albedo0.51
Magnitude (Vo)5.52
Mean cloud temperature-193C
Atmospheric pressure (bars)1.2
Neptune
Neptune is the outermost planet of the gas giants. It has an equatorial
diameter of 49,500 kilometers (30,760 miles). If Neptune were hollow, it could contain nearly 60 Earths.
Neptune orbits the Sun every 165 years. It has eight moons, six of which were found by Voyager. A day
on Neptune is 16 hours and 6.7 minutes. Neptune was discovered on September 23, 1846 by Johann
Gottfried Galle, of the Berlin Observatory, and Louis d'Arrest, an astronomy student, through
mathematical predictions made by Urbain Jean Joseph Le Verrier.
Neptune is a dynamic planet with several large, dark spots reminiscent ofJupiter's
hurricane-like storms. The largest spot, known as the Great Dark Spot, is about the size of the earth and
is similar to the Great Red Spoton Jupiter. Voyager revealed a small, irregularly shaped, eastward-
moving cloud scooting around Neptune every 16 hours or so. This scooteras it has been dubbed could
be a plume rising above a deeper cloud deck.
Neptune Statistics
Discovered byJohann Gotfried Galle
Date of discoverySeptember 23, 1846
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Pluto is usually farther from the Sun than any of the eight planets; however, due to the eccentricity of its
orbit, it is closer than Neptune for 20 years out of its 249 year orbit. Pluto crossed Neptune's orbit
January 21, 1979, made its closest approach September 5, 1989, and remained within the orbit of
Neptune until February 11, 1999. This will not occur again until September 2226.
Pluto Statistics
Discovered byClyde W. Tombaugh
Date of discoveryFebruary 18, 1930
Mass (kg)1.27e+22
Mass (Earth = 1)2.125e-03
Equatorial radius (km)1,137
Equatorial radius (Earth = 1)0.1783
Mean density (gm/cm^3)2.05
Mean distance from the Sun (km)5,913,520,000
Mean distance from the Sun (Earth = 1))39.5294
Rotational period (days)-6.3872
Orbital period (years)248.54
Mean orbital velocity (km/sec)4.74
Orbital eccentricity0.2482
Tilt of axis (degrees)122.52
Orbital inclination (degrees)17.148
Equatorial surface gravity (m/sec^2)0.4
Equatorial escape velocity (km/sec)1.22
Visual geometric albedo0.3
Magnitude (Vo)15.12
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manned missions to date, beginning with the first manned lunar orbiting mission byApollo 8 in 1968, and six manned lunar landings between 1969 and 1972the first being
Apollo 11 in 1969. These missions returned over 380 kg oflunar rocks, which have beenused to develop a detailed geological understanding of the Moon's origins (it is thought to
have formed some 4.5 billion years ago in a giant impact), the formation ofits internal
structure, and its subsequent history.
TheMoon is a differentiated body: it has a geochemically distinct crust, mantle, and core. This
structure is thought to have developed through the fractional crystallization of a global magma ocean
shortly after theMoon's formation 4.5 billion years ago.[23] Crystallization of this magma ocean would
have created a mafic mantle from the precipitation and sinking of the minerals olivine, clinopyroxene,
and orthopyroxene; after about three-quarters of the magma ocean had crystallised, lower-density
plagioclase minerals could form and float into a crust on top.[24]
The final liquids to crystallise would
have been initially sandwiched between the crust and mantle, with a high abundance ofincompatible
and heat-producing elements.[1]
Consistent with this, geochemical mapping from orbit shows the crust is
mostly anorthosite,[5]
and moon rock samples of the flood lavas erupted on the surface from partial
melting in the mantle confirm the mafic mantle composition, which is more iron rich than that of
Earth.[1]
Geophysical techniques suggest that the crust is on average ~50 km thick.[1]