Astronomy,     science that encompasses    the study of all extraterrestrial objects and phenomena. Until    the invention of the telescope and the discovery of the laws of        motion and gravity in the 17th century, astronomy    was primarily concerned with noting and predicting the    positions of the Sun, Moon, and planets, originally for    calendrical and astrological purposes and later for    navigational uses and scientific interest. The catalog of    objects now studied is much broader and includes, in order of    increasing distance, the solar system, the stars that make up    the Milky Way Galaxy, and other, more distant galaxies. With    the advent of scientific space probes, Earth also has come to    be studied as one of the planets, though its more detailed    investigation remains the domain of the geologic sciences.  
    Since the late 19th century astronomy has expanded to include    astrophysics,    the application of physical and chemical knowledge to an    understanding of the nature of celestial objects and the    physical processes that control their formation, evolution, and    emission of radiation. In addition, the gases and dust    particles around and between the stars have become the subjects    of much research. Study of the nuclear reactions that provide    the     energy radiated by stars has shown how the diversity of    atoms found in nature can be derived from a universe that,    following the first few minutes of its existence, consisted    only of     hydrogen,     helium, and a     trace of     lithium. Concerned with phenomena on the largest    scale is cosmology,    the study of the evolution of the universe. Astrophysics has    transformed cosmology from a purely speculative activity to a    modern science capable of predictions that can be tested.  
    Its great advances notwithstanding, astronomy is still subject    to a major constraint: it is inherently an observational rather    than an experimental science. Almost all measurements must be    performed at great distances from the objects of interest, with    no control over such quantities as their     temperature, pressure, or chemical composition.    There are a few exceptions to this limitationnamely,     meteorites, rock and soil samples brought back from    the     Moon, samples of     comet dust returned by robotic     spacecraft, and     interplanetary dust particles collected in or above    the stratosphere. These can be examined with laboratory    techniques to provide information that cannot be obtained in    any other way. In the future, space missions may return surface    materials from Mars, asteroids, or other objects, but much of    astronomy appears otherwise confined to Earth-based    observations augmented by observations from orbiting satellites    and long-range space probes and supplemented by theory.  
    A central undertaking in astronomy is the determination of    distances. Without a knowledge of its distance, the size of an    observed object in space would remain nothing more than an    angular diameter, and the brightness of a star could not be    converted into its true radiated power, or luminosity.    Astronomical distance measurement began with a knowledge of    Earths diameter, which provided a base for triangulation.    Within the inner solar system, some distances can now be better    determined through the timing of radar reflections or, in the    case of the Moon, through laser ranging. For the outer planets,    triangulation is still used. Beyond the solar system, distances    to the closest stars    are determined through triangulation, with the diameter of    Earths orbit serving as the baseline and shifts in stellar    parallax    being the measured quantities. Stellar distances are commonly    expressed by astronomers in parsecs    (pc), kiloparsecs, or megaparsecs.    (1pc=3.0861018 cm, or about 3.26 light-years    [1.92  1013 miles].)    Distances can be measured out to around a kiloparsec by    trigonometric parallax (see     star: Determining stellar distances). The accuracy    of measurements made from Earths surface is limited by    atmospheric effects, but measurements made from the Hipparcos    satellite in the 1990s have extended the scale to    stars as far as 650 parsecs, with an accuracy of about a    thousandth of an arc second. Less-direct measurements must be    used for more-distant stars and for galaxies.  
    Two general methods for determining galactic    distances are described here. In the first, a clearly    identifiable type of star is used as a reference standard    because its luminosity has been well determined. This requires    observation of such stars that are close enough to Earth that    their distances and luminosities have been reliably measured.    Such a star is termed a standard    candle. Examples are     Cepheid variables, whose brightness varies    periodically in well-documented ways, and certain types of        supernova explosions that have enormous brilliance    and can thus be seen out to very great distances. Once the    luminosities of such nearer standard candles have been calibrated, the    distance to a farther standard candle can be calculated from    its calibrated luminosity and its actual measured intensity.    (The measured intensity [I] is related to the    luminosity [L] and distance [d] by the    formula    I=L/4d2). A standard candle can be    identified by means of its spectrum or the pattern of regular    variations in brightness. (Corrections may have to be made for    the absorption of starlight by interstellar gas and dust over    great distances.) This method forms the basis of measurements    of distances to the closest galaxies.  
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    The second method for galactic distance measurements makes use    of the observation that the distances to galaxies generally    correlate with the speeds with which those galaxies    are receding from Earth (as determined from the    Doppler shift in the wavelengths of their emitted light). This    correlation is expressed in the Hubble    law:    velocity=Hdistance, in which    H denotes Hubbles    constant, which must be determined from observations    of the rate at which the galaxies are receding. There is    widespread agreement that H lies between 70 and 76    kilometres per second per megaparsec (km/sec/Mpc), with leading    research groups offering estimates that have an average value    of about 71 km/sec/Mpc. H has been used to determine    distances to remote galaxies in which standard candles have not    been found. (For additional discussion of the recession of    galaxies, the Hubble law, and galactic distance determination,    see         physical science: Astronomy.)  
    The     solar system took shape 4.57 billion years ago, when    it condensed within a large cloud of gas and dust.    Gravitational attraction holds the planets in their elliptical    orbits around the Sun.    In addition to Earth,    five major planets (Mercury,    Venus,    Mars,    Jupiter,    and Saturn)    have been known from ancient times. Since then only two more    have been discovered: Uranus    by accident in 1781 and Neptune    in 1846 after a deliberate search following a theoretical    prediction based on observed irregularities in the orbit of    Uranus. Pluto,    discovered in 1930 after a search for a planet predicted to lie    beyond Neptune, was considered a major planet until 2006, when    it was redesignated a     dwarf planet by the International Astronomical    Union.  
    The average Earth-Sun distance, which originally defined the    astronomical    unit (AU), provides a convenient measure for    distances within the solar system. The astronomical unit is now    defined dynamically (using     Keplers third law; see     Keplers laws of planetary motion) and has the value    1.495978706911013 cm (about 93 million miles),    with an uncertainty of about 2,000 cm. The mean radius of    Earths orbit is 1+(3.1108) AU.     Mercury, at 0.4 AU, is the closest planet to the    Sun, while Neptune, at 30.1 AU, is the farthest. Plutos orbit,    with a mean radius of 39.5, is sufficiently eccentric that    at times it is closer to the Sun than is Neptune. The planes of    the planetary orbits are all within a few degrees of the        ecliptic, the plane that contains Earths orbit    around the Sun. As viewed from far above Earths     North Pole, all planets move in the same    (counterclockwise) direction in their orbits.  
    All of the planets apart from the two closest to the Sun    (Mercury and Venus) have natural satellites (moons) that are    very diverse in    appearance, size, and structure, as revealed in close-up    observations from long-range space probes. Pluto has at least    three moons, including one fully half the size of Pluto itself.    Four planetsJupiter,     Saturn, Uranus, and Neptunehave rings, disklike    systems of small rocks and particles that orbit their parent    planets.  
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    Most of the mass of the solar system is concentrated in the    Sun, with its 1.991033 grams. Together, all of the    planets amount to 2.71030 grams (i.e., about    one-thousandth of the Suns mass), with Jupiter alone    accounting for 71 percent of this amount. The solar system also    contains a few known objects of intermediate size classified as    dwarf planets and a very large number of much smaller objects    collectively called small    bodies. The small bodies, roughly in order of    decreasing size, are the     asteroids, or minor planets;     comets, including     Kuiper belt and     Oort cloud objects; meteoroids (see        meteor and meteoroid); and     interplanetary dust particles. Because of their    starlike appearance when discovered, the largest of these    bodies were termed asteroids, and that name is widely    used, but, now that the rocky nature of these bodies is    understood, their more descriptive name is minor planets.  
    The four inner, terrestrial planetsMercury, Venus, Earth, and    Marsalong with the Moon have average densities in the range of    3.95.5 grams per cubic cm, setting them apart from the four    outer, giant planetsJupiter, Saturn, Uranus, and Neptunewhose    densities are all close to 1 gram per cubic cm, the density of    water. The compositions    of these two groups of planets must therefore be significantly    different. This dissimilarity is thought to be attributable to    conditions that prevailed during the early development of the    solar system (see below     Theories of origin). Planetary temperatures now    range from around 170 C (330 F, 440 K) on Mercurys surface    through the typical 15 C (60 F, 290 K) on Earth to 135 C    (210 F, 140 K) on Jupiter     near its cloud tops and down to 210 C (350 F, 60    K) near Neptunes cloud tops. These are average temperatures;    large variations exist between dayside and nightside for    planets closest to the Sun, except for Venus with its thick    atmosphere.  
    The surfaces of the terrestrial planets and many satellites    show extensive cratering, produced by high-speed impacts    (see     meteorite crater). On Earth, with its large    quantities of water and an active atmosphere, many of these    cosmic footprints have eroded, but remnants of very large    craters can be seen in aerial and spacecraft photographs of the    terrestrial surface. On Mercury, Mars, and the Moon,    the absence of water and any significant atmosphere has left    the craters unchanged for billions of years, apart from    disturbances produced by infrequent later impacts.     Volcanic activity has been an important force in the    shaping of the surfaces of the Moon and the terrestrial    planets. Seismic activity on the Moon has been monitored by    means of seismometers left on its surface by Apollo astronauts    and by Lunokhod robotic rovers. Cratering on the largest scale    seems to have ceased about three billion years ago, although on    the Moon there is clear evidence for a continued cosmic drizzle    of small particles, with the larger objects churning    (gardening) the lunar surface and the smallest producing    microscopic impact pits in crystals in the lunar rocks.  
    During the U.S.     Apollo missions a total weight of 381.7 kg (841.5    pounds) of lunar material was collected; an additional 300    grams (0.66 pounds) was brought back by unmanned Soviet        Luna vehicles. About 15 percent of the Apollo    samples have been distributed for analysis, with the remainder    stored at the     NASA Johnson Space Center, Houston, Texas. The    opportunity to employ a wide range of laboratory techniques on    these lunar samples has revolutionized planetary science. The    results of the analyses have enabled investigators to determine    the composition and age of the lunar surface. Seismic    observations have made it possible to probe the lunar interior.    In addition, retroreflectors left on the Moons surface by    Apollo astronauts have allowed high-power laser beams to be    sent from Earth to the Moon and back, permitting scientists to    monitor the Earth-Moon distance to an accuracy of a few    centimetres. This experiment, which has provided data used in    calculations of the dynamics of the    Earth-Moon system, has shown that the separation of the two    bodies is increasing by 4.4 cm (1.7 inches) each year. (For    additional information on lunar studies, see     Moon.)  
        Mercury is too hot to retain an atmosphere, but        Venuss brilliant white appearance is the result of    its being completely enveloped in thick clouds of carbon    dioxide, impenetrable at visible wavelengths. Below the upper    clouds, Venus has a hostile atmosphere containing clouds of    sulfuric acid droplets. The cloud cover shields the planets    surface from direct sunlight, but the energy that does filter    through warms the surface, which then radiates at infrared    wavelengths. The long-wavelength infrared radiation is trapped    by the dense clouds such that an efficient     greenhouse effect keeps the surface temperature near    465 C (870 F, 740 K). Radar, which can penetrate the thick    Venusian clouds, has been used to map the planets surface. In    contrast, the atmosphere of     Mars is very thin and is composed mostly of carbon    dioxide (95 percent), with very little water vapour; the    planets surface pressure is only about 0.006 that of     Earth. The outer planets have atmospheres composed    largely of light gases, mainly hydrogen and helium.  
    Each planet rotates on its axis, and nearly all of them rotate    in the same directioncounterclockwise as viewed from above the    ecliptic. The two exceptions are Venus, which rotates in the    clockwise direction beneath its cloud cover, and     Uranus, which has its rotation axis very nearly in    the plane of the ecliptic.  
    Some of the planets have magnetic    fields. Earths field extends outward until it is    disturbed by the solar    windan outward flow of protons and electrons from    the Sunwhich carries a magnetic field along with it. Through    processes not yet fully understood, particles from the solar    wind and galactic     cosmic rays (high-speed particles from outside the    solar system) populate two doughnut-shaped regions called the    Van    Allen radiation belts. The inner belt extends from    about 1,000 to 5,000 km (600 to 3,000 miles) above Earths    surface, and the outer from roughly 15,000 to 25,000 km (9,300    to 15,500 miles). In these belts, trapped particles spiral    along paths that take them around Earth while bouncing back and    forth between the Northern and Southern hemispheres, with their    orbits controlled by     Earths magnetic field. During periods of increased    solar activity, these regions of trapped particles are    disturbed, and some of the particles move down into Earths    atmosphere, where they collide with atoms and molecules to    produce auroras.  
        Jupiter has a magnetic field far stronger than    Earths and many more trapped electrons, whose     synchrotron radiation (electromagnetic radiation    emitted by high-speed charged particles that are forced to move    in curved paths, as under the influence of a magnetic field) is    detectable from Earth. Bursts of increased radio emission are    correlated with the position of     Io, the innermost of the four Galilean moons of    Jupiter.     Saturn has a magnetic field that is much weaker than    Jupiters, but it too has a region of trapped particles.    Mercury has a weak magnetic field that is only about 1 percent    as strong as Earths and shows no evidence of trapped    particles. Uranus and     Neptune have fields that are less than one-tenth the    strength of Saturns and appear much more complex than that of    Earth. No field has been detected around Venus or Mars.  
    More than 200,000 asteroids    with well-established orbits are known, and several hundred    additional objects are discovered each year. Hundreds of    thousands more have been seen, but their orbits have not been    as well-determined. It is estimated that several million    asteroids exist, but most are small, and their combined mass is    estimated to be less than a thousandth that of Earth. Most of    the asteroids have orbits close to the ecliptic and move in the    asteroid    belt, between 2.3 and 3.3 AU from the Sun. Because    some asteroids travel in orbits that can bring them close to    Earth, there is a possibility of a collision that could have    devastating results (see     Earth impact hazard).  
    Comets    are considered to come from a vast reservoir, the     Oort cloud, orbiting the Sun at distances of    20,00050,000 AU or more and containing trillions of icy    objectslatent comet nucleiwith the potential to become active    comets. Many comets have been observed over the centuries. Most    make only a single pass through the inner solar system, but    some are deflected by Jupiter or Saturn into orbits that allow    them to return at predictable times.     Halleys Comet is the best-known of these periodic    comets, with its next return into the inner solar system    predicted for 2061 ce. Many    short-period comets are thought to come from the Kuiper    belt, a region lying mainly between 30 AU and 50 AU    from the Sunbeyond Neptunes orbit but including part of    Plutosand housing perhaps hundreds of millions of comet    nuclei. Comet masses have not been well determined, but most    are probably less than 1018 grams, one billionth the mass    of Earth.  
    Since the 1990s more than a thousand comet nuclei in the Kuiper    belt have been observed with large telescopes; a few are about    half the size of Pluto, and at least one,     Eris, is estimated to be slightly larger. Plutos    orbital and physical characteristics had long caused it to be    regarded as an anomaly among the    planets, and, after the discovery of numerous other Pluto-like    objects beyond Neptune, Pluto was seen to be no longer unique    in its neighbourhood but rather a giant member of the local    population. Consequently, in 2006 astronomers at the general    assembly of the International Astronomical Union elected to    create the new category of dwarf    planets for objects with such qualifications. Pluto,    Eris, and     Ceres, the latter being the largest member of the    asteroid belt, were given this distinction. Two other Kuiper    belt objects, Makemake    and Haumea,    were also designated as dwarf planets.  
    Smaller than the observed asteroids and comets are the meteoroids    (see     meteor and meteoroid), lumps of stony or metallic    material believed to be mostly fragments of asteroids and    comets. Meteoroids vary from small rocks to boulders weighing a    ton or more. A relative few have orbits that bring them into    Earths atmosphere and down to the surface as meteorites.    Most if not all meteorites that have been collected on Earth    are probably from asteroids.  
    Meteorites are classified into three broad groups: stony    (chondrites and achondrites; about 94 percent), iron (5    percent), and stony-iron (1 percent). Most meteoroids that    enter the atmosphere heat up sufficiently to glow and appear as    meteors (see     meteor and meteoroid), and the great majority of    these vaporize completely or break up before they reach the    surface. Many, perhaps most, meteors    occur in showers (see     meteor shower) and follow orbits that seem to be    identical with those of certain comets, thus pointing to a    cometary origin. For example, each May, when Earth crosses the    orbit of Halleys Comet, the Eta Aquarid meteor shower occurs.    Micrometeorites (interplanetary    dust particles), the smallest meteoroidal particles,    can be detected from Earth-orbiting satellites or collected by    specially equipped aircraft flying in the stratosphere and    returned for laboratory inspection. Since the late 1960s    numerous meteorites have been found in the Antarctic on the    surface of stranded ice flows (see     Antarctic meteorites). Detailed analyses have shown    that some of these meteorites have come from the Moon and    others from Mars. Yet others contain microscopic crystals whose    isotopic proportions are unique and appear to be dust grains    that formed in the atmospheres of different stars.  
    The age of the solar system, taken to be close to 4.6 billion    years, has been derived from measurements of radioactivity in    meteorites, lunar samples, and Earths crust. Abundances of    isotopes of     uranium,     thorium, and rubidium and their decay products, lead    and strontium, are the measured quantities.  
    Assessment of the chemical composition of the    solar system is based on data from Earth, the Moon, and    meteorites as well as on the spectral analysis of light from    the Sun and planets. In broad outline, the solar system    abundances of the chemical elements decrease with increasing    atomic weight. Hydrogen atoms are by far the most abundant,    constituting    91 percent; helium is next, with 8.9 percent; and all other    types of atoms together amount to only 0.1 percent.  
    The origin of Earth, the Moon, and the solar system as a whole    is a problem that has not yet been settled in detail. The Sun    probably formed by condensation of the     central region of a large cloud of gas and dust,    with the planets and other bodies of the solar system forming    soon after, their composition strongly influenced by the    temperature and pressure gradients in the evolving     solar nebula. Less-volatile materials could condense    into solids relatively close to the Sun to form the terrestrial    planets. The abundant, volatile lighter elements could condense    only at much greater distances to form the giant gas planets.    After the early 1990s astronomers confirmed that stars other    than the Sun have one or more planetlike objects revolving    around them. Studies of the properties of these solar systems    have both supported and challenged astronomers theoretical    models of how Earths solar system formed. (See also        solar system: Origin of the solar system.)  
    The origin of the planetary satellites is not entirely settled.    As to the origin of the Moon, the opinion of astronomers had    long oscillated between theories that saw its origin and    condensation simultaneous with formation of Earth and those    that posited a separate origin for the Moon and its later    capture by Earths gravitational field. Similarities and    differences in abundances of the chemical elements and their    isotopes on Earth and Moon had challenged each group of    theories. Finally, in the 1980s a model emerged that has gained    the support of most lunar scientiststhat of a large impact on    Earth with the expulsion of material that subsequently formed    the Moon. (See     Moon: Origin and evolution.) For the outer planets    with their multiple satellites, many very small and quite    unlike one another, the picture is less clear. Some of these    moons have relatively smooth icy surfaces, whereas others are    heavily cratered; at least one, Jupiters Io, is volcanic. Some    of the moons may have formed along with their parent planets,    and others may have formed elsewhere and been captured.  
    The measurable quantities in stellar astrophysics include the    externally observable features of the     stars: distance, temperature, radiation spectrum and    luminosity, composition (of the outer layers), diameter, mass,    and variability in any of these. Theoretical astrophysicists    use these observations to model the structure of stars and to    devise theories for their formation and evolution. Positional    information can be used for dynamical    analysis, which yields estimates of stellar masses.  
    In a system dating back at least to the Greek    astronomer-mathematician Hipparchus in the 2nd century    bce, apparent stellar    brightness (m) is measured in magnitudes.    Magnitudes are now defined such that a first-magnitude star is    100 times brighter than a star of sixth magnitude. The human    eye cannot see stars fainter than about sixth magnitude, but    modern instruments used with large telescopes can record stars    as faint as about 30th magnitude. By convention, the absolute    magnitude (M) is defined as the magnitude    that a star would appear to have if it were located at a    standard distance of 10 parsecs. These quantities are related    through the expression    mM=5log10r5,    in which r is the stars distance in parsecs.  
    The magnitude scale is anchored on a group of standard stars.    An absolute measure of radiant power is luminosity,    usually expressed in ergs per second (ergs/sec). (Sometimes the    luminosity is stated in terms of the solar luminosity,    3.861033    ergs/sec.) Luminosity can be calculated when m and    r are known. Correction might be necessary for the    interstellar absorption of starlight.  
    There are several methods for measuring a stars    diameter. From the brightness and distance the    luminosity (L) can be calculated, and from    observations of the brightness at different wavelengths the    temperature (T) can be calculated. Because the    radiation from many stars can be well approximated by a        Planck blackbody spectrum (see     Plancks radiation law), these measured quantities    can be related through the expression    L=4R2T4, thus providing a means of    calculating R, the stars radius. In this expression,     is the Stefan-Boltzmann constant,    5.67105ergs/cm2K4sec, in which K is the    temperature in kelvins. (The radius R refers to the    stars     photosphere, the region where the star becomes    effectively opaque to outside    observation.) Stellar angular diameters can be measured through    interference effects. Alternatively, the intensity of the    starlight can be monitored during     occultation by the Moon, which produces diffraction    fringes whose pattern depends on the angular diameter of the    star. Stellar angular diameters of several milliarcseconds can    be measured, but so far only for relatively bright and close    stars.  
    Many stars occur in binary    systems (see     binary star), with the two partners in orbits around    their mutual centre of mass. Such a system provides the best    measurement of stellar masses. The period (P) of a    binary system is related to the masses of the two stars    (m1 and    m2) and the    orbital semimajor axis (mean radius; a) via Keplers    third law: P2=42a3/G(m1+m2).    (G is the universal gravitational constant.) From    diameters and masses, average values of the stellar density can    be calculated and thence the central pressure. With the    assumption of an     equation of state, the central temperature can then    be calculated. For example, in the Sun    the central density is 158 grams per cubic cm; the pressure is    calculated to be more than one billion times the pressure of    Earths atmosphere at sea level and the temperature around 15    million     K (27 million F). At this temperature, all atoms    are ionized, and so the solar interior consists of a     plasma, an ionized gas with hydrogen nuclei (i.e.,    protons), helium nuclei, and electrons as major constituents.    A small fraction of the hydrogen nuclei possess sufficiently    high speeds that, on colliding, their electrostatic repulsion    is overcome, resulting in the formation, by means of a set of        fusion reactions, of helium nuclei and a release of    energy (see     proton-proton cycle). Some of this energy is carried    away by     neutrinos, but most of it is carried by     photons to the surface of the Sun to maintain its    luminosity.  
    Other stars, both more and less massive than the Sun, have    broadly similar structures, but the size, central pressure and    temperature, and fusion rate are functions of the stars mass    and composition. The stars and their internal fusion (and    resulting luminosity) are held stable against collapse through    a delicate balance between the inward pressure produced by    gravitational attraction and the outward pressure supplied by    the photons produced in the fusion reactions.  
    Stars that are in this condition of hydrostatic equilibrium    are termed main-sequence    stars, and they occupy a well-defined band on the        Hertzsprung-Russell (H-R) diagram, in which    luminosity is plotted against colour index or temperature.    Spectral classification, based initially on the colour index,    includes the major spectral types O, B, A, F, G, K and M, each    subdivided into 10 parts (see     star: Stellar spectra). Temperature is deduced from    broadband spectral measurements in several standard     wavelength intervals. Measurement of apparent    magnitudes in two spectral regions, the B and    V bands (centred on 4350 and 5550 angstroms,    respectively), permits calculation of the     colour index, CI=mBmV,    from which the temperature can be calculated.  
    For a given temperature, there are stars that are much more    luminous than main-sequence stars. Given the dependence of    luminosity on the square of the radius and the fourth power of    the temperature (R2T4 of the luminosity expression    above), greater luminosity implies larger radius, and such    stars are termed giant    stars or     supergiant stars. Conversely, stars with    luminosities much less than those of main-sequence stars of the    same temperature must be smaller and are termed white    dwarf stars. Surface temperatures of white dwarfs    typically range from 10,000 to 12,000 K (18,000 to 21,000 F),    and they appear visually as white or blue-white.  
    The strength of spectral lines of the more abundant elements in    a stars atmosphere allows additional subdivisions within a    class. Thus, the Sun, a main-sequence star, is classified as G2    V, in which the V denotes main sequence. Betelgeuse,    a red giant with a surface temperature about half that of the    Sun but with a luminosity of about 10,000 solar units, is    classified as M2 Iab. In this classification, the spectral type    is M2, and the Iab indicates a giant, well above the main    sequence on the H-R diagram.  
    The range of physically allowable masses for stars is very    narrow. If the stars mass is too small, the central    temperature will be too low to sustain fusion reactions. The    theoretical minimum stellar mass is about 0.08 solar mass. An    upper theoretical limit of approximately 100 solar masses has    been suggested, but this value is not firmly defined. Stars as    massive as this will have luminosities about one million times    greater than that of the Sun.  
    A general model of star formation and evolution has been    developed, and the major features seem to be established. A    large cloud of gas and dust can contract under its own    gravitational attraction if its temperature is sufficiently    low. As gravitational energy is released, the contracting    central material heats up until a point is reached at which the    outward     radiation pressure balances the inward gravitational    pressure, and contraction ceases. Fusion reactions take over as    the stars primary source of energy, and the star is then on    the main sequence. The time to pass through these formative    stages and onto the main sequence is less than 100 million    years for a star with as much mass as the Sun. It takes longer    for less massive stars and a much shorter time for those much    more massive.  
    Once a star has reached its main-sequence stage, it evolves    relatively slowly, fusing hydrogen    nuclei in its core to form helium nuclei. Continued fusion not    only releases the energy that is radiated but also results in    nucleosynthesis,    the production of heavier nuclei.  
    Stellar evolution has of necessity been followed through    computer modeling because the timescales for most stages are    generally too extended for measurable changes to be observed,    even over a period of many years. One exception is the supernova,    the violently explosive finale of certain stars. Different    types of supernovas can be distinguished by their spectral    lines and by changes in luminosity during and after the    outburst. In Type Ia, a white    dwarf star attracts matter from its nearby    companion; when the white dwarfs mass exceeds about 1.4 solar    masses, the star implodes and is completely destroyed. Type II    supernovas are not as luminous as Type Ia and are the final    evolutionary stage of stars more massive than about eight solar    masses.  
    The nature of the final products of stellar evolution depend on    stellar mass.    Some stars pass through an unstable stage in which their    dimensions, temperature, and luminosity change cyclically over    periods of hours or days. These so-called     Cepheid variables serve as standard candles for    distance measurements (see above     Determining astronomical distances). Some stars blow    off their outer layers to produce     planetary nebulas. The expanding material can be    seen glowing in a thin shell as it disperses into the    interstellar medium, while the remnant core, initially with a    surface temperature as high as 100,000 K (180,000 F), cools to    become a white dwarf. The maximum stellar mass that can exist    as a white dwarf is about 1.4 solar masses and is known as the        Chandrasekhar limit. More-massive stars may end up    as either     neutron stars or     black holes.  
    The average density of a white dwarf is calculated to exceed    one million grams per cubic cm. Further compression is limited    by a quantum condition    called degeneracy (see     degenerate gas), in which only certain energies are    allowed for the electrons in the stars interior. Under    sufficiently great pressure, the electrons are forced to    combine with protons to form neutrons. The resulting neutron    star will have a density in the range of    10141015 grams per cubic cm, comparable    to the density within atomic nuclei. The behaviour of large    masses having nuclear densities is not yet sufficiently    understood to be able to set a limit on the maximum size of a    neutron star, but it is thought to be in the region of three    solar masses.  
    Still more-massive remnants of stellar evolution would have    smaller dimensions and would be even denser that neutron stars.    Such remnants are conceived to be black    holes, objects so compact that no radiation can    escape from within a characteristic distance called the    Schwarzschild    radius (see     gravitational radius). This critical dimension is    defined by Rs=2GM/c2.    (Rs    is the Schwarzschild radius, G is the gravitational    constant, M is the objects mass, and c is    the speed of light.) For an object of three solar masses, the    Schwarzschild radius would be about three kilometres. Radiation    emitted from beyond the Schwarzschild radius can still escape    and be detected.  
    Although no light can be detected coming from within a black    hole, the presence of a black hole may be manifested    through the effects of its gravitational field, as, for    example, in a binary star system. If a black hole is paired    with a normal visible star, it may pull matter from its    companion toward itself. This matter is accelerated as it    approaches the black hole and becomes so intensely heated that    it radiates large amounts of X-rays from the periphery of the    black hole before reaching the Schwarzschild radius. A few    candidates for stellar black holes have been founde.g., the    X-ray source     Cygnus X-1. Each of them has an estimated mass    clearly exceeding that allowable for a neutron star, a factor    crucial in the identification of possible black holes.    (Supermassive black holes that do not originate as individual    stars are thought to exist at the centres of active galaxies;    see below     Study of other galaxies and related phenomena.)  
    Whereas the existence of stellar black holes has been strongly    indicated, the existence of neutron stars was confirmed in 1968    when they were identified with the then newly discovered    pulsars,    objects characterized by the emission of radiation at short and    extremely regular intervals, generally between 1 and 1,000    pulses per second and stable to better than a part per billion.    Pulsars are considered to be rotating neutron stars, remnants    of some supernovas.  
    Stars are not distributed randomly throughout space. Many stars    are in systems consisting of two or three members separated by    less than 1,000 AU. On a larger scale,     star clusters may contain many thousands of stars.    Galaxies    are much larger systems of stars and usually include clouds of    gas and dust.  
    The solar system is located within the     Milky Way Galaxy, close to its equatorial plane and    about 7.9 kiloparsecs from the galactic centre. The galactic    diameter is about 30 kiloparsecs, as indicated by luminous    matter. There is evidence, however, for nonluminous    matterso-called dark    matterextending out nearly twice this distance. The    entire system is rotating such that, at the position of the    Sun, the orbital speed is about 220 km per second (almost    500,000 miles per hour) and a complete circuit takes roughly    240 million years. Application of Keplers third law leads to    an estimate for the galactic mass of about 100 billion solar    masses. The rotational velocity can be measured from the    Doppler shifts (see     Doppler effect) observed in the 21-cm emission line    of neutral hydrogen and the lines of millimetre wavelengths    from various molecules, especially carbon monoxide. At great    distances from the galactic centre, the rotational velocity    does not drop off as expected but rather increases slightly.    This behaviour appears to require a much larger galactic mass    than can be accounted for by the known (luminous) matter.    Additional evidence for the presence of dark matter comes from    a variety of other observations. The nature and extent of the    dark matter (or missing mass) constitutes    one of todays major astronomical puzzles.  
    There are about 100 billion stars in the Milky Way Galaxy. Star    concentrations within the galaxy fall into three types: open    clusters,    globular clusters, and associations (see     star cluster). Open    clusters lie primarily in the disk of the galaxy;    most contain between 50 and 1,000 stars within a region no more    than 10 parsecs in diameter. Stellar    associations tend to have somewhat fewer stars;    moreover, the constituent    stars are not as closely grouped as those in the clusters and    are for the most part hotter. Globular    clusters, which are widely scattered around the    galaxy, may extend up to about 100 parsecs in diameter and may    have as many as a million stars. The importance to astronomers    of globular clusters lies in their use as indicators of the age    of the galaxy. Because massive stars evolve more rapidly than    do smaller stars, the age of a cluster can be estimated from    its H-R diagram. In a young cluster the main sequence will be    well-populated, but in an old cluster the heavier stars will    have evolved away from the main sequence. The extent of the    depopulation of the main sequence provides an index of age. In    this way, the oldest globular clusters have been found to be    about 14 billion  1 billion years old, which should therefore    be the minimum age for the galaxy.  
    The interstellar    medium, composed primarily of gas and dust, occupies    the regions between the stars. On average, it contains less    than one atom in each cubic centimetre, with about 1 percent of    its mass in the form of minute dust grains. The gas, mostly    hydrogen,    has been mapped by means of its 21-cm emission line. The gas    also contains numerous molecules. Some of these have been    detected by the visible-wavelength absorption lines that they    impose on the spectra of more-distant stars, while others have    been identified by their own emission lines at millimetre    wavelengths. Many of the interstellar molecules are found in    giant molecular clouds, wherein complex organic    molecules have been discovered.  
    In the vicinity of a very hot O- or B-type star, the intensity    of     ultraviolet radiation is sufficiently high to ionize    the surrounding hydrogen out to a distance as great as 100    parsecs to produce an H    II region, known as a Strmgren sphere. Such regions are    strong and characteristic emitters of radiation at radio    wavelengths, and their dimensions are well calibrated in terms    of the luminosity of the central star. Using radio    interferometers, astronomers are able to measure the angular    diameters of H II regions even in some external galaxies and    can thereby deduce the great distances to those remote systems.    This method can be used for distances up to about 30    megaparsecs. (For additional information on H II regions,    see     nebula: Diffuse nebulae (H II regions).)  
    Interstellar    dust grains (see     nebula: Interstellar dust) scatter and absorb    starlight, with the effect being roughly inversely proportional    to wavelength from the infrared to the near ultraviolet. As a    result, stellar spectra tend to be reddened. Absorption amounts    typically to about one magnitude per kiloparsec but varies    considerably in different directions. Some dusty regions    contain silicate materials, identified by a broad absorption    feature around a wavelength of 10 m. Other prominent spectral    features in the infrared range have been sometimes, but not    conclusively, attributed to graphite grains and polycyclic    aromatic hydrocarbons.  
    Starlight often shows a small degree of     polarization (a few percent), with the effect    increasing with stellar distance. This is attributed to the    scattering of the starlight from dust grains that have been    partially aligned in a weak interstellar magnetic field. The    strength of this field is estimated to be a few microgauss,    very close to the strength inferred from observations of    nonthermal cosmic radio noise. This radio background has been    identified as synchrotron radiation, emitted by cosmic-ray    electrons traveling at nearly the speed of light and moving    along curved paths in the interstellar magnetic field. The    spectrum of the cosmic radio noise is close to what is    calculated on the basis of measurements of the cosmic    rays near Earth.  
        Cosmic rays constitute    another component of the interstellar medium. Cosmic rays that    are detected in the vicinity of Earth comprise    high-speed nuclei and electrons. Individual particle energies,    expressed in electron volts (eV; 1    eV=1.61012 erg), range with decreasing    numbers from about 106    eV to more than 1020    eV. Among the nuclei, hydrogen nuclei are the most plentiful at    86 percent, helium nuclei next at 13 percent, and all other    nuclei together at about 1 percent. Electrons are about 2    percent as abundant as the nuclear component. (The relative    numbers of different nuclei vary somewhat with kinetic energy,    while the electron proportion is strongly energy-dependent.)  
    A minority of cosmic rays detected in Earths vicinity are    produced in the Sun, especially at times of increased solar    activity (as indicated by     sunspots and     solar flares). The origin of galactic cosmic rays    has not yet been conclusively identified, but they are thought    to be produced in stellar processes such as supernova    explosions, perhaps with additional acceleration occurring in    the interstellar regions. (For additional information on    interstellar matter, see     Milky Way Galaxy: The general interstellar medium.)  
    The central region of the     Milky Way Galaxy is so heavily obscured by dust that    direct observation has become possible only with the    development of astronomy at nonvisual wavelengthsnamely,    radio, infrared, and, more recently, X-ray and gamma-ray    wavelengths. Together, these observations have revealed a    nuclear region of intense activity, with a large number of    separate sources of emission and a great deal of dust.    Detection of gamma-ray emission at a line energy of 511,000 eV,    which corresponds to the annihilation of electrons and        positrons (the     antimatter counterpart of electrons), along with    radio mapping of a region no more than 20 AU across, points to    a very compact and energetic source, designated Sagittarius    A*, at the centre of the galaxy (see        Sagittarius A). Sagittarius A* is a supermassive    black hole with a mass equivalent to 4,310,000 Suns.  
        Galaxies are normally classified into three    principal types according to their appearance: spiral,    elliptical, and irregular. Galactic diameters are typically in    the tens of kiloparsecs and the distances between galaxies    typically in megaparsecs.  
    Spiral    galaxiesof which the Milky Way system is a    characteristic exampletend to be flattened, roughly circular    systems with their constituent stars strongly concentrated    along spiral arms. These arms are thought to be produced by    traveling density waves, which compress and expand the galactic    material. Between the spiral arms exists a diffuse interstellar    medium of gas and dust, mostly at very low temperatures (below    100 K [280 F, 170 C]). Spiral galaxies are typically a few    kiloparsecs in thickness; they have a central bulge and taper    gradually toward the outer edges.  
    Ellipticals    show none of the spiral features but are more densely packed    stellar systems. They range in shape from nearly spherical to    very flattened and contain little interstellar matter. Irregular    galaxies number only a few percent of all stellar    systems and exhibit none of the regular features associated    with spirals or ellipticals.  
    Properties vary considerably among the different types of    galaxies. Spirals typically have masses in the range of a    billion to a trillion solar masses, with ellipticals having    values from 10 times smaller to 10 times larger and the    irregulars generally 10100 times smaller. Visual galactic    luminosities show similar spreads among the three types, but    the irregulars tend to be less luminous. In contrast, at radio    wavelengths the maximum luminosity for spirals is usually    100,000 times less than for ellipticals or irregulars.  
    Quasars    are objects whose spectra display very large redshifts,    thus implying (in accordance with the Hubble law) that they lie    at the greatest distances (see above     Determining astronomical distances). They were    discovered in 1963 but remained enigmatic for    many years. They appear as starlike (i.e., very compact)    sources of radio waveshence their initial designation as    quasi-stellar radio sources, a term later shortened to    quasars. They are now considered to be the exceedingly    luminous cores of distant galaxies. These energetic cores,    which emit copious quantities    of X-rays and gamma rays, are termed active galactic nuclei and    include the object     Cygnus A and the nuclei of a class of galaxies    called     Seyfert galaxies. They may be powered by the infall    of matter into supermassive black holes.  
    The Milky Way Galaxy is one of the Local    Group of galaxies, which contains more than three    dozen members and extends over a volume about one megaparsec in    diameter. Two of the closest members are the     Magellanic Clouds, irregular galaxies about 50    kiloparsecs away. At about 740 kiloparsecs the     Andromeda Galaxy is one of the most distant in the    Local Group. Some members of the group are moving toward the    Milky Way system, while others are traveling away from it. At    greater distances all galaxies are moving away from the Milky    Way Galaxy. Their speeds (as determined from the redshifted    wavelengths in their spectra) are generally proportional to    their distances. The Hubble law relates these two quantities    (see above     Determining astronomical distances). In the absence    of any other method, the Hubble law continues to be used for    distance determinations to the farthest objectsthat is,    galaxies and quasars for which redshifts can be measured.  
        Cosmology is the scientific study of the universe    as a unified whole, from its earliest moments through its    evolution to its ultimate fate. The currently accepted    cosmological model is the big    bang. In this picture, the expansion of the universe    started in an intense explosion 13.8 billion years ago. In this    primordial fireball, the temperature exceeded    one trillion K, and most of the energy was in the form of    radiation. As the expansion proceeded (accompanied by cooling),    the role of the radiation diminished, and other physical    processes dominated in turn. Thus, after about three minutes,    the temperature had dropped to the one-billion-K range, making    it possible for nuclear reactions of protons to take place and    produce nuclei of deuterium and helium. (At the higher    temperatures that prevailed earlier, these nuclei would have    been promptly disrupted by high-energy photons.) With further    expansion, the time between nuclear collisions had increased    and the proportion of deuterium and helium nuclei had    stabilized. After a few hundred thousand years, the temperature    must have dropped sufficiently for electrons to remain attached    to nuclei to constitute atoms. Galaxies are thought to have    begun forming after a few million years, but this stage is very    poorly understood. Star formation probably started much later,    after at least a billion years, and the process continues    today.  
    Observational support for this general model comes from several    independent directions. The expansion has been documented by    the redshifts observed in the spectra of galaxies. Furthermore,    the radiation left over from the original fireball would have    cooled with the expansion. Confirmation of this relic energy    came in 1965 with one of the most striking cosmic discoveries    of the 20th centurythe observation, at short radio    wavelengths, of a widespread cosmic radiation corresponding to    a temperature of almost 3 K (about 454 F or 270 C). The    shape of the observed spectrum is an excellent fit to the    theoretical Planck blackbody spectrum. (The present best value    for this temperature is 2.735 K, but it is still called    three-degree radiation or the cosmic microwave background.) The    spectrum of this cosmic radio noise peaks at approximately    one-millimetre wavelength, which is in the far infrared, a    difficult region to observe from Earth; however, the spectrum    has been well mapped by the Cosmic Background Explorer (COBE)    and the     Wilkinson Microwave Anisotropy Probe satellites.    Additional support for the big bang theory comes from the    observed cosmic abundances of deuterium and helium. Normal    stellar nucleosynthesis cannot produce their measured    quantities, which fit well with calculations of production    during the early stages of the big bang.  
    Early surveys of the cosmic background radiation indicated that    it is extremely uniform in all directions (isotropic).    Calculations have shown that it is difficult to achieve this    degree of isotropy unless there was a very early and rapid    inflationary period before the expansion settled into its    present mode. Nevertheless, the isotropy posed problems for    models of galaxy formation. Galaxies originate from turbulent    conditions that produce local fluctuations of density, toward    which more matter would then be gravitationally attracted. Such    density variations were difficult to reconcile with    the isotropy required by observations of the 3 K radiation.    This problem was solved when the COBE satellite was able to    detect the minute fluctuations in the cosmic background from    which the galaxies formed.  
    The very earliest stages of the big bang are less well    understood. The conditions of temperature and pressure that    prevailed prior to the first microsecond require the    introduction of theoretical ideas of     subatomic particle physics. Subatomic particles are    usually studied in laboratories with giant accelerators, but    the region of particle energies of potential significance to    the question at hand lies beyond the range of accelerators    currently available. Fortunately, some important conclusions    can be drawn from the observed cosmic helium abundance, which    is dependent on conditions in the early big bang. The observed    helium abundance sets a limit on the number of families of    certain types of subatomic particles that can exist.  
    The age of the universe can be calculated in several ways.    Assuming the validity of the big bang model, one attempts to    answer the question: How long has the universe been expanding    in order to have reached its present size? The numbers relevant    to calculating an answer are Hubbles constant (i.e., the    current expansion rate), the density of matter in the universe,    and the cosmological constant, which allows for change in the    expansion rate. In 2003 a calculation based on a fresh    determination of Hubbles constant yielded an age of    13.7billion 200 million years, although the    precise value depends on certain assumed details of the model    used. Independent estimates of stellar ages have yielded values    less than this, as would be expected, but other estimates,    based on supernova distance measurements, have arrived at    values of about 15 billion years, still consistent, within the    errors. In the big bang model the age is proportional to the    reciprocal of Hubbles constant, hence the    importance of determining H as reliably as possible.    For example, a value for H of 100 km/sec/Mpc would    lead to an age less than that of many stars, a physically    unacceptable result.  
    A small minority of astronomers have developed alternative    cosmological theories that are seriously pursued. The    overwhelming professional opinion, however, continues to    support the big bang model.  
    Finally, there is the question of the future behaviour of the    universe: Is it open? That is to say, will the expansion    continue indefinitely? Or is it closed, such that the expansion    will slow down and eventually reverse, resulting in    contraction? (The final collapse of such a contracting universe    is sometimes termed the big crunch.) The density of the universe seems    to be at the critical density; that is, the universe is neither    open nor closed but flat. So-called dark    energy, a kind of repulsive force that is now    believed to be a major component of the universe, appears to be    the decisive factor in predictions of the long-term fate of the        cosmos. If this energy is a cosmological constant    (as proposed in 1917 by Albert Einstein to correct certain    problems in his model of the universe), then the result would    be a big    chill. In this scenario, the universe would continue to    expand, but its density would decrease. While old stars would    burn out, new stars would no longer form. The universe would    become cold and dark. The dark (nonluminous) matter component    of the universe, whose composition remains unknown, is not    considered sufficient to close the universe and cause it to    collapse; it now appears to contribute only a fourth of the    density needed for closure.  
    An additional factor in deciding the fate of the universe might    be the mass of neutrinos.    For decades the neutrino had been postulated to have zero mass,    although there was no compelling theoretical reason for this to    be so. From the observation of neutrinos generated in the Sun    and other celestial sources such as supernovas, in cosmic-ray    interactions with Earths atmosphere, and in particle    accelerators, investigators have concluded that neutrinos have    some mass, though only an extremely small fraction of the mass    of an electron. Although there are vast numbers of neutrinos in    the universe, the sum of such small neutrino masses appears    insufficient to close the universe.  
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