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The distributions and ages of refractory objects in the solar nebula
The distributions and ages of refractory objects in the solar nebula

... necessary to form refractory objects in the solar nebula requires an additional source energy beyond irradiation from the central star. One possible source of energy is internal dissipation of the type predicted in a viscous protoplanetary disk, such as that invoked to explain the accretion of mass ...
Mass and the Properties of Main Sequence Stars
Mass and the Properties of Main Sequence Stars

ppt
ppt

A rocky planet transiting a nearby low-mass star
A rocky planet transiting a nearby low-mass star

... pure magnesium silicate, and the interior contains no water21 . These simplifications mean that the iron fraction should not be taken as absolute; the model simply represents a characteristic mass-radius locus that matches Earth and Venus. This same composition also matches the masses and radii of K ...
Science Project
Science Project

... Outer planets The four outer planets, or gas giants (sometimes called Jovian planets), collectively make up 99 percent of the mass known to orbit the Sun. Jupiter and Saturn are each many tens of times the mass of the Earth and consist overwhelmingly of hydrogen and helium; Uranus and Neptune are f ...
The Milky Way Galaxy
The Milky Way Galaxy

Dynamical habitability of planetary systems
Dynamical habitability of planetary systems

... days), the planet is far too hot to be habitable; the estimated temperature is more than 1000 degrees! In fact, most of the exoplanets are in close-by orbits to their stars, which is most certainly a biased value, given that we have only observed them over the course of about 15 years with technique ...
The Physics and Chemistry of Nebular Evolution
The Physics and Chemistry of Nebular Evolution

PPT
PPT

... • Monitoring of hundreds of thousands of stars to 200 pc for 1MJ planets with P < 10 years: – complete census of all stellar types (P=2-9 years) – actual masses, not just lower limits (m sin i) – 20,000-30,000 planets expected to 150-200 pc ...
Archaeology of the Milky Way - Max-Planck
Archaeology of the Milky Way - Max-Planck

minimum mass extrasolar nebula derived from the
minimum mass extrasolar nebula derived from the

Structure of Neutron Stars
Structure of Neutron Stars

VESPA`s bins
VESPA`s bins

The Solar Nebula on Fire: A Solution to the Carbon Deficit in the
The Solar Nebula on Fire: A Solution to the Carbon Deficit in the

... at the depth (0.122 AU) where Tgas = 500 K. These results demonstrate that, assuming no source term, there is a rapid decay of carbon grains to reduced carbon content and size. We define tdest of a certain size of grain when X(g1 ) decreases by 4 orders of magnitude in the reservoir. Therefore, 0.00 ...
p - INAF-OAT Trieste Users site
p - INAF-OAT Trieste Users site

Death of the Stars
Death of the Stars

A scenario of planet erosion by coronal radiation*
A scenario of planet erosion by coronal radiation*

Dark Matter: Observational Constraints Properties of Dark Matter:
Dark Matter: Observational Constraints Properties of Dark Matter:

... • dN(m)/dm ~ m-2.3 implies most mass is at the low mass end of the spectrum. ...
life cycles of stars
life cycles of stars

... and Carbon • “White dwarf” cools but does not contract because core is degenerate • No energy from fusion, no energy from gravitational contraction • White dwarf slowly fades away… ...
Age Aspects of Habitability
Age Aspects of Habitability

... presume the presence of an oxygen atmosphere as necessary for a planet to host a complex life. Such life would have modified the global planetary (or atmospheric) properties to be noticed from space, and from very far away; after all, the closest potentially habitable planet is at about 12 light yea ...
Orbital and Physical Characteristics of Extrasolar Planets Systems
Orbital and Physical Characteristics of Extrasolar Planets Systems

... To the very time of the detection of the first extrasolar planet system, our concept was based only upon the study of the Solar system structure. As is well known, the later has been formed around a main sequence star (The Sun) of late spectral type-G2V. According to the statistical analysis of the ...
PDF only - at www.arxiv.org.
PDF only - at www.arxiv.org.

... systems during their stars’ main sequence lifetimes, our first step was to model the main sequence lifetime of theoretical stars. This allowed us to follow the changes in their total power output i.e. the luminosity L, and in the surface temperature as represented by the effective temperature Te, th ...
The Changing Earth Atmosphere
The Changing Earth Atmosphere

... a) The Earth’s atmosphere is simply called air. It is primarily composed of many discrete gases, each with its own physical properties, in which varying quantities of tiny solid and liquid particles are suspended. b) ...
DoAr21_AAS2005 - Astronomy at Swarthmore College
DoAr21_AAS2005 - Astronomy at Swarthmore College

From Hot Jupiters to Hot Neptunes and Below
From Hot Jupiters to Hot Neptunes and Below

... The saga of the detection of exoplanets has been constantly driven by the evenincreasing accuracy of the radial velocity determination. Until the end of the eighties, the most accurate radial velocities were obtained with cross-correlation spectrographs like CORAVEL with a precision on individual me ...
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Nebular hypothesis

The nebular hypothesis is the most widely accepted model in the field of cosmogony to explain the formation and evolution of the Solar System. It suggests that the Solar System formed from nebulous material. The theory was developed by Immanuel Kant and published in his Universal Natural History and Theory of the Heaven. Originally applied to our own Solar System, this process of planetary system formation is now thought to be at work throughout the universe. The widely accepted modern variant of the nebular hypothesis is the solar nebular disk model (SNDM) or simply solar nebular model. This nebular hypothesis offered explanations for a variety of properties of the Solar System, including the nearly circular and coplanar orbits of the planets, and their motion in the same direction as the Sun's rotation. Some elements of the nebular hypothesis are echoed in modern theories of planetary formation, but most elements have been superseded.According to the nebular hypothesis, stars form in massive and dense clouds of molecular hydrogen—giant molecular clouds (GMC). These clouds are gravitationally unstable, and matter coalesces within them to smaller denser clumps, which then rotate, collapse, and form stars. Star formation is a complex process, which always produces a gaseous protoplanetary disk around the young star. This may give birth to planets in certain circumstances, which are not well known. Thus the formation of planetary systems is thought to be a natural result of star formation. A Sun-like star usually takes approximately 1 million years to form, with the protoplanetary disk evolving into a planetary system over the next 10-100 million years.The protoplanetary disk is an accretion disk that feeds the central star. Initially very hot, the disk later cools in what is known as the T tauri star stage; here, formation of small dust grains made of rocks and ice is possible. The grains eventually may coagulate into kilometer-sized planetesimals. If the disk is massive enough, the runaway accretions begin, resulting in the rapid—100,000 to 300,000 years—formation of Moon- to Mars-sized planetary embryos. Near the star, the planetary embryos go through a stage of violent mergers, producing a few terrestrial planets. The last stage takes approximately 100 million to a billion years.The formation of giant planets is a more complicated process. It is thought to occur beyond the so-called frost line, where planetary embryos mainly are made of various types of ice. As a result, they are several times more massive than in the inner part of the protoplanetary disk. What follows after the embryo formation is not completely clear. Some embryos appear to continue to grow and eventually reach 5–10 Earth masses—the threshold value, which is necessary to begin accretion of the hydrogen–helium gas from the disk. The accumulation of gas by the core is initially a slow process, which continues for several million years, but after the forming protoplanet reaches about 30 Earth masses (M⊕) it accelerates and proceeds in a runaway manner. Jupiter- and Saturn-like planets are thought to accumulate the bulk of their mass during only 10,000 years. The accretion stops when the gas is exhausted. The formed planets can migrate over long distances during or after their formation. Ice giants such as Uranus and Neptune are thought to be failed cores, which formed too late when the disk had almost disappeared.
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