Structure and Energy Transport of the Solar Convection Zone A
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Solar Radiation
5 Solar Radiation In this chapter we discuss the aspects of solar radiation, which are important for solar en- ergy. After defining the most important radiometric properties in Section 5.2, we discuss blackbody radiation in Section 5.3 and the wave-particle duality in Section 5.4. Equipped with these instruments, we than investigate the different solar spectra in Section 5.5. How- ever, prior to these discussions we give a short introduction about the Sun. 5.1 The Sun The Sun is the central star of our solar system. It consists mainly of hydrogen and helium. Some basic facts are summarised in Table 5.1 and its structure is sketched in Fig. 5.1. The mass of the Sun is so large that it contributes 99.68% of the total mass of the solar system. In the center of the Sun the pressure-temperature conditions are such that nuclear fusion can Table 5.1: Some facts on the Sun Mean distance from the Earth 149 600 000 km (the astronomic unit, AU) Diameter 1392000km(109 × that of the Earth) Volume 1300000 × that of the Earth Mass 1.993 ×10 27 kg (332 000 times that of the Earth) Density(atitscenter) >10 5 kg m −3 (over 100 times that of water) Pressure (at its center) over 1 billion atmospheres Temperature (at its center) about 15 000 000 K Temperature (at the surface) 6 000 K Energy radiation 3.8 ×10 26 W TheEarthreceives 1.7 ×10 18 W 35 36 Solar Energy Internal structure: core Subsurface ows radiative zone convection zone Photosphere Sun spots Prominence Flare Coronal hole Chromosphere Corona Figure 5.1: The layer structure of the Sun (adapted from a figure obtained from NASA [ 28 ]). -
The Sun and the Solar Corona
SPACE PHYSICS ADVANCED STUDY OPTION HANDOUT The sun and the solar corona Introduction The Sun of our solar system is a typical star of intermediate size and luminosity. Its radius is about 696000 km, and it rotates with a period that increases with latitude from 25 days at the equator to 36 days at poles. For practical reasons, the period is often taken to be 27 days. Its mass is about 2 x 1030 kg, consisting mainly of hydrogen (90%) and helium (10%). The Sun emits radio waves, X-rays, and energetic particles in addition to visible light. The total energy output, solar constant, is about 3.8 x 1033 ergs/sec. For further details (and more accurate figures), see the table below. THE SOLAR INTERIOR VISIBLE SURFACE OF SUN: PHOTOSPHERE CORE: THERMONUCLEAR ENGINE RADIATIVE ZONE CONVECTIVE ZONE SCHEMATIC CONVECTION CELLS Figure 1: Schematic representation of the regions in the interior of the Sun. Physical characteristics Photospheric composition Property Value Element % mass % number Diameter 1,392,530 km Hydrogen 73.46 92.1 Radius 696,265 km Helium 24.85 7.8 Volume 1.41 x 1018 m3 Oxygen 0.77 Mass 1.9891 x 1030 kg Carbon 0.29 Solar radiation (entire Sun) 3.83 x 1023 kW Iron 0.16 Solar radiation per unit area 6.29 x 104 kW m-2 Neon 0.12 0.1 on the photosphere Solar radiation at the top of 1,368 W m-2 Nitrogen 0.09 the Earth's atmosphere Mean distance from Earth 149.60 x 106 km Silicon 0.07 Mean distance from Earth (in 214.86 Magnesium 0.05 units of solar radii) In the interior of the Sun, at the centre, nuclear reactions provide the Sun's energy. -
The Solar Core As Never Seen Before
The solar core as never seen before A. Eff-Darwich1;2, S.G. Korzennik3 1 Instituto de Astrof´ısicade Canarias (IAC), E-38200 La Laguna, Tenerife, Spain 2 Dept. de Edafolog´ıay Geolog´ıa,Universidad de La Laguna (ULL), E-38206 La Laguna, Tenerife, Spain 3 Harvard-Smithsonian Center for Astrophysics, 60 Garden St. Cambridge, MA,02138, USA E-mail: [email protected], [email protected] Abstract. One of the main drawbacks in the analysis of the dynamics of the solar core comes from the lack of consistent data sets that cover the low and intermediate degree range (` = 1; 200). It is usually necessary to merge data obtained from different instruments and/or fitting methodologies and hence one introduces undesired systematic errors. In contrast, we present the results of analyzing MDI rotational splittings derived by a single fitting methodology applied to 4608-, 2304-, etc..., down to 182-day long time series. The direct comparison of these data sets and the analysis of the numerical inversion results have allowed us to constrain the dynamics of the solar core and to establish the accuracy of these data as a function of the length of the time-series. 1. Introduction Ground-based helioseismic observations, e.g., GONG [5], and space-based ones, e.g., MDI [10] or GOLF [4], have allowed us to derive a good description of the dynamics of the solar interior [12], [2], [6]. Such helioseismic inferences have confirmed that the differential rotation observed at the surface persists throughout the convection zone. The outer radiative zone (0:3 < r=R < 0:7) appears to rotate approximately as a solid body at an almost constant rate (≈ 430 nHz), whereas the innermost core (0:19 < r=R < 0:3) rotates slightly faster than the rest of the radiative region. -
The Solar System
The Solar System Our automated spacecraft have traveled to the Moon and to all the planets beyond our world The Sun appears to have been active for 4.6 billion years and has enough fuel for another 5 except Pluto; they have observed moons as large as small planets, flown by comets, and billion years or so. At the end of its life, the Sun will start to fuse helium into heavier elements sampled the solar environment. The knowledge gained from our journeys through the solar and begin to swell up, ultimately growing so large that it will swallow Earth. After a billion years system has redefined traditional Earth sciences like geology and meteorology and spawned an as a "red giant," it will suddenly collapse into a "white dwarf" -- the final end product of a star like entirely new discipline called comparative planetology. By studying the geology of planets, ours. It may take a trillion years to cool off completely. moons, asteroids, and comets, and comparing differences and similarities, we are learning more about the origin and history of these bodies and the solar system as a whole. We are also Mercury gaining insight into Earth's complex weather systems. By seeing how weather is shaped on other worlds and by investigating the Sun's activity and its influence through the solar system, Obtaining the first close-up views of Mercury was the primary objective of the Mariner 10 we can better understand climatic conditions and processes on Earth. spacecraft, launched Nov 3, 1973. After a journey of nearly 5 months, including a flyby of Venus, the spacecraft passed within 703 km (437 mi) of the solar system's innermost planet on Mar 29, The Sun 1974. -
Stellar Evolution
AccessScience from McGraw-Hill Education Page 1 of 19 www.accessscience.com Stellar evolution Contributed by: James B. Kaler Publication year: 2014 The large-scale, systematic, and irreversible changes over time of the structure and composition of a star. Types of stars Dozens of different types of stars populate the Milky Way Galaxy. The most common are main-sequence dwarfs like the Sun that fuse hydrogen into helium within their cores (the core of the Sun occupies about half its mass). Dwarfs run the full gamut of stellar masses, from perhaps as much as 200 solar masses (200 M,⊙) down to the minimum of 0.075 solar mass (beneath which the full proton-proton chain does not operate). They occupy the spectral sequence from class O (maximum effective temperature nearly 50,000 K or 90,000◦F, maximum luminosity 5 × 10,6 solar), through classes B, A, F, G, K, and M, to the new class L (2400 K or 3860◦F and under, typical luminosity below 10,−4 solar). Within the main sequence, they break into two broad groups, those under 1.3 solar masses (class F5), whose luminosities derive from the proton-proton chain, and higher-mass stars that are supported principally by the carbon cycle. Below the end of the main sequence (masses less than 0.075 M,⊙) lie the brown dwarfs that occupy half of class L and all of class T (the latter under 1400 K or 2060◦F). These shine both from gravitational energy and from fusion of their natural deuterium. Their low-mass limit is unknown. -
198Lapj. . .243. .945G the Astrophysical Journal, 243:945-953
.945G .243. The Astrophysical Journal, 243:945-953, 1981 February 1 . © 1981. The American Astronomical Society. All rights reserved. Printed in U.S.A. 198lApJ. CONVECTION AND MAGNETIC FIELDS IN STARS D. J. Galloway High Altitude Observatory, National Center for Atmospheric Research1 AND N. O. Weiss Sacramento Peak Observatory2 Received 1980 March 10; accepted 1980 August 18 ABSTRACT Recent observations have demonstrated the unity of the study of stellar and solar magnetic fields. Results from numerical experiments on magnetoconvection are presented and used to discuss the concentration of magnetic flux into isolated ropes in the turbulent convective zones of the Sun or other late-type stars. Arguments are given for siting the solar dynamo at the base of the convective zone. Magnetic buoyancy leads to the emergence of magnetic flux in active regions, but weaker flux ropes are shredded and dispersed throughout the convective zone. The observed maximum field strengths in late-type stars should be comparable with the field (87rp)1/2 that balances the photospheric pressure. Subject headings: convection — hydrodynamics — stars: magnetic — Sun : magnetic fields I. INTRODUCTION In § II we summarize the results obtained for simplified The Sun is unique in having a magnetic field that can be models of hydromagnetic convection. The structure of mapped in detail, but magnetic activity seems to be a turbulent magnetic fields is then described in § III. standard feature of stars with deep convective envelopes. Theory and observation are brought together in § IV, Fields of 2000 gauss or more have been found in two where we discuss the formation of isolated flux tubes in late-type main sequence stars (Robinson, Worden, and the interior of the Sun. -
Structure of the Sun
HELIOSEISMOLOGY (I) STRUCTURE OF THE SUN ² The Sun is the only star for which we can measure internal properties ! test of stellar structure theory ² acoustic mode Composition (heavy elements) from meteorites in the Sun ² (p mode Density, internal rotation from helioseismology n=14, l -20) ² Central conditions from neutrinos HELIOSEISMOLOGY ² The Sun acts as a resonant cavity, oscillating in mil- lions of (acoustic, gravity) modes (like a bell) ! can be used to reconstruct the internal density struc- ture (like earthquakes on Earth) full-disk ² oscillation modes are excited by convective eddies Dopplergram ² periods of typical modes: 1.5 min to 20 min ² velocity amplitudes: » 0:1 m/s ² need to measure Doppler shifts in spectral lines rela- tive to their width to an accuracy of 1:106 . possible with good spectrometers and long integra- tion times (to average out noise) Results ² density structure, sound speed ² depth of outer convective zone: » 0:28 R¯ velocity (km/s) ² rotation in the core is slow (almost like a solid-body) ! the core must have been spun-down with the enve- lope (e±cient core{envelope coupling) SOLAR NEUTRINOS ² Neutrinos, generated in solar core, escape from the Sun and carry away 2 ¡ 6 % of the energy released in H-burning reactions HELIOSEISMOLOGY (II) ² they can be observed in underground experiments ! direct probe of the solar core ² neutrino-emitting reactions (in the pp chains) 1 1 2 + max + ! + + = : H H D e E 0 42 Mev 7 ¡ 7 max + ! + = : Be e Li E 0 86 Mev 8 8 + max ! + + = : B Be e E 14 0 Mev ² The Davis experiment (starting around 1970) has shown that the neutrino flux is about a factor of 3 lower than predicted ! the solar neutrino problem The Homestake experiment (Davis) ² neutrino detector: underground tank ¯lled with 600 tons of Chlorine (C2 Cl4 : dry-cleaning fluid) ² some neutrinos react with Cl 37 37 ¡ e + Cl ! Ar + e ¡ 0:81 Mev ² rate of absorption » 3 £ 10¡35 s¡1 per 37Cl atom ² every 2 months each 37Ar atom is ¯ltered out of the rotation rate (nHz) tank (expected number: 54; observed number: 17) ² caveats convection zone . -
How Stars Work: • Basic Principles of Stellar Structure • Energy Production • the H-R Diagram
Ay 122 - Fall 2004 - Lecture 7 How Stars Work: • Basic Principles of Stellar Structure • Energy Production • The H-R Diagram (Many slides today c/o P. Armitage) The Basic Principles: • Hydrostatic equilibrium: thermal pressure vs. gravity – Basics of stellar structure • Energy conservation: dEprod / dt = L – Possible energy sources and characteristic timescales – Thermonuclear reactions • Energy transfer: from core to surface – Radiative or convective – The role of opacity The H-R Diagram: a basic framework for stellar physics and evolution – The Main Sequence and other branches – Scaling laws for stars Hydrostatic Equilibrium: Stars as Self-Regulating Systems • Energy is generated in the star's hot core, then carried outward to the cooler surface. • Inside a star, the inward force of gravity is balanced by the outward force of pressure. • The star is stabilized (i.e., nuclear reactions are kept under control) by a pressure-temperature thermostat. Self-Regulation in Stars Suppose the fusion rate increases slightly. Then, • Temperature increases. (2) Pressure increases. (3) Core expands. (4) Density and temperature decrease. (5) Fusion rate decreases. So there's a feedback mechanism which prevents the fusion rate from skyrocketing upward. We can reverse this argument as well … Now suppose that there was no source of energy in stars (e.g., no nuclear reactions) Core Collapse in a Self-Gravitating System • Suppose that there was no energy generation in the core. The pressure would still be high, so the core would be hotter than the envelope. • Energy would escape (via radiation, convection…) and so the core would shrink a bit under the gravity • That would make it even hotter, and then even more energy would escape; and so on, in a feedback loop Ë Core collapse! Unless an energy source is present to compensate for the escaping energy. -