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Published byOsborn McDowell Modified over 9 years ago
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Ch. 28 The SUN
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28.1 The Structure of the Sun 3 Parts 1.Core 2.Inner Zones Radiative Zone Convective Zone 3.Atmosphere
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The Core Entirely composed of Gas Nuclear Fusion Reactor H + H He + energy Energy is released as heat and light E = mc 2 Energy = (mass)(speed of light) 2
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The Inner Zones Radiative Zone: Energy is moving from atom to atom in the form of waves (radiation) Convective Zone: Energy is transferred through the movement of unevenly heated gases (convection)
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The Sun’s Atmosphere Photosphere: Inner most layer Chromosphere: gasses that appear to glow red Corona: The outermost layer – Solar Wind: Charged atomic particles that stream out into space
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Solar Activity Sun Spots: Cooler gases that appear dark in comparison to surrounding gasses.
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Prominences: clouds of gasses that arch into space.
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Solar Flares: outward eruption of electrically charged particles. Auroras: When electrically charged particles of a solar wind reach earth.
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Stop for Today
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28.3 Formation of the Solar System 1.About 4-5 billion years ago, a Solar Nebula contracted due to an outside force. 2.The Sun began to form at the center of the contacting nebula – 99% of the matter in the nebula became the sun 3.Left over matter aggregated to form the planets
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Temperature and Distance from the Sun affected the planetary composition. – Proto-planets closest to the sun contain large amounts of heavier elements, such as iron – Proto-planets further away consist of gasses and lighter elements
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Formation of Earth Early Earth was very hot compared to Earth today. – Heat from collisions with plantesimals – Increasing mass of the outer core, increased inner pressure and temperature – Radioactive materials were very abundant
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Separation into 3 layers Dense materials, such as iron, flowed into the center Less dense materials were forced to the outer layers
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Formation of the Atmosphere Original atmosphere just hydrogen and helium
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Earth’s “second atmosphere” came from Earth itself. The volcanoes released: - steam (H 2 O) - carbon dioxide (CO 2 ) - ammonia (NH 3 )
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Eventually photosynthetic organisms converted the carbon dioxide gas found in the oceans into oxygen. This formed our current atmosphere
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