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Science of the Physical Universe 30: Life as a Planetary Phenomenon
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Formerly … Science Core A-54: Life as a Planetary Phenomenon Instructor: Dimitar Sasselov
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Instructor: Dimitar Sasselov Teaching Fellows: Wade Henning (Head TF), Darin Ragozzine, Li Zeng, Jessica Haurin, Maggie McLean Science of the Physical Universe 30: Life as a Planetary Phenomenon
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1.Course structure 2.Grading 3.Organizational matters Science of the Physical Universe 30: Life as a Planetary Phenomenon
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Course Structure: 5 themes 1.The Origin and Evolution of Planets 2.The Origin and Evolution of Life 3.Exploring the Solar System for Life 4.Searching for Life beyond the Solar System 5.Extraterrestrial Intelligence
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1.Course structure 2.Grading 3.Organizational matters: Midterm Exam - on March 3 or 8-th ? Sections Science of the Physical Universe 30: Life as a Planetary Phenomenon
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TEXTBOOKS: Science of the Physical Universe 30: Life as a Planetary Phenomenon
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Opportunities for Undergraduates at Harvard Undergraduate Research Fellowships Individual awards of up to $2,000 are available for Harvard undergraduates for research during the academic year. Summer Undergraduate Research Fellowships - 2011 Funding Summer Undergraduate Research Grants of up to $5,000 are available for undergraduates working in Origins team member labs on Origins-related projects. For more information on any of these programs, please contact: Carol Knell, Origins Program Coordinator, at cknell@cfa.harvard.edu.
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The discovery of Kepler’s first rocky planet (announced Jan. 9, 2011) Radius: 1.4 Earth Earth
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Lecture 2: In the Beginning: Origins of the Elements 1.The Periodic Table: elements and isotopes 2.Synthesis of elements in the Early Universe 3.Stars: making the “elements of life” 4.We are made of star stuff.
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What is the Universe made of ?
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13 NASA Hubble Space Telescope - Jan. 2010
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14 Millenium Run, Springel et al. 2006
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The Periodic Table
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Electron Orbits in Atoms
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The Periodic Table
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Electron Orbits in Atoms
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Plots of electron density shapes of 1s, 2p and 3d orbitals:
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The Periodic Table … in terms of electron subshells:
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The Periodic Table … the elements of Earth life:
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Lecture 2: In the Beginning: Origins of the Elements 1.The Periodic Table: elements and isotopes 2.Synthesis of elements in the Early Universe 3.Stars: making the “elements of life” 4.We are made of star stuff.
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Looking Back into the Past Hot Dense Smooth Cold Thin Clumpy
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Looking Back into the Past NASA’s WMAP mission mapped the sky in microwaves
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Looking Back into the Past False-color map of the temperature fluctuations seen by measured by WMAP. This pattern appears to be random, but it is the superposition of waves of different size. It is like a fingerprint. The pattern seen is consistent only if 75% of H and 25% of He constitute the gas.
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Stars like our Sun expand and disperse their envelopes It takes 3 to 10 Ga for the the synthesis of light and heavy elements in these stars. Their envelopes are rich in heavy elements - yet, especially in C, N, and O. Eventually new stars are formed from this gas. How do we know that ? a)We see the spectral signatures of these newly synthesized elements in their light.
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The most massive stars end their thermonuclear cycles as Supernovae Supernova 1994D: the bright explosion of a star in the outskirts of a distant galaxy. During the explosion, in a matter of minutes, hours and days, large quantities of iron and other heavy elements are synthesized.
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The most massive stars end their thermonuclear cycles as Supernovae During the explosion, in a matter of hours and days, large quantities of iron and other heavy elements are synthesized. How do we know that ? a)We see the spectral signatures in the light from the explosion; b)Computer models reproduce measured isotopic ratios in Solar System objects and other stars.
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We are made of star stuff By mass - Human body: H = 10%, He = 0%, C = 18%, N = 3%, O = 65%, Ca = 2%, Fe = 0.004%. Earth’s crust: H = 1 %, He = 0%, C = 2%, N = 0%, O = 47%, Si = 26%, Ca = 3%, Fe = 5% Sun & stars: H = 71%, He = 27%, all other elements = 2% (with O most abundant).
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The Periodic Table … the elements of Earth life:
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Main points to take home: 1) Elements: def. by protons in atom (90 stable); Isotopes: def. by neutrons in atom (266 stable) The Periodic Table of the Elements allows the analytical description of all species of mineral or biological origin. 2)There are 2 main sources of their origin: a) H, He, & Li were synthesized ~13.7 Ga ago in the Early Universe; b) stars transform H & He into all the rest. 3) Planets and life are here thanks to many past generations of stars.
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The Periodic Table
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We are made of star stuff By mass - Human body: H = 10%, He = 0%, C = 18%, N = 3%, O = 65%, Ca = 2%, Fe = 0.004%. Plants: H = 10%, He = 0%, C = 3%, N = 0.3%, O = 79%, Ca = 0.1%, Fe = 0.02%. Earth’s crust: H = 1 %, He = 0%, C = 2%, N = 0%, O = 47%, Si = 26%, Ca = 3%, Fe = 5% Sun & stars: H = 71%, He = 27%, all other elements = 2% (with O most abundant).
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