core course science a-54: life as a planetary phenomenon

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Core Course Science A-54: Life as a Planetary Phenomenon

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Page 1: Core Course Science A-54: Life as a Planetary Phenomenon

Core Course Science A-54: Life as a Planetary Phenomenon

Page 2: Core Course Science A-54: Life as a Planetary Phenomenon

Lecture 3: In the Beginning: Origins of the Elements

1. The Periodic Table: elements and isotopes2. Synthesis of elements in the Early Universe

3. Stars: making the “elements of life”

4. We are made of star stuff.

Page 3: Core Course Science A-54: Life as a Planetary Phenomenon

What is the Universe made of ?

Page 4: Core Course Science A-54: Life as a Planetary Phenomenon

4

NASA Hubble Space Telescope - Jan. 2010

Page 5: Core Course Science A-54: Life as a Planetary Phenomenon

5

Millenium Run, Springel et al. 2006

Page 6: Core Course Science A-54: Life as a Planetary Phenomenon

The Periodic Table

Page 7: Core Course Science A-54: Life as a Planetary Phenomenon

Electron Orbits in Atoms

Page 8: Core Course Science A-54: Life as a Planetary Phenomenon
Page 9: Core Course Science A-54: Life as a Planetary Phenomenon

The Periodic Table

Page 10: Core Course Science A-54: Life as a Planetary Phenomenon

Electron Orbits in Atoms

Page 11: Core Course Science A-54: Life as a Planetary Phenomenon

Electron Orbits in AtomsPlots of electron density shapes of 1s, 2p and 3d orbitals:

Page 12: Core Course Science A-54: Life as a Planetary Phenomenon

The Periodic Table

… in terms of electron subshells:

Page 13: Core Course Science A-54: Life as a Planetary Phenomenon

The Periodic Table

… the elements of Earth life:

Page 14: Core Course Science A-54: Life as a Planetary Phenomenon

Lecture 2: In the Beginning: Origins of the Elements

1. The Periodic Table: elements and isotopes2. Synthesis of elements in the Early Universe

3. Stars: making the “elements of life”

4. We are made of star stuff.

Page 15: Core Course Science A-54: Life as a Planetary Phenomenon
Page 16: Core Course Science A-54: Life as a Planetary Phenomenon
Page 17: Core Course Science A-54: Life as a Planetary Phenomenon

Looking Back into the Past

HotDenseSmooth

ColdThinClumpy

Page 18: Core Course Science A-54: Life as a Planetary Phenomenon

Looking Back into the Past

NASA’s WMAP mission mapped the sky in microwaves

Page 19: Core Course Science A-54: Life as a Planetary Phenomenon

Looking Back into the Past

False-color map of thetemperature fluctuationsseen by measured byWMAP.

This pattern appears tobe random, but it is the superposition of wavesof different size. It islike a fingerprint.

The pattern seen isconsistent only if 75% ofH and 25% of Heconstitute the gas.

Page 20: Core Course Science A-54: Life as a Planetary Phenomenon

Stars like our Sun expand and disperse their envelopes

It takes 3 to 10 Ga for thethe synthesis of light and heavyelements in these stars.Their envelopes are rich in heavyelements - yet, especially inC, N, and O. Eventually new stars are formedfrom this gas.

How do we know that ?a) We see the spectral signaturesof these newly synthesized elements in their light.

Page 21: Core Course Science A-54: Life as a Planetary Phenomenon

The most massive stars end their thermonuclear cycles as Supernovae

Supernova 1994D:the bright explosion of astar in the outskirts of adistant galaxy.

During the explosion, in a matter of minutes, hours anddays, large quantities of iron and other heavy elements are synthesized.

Page 22: Core Course Science A-54: Life as a Planetary Phenomenon

The most massive stars end their thermonuclear cycles as Supernovae

During the explosion, in a matter of hours and days, large quantities of iron andother heavy elements aresynthesized.

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 SolarSystem objects and other stars.

Page 23: Core Course Science A-54: Life as a Planetary Phenomenon

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).

Page 24: Core Course Science A-54: Life as a Planetary Phenomenon

The Periodic Table

… the elements of Earth life:

Page 25: Core Course Science A-54: Life as a Planetary Phenomenon

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.

Page 26: Core Course Science A-54: Life as a Planetary Phenomenon
Page 27: Core Course Science A-54: Life as a Planetary Phenomenon

The Periodic Table

Page 28: Core Course Science A-54: Life as a Planetary Phenomenon

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).