283x Filetype PPTX File size 0.68 MB Source: projects.iq.harvard.edu
HISTORY OF EARTH’S ATMOSPHERE
N
2
CO2
O
2 O reaches
HO 2
2 current levels;
oceans CO
form 2 life invades
dissolves continents
Outgassing Life forms Onset of
in oceans photosynthesis
4.5 Gy 4 Gy 3.5 Gy 0.4 Gy present
B.P B.P. B.P. B.P.
Evolution of oxygen and ozone over Earth’s history
Life appears on land
RUNAWAY GREENHOUSE EFFECT ON VENUS
due to accumulation of water vapor from volcanic outgassing early in its history
…did not happen on Earth because farther from Sun; as water accumulated it
reached saturation and precipitated, forming the oceans
EARTH VENUS
Comparing the atmospheres of Earth and Venus
Venus Earth
Radius (km) 6100 6400
Surface pressure (atm) 91 1
-4
CO (mol/mol) 0.96 3x10
2
-2
N (mol/mol) 3.4x10 0.78
2
-5
O (mol/mol) 6.9x10 0.21
2
-3 -2
HO (mol/mol) 3x10 1x10
2
BIOGEOCHEMICAL CYCLING OF ELEMENTS:
examples of major processes
Physical exchange, redox chemistry, biochemistry are involved
Surface
reservoirs
no reviews yet
Please Login to review.