Lecture 7 - Lecture notes for L8 Geosciences...

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Lecture notes for L8 Geosciences 040-Arthur/Marone (copyright Pennsylvania State University, 2005) Sep 22nd Reading: Chapt. 6 in Garrison Add these notes in to continue from Lecture of Sep 20th EVAPORATION and SALT PRECIPITATION Evaporation of seawater produces predictable sequence of mineral salts (minerals become saturated at certain point) --after evaporation of a few % of water mass CaCO3 (Calcite) precipitates; --after evaporation of 81%, CaSO4 (Gypsum) fully precipitated; --after evaporation of about 90.5%, NaCl (Halite) is fully precipitated; --at 96% evaporation, the K and Mg salts (w/ SO4 and Cl) drop out. (Enough salt in ocean to cover land with layer 170 m thick) Natural deposits from ancient oceans like this-- called "evaporites" THE CHEMISTRY OF ANCIENT OCEANS This is how we can tell something about the chemistry of ancient oceans --types of salts and sequence in ancient evaporite deposits provide indication of ocean chemical change --inclusions of "brines" in salt minerals also allow us to constrain major element ratios in ancient seawater --new data suggests that ocean chemistry varied considerably in the past, possibly due to changes in sea floor spreading rates and cycling of seawater through hydrothermal systems. All other dissolved substances in seawater are at very low concentrations
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This note was uploaded on 03/30/2008 for the course GEOSC 040 taught by Professor Arthur during the Fall '08 term at Pennsylvania State University, University Park.

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Lecture 7 - Lecture notes for L8 Geosciences...

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