Lecture 3 Jan 10.docx

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Department
Geological Sciences and Geological Engineering
Course
GEOL 106
Professor
Paul Grogan
Semester
Winter

Description
Lecture 3 Coal Production - Has increased since 1800’s and took a steep increase since 1960. - Coal = mainly Carbon (C)  Burn it with Oxygen (O)  Produce Carbon Dioxide (CO2)  which is a Greenhouse gas and warms the atmosphere 1) Measure it directly Day-to-Day (we’ve only been doing this since 1950’s)  Charles Reeling began measuring it at the top of a Hawaiian volcano. - Created the Keeling curve, pretty consistent rise in CO2 in atmosphere since began recording. 2) To go back further in time, measure CO2 in air bubbles trapped in ice sheets in Antarctic and Greenland Glaciers  This takes us back about 400,000 years. - Just like how they analyzed the dust in ice layers, that took the air bubbles trapped in the ice and analyzed the amount of CO2 in the air. - These helped show that the scale of human impact has risen dramatically in CO2 in the atmosphere exponentially. How does past E.S.E compare to future E.S.E. (Earth systems engineering)? 2 main differences. 1) Scale: in past, was more local, less global 2) Intent: in past, effects were unintended and unanticipated Thomas Midgely “had more impact on the atmosphere than any other single organism in earth history”. - Leaded gasoline - In 1921, Midgley invented leaded gasoline, tetra-ethyl lead
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