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Climate Science Lecture 7 – Chemical Weathering and Carbon 1) Carbon Reserviors on Earth a) Vast majority in Sediments and Rocks i) Limestone CaCO3 ii) Hydrocarbons – fossil fuels b) A bit in the Deep Ocean c) Tiny amounts in vegetation, ocean surface water, soil, and atmosphere ii) Dissolution – rain + atmospheric CO2 makes acid – acid weathers carbonate rocks (common rocks at earth’s surface) – creates ions that are used to build shells and CO2 which returns to the atmosphere (1) Dissolution generally returns the CO2 to the atmosphere, so it doesn’t help store much iii) So we rely on hydrolysis – the weathering of silicate rocks to pull CO2 out of the atmosphere and store it in sediments and then rocks 2) Movement of Carbon between reservoirs a) Rate inversely related to size of reservoir i) e.g. vegetation to atmosphere has continuously, second after second ii) but, deep ocean to atmosphere is very slow – centuries 4) Weathering depends on iii) and, rocks to atmosphere takes millions of a) Temperature – Bunsen burner in chem. lab years b) Precipitation – the water to make the acid (1) Until recently (burning fossil fuels) c) Vegetations – transfer CO2 to soil to make b) Volcanic activity as a transfer mechanism the acid from earth’s interior (rocks) to atmosphere i) Also, physical break rocks into smaller i) Eruptions suddenly inject a large amount bits – allows faster chemical weathering of CO2 into the atmosphere ii) Happens at such a rate that it does keep a 5) Weathering thermostat - negative feedback certain flow of carbon from interior of system earth to the atmosphere a) More CO2 in atmosphere (volcano or other iii) Could this mechanism be the thermostat source) we are looking for – NO b) Causes increase temp iv) Thermostat must be effected by the c) Causes increase precip change they cause d) Causes increase vegetation (1) Explain spring of home thermostat e) All 3 cause more weathering v) Volcanic activity is unaffected by the f) Weathering removes CO2 from atmosphere concentration of CO2 in the atmosphere, i) Over millions of years (response time) therefore cannot be the thermostat g) Less CO2 in atmosphere vi) But volcanoes have been adding CO2 to h) Causes decrease temp – decrease precip – the atmosphere forever, why hasn’t it decrease vegetation - negative feedback built up and caused problems? i) If CO2 decreases in atmosphere – temp dec – (1) Especially considering the Young Sun precip dec – vegetation dec – weathering dec Paradox – less CO2 removed from atmosphere – vii) Answer – something must be removing atmosphere warms, etc. CO2 from the atmosphere at a rate comparable to volcanic activities input 3) Chemical Weather as a removal mechanism a) Two chemical reactions do this i) Hydrolysis – rain + atmospheric CO2 makes acid – acid weathers silicate rocks (most common rocks in earth’s crust, especially in young mountains) – creates ions that are used to build shells – which end up as sediment then rock