ENVR 200 Lecture Notes - Lecture 14: Solubility Pump, Biological Pump, Volumetric Flow Rate

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Huge pools of carbon being released in small amount at a time over long period. Carbon exchange between terrestrial and atmosphere: co2 in atmosphere is converted to organic carbon through photosynthesis. Note that 95% of organic matter is carbon. Organic carbon passes through the food chain from primary producers to consumers. Decomposition of organic material releases inorganic carbon as co2 and is releases back to atmosphere. Carbon is stored in different reservoirs and is exchanged between these reservoirs. Material enters and leaves at certain rates; remains only temporarily in the reservoir. Residence time of material = reservoir volume / flow rate. Terrestrial reservoir: soil, organic matters, primary producers, consumers, etc. Carbon exchange between atmosphere & terrestrial plants: photosynthesis (outflow) respiration and decomposition (inflow) Removing trees removes a co2 sink and replaces it by a source (agricultural field, industrial plant, etc. ) If forests are burned, stored c is released as co2.

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