BIOA02H3 Lecture Notes - Biogeochemical Cycle, Smog, Convection Zone

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BIOA02H3 Full Course Notes
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BIOA02H3 Full Course Notes
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Unlike energy, which is lost as it travels up the trophic levels; chemical compounds remain unchanged and can be reused, in processes which are often cyclic. The movement of energy and materials on earth is between 4 compartments: oceans, fresh waters, At one point or another, most materials that cycle through the four compartments end up in oceans. Despite their massive size, oceans only exchange materials with the atmosphere on the surface therefore they respond very slowly from input of other departments. In most of the oceans, there is very slow mixture. Most material sink to the bottom and stay there for millions of years, however sometimes the material is brought back up to surface water, causing upwelling zones which support high rates of photosynthesis. In lakes, minerals and nutrients are taken up by organisms which they incorporate into their cells. Once these organisms die, they take with them the nutrients and minerals.

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