Carbon Dioxide and the Carbonate Compensation Depth (CCD)

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Carbon Dioxide and the Carbonate Compensation Depth (CCD) Railsback's Some Fundamentals of Mineralogy and Geochemistry Variation in concentration of solutes in the oceans IIIa: carbon dioxide and the carbonate compensation depth (CCD) 0 Concentration In the deeper reaches of the ocean, CaCO is more prone to dissolve for three reasons: 3 1 0 a) lower temperature (Ksp for both calcite and aragonite increases with decreasing T) 2 b) greater pressure (Ksp for both calcite and aragonite increases with increasing P) c) acidity resulting from the presence of CO2, as suggested by these reactions: 1 CO CO2 + H2O --> H2CO3 2 Carbonic acid (Chester 1990) Carbon dioxide 2+ - H2CO3 + CaCO3 --> Ca + 2HCO3 Carbonic acid Calcite Bicarbonate 2 Depth As discussed in Part III of this series, concentrations of CO2 in abyssal waters are greater (km) than those in surface waters because oxidation of sinking organic particles produces CO2. 3 3 Thus at depth in the ocean, temperature, the carbonate compensation depth (CCD), which pressure and acidity commonly combine to is thus named because it is the depth at which the make seawater undersaturated with respect to rate of dissolution of CaCO3 equals ("compen- 4 Pacific calcite. Calcite particles sinking past this depth sates for") the rate of CaCO3 sedimentation. Atlantic begin to dissolve in a lysocline (the depth zone Thus seafloor deeper than the CCD will be devoid of increasing dissolution rate) and eventually of carbonate sediments. The CCD is higher (less 5 reach a depth at which no carbonate sediment deep) in the Pacific because deep water in the will accumulate on the seafloor. This depth is Pacific has more CO2 and so is more acidic. Notes: 1 Morse & Mackenzie (1990) p. 23 etc. 2 Morse & Mackenzie (1990) p. 24. Carbonate ooze (abyssal carbonate sediments, consisting 3 More technically, one speaks of a "calcite compensation depth" and higher (lesser) largely of tests of foraminifera and coccolithophores) "aragonite compensation depth" (ACD). Northern & eastern CO2-poor deep waterAtlantic Pacific CO2-rich deep water Pacific N A W D B W A A CCD Greenland Mid-Atlantic Ridge AntarcticaSeamount East Pacific Rise Seamounts: "the snow-capped peaks of the abyssal Pacific" LBR OceanSolutes18 5/2008.
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