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Alkalinity water column profiles

Rapid increases in the interstitial water concentrations of dissolved strontium with increasing burial depth of deep-sea carbonate sediments have been interpreted as evidence of the recrystallization reaction (Baker et al., 1982 Elderfield et al., 1982 Gieskes, 1983). Figure 8.17 shows an example of interstitial-water profiles of dissolved alkaline-earth species from a carbonate nanno-fossil ooze from the Ontong Java Plateau (DSDP site 288 5°58 S, 161°50 E). At this site calcium and magnesium concentrations are linearly correlated, and their gradients are governed by chemical reactions deep in the sediment column. [Pg.402]

See other pages where Alkalinity water column profiles is mentioned: [Pg.315]    [Pg.325]    [Pg.293]    [Pg.4]    [Pg.209]    [Pg.328]    [Pg.48]    [Pg.394]    [Pg.145]    [Pg.35]    [Pg.318]    [Pg.234]    [Pg.297]   
See also in sourсe #XX -- [ Pg.317 ]



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