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- W2013757984 abstract "The dissolution kinetics of Antarctic diatom ooze was investigated in seawater at various pH's and temperatures. The slow dissolution rate of the ooze was mostly due to the presence of inhibitors postfixed on the surface layer of silica skeletons, which partly were removed by the acid treatment; inhibitors reformed gradually around the surface of acid-cleaned skeletons. The dissolution process was quite different from that of silica skeletons prepared from living diatoms, and could be described by parabolic kinetics; the concentration of dissolved silica from the diatom ooze is proportional to square root of time. The parabolic rate constant, K, had a good relationship with pH and with temperature; the constant estimated by temperature and pH in deep waters of the Antarctic area was calculated to be (1.1 ∼ 2.3) × 10−11mol cm−2 h−12." @default.
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- W2013757984 date "1988-07-01" @default.
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- W2013757984 title "The dissolution kinetics of diatom ooze from the Antarctic area" @default.
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- W2013757984 doi "https://doi.org/10.1016/0198-0149(88)90010-6" @default.
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