Py. Tishchenko et al., The alkali reserve of interstitial water at the sites of methane emission in the Sea of Okhotsk, GEOCHEM INT, 39(6), 2001, pp. 597-603
The chemical composition (alkalinity, pH, NH4+, PO43-, Si, H2S, Cl-, Ca2+,
and SO42-) of interstitial water was studied in the sediments of the Sea of
Okhotsk at sites of methane emission. Variations in alkalinity were observ
ed in the sediments from a typical seawater value (2.3 mM/kg) to 63 mM/kg.
It is demonstrated that they are caused by the processes of sulfate reducti
on and methane generation. Based on the balance relationships, an equation
was constructed connecting changes in alkalinity with variations of Ca2+, S
O42- and NH4+ in interstitial solutions.