Effects of pH, temperature, and oxygen on the production and release of phosphine in eutrophic lake sediments were investigated
under laboratory tests. Results indicated that the elimination of matrix-bound phosphine was accelerated under initial pH
1 or 12. Phosphine levels could reach maximum under initial pH 10. The contents of phosphine increased with the addition of
alkali under pH 4–12. The rates of phosphine production and release from lake sediments varied with temperature. 20°C was
the most favorable temperature for the production of matrix-bound phosphine. Oxygen showed little effect on matrix-bound phosphine.
Matrix-bound phosphine concentrations in lake sediments were concluded to be dependent on a balance of natural generation
and depletion processes.
Translated from Acta Scientise Circumstantiae, 2005, 25(5): 681–685 [译自: 环境科学学报] 相似文献
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