In order to study the migration characters of organophosphorus in clay, experiment was designed to simulate the process of organophosphor leakage permeating the aquitard, searching the migration characters of organophosphorus in clay with different pH. It is shown that the ability of migration of organophosphor leakage permeating the cohesive soil fall with increase of pH between7.5 and 9.5, and the extent of mineralization for organophosphor in clay rise with increase of pH.
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