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Fig. 2. Persistence of testosterone in three different soils. [14C]-Testosterone at an initial concentration of 1 mg/kg soil was mineralized to 14CO2 (top panel), total 14C residues in soil extracts were determined by liquid scintillation counting (LSC) (middle panel), and loss of androgenic activity in soil extracts was measured using a human androgen receptor recombinant yeast strain (bottom panel). Note the different time scale in the top panel.
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