不同土壤有机矿质复合体中活性磷和中等活性磷的分布，与有机磷化合物中的核酸磷和肌醇磷的含量有关。
The results show that the distribution of labile and moderately labile pool in organo-mineral complexes of different soils is related to the contents of nucleic acid-P and inositol-P.
菲在有机-矿质复合体上的解吸表现出明显的滞后现象。
Apparent hysteresis existed in phenanthrene desorption from organo-mineral aggregates.
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