潜山储层和上覆沉积层砂岩储层特性明显不同，因此其损害机理有较大差异。
Formation damage mechanism of buried-hill reservoir may differ seriously from the overlying sandstone reservoir because of the different reservoir characteristics.
在高有机磷、高铁结合态磷、高铝结合态磷的沉积物中，随着温度的升高，上覆水中和层间水中DRP浓度会随之增加。
The warming would be more favorable to enhance the concentrations of TP and DRP in overlying water and porewater for the sediments rich of Fe-P and Al-P.
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