The stratigraphic occurrence will also influence the release velocity of pore water directly.
岩层产状也将直接影响孔隙级水的衰减速度。
Thermal dispersion and solute dispersion, resulting from the discrepancies of pore water velocity, are important parameters in studying water, heat, and solute transport in porous media.
由土壤孔隙水流速率差异引起的热弥散和溶质弥散对于了解水热盐耦合运移非常重要。
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