While infiltration water generated from filtration of meteoric water and surface water flows from basin edge to its center in gravity -induced centripetal flow.
渗入水由大气降水和地表水的渗入产生,受重力作用由盆地边缘向盆地中心呈向心流。
The results indicated that desalt depth increased exponentially with cumulative infiltration water volume, decreased with water salinity and initial water content.
结果表明,脱盐深度随入渗水量的增加呈幂函数增加,随入渗水矿化度和土壤初始含水量的增加而减小;
The results show that the infiltration water temperature has strong influence on infiltration into frozen soil, the infiltration capacity enhanced with the water temperature increasing.
试验结果表明,入渗水温对冻土入渗规律的影响十分明显,冻土的入渗能力随入渗水温的升高而增强。
The interaction of sedimentary water and infiltration water results in a pressure equilibrium zone, where hydrocarbons accumulate.