The impacts of the silt layer, the leakage andthe storativity of the semi-permeable layer on the tide-induced groundwater headfluctuation in the confined aquifer were analyzed and demonstrated to be significant.
分析同时表明弱透水层的越流、贮水率及淤泥层的存在均对承压含水层中水头波动有显著影响。
参考来源 - 露头处被淤泥层覆盖的滨海承压层中水头波动的解析研究·2,447,543篇论文数据，部分数据来源于NoteExpress
The inter-porosity flow factor and the elastic storativity ratio determine the occurrence time and the degree of the inter-porosity flow.
窜流系数和裂缝弹性储容比的变化决定了窜流段发生的早晚和程度；
Effects of permeability modulus, interporosity flow parameter, storativity-ratio, outer-boundary and skin parameter to the pressure response are discussed.
讨论了溶洞和裂缝无因次渗透率模数、介质间窜流、弹性储容比、外边界条件及表皮系数对压力响应的影响。
The amplitude of the head fluctuation decreases with the storativity and leakage of both semi-permeable layers and increases with the leakance of the silt-layer.
分析表明，承压含水层中地下水水头波幅是上、下弱透水层贮水率和越流系数的减函数，是淤泥层相对透水系数的增函数；
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