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.
析表明，承压含
层中地下头波幅是上、下弱透层贮率和越流系数
减函数，是淤泥层相对透系数增函数；
系数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.
析表明，承压含层中地下头波幅是上、下弱透层贮率和越流系数减函数，是淤泥层相对透系数增函数；
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