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，
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
减函数，是淤泥层相对透水系数增函数；
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，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减函数，是淤泥层相对透水系数增函数；
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