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《利用地下水潮汐效应估算含水层参数及预测水位变化》一文存在不足之处,主要表现在地下水与海潮关系模型的适用性有问题,在海潮传播系数中利用孔隙度反算渗透系数方法不合理,渗透系数的估算结果不符合其研究区的水文地质条件等。
There are some shortcomings in the article “Estimating aquifer parameters by using groundwater tide effect and predicting water level change”, which is mainly manifested in the problem of applicability of the relation model between groundwater and ocean tide. It is unreasonable to use the porosity inversion permeability coefficient in tide propagation coefficient, The estimated permeability coefficient does not meet the hydrogeological conditions of the study area.