Understanding the lithology helps predict groundwater flow.

了解岩性有助于预测地下水的流动。

Scientists study karst regions to understand groundwater flow.

科学家们研究喀斯特地貌区域以了解地下水流动。

Scientists study the porosity of rocks to understand groundwater flow.

科学家研究岩石的孔隙率以了解地下水流动。

It couples the groundwater flow equation with the solute-transport equation.

它把地下水流动方程与溶质输运方程耦合在一起。

Laws of migration of the groundwater flow in the Anba ore block are defined.

借助计算机技术对矿区地下水等水头线进行了模拟,确定了区内地下水流的运移规律.

It couples the groundwater flow equation with the solute - transport equation.

它把地下水流动方程与溶质输运方程耦合在一起.

It can be used to forecast the groundwater flow, land subsidence and the workable reserves.

利用该模型计算了地下水可开采量及地下水流场和地面沉降的预报。

The determination of free surface of seepage is very important in the analysis of groundwater flow.

在地下水流分析中,渗流自由面位置的确定至关重要.

The relation between hydrocarbon and groundwater flow system with underpressure and normal hydrostatic pressure is discussed.

探讨了低压系统和常压系统的水文地质开启程度及其水流系统与油气的关系.

Dewatering becomes a major operation when the excavation lies below the natural water table and intercepts the groundwater flow.

当挖方位于天然地下水面以下时或有地下水流经时，排水就成为一个主要的工序。