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FEFLOW modeling of groundwater-surface water system of Maozui area of Jianghan Plain, Central China

机译:中部江汉平原茅嘴地区地下水-地表水系统的FEFLOW模型

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摘要

The objective of this study is to get a better understanding of local groundwater system mechanism at a characteristic spot of the Jianghan plain, in the vicinity of Maozui, and eventually to give a perspective in order to understand the regional hydrogeological system of Jianghan Plain. Conceptual and analytical models were developed before modelling using FEFLOW. Steady state represents an equilibrium state of the system or in other words, the average situation of the system. Such situation is very useful to calibrate the model. Models were elaborated and improved with information notably about the aquifer physical configuration and altitude of piezometric levels.
机译:这项研究的目的是为了更好地了解毛嘴附近的江汉平原特征点的局部地下水系统机理,并最终为理解江汉平原的区域水文地质系统提供一个视角。在使用FEFLOW进行建模之前,先开发了概念模型和分析模型。稳态代表系统的平衡状态,换句话说,代表系统的平均状态。这种情况对于校准模型非常有用。利用特别是有关含水层物理构造和测压高度的信息对模型进行了完善和完善。

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