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A seamlessly coupled GIS and distributed groundwater flow model

机译:无缝耦合的GIS和分布式地下水流模型

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摘要

There are three approaches for coupling groundwater models with GISs, i.e. loose, tight, and seamless. In seamless coupling a model code is written into, and run from within, a GIS. We implemented BGS GISGroundwater in a GIS in this way for the first time. It facilitates the construction and simulation of the model, and the visualisation of the results all within the GIS environment. The model consists of a 2D finite-difference groundwater flow model and a simple user-interface. It can represent heterogeneous aquifers, variably confined and unconfined conditions, and distributed groundwater recharge and abstraction. It offers benefits in terms of ease of use and in streamlining the model construction and application process. BGS GISGroundwater has been validated against analytical solutions to groundwater-head profiles for a range of aquifer configurations. This model lowers barriers to entry to groundwater flow modelling for a wider group of environmental scientists. (C) 2016 Natural Environment Research Council. Published by Elsevier Ltd. All rights reserved.
机译:有三种将地下水模型与GIS耦合的方法,即松散,紧密和无缝。在无缝耦合中,将模型代码写入GIS,并在GIS内部运行。我们首次以这种方式在GIS中实现了BGS GISGroundwater。它促进了模型的构建和仿真以及结果在GIS环境中的可视化。该模型由一个二维有限差分地下水流模型和一个简单的用户界面组成。它可以代表非均质含水层,不同程度的受限和非受限条件以及分布式的地下水补给和抽取。它在易用性以及简化模型构建和应用过程方面提供了好处。 BGS GIS地下水已针对各种含水层配置的地下水压剖面分析解决方案进行了验证。该模型为更广泛的环境科学家降低了进入地下水流模型的障碍。 (C)2016自然环境研究委员会。由Elsevier Ltd.出版。保留所有权利。

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