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GIS as a tool for modelling groundwater flow

机译:GIS作为建模地下水流动的工具

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摘要

Groundwater is important and precious freshwater found under the earth's surface. For effective groundwater management, quantitative and qualitative status of groundwater is usually assessed using various groundwater models (such as numerical and analytical model). However, these models usually suitable for major aquifers and application in minor aquifers are always lag behind due to the requirement of extensive and detailed groundwater data. Since all groundwater bodies are significantly important, GIS functionality was explored in this study to model groundwater using minimal and accessible input data. GIS was used to represent the subsurface geology particularly the aquifer system and to model groundwater flow. The model was used to estimate the groundwater discharge for the Lincolnshire Limestone aquifer in the Slea catchment, United Kingdom. Although there is discrepancy between estimated and measured spring discharge, the model has confirmed the usefulness of using GIS tool in modelling groundwater using minimal input data and basic modelling procedures.
机译:地下水是地球表面上的重要且珍贵的淡水。为了有效地下水管理,通常使用各种地下水模型(如数值和分析模型)进行评估地下水的定量和定性状态。然而,由于需要广泛和详细的地下水数据,这些模型通常适用于主要含水层和在轻微含水层中的应用始终滞后。由于所有地下水位都很重要,因此在本研究中探讨了GIS功能,以利用最小和可访问的输入数据模型地下水。 GIS用于表示地下地质,特别是含水层系统和地下水流量。该模型用于估计英国斯利亚集水区林肯郡石灰石含水层的地下水排放。尽管估计和测量的弹簧放电之间存在差异,但该模型已经确认使用GIS工具使用最小输入数据和基本建模程序在地下水中使用GIS工具的有用性。

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