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Development of a spreadsheet-based model for transient groundwater modelling

机译:基于电子地下水建模的电子表格的开发

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Understanding and modelling the passage of groundwater is important for a wide range of environmental and earth science disciplines. The science of groundwater modelling is mature, and advanced modelling algorithms are routinely implemented, for example via the widely used MODFLOW software. However, for the non-specialist scientist or student, the fundamentals of such software can be difficult to comprehend, whilst the algorithms are arguably too complex to be easily applied for many applications which require integration of a groundwater model with climate, surface-water, soil or ecological data. In this context, a spreadsheet-based groundwater model (A2016), capable of solving transient groundwater behaviour in multiple spatial dimensions, was developed. Inter-comparison tests investigating nine transient groundwater scenarios were performed between MODFLOW, A2016 and the Time-dependent Groundwater Modeling using Spreadsheet Simulation (TGMSS) model. Results demonstrated that A2016 is directly comparable to MODFLOW, with identical hydraulic heads in all model experiments. TGMSS was not able to accurately simulate hydraulic heads for any of the model experiments. A groundwater-lake interaction scenario was identified for which MODFLOW will produce unrealistic results, due to the way conductance beneath lakes is determined. Applying a specified saturated thickness approximation for the region beneath the lake resulted in improved lake-groundwater interactions. A2016 is potentially useful for educational purposes and as a tool for groundwater experiments by non-specialists, as it is modular in nature and incorporates MODFLOW terminology and techniques.
机译:理解和建模地下水的通过对广泛的环境和地球科学学科很重要。地下水建模科学是成熟的,并且通过广泛使用的Modflow软件常规实现高级建模算法。然而,对于非专业科学家或学生来说,这种软件的基本原理可能难以理解,而算法可谓太复杂,以便很容易地应用于许多需要与气候,地面水集成的地下水模型集成的应用程序,土壤或生态数据。在这种情况下,开发了一种基于电子表的地下水模型(A2016),其能够在多个空间尺寸下解决瞬态地下水行为。使用电子表格仿真(TGMSS)模型在Modflow,A2016和时间依赖地下水建模中执行调查九个瞬态地下水场景的比较测试。结果表明,A2016与Modflow直接相当,在所有模型实验中具有相同的液压头。 TGMSS无法准确模拟用于任何模型实验的液压头。由于确定了湖泊下方的电导的方式,确定了地下水 - 湖互动场景,该模型将产生不切实际的结果。施加湖下方区域的指定饱和厚度近似导致湖泊地下水相互作用改善。 A2016可能对教育目的有用,作为非专家的地下水实验工具,因为它是模块化的,并包含Modflow术语和技术。

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