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用于模拟岩溶系统的半分布式管网模型和分布式有限差分模型的评估

An evaluation of semidistributed-pipe-network and distributed-finite-difference models to simulate karst systems.

作者信息

Gill L W, Schuler P, Duran L, Morrissey P, Johnston P M

机构信息

Department of Civil, Structural and Environmental Engineering, University of Dublin Trinity College, Dublin 2, Ireland.

出版信息

Hydrogeol J. 2021;29(1):259-279. doi: 10.1007/s10040-020-02241-8. Epub 2020 Nov 11.

DOI:10.1007/s10040-020-02241-8
PMID:33603565
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC7870641/
Abstract

Several different approaches have been developed to model the specific characteristics of karst aquifers, taking account of their inherent complex spatial and temporal heterogeneities. This paper sets out the development of a semidistributed modelling approach for applications in an Irish karst context using urban drainage software. The models have proven to be very useful for different studies, with examples given for the ecohydrology of ephemeral karst lakes, extreme groundwater-flood alleviation, karst network investigation, submarine groundwater discharge, and quantification of different recharge and flow components. The limitations of the approach are also highlighted, in particular not being able to simulate diffuse infiltration and flow paths explicitly across the groundwater catchment. Hence, a more distributed, finite-difference modelling approach using MODFLOW Unstructured Grid (USG) with the newly developed Connected Linear Network (CLN) process is then compared against the semidistributed approach on the same karst catchment. Whilst it has proven difficult to achieve the same levels of model performance in simulating the spring flows in the distributed model compared to the semidistributed model, the ability to interrogate the flow paths at any point on the three-dimensional aquifer is demonstrated, which can give new insights into flows (and potential contaminant transport) through such complex systems. The influence of the proximity of highly transmissive conduits on the flow dynamics through the much-lower transmissive matrix cells in which the network is embedded has been particularly investigated.

摘要

考虑到岩溶泉含水层固有的复杂空间和时间非均质性,已经开发了几种不同的方法来模拟其特定特征。本文阐述了一种使用城市排水软件在爱尔兰岩溶地区应用的半分布式建模方法的发展情况。这些模型已被证明对不同的研究非常有用,并给出了一些例子,如季节性岩溶湖的生态水文学、极端地下水洪水缓解、岩溶网络调查、海底地下水排放以及不同补给和水流成分的量化。该方法的局限性也得到了强调,特别是无法明确模拟整个地下水集水区的扩散入渗和水流路径。因此,将一种使用MODFLOW非结构化网格(USG)和新开发的连通线性网络(CLN)过程的更分布式有限差分建模方法与同一岩溶集水区的半分布式方法进行了比较。虽然事实证明,与半分布式模型相比,在分布式模型中模拟泉流量时难以达到相同的模型性能水平,但展示了在三维含水层的任何点查询水流路径的能力,这可以为通过这种复杂系统的水流(以及潜在的污染物传输)提供新的见解。特别研究了高导水率管道的 proximity 对通过网络所嵌入的低得多导水率基质单元的流动动力学的影响。 (注:“proximity”在句中可能有误,结合语境推测可能是“ximity”之类拼写错误,若原文无误,此处可灵活意译为“临近性”等)

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Introduction of wavelet analyses to rainfall/runoffs relationship for a karstic basin: the case of Licq-Atherey karstic system (France).将小波分析引入岩溶流域降雨/径流关系研究:以法国利克-阿泰雷岩溶系统为例
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