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

IF 2.4 3区 地球科学 Q2 GEOSCIENCES, MULTIDISCIPLINARY
Hydrogeology Journal Pub Date : 2021-01-01 Epub Date: 2020-11-11 DOI:10.1007/s10040-020-02241-8
L W Gill, P Schuler, L Duran, P Morrissey, P M Johnston
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引用次数: 14

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.

半分布管网和分布有限差分模型在岩溶系统模拟中的评价。
考虑到喀斯特含水层固有的复杂时空异质性,已经开发了几种不同的方法来模拟喀斯特含水层的具体特征。本文阐述了利用城市排水软件在爱尔兰喀斯特环境中应用的半分布式建模方法的发展。这些模型已被证明对不同的研究非常有用,例如喀斯特湖泊生态水文、极端地下水洪水缓解、喀斯特网络调查、海底地下水排放以及不同补给和流量分量的量化。该方法的局限性也被强调,特别是不能模拟扩散渗透和穿越地下水集水区的流动路径。因此,使用MODFLOW非结构化网格(USG)和新开发的连接线性网络(CLN)过程的更分布式有限差分建模方法,然后与同一喀斯特流域的半分布式方法进行比较。虽然与半分布式模型相比,分布式模型在模拟泉水流动时很难达到相同水平的模型性能,但研究人员证明了在三维含水层上任意点询问流动路径的能力,这可以为通过这种复杂系统的流动(以及潜在的污染物输送)提供新的见解。高透射率管道的邻近性对通过低透射率矩阵单元的流动动力学的影响已经被特别研究。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Hydrogeology Journal
Hydrogeology Journal 地学-地球科学综合
CiteScore
5.40
自引率
7.10%
发文量
128
审稿时长
6 months
期刊介绍: Hydrogeology Journal was founded in 1992 to foster understanding of hydrogeology; to describe worldwide progress in hydrogeology; and to provide an accessible forum for scientists, researchers, engineers, and practitioners in developing and industrialized countries. Since then, the journal has earned a large worldwide readership. Its peer-reviewed research articles integrate subsurface hydrology and geology with supporting disciplines: geochemistry, geophysics, geomorphology, geobiology, surface-water hydrology, tectonics, numerical modeling, economics, and sociology.
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