影响浅层含水层的河流地下水流量模型的标定过程

Andrea Kolencsik-Tóth, Balázs Kovács
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引用次数: 1

摘要

了解和模拟地下水和地表水的相互作用对水文学家来说是必不可少的。供水和水质方面是常见水资源问题的几个例子,了解地下水和地表水的相互联系对于制定有效的水资源管理和政策至关重要。在我们的研究中,对河岸含水层进行了详细的调查,以便能够模拟和预测流动系统的行为。研究区水头连续测量结果表明,在距离河流3500米的范围内,水头剧烈变化对水头场的影响较大。在此基础上,对稳态流场和瞬态流场的计算结果进行了比较,力求使模型能更准确地描述时空变化的流场。除满足标准校准要求外,还进行了多步校准过程。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Calibration process for groundwater flow model of a river influenced shallow aquifer
Understanding and simulating the interaction of groundwater and surface water is essential to hydrologists. Water supply and water quality aspects are a few examples of common water-resource issues where understanding the interconnections of groundwater and surface water is fundamental to develop an effective water-resource management and policy. In our study a detailed investigation of a riverbank aquifer was performed to be able to simulate and predict the behavior of the flow system. The continuous hydraulic head measurements in the area of interest showed strong influence on the hydraulic head field caused by intensively changing river head at a distance from the river up to 3,500 m. Based on the results steady state and transient flow calculations were compared, and a great effort has been made to ensure that the model more precisely describe the time and space variable flow field. Beside fulfilling the standard calibration requirements, a multi-step calibration process was performed.
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来源期刊
Central European Geology
Central European Geology Earth and Planetary Sciences-Geology
CiteScore
1.40
自引率
0.00%
发文量
8
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