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模拟地下水与湖泊的相互作用:方法与见解。

Simulating ground water-lake interactions: approaches and insights.

作者信息

Hunt Randall J, Haitjema Henk M, Krohelski James T, Feinstein Daniel T

机构信息

U.S. Geological Survey, 8505 Research Way, Middleton, WI 53562, USA.

出版信息

Ground Water. 2003 Mar-Apr;41(2):227-37. doi: 10.1111/j.1745-6584.2003.tb02586.x.

Abstract

Approaches for modeling lake-ground water interactions have evolved significantly from early simulations that used fixed lake stages specified as constant head to sophisticated LAK packages for MODFLOW. Although model input can be complex, the LAK package capabilities and output are superior to methods that rely on a fixed lake stage and compare well to other simple methods where lake stage can be calculated. Regardless of the approach, guidelines presented here for model grid size, location of three-dimensional flow, and extent of vertical capture can facilitate the construction of appropriately detailed models that simulate important lake-ground water interactions without adding unnecessary complexity. In addition to MODFLOW approaches, lake simulation has been formulated in terms of analytic elements. The analytic element lake package had acceptable agreement with a published LAKI problem, even though there were differences in the total lake conductance and number of layers used in the two models. The grid size used in the original LAKI problem, however, violated a grid size guideline presented in this paper. Grid sensitivity analyses demonstrated that an appreciable discrepancy in the distribution of stream and lake flux was related to the large grid size used in the original LAKI problem. This artifact is expected regardless of MODFLOW LAK package used. When the grid size was reduced, a finite-difference formulation approached the analytic element results. These insights and guidelines can help ensure that the proper lake simulation tool is being selected and applied.

摘要

用于模拟湖泊与地下水相互作用的方法已从早期使用指定为恒定水头的固定湖泊水位的模拟显著发展到用于MODFLOW的复杂LAK软件包。尽管模型输入可能很复杂,但LAK软件包的功能和输出优于依赖固定湖泊水位的方法,并且与可以计算湖泊水位的其他简单方法相比效果良好。无论采用何种方法,此处给出的关于模型网格大小、三维水流位置和垂直捕获范围的指导原则都有助于构建适当详细的模型,该模型能够模拟重要的湖泊与地下水相互作用,而不会增加不必要的复杂性。除了MODFLOW方法外,湖泊模拟还可以根据解析单元来制定。解析单元湖泊软件包与已发表的LAKI问题具有可接受的一致性,尽管两个模型中使用的总湖泊传导率和层数存在差异。然而,原始LAKI问题中使用的网格大小违反了本文提出的网格大小指导原则。网格敏感性分析表明,溪流和湖泊通量分布的明显差异与原始LAKI问题中使用的大网格大小有关。无论使用何种MODFLOW LAK软件包,预计都会出现这种假象。当网格大小减小时,有限差分公式接近解析单元结果。这些见解和指导原则有助于确保选择并应用合适的湖泊模拟工具。

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