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Representation of water abstraction from a karst conduit with numerical discrete-continuum models

机译:用数值离散连续模型表示岩溶导管中的取水量

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Karst aquifers are characterized by highly conductive conduit flow paths embedded in a less conductive fissured and fractured matrix, resulting in strong permeability contrasts with structured heterogeneity and anisotropy. Groundwater storage occurs predominantly in the fissured matrix. Hence, most mathematical karst models assume quasi-steady-state flow in conduits neglecting conduit-associated drainable storage (CADS). The concept of CADS considers storage volumes, where karst water is not part of the active flow system but hydraulically connected to conduits (for example karstic voids and large fractures). The disregard of conduit storage can be inappropriate when direct water abstraction from karst conduits occurs, e.g., large-scale pumping. In such cases, CADS may be relevant. Furthermore, the typical fixed-head boundary condition at the karst outlet can be inadequate for water abstraction scenarios because unhampered water inflow is possible. brbr The objective of this work is to analyze the significance of CADS and flow-limited boundary conditions on the hydraulic behavior of karst aquifers in water abstraction scenarios. To this end, the numerical discrete-continuum model MODFLOW-2005 Conduit Flow Process Mode 1 (CFPM1) is enhanced to account for CADS. Additionally, a fixed-head limited-flow (FHLQ) boundary condition is added that limits inflow from constant head boundaries to a user-defined threshold. The effects and the proper functioning of these modifications are demonstrated by simplified model studies. Both enhancements, CADS and FHLQ boundary, are shown to be useful for water abstraction scenarios within karst aquifers. An idealized representation of a large-scale pumping test in a karst conduit is used to demonstrate that the enhanced CFPM1 is able to adequately represent water abstraction processes in both the conduits and the matrix of real karst systems, as illustrated by its application to the Cent Fonts karst system.
机译:岩溶含水层的特征是高传导性的导管流动路径埋在传导性较差的裂隙和破裂的基质中,从而形成强渗透性对比,并具有结构异质性和各向异性。地下水储存主要发生在裂隙基质中。因此,大多数数学岩溶模型都假定管道中的准稳态流忽略了与管道相关的可排水存储(CADS)。 CADS的概念考虑了存储量,其中岩溶水不是主动流系统的一部分,而是通过液压方式连接到导管(例如,岩溶空隙和大裂缝)。当从岩溶导管中直接取水时,例如大规模抽水,忽略导管存储可能是不合适的。在这种情况下,CADS可能是相关的。此外,在岩溶出口的典型固定水头边界条件可能不足以用于取水方案,因为可能会阻碍进水。 这项工作的目的是分析取水情况下的CADS和限流边界条件对岩溶含水层水力行为的重要性。为此,对离散离散连续体模型MODFLOW-2005导线管流动过程模式1(CFPM1)进行了增强,以解决CADS问题。此外,添加了固定头有限流量(FHLQ)边界条件,该条件限制了从恒定头边界向用户定义的阈值的流入。通过简化的模型研究证明了这些修饰的效果和适当的功能。两种改进(CADS和FHLQ边界)均显示对岩溶含水层内的取水方案很有用。岩溶管道中大型抽水试验的理想化表示用于证明增强型CFPM1能够充分代表管道和实际岩溶系统矩阵中的取水过程,如其在Cent中的应用所示字体岩溶系统。

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