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季节性地下水抽取和含水层人工补给条件下的河流-含水层相互作用建模

Modeling Stream-Aquifer Interactions Under Seasonal Groundwater Pumping and Managed Aquifer Recharge.

作者信息

Lee Hyeonju, Koo Min-Ho, Oh Sebong

机构信息

Department of Geoenvironmental Sciences, Kongju National University, Kongju, Republic of Korea.

Korea Rural Community Corporation, Naju, Republic of Korea.

出版信息

Ground Water. 2019 Mar;57(2):216-225. doi: 10.1111/gwat.12799. Epub 2018 Jul 5.

DOI:10.1111/gwat.12799
PMID:29896845
Abstract

In South Korea, a significant amount of groundwater is used for the heating of water-curtain insulated greenhouses during the winter dry season, which had led to problems of groundwater depletion. A managed aquifer recharge (MAR) project is currently underway with the goal of preventing such groundwater depletion in a typical cultivation area, located on an alluvial aquifer near the Nam River. In the present study, FEFLOW, a three-dimensional finite element model, was used to evaluate different strategies for MAR of the cultivation areas. A conceptual model was developed to simulate the stream-aquifer dynamics under the influence of seasonal groundwater pumping and MAR. The optimal rates and duration of MAR were assessed by analyzing the recovery of the groundwater levels and the change in the groundwater temperature. The simulation results indicate that a MAR rate of 8000 m /d effectively restores the groundwater level when the injection wells are located inside the groundwater depletion area. It is also demonstrated that starting the MAR before the beginning of the seasonal pumping is more effective. Riverbank filtration is preferable for securing the injection water owing to plentiful source of induced recharge from the river. Locating the pumping wells adjacent to the river where there are thick permeable layers could be a good strategy for minimizing decreases in the groundwater level and temperature.

摘要

在韩国,冬季旱季期间大量地下水被用于水幕隔热温室的供暖,这导致了地下水枯竭问题。目前正在进行一个有管理的含水层补给(MAR)项目,目标是防止位于南河附近冲积含水层上的典型种植区出现此类地下水枯竭情况。在本研究中,使用三维有限元模型FEFLOW来评估种植区MAR的不同策略。开发了一个概念模型来模拟季节性地下水抽水和MAR影响下的河流 - 含水层动态。通过分析地下水位的恢复情况和地下水温度的变化来评估MAR的最佳速率和持续时间。模拟结果表明,当注入井位于地下水枯竭区域内时,MAR速率为8000立方米/天可有效恢复地下水位。还表明在季节性抽水开始之前启动MAR更有效。由于河流诱导补给水源丰富,河岸过滤对于确保注入水更为可取。将抽水井设置在河流附近有厚渗透层的地方可能是使地下水位和温度下降最小化的一个好策略。

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