Article(id=1222925286874796742, tenantId=1146029695717560320, journalId=1205116964453384197, issueId=1222925278838513745, articleNumber=null, orderNo=null, doi=10.20040/j.cnki.1000-7709.2023.20220909, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1649001600000, receivedDateStr=2022-04-04, revisedDate=1652716800000, revisedDateStr=2022-05-17, acceptedDate=null, acceptedDateStr=null, onlineDate=1769497709243, onlineDateStr=2026-01-27, pubDate=1677254400000, pubDateStr=2023-02-25, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1769497709243, onlineIssueDateStr=2026-01-27, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1769497709243, creator=13701087609, updateTime=1769497709243, updator=13701087609, issue=Issue{id=1222925278838513745, tenantId=1146029695717560320, journalId=1205116964453384197, year='2023', volume='41', issue='2', pageStart='1', pageEnd='220', issueExtLink='null', onlineDate='null', pubDate='null', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=null, createTime=1769497707328, creator=13701087609, updateTime=1769497707328, updator=13701087609, preIssue=null, nextIssue=null, ext=null, issueFiles=null}, startPage=15, endPage=18, ext={EN=ArticleExt(id=1222925289248772955, articleId=1222925286874796742, tenantId=1146029695717560320, journalId=1205116964453384197, language=EN, title=Numerical Simulation of Dynamic Change of Groundwater Level in Linfen Basin, columnId=1222925279849341011, journalTitle=Water Resources and Power, columnName=HYDROLOGY, WATER RESOURCES AND ENVIRONMENT, runingTitle=null, highlight=null, articleAbstract=

Based on the GMS software, a numerical model of groundwater flow in the Linfen Basin was established to predict the groundwater level under different driving factor scenarios, and the impact of different driving factors on groundwater level changes was quantified. The results show that only in the precipitation scenarios (dry, normal, and wet), the variation of shallow groundwater is greater than that of confined groundwater. When the precipitation is from 458.8 mm to 568.0 mm, the absolute value of the difference in the annual average water level change rate of the shallow groundwater is 0.11 m; Only under the pressure extraction scenario (extraction volume in 2018 as the benchmark), both shallow groundwater and confined groundwater have great changes. When the pressure extraction increases from 0% to 50%, the absolute value of the annual average water level change rate difference between shallow groundwater and middle-deep confined water is 0.16 m and 0.25 m, respectively; Under the situation of the rising water level of the Fenhe River, only the shallow groundwater on both sides of the river will be affected to a certain extent. The research results can provide a certain scientific basis for the rational utilization of groundwater in the Linfen Basin.

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采用GMS软件构建临汾盆地地下水数值模型，预测了不同驱动因素情景下地下水位的变化规律，并量化不同驱动因素对地下水位变化的影响程度，发现仅降水情景（枯、平、丰）时，浅层地下水位变幅大于承压地下水水位，降水量由458.8 mm至568.0 mm时，浅层地下水年平均水位变化速率差绝对值为0.11 m；仅压采情景（以2018年开采量为基准）下，浅层地下水位与承压地下水位有较大变化，压采由0%升至50%时，浅层地下水和中深层承压水年平均水位变化速率差绝对值分别为0.16、0.25 m；在汾河水位抬升情境下，仅对河流两侧的浅层地下水产生一定影响。研究结果可为临汾盆地地下水的合理利用提供参考依据。

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段旭东（1996-），男，硕士研究生，研究方向为地下水数值模拟，E-mail：820397359@qq.com

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段旭东（1996-），男，硕士研究生，研究方向为地下水数值模拟，E-mail：820397359@qq.com

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