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Article(id=1314917920031990698, tenantId=1146029695717560320, journalId=1234093305789726721, issueId=1314917704910340427, articleNumber=null, orderNo=null, doi=null, pmid=null, cstr=null, oa=null, hot=null, price=null, onlineType=0, articleFormat=0, articleType=null, articleTypeStr=null, receivedDate=1735747200000, receivedDateStr=2025-01-02, revisedDate=null, revisedDateStr=null, acceptedDate=null, acceptedDateStr=null, onlineDate=1791430462128, onlineDateStr=2026-10-08, pubDate=1755619200000, pubDateStr=2025-08-20, doiRegisterDate=null, doiRegisterDateStr=null, onlineIssueDate=1791430462128, onlineIssueDateStr=2026-10-08, onlineJustAcceptDate=null, onlineJustAcceptDateStr=null, onlineFirstDate=null, onlineFirstDateStr=null, sourceXml=null, magXml=null, createTime=1791430462128, creator=13701087609, updateTime=1791430462128, updator=13701087609, issue=Issue{id=1314917704910340427, tenantId=1146029695717560320, journalId=1234093305789726721, year='2025', volume='45', issue='8', pageStart='4145', pageEnd='4736', issueExtLink='null', onlineDate='null', pubDate='1755619200000', pubDateStr='2025-08-20', beforeIssueId=null, nextIssueId=null, price=null, status=1, issueComplete=1, articleOrder=1, issueType=-1, specialIssue=null, createTime=1791430410840, creator='13701087609', updateTime=1791431909627, updator='13701087609', preIssue=null, nextIssue=null, articleTotal=null, ext={EN=IssueExt(id=1314923991341555972, tenantId=1146029695717560320, journalId=1234093305789726721, issueId=1314917704910340427, language=EN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=), CN=IssueExt(id=1314923991345750277, tenantId=1146029695717560320, journalId=1234093305789726721, issueId=1314917704910340427, language=CN, specialIssueTitle=, coverIllustrator=null, specialIssueEditor=, specialIssueAbout=)}, issueFiles=null, downloadFileDto=null}, startPage=4538, endPage=4550, ext={EN=ArticleExt(id=1314917920308814763, articleId=1314917920031990698, tenantId=1146029695717560320, journalId=1234093305789726721, language=EN, title=Hydrogeochemical characteristics and hydraulic connection identification of aquifer in the northern mining area of Zhungeer Coalfield, columnId=1234106388083954308, journalTitle=China Environmental Science, columnName=Environmental Ecology, runingTitle=null, highlight=null, articleAbstract=

To explore the hydrochemical characteristics and hydraulic connections of different aquifers in the northern mining area of the Zhungeer Coalfield, and to reveal the regional water circulation patterns under coal mining activities, a total of 39water samples were collected from different aquifers in the mining area. The hydrochemical characteristics, controlling factors, and hydraulic connection degrees were analyzed using methods such as Piper trilinear diagrams, Gibbs diagrams, ion ratio analysis, chloride-alkalinity index, factor analysis, and connectivity index. The results show that the water in the mining area is generally weakly alkaline. The main hydrochemical type of the Quaternary and Shiqianfeng Formation aquifers is HCO--Ca type water, which is mainly influenced by silicate weathering and mining activities, with positive cation exchange occurring. The main hydrochemical type of the Zhidan Group aquifer is HCO3-Ca type water, followed by HCO3-Na and Cl-Ca types. Its sources are mainly influenced by the weathering dissolution of silicate rock minerals and the impacts of mining and agricultural activities, with positive cation exchange occurring. The main hydrochemical type of mine water is Cl-Ca type water, which is influenced by the weathering dissolution of silicate and evaporite minerals and mining activities, with reverse cation exchange occurring. The hydraulic connectivity indices between the Quaternary aquifer and the Zhidan Formation, and between the Zhidan Formation aquifer and the Shiqianfeng Formation are 27% and 20%, respectively, indicating the presence of hydraulic connections. The hydraulic connectivity index between the Shiqianfeng Formation aquifer and the mine water is 39%, indicating a weak hydraulic connection.

, authors=Yan-na LI1, 2, Lei HUANG1, 2, *, Jun-li GAN3, Xuan HAN1, 2, Jiang XU1, 2, Meng-fan YANG1, 2, Guang-yan ZHU1, 2, authorsList=Yan-na LI, Lei HUANG, Jun-li GAN, Xuan HAN, Jiang XU, Meng-fan YANG, Guang-yan ZHU, authorCompany=null, correspAuthors=Lei HUANG, authorNote=null, correspAuthorsNote=null, copyrightStatement=null, copyrightOwner=null, extLink=null, articleAbsUrl=null, sourceXml=null, magXml=null, pdfUrl=null, pdf=null, pdfFileSize=null, pdfExtLink=null, richHtmlUrl=null, mobilePdfUrl=null, reviewReport=null, pdfFirstPage=null, abstractGraph=null, abstractGraphContent=null, abstractVideo=null, citation=null, cebUrl=null, magXmlContent=null, mapNumber=null, fund=null), CN=ArticleExt(id=1314917920606610348, articleId=1314917920031990698, tenantId=1146029695717560320, journalId=1234093305789726721, language=CN, title=准格尔煤田北部矿区含水层水文地球化学特征及水力联系辨识, columnId=1234106388268503686, journalTitle=中国环境科学, columnName=环境生态, runingTitle=null, highlight=null, articleAbstract=

为探究准格尔煤田北部矿区不同含水层的水化学特征及水力联系，揭示采煤活动下区域水循环规律，采集了矿区不同含水层的水样品共39组，利用Piper三线图、Gibbs图、离子比例分析、氯碱指数、因子分析以及连通性指数等方法分析了水化学特征、控制因素以及水力联系程度．结果表明，矿区的水体整体呈现弱碱性；第四系、石千峰组含水层主要水化学类型是HCO3-Ca型水，主要受硅酸盐风化和矿业活动影响，存在正向的阳离子交换作用；志丹群含水层主要水化学类型是HCO3-Ca型水，其次是HCO3-Na、Cl-Ca型，其来源主要受硅酸盐岩矿物的风化溶解以及矿业和农业生活作用的影响，存在正向的阳离子交换作用；矿井水主要水化学类型是Cl-Ca型水，受硅酸盐和蒸发岩矿物的风化溶解以及矿业活动影响，存在反向阳离子交换作用．第四系含水层与志丹群、志丹群含水层与石千峰组的水力连通性指数为27%和20%，存在水力联系；石千峰组含水层与矿井水的水力连通性指数为39%，存在微弱的水力联系．

, authors=李艳娜1, 2, 黄磊1, 2, *, 甘俊礼3, 韩萱1, 2, 许江1, 2, 杨梦凡1, 2, 朱廣岩1, 2, authorsList=李艳娜, 黄磊, 甘俊礼, 韩萱, 许江, 杨梦凡, 朱廣岩, authorCompany=null, correspAuthors=黄磊, authorNote=

李艳娜（1999-），女，山西运城人，硕士研究生，主要研究方向为水文学与水资源．发表论文1篇．.

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* 责任作者，副教授，
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李艳娜（1999-），女，山西运城人，硕士研究生，主要研究方向为水文学与水资源．发表论文1篇．.

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李艳娜（1999-），女，山西运城人，硕士研究生，主要研究方向为水文学与水资源．发表论文1篇．.

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准格尔煤田北部矿区含水层水文地球化学特征及水力联系辨识
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李艳娜 1, 2 , 黄磊 1, 2, * , 甘俊礼 3 , 韩萱 1, 2 , 许江 1, 2 , 杨梦凡 1, 2 , 朱廣岩 1, 2
中国环境科学 | 环境生态 2025,45(8): 4538-4550
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中国环境科学 |环境生态 2025 , 45 (8) : 4538 -4550
准格尔煤田北部矿区含水层水文地球化学特征及水力联系辨识
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李艳娜1, 2 , 黄磊1, 2, * , 甘俊礼3, 韩萱1, 2, 许江1, 2, 杨梦凡1, 2, 朱廣岩1, 2
作者信息
  • 1.内蒙古农业大学，旱区水工程生态环境全国重点实验室，黄河流域内蒙段水资源与水环境综合治理自治区协同创新中心，内蒙古 呼和浩特 010018
  • 2.内蒙古农业大学水利与土木建筑工程学院，内蒙古自治区生态水文与水资源高效利用重点实验室，内蒙古 呼和浩特 010018
  • 3.准格尔旗水利事业发展中心，内蒙古 鄂尔多斯 010321
通讯作者:
* 责任作者，副教授，
作者简介:

李艳娜（1999-），女，山西运城人，硕士研究生，主要研究方向为水文学与水资源．发表论文1篇．.

Hydrogeochemical characteristics and hydraulic connection identification of aquifer in the northern mining area of Zhungeer Coalfield
Yan-na LI1, 2 , Lei HUANG1, 2, * , Jun-li GAN3, Xuan HAN1, 2, Jiang XU1, 2, Meng-fan YANG1, 2, Guang-yan ZHU1, 2
Affiliations
  • 1.State Key Laboratory of Water Engineering Ecology and Environment in Arid Area, Inner Mongolia Agricultural University, Autonomous Region Collaborative Innovation Center for Integrated Management of Water Resources and Water Environment in the Inner Mongolia Reaches of the Yellow River, Hohhot 010018, China
  • 2.Water Conservancy and Civil Engineering College, Inner Mongolia Agricultural University, Inner Mongolia Key Laboratory of Ecohydrology and High Efficient Utilization of Water Resources, Hohhot 010018, China
  • 3.Zhungeer Banner Water Conservancy Development Center, Ordos 010321, China
出版时间: 2025-08-20
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为探究准格尔煤田北部矿区不同含水层的水化学特征及水力联系，揭示采煤活动下区域水循环规律，采集了矿区不同含水层的水样品共39组，利用Piper三线图、Gibbs图、离子比例分析、氯碱指数、因子分析以及连通性指数等方法分析了水化学特征、控制因素以及水力联系程度．结果表明，矿区的水体整体呈现弱碱性；第四系、石千峰组含水层主要水化学类型是HCO3-Ca型水，主要受硅酸盐风化和矿业活动影响，存在正向的阳离子交换作用；志丹群含水层主要水化学类型是HCO3-Ca型水，其次是HCO3-Na、Cl-Ca型，其来源主要受硅酸盐岩矿物的风化溶解以及矿业和农业生活作用的影响，存在正向的阳离子交换作用；矿井水主要水化学类型是Cl-Ca型水，受硅酸盐和蒸发岩矿物的风化溶解以及矿业活动影响，存在反向阳离子交换作用．第四系含水层与志丹群、志丹群含水层与石千峰组的水力连通性指数为27%和20%，存在水力联系；石千峰组含水层与矿井水的水力连通性指数为39%，存在微弱的水力联系．

含水层  /  水化学特征  /  水岩作用  /  氢氧稳定同位素  /  水力联系

To explore the hydrochemical characteristics and hydraulic connections of different aquifers in the northern mining area of the Zhungeer Coalfield, and to reveal the regional water circulation patterns under coal mining activities, a total of 39water samples were collected from different aquifers in the mining area. The hydrochemical characteristics, controlling factors, and hydraulic connection degrees were analyzed using methods such as Piper trilinear diagrams, Gibbs diagrams, ion ratio analysis, chloride-alkalinity index, factor analysis, and connectivity index. The results show that the water in the mining area is generally weakly alkaline. The main hydrochemical type of the Quaternary and Shiqianfeng Formation aquifers is HCO--Ca type water, which is mainly influenced by silicate weathering and mining activities, with positive cation exchange occurring. The main hydrochemical type of the Zhidan Group aquifer is HCO3-Ca type water, followed by HCO3-Na and Cl-Ca types. Its sources are mainly influenced by the weathering dissolution of silicate rock minerals and the impacts of mining and agricultural activities, with positive cation exchange occurring. The main hydrochemical type of mine water is Cl-Ca type water, which is influenced by the weathering dissolution of silicate and evaporite minerals and mining activities, with reverse cation exchange occurring. The hydraulic connectivity indices between the Quaternary aquifer and the Zhidan Formation, and between the Zhidan Formation aquifer and the Shiqianfeng Formation are 27% and 20%, respectively, indicating the presence of hydraulic connections. The hydraulic connectivity index between the Shiqianfeng Formation aquifer and the mine water is 39%, indicating a weak hydraulic connection.

aquifer  /  hydrochemical characteristics  /  hydroaction  /  hydrogen and oxygen stable isotopes  /  hydraulic connection
李艳娜, 黄磊, 甘俊礼, 韩萱, 许江, 杨梦凡, 朱廣岩. 准格尔煤田北部矿区含水层水文地球化学特征及水力联系辨识. 中国环境科学, 2025 , 45 (8) : 4538 -4550 .
Yan-na LI, Lei HUANG, Jun-li GAN, Xuan HAN, Jiang XU, Meng-fan YANG, Guang-yan ZHU. Hydrogeochemical characteristics and hydraulic connection identification of aquifer in the northern mining area of Zhungeer Coalfield[J]. China Environmental Science, 2025 , 45 (8) : 4538 -4550 .
基金
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  • 国家重点研发计划项目(2023YFC3709900)
  • 国家自然科学基金资助项目(52369003)
  • 准格尔旗科技计划项目(2023YY-18; 2023YY-19; 2024YF-11)
  • 内蒙古自治区自然科学基金资助项目(2023LHMS04011)
  • 内蒙古自治区教育厅一流学科科研专项(YLXKZX-NND-010)
  • 内蒙古自治区科技领军人才团队项目(2022LJRC0007)
  • 内蒙古农业大学基本科研业务费专项资金资助项目(BR22-12-04)
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2025年第45卷第8期
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  • 接收时间：2025-01-02
  • 首发时间：2026-10-08
  • 出版时间：2025-08-20
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  • 收稿日期：2025-01-02
基金
国家重点研发计划项目(2023YFC3709900)
国家自然科学基金资助项目(52369003)
准格尔旗科技计划项目(2023YY-18; 2023YY-19; 2024YF-11)
内蒙古自治区自然科学基金资助项目(2023LHMS04011)
内蒙古自治区教育厅一流学科科研专项(YLXKZX-NND-010)
内蒙古自治区科技领军人才团队项目(2022LJRC0007)
内蒙古农业大学基本科研业务费专项资金资助项目(BR22-12-04)
作者信息
    1.内蒙古农业大学，旱区水工程生态环境全国重点实验室，黄河流域内蒙段水资源与水环境综合治理自治区协同创新中心，内蒙古 呼和浩特 010018
    2.内蒙古农业大学水利与土木建筑工程学院，内蒙古自治区生态水文与水资源高效利用重点实验室，内蒙古 呼和浩特 010018
    3.准格尔旗水利事业发展中心，内蒙古 鄂尔多斯 010321

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鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
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红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
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