|本期目录/Table of Contents|

[1]唐泽宇,赵瑞超,徐文杰,等.鄂西南地区岩溶槽谷地质构造对地下水动态的影响[J].地球科学与环境学报,2025,47(06):1114-1125.[doi:10.19814/j.jese.2025.03002]
　TANG Ze-yu,ZHAO Rui-chao,XU Wen-jie,et al.Impact of Geological Structure on Groundwater Dynamics in a Karstic Valley of the Southwestern Hubei, China[J].Journal of Earth Sciences and Environment,2025,47(06):1114-1125.[doi:10.19814/j.jese.2025.03002]
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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:
第47卷
期数:
2025年第06期
页码:
1114-1125
栏目:
水资源与水文地质
出版日期:
2025-12-10

文章信息/Info

Title:
Impact of Geological Structure on Groundwater Dynamics in a Karstic Valley of the Southwestern Hubei, China
文章编号:
1672-6561(2025)06-1114-12
作者:
唐泽宇1; 赵瑞超2; 徐文杰1; 陈乾龙3; 牛俊强4; 陈 伟1; 5; 6; 刘 伟1*
(1. 中国地质大学(武汉)自然资源调查研究院,湖北 武汉 430074; 2. 潍坊市水文中心,山东 潍坊 261061; 3. 中国电力工程顾问集团中南电力设计院有限公司,湖北 武汉 430071; 4. 湖北省地质局水文地质工程地质大队,湖北 荆州 434020; 5. 中国地质大学(武汉)环境学院,湖北 武汉 430078; 6. 山东省地质矿产勘查开发局第五地质大队,山东 泰安 271021)
Author(s):
TANG Ze-yu1;  ZHAO Rui-chao2;  XU Wen-jie1;  CHEN Qian-long3;  NIU Jun-qiang4;  CHEN Wei1; 5; 6;  LIU Wei1*
(1. Institute of Natural Resource Survey, China University of Geosciences, Wuhan 430074, Hubei, China; 2. Weifang Hydrology Center, Weifang 261061, Shandong, China; 3. Central Southern China Electric Power Design Institute Co., LTD. of China Power Engineering Consulting Group, Wuhan 430071, Hubei, China; 4. Hydrogeology and Engineering Geology Institute of Hubei Geological Bureau, Jingzhou 434020, Hubei, China; 5. School of Environmental Studies, China University of Geosciences, Wuhan 430078, Hubei, China; 6. No.5 Geological Brigade of Shandong Provincial Bureau of Geology and Mineral Resources, Tai'an 271021, Shandong, China)
关键词:
地下水;  地质构造;  水文时间序列分析;  流量衰减分析;  含水介质;  释水过程;  岩溶槽谷;  湖北
Keywords:
groundwater;  geological structure;  hydrological time series analysis;  flow recession analysis;  aquifer media;  discharge pattern;  karstic valley;  Hubei
分类号:
P641.7; P642.25
DOI:
10.19814/j.jese.2025.03002
文献标志码:
A
摘要:
鄂西南地区岩溶区地下水资源丰富,但高度发育的岩溶地质地貌导致地下水动态变化过程极为复杂。选取湖北省秭归县泗溪流域鱼泉洞和迷宫泉两处相邻地下水系统为研究对象,综合利用水文时间序列分析与流量衰减分析方法,分析了典型降雨事件中鱼泉洞和迷宫泉的流量动态特征,揭示了岩溶槽谷地貌及地下含水介质对其动态过程的影响规律。结果表明:①鱼泉洞—迷宫泉含水介质表现为较大裂隙与孔隙-较小裂隙共存的二元结构,均表现出显著的快速流与慢速流过程; 鱼泉洞峰值流量对强、弱降雨事件响应的滞后时间分别为4和9 h,迷宫泉峰值流量对强、弱降雨事件响应的滞后时间分别为3和6 h。②在岩溶槽谷地表地貌和地质结构共同作用下,强降雨事件中鱼泉洞和迷宫泉的流量衰减均存在坡面径流-落水洞释水、宽裂隙-管道释水、中宽裂隙释水、孔隙-微小裂隙释水等4个不同过程,其中槽谷地貌加强了地表产流过程; 弱降雨事件中鱼泉洞和迷宫泉的流量衰减仅有一个过程,均为中宽裂隙释水、孔隙-微小裂隙释水。③鱼泉洞、迷宫泉地质结构的差异性导致其水文动态过程存在不同。迷宫泉发育于较纯的厚层白云岩中,垂向裂隙相对发育,而鱼泉洞发育于中薄层泥质灰岩中,而且上下相邻地层均含有较多泥质成分,导致鱼泉洞上覆较厚土层,下伏岩层垂向裂隙发育较弱; 强降雨事件中,迷宫泉的快速流占比(52.4%)比鱼泉洞的快速流占比(7.8%)更高; 弱降雨事件中,鱼泉洞水流会在降雨入渗后的土-岩界面上形成临时饱水层并发生横向水流,再通过较大的垂向管道快速运输到地下水含水层,表现为鱼泉洞的快速流占比(33.6%)略高于迷宫泉的快速流占比(29.4%)。
Abstract:
The karst region in the southwestern Hubei is endowed with abundant groundwater resources; however, its highly developed karst geology leads to complex hydrological variations. Two adjacent groundwater systems Yuquandong and Migongquan, located in the Sixi river basin of Zigui county, Hubei province, were focused on; hydrological time series analysis and flow recession analysis were applied to examine the flow dynamics of these two systems during typical rainfall events, and the influence of karst geological structures on the flow dynamics was investigated. The results show that ① hydrological time series analysis reveals a dual-structure aquifer in both systems, consisting of large fractures as well as pore-small fissure networks; the peak flow response times at Yuquandong are 4 hours(during intense rainfall)and 9 hours(during weak rainfall), whereas at Migongquan, the response times are shorter, at 3 hours and 6 hours, respectively. ② Flow recession analysis identifies four stages during intense rainfall, including slope runoff-sinkhole discharge, large fissure-conduit discharge, medium fissure discharge, and micro-fissure-pore discharge; in contrast, only medium and micro-fissure discharges dominate during weak rainfall in both systems. ③ Differences in geological structures between the two systems lead to distinct hydrological behaviors; the Migongquan groundwater system lies within pure, thick dolomite with well-developed vertical fractures; in contrast, the Yuquandong system is developed in medium to thin argillaceous limestone, with adjacent strata rich in argillaceous material; a thicker soil layer overlies the Yuquandong system, and the underlying rock has relatively less developed vertical fractures. As a result, during intense rainfall, the Migongquan system exhibits a higher proportion of rapid flow(52.4%). During weak rainfall, infiltration in the Yuquandong system leads to the formation of a temporary saturated zone at the soil-rock interface, where lateral flow develops and is transmitted to the aquifer through larger vertical conduits. This results in a slightly higher proportion of rapid flow in Yuquandong under weak rainfall conditions(33.6%).

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备注/Memo

备注/Memo:
收稿日期:2025-03-01; 修回日期:2025-06-27投稿网址:http:∥jese.chd.edu.cn/
基金项目:国家重点研发计划项目(2021YFA0716902); 长安大学研究生科研创新实践项目(300103725010)
*通信作者:李庆春(1961-),男,山东郓城人,教授,博士研究生导师,工学博士,E-mail:dcliqc@chd.edu.cn。
更新日期/Last Update: 2025-12-10