泸西喀斯特断陷盆地地表水与地下水流域边界与水动力性质

王波; 张华; 王宇; 张贵; 张文鋆; 高瑜; 罗为群

doi:10.11932/karst20200302

泸西喀斯特断陷盆地地表水与地下水流域边界与水动力性质

doi: 10.11932/karst20200302

王波¹,
张华¹,
王宇²,
张贵¹,
张文鋆¹,
高瑜¹,
罗为群³

1.
云南省地质环境监测院，昆明 650216
2.
云南省地质调查局，昆明 650051
3.
中国地质科学院岩溶地质研究所，广西桂林 541004

基金项目: 国家重点研发计划项目课题“断陷盆地地表、地下水资源高效利用与优化调控”（2016YFC0502502）；中国地质调查局项目“南方石漠化重点区综合地质调查与评价”（DD20190502）

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出版历程
- 发布日期: 2020-06-25

Watershed boundaries and hydrodynamic properties of surface water and groundwater in the Luxi karst fault-depression basin

1.
Yunnan Institute of Geological Environment Monitoring，Kunming ,Yunnan 650216，China
2.
Yunnan Institute of Geological Survey，Kunming, Yunnan 650051,China
3.
Institute of Karst Geology,CAGS,Guilin,Guangxi 541004,China

摘要

摘要: 在详细调查基础上，采用系统科学及水文地质分析方法，依据地形地貌、地层岩性、地质构造、示踪试验、地下水排泄基准面、喀斯特发育条件及发育规律等剖析论证流域边界，并通过钻探及示踪试验进行验证。研究结果：（1）对泸西喀斯特断陷盆地南东部的水系统边界向北移进行了修正，证实了三塘一带深部不发育的喀斯特是地下水分水岭边界，使得泸西喀斯特断陷盆地流域的径流系统和边界圈化更加准确；（2）泸西喀斯特断陷盆地流域地表水、地下水转化频繁，地表水径流特征主要以小江河在水库、河流、伏流间的径流转化过程为体现，地下水在侵溶山区接受大气降水补给后，上层径流以泉、暗河的形式在泸西盆地底面排泄后转化成地表水，最终汇集于盆地南部、通过工农隧洞及落水洞排向小江，而下层径流则以小江水面为基准，通过深层径流排泄。
- 喀特斯特断陷盆地 /
- 流域边界 /
- 地下水 /
- 地表水 /
- 水动力性质
Abstract: The Luxi karst fault-depression basin is located on the marginal slope of the southeast Yunnan plateau and is a tributary on the left bank of the Nanpan river system. It hosts two types of landforms, karst basins and karst river valleys. This basin also lies at the upstream in north, while the Xiaojiang karst river valley is at downstream in the south; both are connected by the underground flow system in the Maoshui cave to form a karst water system with complete recharge, runoff and discharge processes. The watershed boundary and hydrodynamic properties are the most important determinants of the watershed eco-geological environment and water flow characteristics. Accurate determination of the boundary and hydrodynamic properties of surface water and groundwater in the basins is a necessary prerequisite for runoff system simulation, water resource evaluation, searching and utilizing groundwater resources, development and protection planning of resources and environments, solution of environmental problems, and ecological restoration and protection. However, in previous work, the boundary of the groundwater basin divided by the hydrogeological environmental geological survey and evaluation is mainly along the boundary of the surface watershed, aquifer and aquiclude (band, body), most of which are not accurate enough. The hydrodynamic property of the boundary was mainly the result of hydrogeological analysis and inference. In this work, through detailed hydrogeological investigation and analysis, we initially delineated the boundary between surface water and groundwater basins in the Luxi karst fault-depression basin, and then revealed and controlled the hidden and inaccurate sections through drilling, tracer tests, and geophysical surveys, thus making the boundaries of watersheds and water systems revised more accurate. At the same time, we clarified the hydrodynamic properties of watershed boundaries, and obtained basic hydrogeological parameters, so as to provide a basis for model construction and solution conditions to the surface water and groundwater runoff systems in the basin.
- karst fault-depression basin, basin boundary, groundwater, surface water /
- hydrodynamic property /

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参考文献(17)

[1]	张人权，梁杏，靳孟贵，等．水文地质学基础（第六版）［M］.北京：地质出版社,2011:86-95.
[2]	袁道先，蔡桂鸿．岩溶环境学［M］.重庆：重庆出版社,1988:112-126.
[3]	王宇．岩溶区地表水与地下水资源及环境统一评价的流域边界划分研究［J］.中国岩溶，2019，38(4)：398-403.
[4]	王宇，张贵，张华，等.喀斯特断陷盆地环境地质分区及功能［J］.中国岩溶,2017，36（3）：283-295.
[5]	水利部珠江水利委员会珠江水利综合技术中心.云南省泸西县水资源综合规划［R］.2015.
[6]	云南省地质调查院.云南泸西小江流域岩溶地下水调查与地质环境整治示范报告［R］.桂林：中国地质科学院岩溶地质研究所，2006.
[7]	云南省地质矿产局滇南工程勘察公司.泸西县白水塘水库渗漏处理可行性研究勘察［R］.1992.
[8]	云南省地质局.1∶20万弥勒幅区域水文地质普查报告［R］.1979.
[9]	王宇.西南岩溶石山区断陷盆地岩溶水系统分类及供水意义［J］.中国岩溶，2003，22（6）：220-224.
[10]	王宇.西南岩溶地区岩溶水系统分类特征及勘查评价要点［J］.中国岩溶，2002，21(2)：114-119.
[11]	裴建国，梁茂珍，陈阵.西南岩溶石山地区岩溶地下水系统划分及其主要特征值统计［J］.中国岩溶，2008，27(1)：7-10.
[12]	莫美仙，王宇，李峰，等.云南南洞地下河系统边界及性质研究［J］.中国岩溶，2018，37(4):398-403.
[13]	康晓波，王宇，张华，等．丽江黑龙潭群泉水文地质特征及断流的影响因素分析［J］.中国岩溶,2013,32(4)：398-403.
[14]	王宇，李燕，谭继中，等．断陷盆地岩溶水赋存规律［M］.昆明：云南科技出版社,2003:32-37.
[15]	张华，王宇，张贵．云南重点岩溶流域水文地质及环境地质调查成果评析［J］.云南地质，2014，33(2):259-263.
[16]	王宇.云南泸西小江流域岩溶水有效开发模式研究［D］.昆明：昆明理工大学，2006：31-70.
[17]	王宇．岩溶高原地下水径流系统垂向分带［J］.中国岩溶，2018，37（1）：1-8.