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典型背斜槽谷区岩溶水资源空间分布格局与水质特征——以宜居河流域为例

张红波 杨森 甘鑫 罗富恒

中国岩溶2018,Vol.37Issue(1):27-36,10.
中国岩溶2018,Vol.37Issue(1):27-36,10.DOI:10.11932/karst2017y56

典型背斜槽谷区岩溶水资源空间分布格局与水质特征——以宜居河流域为例

Study of the spatial distribution pattern and water quality characteristics of karst water resources in a typical anticlinal trough valley:A case study of Yiju river basin

张红波 1杨森 1甘鑫 1罗富恒1

作者信息

  • 1. 重庆市地质矿产勘查开发局南江水文地质工程地质队/重庆市地下水资源利用与环境保护实验室,重庆401121
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摘要

Abstract

Karst springs are the mainly water sources of domestic water supply in karst mountainous areas,where anticlinal trough valley is an important part in the areas.To study the spatial distribution pattern and water quality characteristics in Chongqing karst anticline region,through the hydrogeology survey in the Yiju river basin,and combined with different hydrogeological units within the basin,of which is mainly composed of Permian and Triassic and Cambrian Ordovician aquifer,we analyzed the water quality and studied the distribution of the karst springs in different hydrogeological units.The results show that,(1) The pH value of karst spring in this basin is between 7.27 and 8.07,with the average value of 7.84 and most of them are neutral and weak alkaline.The total salinity of the samples falls in the range of 129-310 mg · L-1.The Permian and Triassic aquifer water chemistry type spring survey all belong to HCO3-Ca type water,while the Cambrian and Ordovician aquifer part spring belongs to HCO3 SO4-Ca type water,which may be related to lithology and human activities in the area;93.8% karst spring water is of excellent and good quality,which can be used as drinking water resources.(2) The average flow rate of these karst spring is 0.84 L · s-1 and 78% of them have a flow of less than 10 L · s-1.The average flow of large karst springs with more than 10 L · s-1 is 76.56 L · s-1.There are differences in quantity and flow of karst springs in different lithologic stratums,which shows the extreme nonuniformity of karst spring development.(3) In the basin with different hydrogeologic units,there are five preferential localities where the karst springs often occur,namely,the karst and non-karst contact zones,fault fractured zones,steep cliff,the low lying discharge areas with low confined,deep valleys and both sides of cutting canyons.

关键词

渝东南/背斜槽谷/岩溶泉/水化学/分布特征

Key words

southeast Chongqing/anticlinal trough valley/karst spring/water chemistry/distribution characteristics

分类

天文与地球科学

引用本文复制引用

张红波,杨森,甘鑫,罗富恒..典型背斜槽谷区岩溶水资源空间分布格局与水质特征——以宜居河流域为例[J].中国岩溶,2018,37(1):27-36,10.

基金项目

西南岩溶地区1∶5万水文地质环境地质调查(重庆:宜居幅、丁市幅)(12120114069001-06) (重庆:宜居幅、丁市幅)

中国岩溶

OA北大核心CSCDCSTPCD

1001-4810

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