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2017 Vol. 44, No. 5
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XIAO Qiong, ZHANG Zhicheng, XIE Lei, WU Kunyu, HE Jie, HAO Zhiqiang, JIN Yi. 2017. A study of hydrogeological characteristics of aquifers in the Changyuan River National Wetland Park[J]. Geology in China, 44(5): 1006-1016. doi: 10.12029/gc20170512
Citation: XIAO Qiong, ZHANG Zhicheng, XIE Lei, WU Kunyu, HE Jie, HAO Zhiqiang, JIN Yi. 2017. A study of hydrogeological characteristics of aquifers in the Changyuan River National Wetland Park[J]. Geology in China, 44(5): 1006-1016. doi: 10.12029/gc20170512
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A study of hydrogeological characteristics of aquifers in the Changyuan River National Wetland Park

  • 1.

    Key Laboratory of Karst Dynamics of MLR & Guangxi, Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, Guangxi, China

  • 2.

    School of Geoscience and Technology, Southwest Petroleum University, Chengdu 610500, Sichuan, China

  • 3.

    School of Foreign Languages, Southeast Petroleum University, Chengdu 610500, Sichuan China

  • 4.

    Administration of Changyuan River National Wetland Park(CNWP), Jinzhong 030999, Shanxi, China

  • 5.

    Sichuan Furong Group Co., Ltd., Yibin 644000, Sichuan China

    • Fund Project: Supported by National Key Research and Developmental Program of China (No.2016YFC0502306), Project of Chinese Academy of Geological Sciences (No.YYWF201639), Guangxi Science Foundation (No.2016GXNSFAA380064), French Development Agency "Construction Project of the Changyuan River National Wetland Park" (No.J131400345K03)
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  • Author Bio: XIAO Qiong, female, born in 1984, Ph.D, majors in hydrogeology, engages in the study of hydrogeology; E-mail:xiaoqiong-8423@163.com
Received Date:  12 May 2016
Revised Date:  09 August 2016
Publish Date:  25 October 2017
    Abstract

  • The data from 19 drill holes located in the hilly-plain region of the middle-lower reaches of the Changyuan River were systemically analyzed and, as a result, the predominant rock types of aquifers in the middle-lower reaches of the Changyuan River wetland were identified. Furthermore, based on the burial depth and development characteristics of aquifers and aquifuges, the authors divided the Quaternary aquifers in the study area into three aquifer sets, i.e., shallow, middle and deep aquifer sets. The features of spatial distribution of the aquifers in the study area were also summarized via correlation of cross sections and fence diagrams. In addition, the burial depths of groundwater tables were analyzed by using Kriging interpolation method. The results indicate that the predominant rock types of the aquifers are Quaternary sandy and gravel sediments. The profile of the shallow aquifer is like a wedged body in the downriver direction of the Changyuan River, but the thickness of the aquifer is not stable in the perpendicular direction of the river. This is in accordance with the sedimentary environment of the alluvial/fluvial fan. The results of interpolation analysis show that there are widely distributed precipitation funnels in the milled-lower reaches of the Changyuan River basin. Such a situation would impact the eco-hydrogeological process in the Changyuan River wetland park and the drainage basin. Finally, the authors discussed the recharge-discharge processes of the groundwater in the Changyuan River drainage basin and established a recharge-discharge model.

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