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Arid Land Geography >

2023 , Vol. 46 >Issue 10: 1612 - 1621

DOI: https://doi.org/10.12118/j.issn.1000-6060.2023.012

Climatology and Hydrology

Transformation relationship between surface water and groundwater in Kushui River Basin of Ningxia

  • Weibo JI ,
  • Yinxin ZHAO ,
  • Bowen HU ,
  • Lihu YANG ,
  • Liang GONG ,
  • Yuxue MA
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  • 1. Ningxia Fundamental Geological Survey Institute, Yinchuan 750021, Ningxia, China
    2. Key Laboratory of Water Cycle and Related Land Surface Processes, Institute of Geographic Sciences and Natural Resources Research, Chinese Academy of Sciences, Beijing 100101, China

Received date: 2023-01-05

  Revised date: 2023-04-03

  Online published: 2023-11-10

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Abstract

Brackish water is widely distributed in the arid and semiarid areas of northwest China. Understanding the relationship between surface water and groundwater transformation in brackish water areas is significant for promoting the rational development of brackish water resources. Taking the Kushui River Basin in Ningxia, China as the research object, this study analyzes the spatial and temporal distribution characteristics of hydrochemistry and hydrogen-oxygen stable isotopes of surface water and groundwater using hydrogen-oxygen stable isotope technology combined with field investigation, statistical analysis, and hydrochemical analysis. The spatial and temporal variations in the conversion relationship between surface water and groundwater in the basin were systematically revealed. The following results were observed: (1) SO4·Cl-Na·Mg is the main hydrochemical type of surface water and upstream and midstream groundwater in the Kushui River Basin. The hydrochemical formation of surface water was evaporation concentration, and the hydrochemical type of downstream groundwater was transformed into a mixed type, which was controlled by rock weathering. (2) Atmospheric precipitation has a significant recharge effect on surface water and groundwater in the wet season and has a limited recharge effect in the dry season. Climate, topography, and hydrogeological conditions controlled the upper and middle reaches of the river basin, and the relationship between surface water and groundwater showed significant differences and complexity in different river reaches and periods. The irrigation of the Yellow River obviously affected the downstream. (3) In the dry season, the areas with close hydraulic connection between surface water and groundwater are distributed in the middle and lower reaches. The water cycle mode was referred to as groundwater recharge surface water, with recharge ratios of 51.8% and 57.8%, respectively. In the wet season, the hydraulic connection between the surface water of the mainstream and the groundwater in the upper and middle reaches is weak. The downstream surface water supplied the groundwater, with a recharge ratio of 38.8%. At the same time, the downstream canal water supplied the surface water to a certain extent, with a recharge ratio of 29.8%.

Key words： brackish water; hydrogen-oxygen stable isotope; water chemistry; transforming relationship; Kushui River Basin

Cite this article

Weibo JI , Yinxin ZHAO , Bowen HU , Lihu YANG , Liang GONG , Yuxue MA . Transformation relationship between surface water and groundwater in Kushui River Basin of Ningxia[J]. Arid Land Geography, 2023 , 46(10) : 1612 -1621 . DOI: 10.12118/j.issn.1000-6060.2023.012

References

[1] 陈文, 郑自宽, 谢军健, 等. 我国非常规水源苦咸水资源及其分布特征研究[J]. 水文, 2021, 41(5): 1-6.
[1] [Chen Wen, Zheng Zikuan, Xie Junjian, et al. Study on the unconventional water sources: Bitter-salty water resources and its distribution characteristics in China[J]. Journal of China Hydrology, 2021, 41(5): 1-6. ]
[2] 吴琼, 梁伊, 高凡, 等. 新疆阿拉尔市苦咸水水化学特征、分布及成因分析[J]. 环境化学, 2021, 40(3): 737-745.
[2] [Wu Qiong, Liang Yi, Gao Fan, et al. Analysis of chemical characteristics, distribution and cause of formation of brackish water in Alar City, Xinjiang[J]. Environment Chemistry, 2021, 40(3): 737-745. ]
[3] 马涛, 刘九夫, 彭安帮, 等. 中国非常规水资源开发利用进展[J]. 水科学进展, 2020, 31(6): 969-978.
[3] [Ma Tao, Liu Jiufu, Peng Anbang, et al. Progress in development and utilization of non-conventional water resources in China[J]. Advances in Water Science, 2020, 31(6): 969-978. ]
[4] 俄有浩, 严平, 李文赞, 等. 中国内陆干旱、半干旱区苦咸水分布特征[J]. 中国沙漠, 2014, 34(2): 565-573.
[4] [E Youhao, Yan Ping, Li Wenzan, et al. Characteristics and distribution of brackish water in arid and semi-arid interior of China[J]. Journal of Desert Research, 2014, 34(2): 565-573. ]
[5] 朱金峰, 刘悦忆, 章树安, 等. 地表水与地下水相互作用研究进展[J]. 中国环境科学, 2017, 37(8): 3002-3010.
[5] [Zhu Jinfeng, Liu Yueyi, Zhang Shu’an, et al. Review on the research of surface water and groundwater interactions[J]. China Environment Science, 2017, 37(8): 3002-3010. ]
[6] Rozemeijer J, Klein J, Hendriks D, et al. Groundwater-surface water relations in regulated lowland catchments; hydrological and hydrochemical effects of a major change in surface water level management[J]. Science of the Total Environment, 2019, 660(10): 1317-1326.
[7] 胡兴林, 肖洪浪, 蓝永超, 等. 黑河中上游段河道渗漏量计算方法的试验研究[J]. 冰川冻土, 2012, 34(2): 460-468.
[7] [Hu Xinglin, Xiao Honglang, Lan Yongchao, et al. Experiment study of calculating method of river seepage in middle and upper reaches of the Heihe River[J]. Journal of Glaciology and Geocryology, 2012, 34(2): 460-468. ]
[8] 杨海娇, 魏加华, 任倩慧, 等. 柴达木盆地典型流域地表水-地下水转化关系及水化学特征[J]. 干旱区研究, 2022, 39(5): 1543-1554.
[8] [Yang Haijiao, Wei Jiahua, Ren Qianhui, et al. Interaction between surface water and ground water and hydrochemical characteristics in the typical watersheds of the Qaidam Basin[J]. Arid Zone Research, 2022, 39(5): 1543-1554. ]
[9] Kebede S, Travi Y, Alemayehu T, et al. Groundwater recharge, ciculation and geochemical evolution in the source region of the Blue Nile River, Ethiopia[J]. Applied Geochemistry, 2005, 20(9): 1658-1676.
[10] 张应华, 仵彦卿, 温小虎, 等. 环境同位素在水循环研究中的应用[J]. 水科学进展, 2006, 17(5): 738-747.
[10] [Zhang Yinghua, Wu Yanqing, Wen Xiaohu, et al. Application of environmental isotopes in water cycle[J]. Advances in Water Science, 2006, 17(5): 738-747. ]
[11] 段丽洪, 王圣杰, 张明军, 等. 阿尔泰山降水氢氧同位素及水汽来源分析[J]. 干旱区地理, 2022, 45(4): 1042-1049.
[11] [Duan Lihong, Wang Shengjie, Zhang Mingjun, et al. Stable hydrogen and oxygen isotopes in precipitation and water vapor source in the Altay Mountains[J]. Arid Land Geography, 2022, 45(4): 1042-1049. ]
[12] 赵明华. 黄土高原降水稳定同位素空间分布及水汽来源分析[D]. 西安: 西北农林科技大学, 2020.
[12] [Zhao Minghua. Spatial distribution of stable isotopes of precipitation and analysis of water vapor sources in the Loess Plateau[D]. Xi’an: Northwest A & F University, 2020. ]
[13] Zheng L L, Jiang C L, Chen X, et al. Combining hydrochemistry and hydrogen and oxygen stable isotopes to reveal the influence of human activities on surface water quality in Chaohu Lake Basin[J]. Journal of Environmental Management, 2022, 312: 114933, doi: 10.1016/j.jenvman.2022.114933.
[14] 祁晓凡, 李文鹏, 崔虎群, 等. 黑河流域中游盆地地表水与地下水转化机制研究[J]. 水文地质工程地质, 2022, 49(3): 29-43.
[14] [Qi Xiaofan, Li Wenpeng, Cui Huqun, et al. Study on the conversion mechanism of surface water and groundwater in the middle reaches of the Heihe River Basin[J]. Hydrogeology & Engineering Geology, 2022, 49(3): 29-43. ]
[15] 文广超, 王文科, 段磊, 等. 基于水化学和稳定同位素定量评价巴音河流域地表水与地下水转化关系[J]. 干旱区地理, 2018, 41(4): 734-743.
[15] [Wen Guangchao, Wang Wenke, Duan Lei, et al. Quantitatively evaluating exchanging relationship between river water and groundwater in Bayin River Basin of northwest China using hydrochemistry and stable isotope[J]. Arid Land Geography, 2018, 41(4): 734-743. ]
[16] 雷米, 周金龙, 张杰, 等. 新疆博尔塔拉河流域平原区地表水与地下水水化学特征及转化关系[J]. 环境科学, 2022, 43(4): 1873-1884.
[16] [Lei Mi, Zhou Jinlong, Zhang Jie, et al. Hydrochemical characteristics and transformation relationship of surface water and groundwater in the plain area of Bortala River Basin, Xinjiang[J]. Environmental Science, 2022, 43(4): 1873-1884. ]
[17] 张春辉. 基于SWAT模型的苦水河流域水文过程模拟[D]. 银川: 宁夏大学, 2018.
[17] [Zhang Chuihui. The hydrological process simulation of Kushui River Basin based on the SWAT model[D]. Yinchuan: Ningxia University, 2018. ]
[18] 李小妹, 严平, 郭金蕊, 等. 宁夏东南部清水河、苦水河流域苦咸水水质综合评价[J]. 干旱区资源与环境, 2014, 28(2): 136-142.
[18] [Li Xiaomei, Yan Ping, Guo Jinrui, et al. Comprehensive evaluation of the brackish water quality in the Qingshui River and Kushui River Basin, southeast Ningxia[J]. Journal of Arid Land Resources and Environment, 2014, 28(2): 136-142. ]
[19] 王旭虎, 徐先英, 柴成武, 等. 民勤绿洲苦咸水空间分布及成因分析[J]. 干旱区研究, 2014, 31(2): 193-200.
[19] [Wang Xuhu, Xu Xianying, Chai Chengwu, et al. Spatial distribution of brackish groundwater and its formation causes in the Minqin Oasis in lower reaches of the Shiyang River[J]. Arid Zone Research, 2014, 31(2): 193-200. ]
[20] 谷洪彪, 迟宝明, 王贺, 等. 柳江盆地地表水与地下水转化关系的氢氧稳定同位素和水化学证据[J]. 地球科学进展, 2017, 32(8): 789-799.
[20] [Gu Hongbiao, Chi Baoming, Wang He, et al. Relationship between surface water and groundwater in the Liujiang Basin: Hydrochemical constrains[J]. Advances in Earth Science, 2017, 32(8): 789-799. ]
[21] 沈贝贝, 吴敬禄, 吉力力·阿不都外力, 等. 巴尔喀什湖流域水化学和同位素空间分布及环境特征[J]. 环境科学, 2020, 41(1): 173-182.
[21] [Shen Beibei, Wu Jinglu, Abuduwail Jilili, et al. Hydrochemical and isotopic characteristics of the Lake Balkhash Catchment Kazakhstan[J]. Environmental Science, 2020, 41(1): 173-182. ]
[22] 范广群. 银川平原水体氢氧同位素及水化学特征研究[D]. 兰州: 兰州大学, 2018.
[22] [Fan Guangqun. The study of hydrogen and oxygen isotopic and hydrochemical characteristics of water in Yinchuan Plain[D]. Lanzhou: Lanzhou University, 2018. ]
[23] 顾显祖. 同位素水文学[M]. 北京: 科学出版社, 2011: 124-127.
[23] [Gu Xianzu. Isotope hydrology[M]. Beijing: Science Press, 2011: 124-127. ]
[24] Liu Z H, Tan H B, Brusseau M L. Significance of isotopic and geochemical methods to determine the evolution of inland brackish and bitter water: An example from the Zuli River in the upper reaches of the Yellow River, China[J]. Hydrological Processes, 2021, 35(1): e14020, doi: 10.1002/HYP.14024.
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