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LUO Jie, WANG Wenke, DUAN Lei, et al. Dynamic Analysis of Groundwater Level in Yinchuan Plain[J]. Northwestern Geology, 2020, 53(1): 195-204. DOI: 10.19751/j.cnki.61-1149/p.2020.01.018
Citation: LUO Jie, WANG Wenke, DUAN Lei, et al. Dynamic Analysis of Groundwater Level in Yinchuan Plain[J]. Northwestern Geology, 2020, 53(1): 195-204. DOI: 10.19751/j.cnki.61-1149/p.2020.01.018

Dynamic Analysis of Groundwater Level in Yinchuan Plain

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  • Received Date: March 09, 2019
  • Revised Date: October 18, 2019
  • Available Online: July 28, 2022
  • Published Date: March 04, 2020
  • Based on the groundwater monitoring data from 2013 to 2015, SPSS cluster analysis and land-use-type were used to analyze the variation rules and influencing factors of the dynamic change of water level in Yinchuan plain on the time scale and space scale. It is found that the groundwater dynamics in Yinchuan plain are divided into four types:runoff type, irrigation type, rainfall-evaporation type and mining type. The dynamic types of human-influence (irrigation type and mining type) are widely distributed among them, accounting for about 1/2 of the total area of Yinchuan plain. In terms of time scale, the change trend of the four dynamic types is obviously different because of different influence factors. From the perspective of the dynamic trend of the whole year, the runoff-type shows M-type change. The irrigation-type shows W type change. Rainfall evaporation type shows Λ type change. The mining type shows Z type change. Through simulation, the optimal annual mining volume is 45%~50% in summer and 15%~20% in winter. On the spatial scale, due to the influence of topographic factors, the groundwater dynamic type changed from west to east as runoff type, mining type and irrigation type. On this basis, a reasonable way of exploiting groundwater resources in Yinchuan plain is discussed, which provides a scientific proof for sustainable exploitation and utilization of groundwater resources.
  • 李琦.渭河流域地下水对气候变化的响应研究[D].西安:长安大学,2015.
    LI Qi. Mechanism ofgroundwater respone to climate change in Weihe River basin[D].Xi'an:Chang'an University, 2015.
    赵建忠,魏莉莉,赵玉苹,等.黑河流域地下水与地表水转化研究进展[J].西北地质,2010,43(03):120-126.
    ZHAO Jianzhong, WEI Lili, ZHAO Yuping, et al. Surface Water and Groundwater Transformation Research in Heihe River Basin[J]. Northwestern Geology, 2010,43(03):120-126.
    马雄德,范立民,严戈,等.植被对矿区地下水位变化响应研究[J].煤炭学报,2017,42(01):44-49.
    MA Xiongde, FAN Limin, YAN Ge, et al. Vegetation responses to groundwater level change in mining Area[J]. Journal of China Coal Society, 2017,42(01):44-49.
    古力米热·哈那提,王光焰.干旱区间歇性生态输水对地下水位与植被的影响机理研究[J].干旱区地理,2018,41(04):726-733.
    HANATI Gulimire, WANG Guangyan. Influence Mechanism of intermittent ecological water conveyance on groundwater level and vegetation in arid land[J]. Arid Land Geography, 2018,41(04):726-733.
    杨胜科,王文科,李翔,等.水溶性污染物在土壤中转化的原位实验方法[J].西北地质,2002,35(02):20-23.
    YANG Shengke, WANG Wenke, LI Xiang, et al. A site experimental method to study the transfer and transform of water-soluble contamination in soil[J]. Northwestern Geology, 2002,35(02):20-23.
    王仕琴,宋献方,王勤学,等.华北平原浅层地下水水位动态变化[J].地理学报, 2008, 63(5):462-472.
    WANG Shiqin, SONG Xianfang, WANG Qinxue, et al. Dynamic Features of Shallow Groundwater in North China Plain[J]. Acta Geographica Sinica,2008, 63(5):462-472.
    黄金廷,侯光才,尹立河,等.干旱半干旱区天然植被的地下水水文生态响应研究[J].干旱区地理, 2011, 34(5):788-793.
    HUANG Jinting, HOU Guangcai, YIN Lihe, et al. Eco-hydrological response of natural vegetation in arid and semi-arid area:A review[J]. Arid Area Geography, 2011, 34(5):788-793.
    杨泽元,王文科.干旱半干旱区地下水引起的生态效应的研究现状与发展趋势[J].干旱区地理, 2009, 32(5):739-745.
    YANG Zeyuan, WANG Wenke. Research Status and Development Trend of Ecological Effects Caused by Groundwater in Arid and Semi-arid Areas[J]. Arid Land Geography, 2009, 32(5):739-745.
    胡海华,丁宏伟,贺兵英.石羊河流域中下游近40a地下水位动态特征分析[J].西北地质,2016,49(03):164-174.
    HU Haihua, DING Hongwei, HE Bingying. Dynamic Variation of Groundwater Level in the Middlelower Reaches of Shiyanghe River Basin for Nearly 40 Years[J]. Northwestern Geology, 2016,49(03):164-174.
    于艳青,张作辰.宁夏河套平原地下水资源开发潜力分析[J].水文地质工程地质,2002,(02):56-58.
    YU Yanqing, ZHANG Zuochen. Analysis on groundwater resources exploitation potentiality in Hetao plain of Ning xia[J]. Hydrogeology & Engineering Geology, 2002,(02):56-58.
    王文科,韩锦萍,赵彦琦,等.银川平原水资源优化配置研究[J].资源科学,2004,(02):36-45.
    WANG Wenke, HAN Jinping, ZHAO Yanqi, et al. Optimal Allocation of Water Resources in Yinchuan Plain[J]. Resource Science, 2004,(02):36-45.
    王尧,张茂省,杨建锋.中国地质环境脆弱性评价[J].西北地质,2019,52(02):198-206.
    WANG Yao, ZHANG Maosheng, YANG Jianfeng. Evaluation Research on the Fragility of Geological Environment in China[J]. Northwestern Geology, 2019,52(02):198-206.
    王改平,吴学华,杨建,等.银川平原与地下水相关的生态环境及演变[J].宁夏工程技术,2006,(03):226-229.
    WANG Gaiping, WU Xuehua, YANG Jian, et al.The ecological environment and evolution of groundwater in Yinchuan plain[J]. Ningxia Engineering Technology, 2006,(03):226-229.
    魏建成.银川平原地下水位动态影响因素及变化类型分析[J].宁夏工程技术,2013,12(03):209-211.
    WEI Jiancheng. The groundwater level dynamic effect factors and changing types of Yinchuan plain[J]. Ningxia Engineering Technology, 2013,12(03):209-211.
    王枫.银川平原地下水动态特征及地下水年龄分布特征研究[D].北京:中国地质大学(北京),2017.
    WANG Feng, Study onDynamic Characteristics of Groundwater and Age Distribution of Groundwater in Yinchuan Plain[D]. Beijing:China University of Geosciences, 2017.
    董佩,王旭升.MODFLOW模拟自由面渗流的应用与讨论[J].工程勘察,2009,37(07):27-30.
    DONG Pei, WANG Xusheng. Application and discussion of MODFLOW's simulation to the seepage of free surface[J]. Geotechnical Investigation & Surveying, 2009,37(07):27-30.
    冯丽媛,段汉明.银川平原人口空间分布研究[J].西北人口,2012,33(05):90-94.
    FENG Liyuan, DUAN Hanming.Spatial Distribution of Population in Yinchuan Plain[J]. Northwest Population Journal, 2012,33(05):90-94.
    魏礼宁,张学文,陈玉春,等.2014宁夏水资源公报[R].银川:宁夏回族自治区水利厅,2015.
    徐映雪,邵景力,崔亚莉,等.银川平原地下水流模拟与地下水资源评价[J].水文地质工程地质,2015,42(03):7-12.
    XU Yingxue, SHAO Jingli, CUI Yali, et al. Application of groundwater modeling systems to the evaluation of groundwater resources in the Yinchuan Plain[J]. Hydrogeology & Engineering Geology, 2015,42(03):7-12.
    GONGJinnan, WANG Kaiyun, Seppo Kellomäki,Modeling, et al. Modeling water table changes in boreal peatlands of Finland under changing climate conditions[J]. Ecological Modelling,2012,244.
    JARKKOOkkonen,BJØRN Kløve. A conceptual and statistical approach for the analysis of climate impact on ground water table fluctuation patterns in cold conditions[J]. Journal of Hydrology,2010,388.
    PHILIPPE Marcotte,VINCENT Roy,ANDRÉP. Plamondon,Isabelle Auger. Ten-year water table recovery after clearcutting and draining boreal forested wetlands of eastern Canada[J]. Hydrological Processes,2008,22.
    MARINI L, NASCIMBENE J, SCOTTON M, et al. Hydrochemistry, water table depth and related distribution Patterns of vascular plants in a mixed mire[J]. Plant Biosystems An International Journal Dealing with all Aspects of Plant Biology, 2008, 142(1):79-86.
    BHULLAR Gurbir S,IRAVANI Majid,EDWARDS Peter J. Olde Venterink Harry. Methane transport and emissions from soil as affected by water table and vascular plants.[J]. BMC Ecology,2013,13.
    P. BONNAUD, Ph. SANTENOISE, D. Tisserand, et al. Impact of compaction on two sensitive forest soils in Lorraine (France) assessed by the changes occurring in the perched water table[J]. Forest Ecology and Management,2019,437.
    SRDAN Kostić,MILAN Stojković,IVA Guranov,Nebojša Vasović. Revealing the background of groundwater level dynamics:contributing factors, complex modeling and engineering applications[J]. Chaos, Solitons and Fractals:the interdisciplinary journal of Nonlinear Science, and Nonequi-librium and Complex Phenomena,2019,127.
    LUMINDA Niroshana Gunawardhana,SO Kazama. Statistical and numerical analyses of the influence of climate variability on aquifer water levels and groundwater temperatures:The impacts of climate change on aquifer thermal regimes[J]. Global and Planetary Change,2012,86-87.
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