北京西郊浅层地下水回灌的水质预测
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  • 英文篇名:Water quality prediction of shallow groundwater recharge in the western suburbs of Beijing
  • 作者:李倩雯 ; 邢国章 ; 孙红福 ; 杨萌 ; 褚闪闪 ; 张玉虎 ; 乔丽
  • 英文作者:LI Qianwen;XING Guozhang;SUN Hongfu;YANG Meng;CHU Shanshan;ZHANG Yuhu;QIAO Li;School of Earth Sciences and Surveying Engineering,China University of Mining and Technology (Beijing);Beijing Institute of Geological & Prospecting Engineering;
  • 关键词:回灌试验 ; PHREEQC ; 水质 ; 预测 ; 混合模拟
  • 英文关键词:recharge test;;PHREEQC;;water quality;;prediction;;hybrid simulation
  • 中文刊名:NSBD
  • 英文刊名:South-to-North Water Transfers and Water Science & Technology
  • 机构:中国矿业大学(北京)地球科学与测绘工程学院;北京市地质工程勘察院;
  • 出版日期:2019-04-15 16:08
  • 出版单位:南水北调与水利科技
  • 年:2019
  • 期:v.17;No.102
  • 基金:国家水体污染控制与治理科技重大专项“北京受水区饮用水安全保障技术研究与工程示范项目”~~
  • 语种:中文;
  • 页:NSBD201903013
  • 页数:11
  • CN:03
  • ISSN:13-1334/TV
  • 分类号:109-118+158
摘要
地下水回灌不仅能够弥补地下水资源的亏空,而且能够稀释净化受污染的地下水。根据北京水源四厂的回灌试验数据,利用PHREEQC模拟软件进行了水质混合模拟和水质预测研究。回灌试验对南井水质影响较大,北井和东井的水质基本没有变化;南井的水质由Ⅲ类水质提升为Ⅱ类水质,其氯化物、硫酸盐、硝酸盐和碳酸氢盐浓度在回灌结束时与回灌井的浓度非常接近;而钾、钙和镁的最终浓度略微低于回灌井中相应指标的浓度,可能是由于阳离子交换作用导致。混合模拟水质与其回灌实测水质数据具有很好的相关性,由此获得南井的模拟混合比与回灌时间的线性方程,其R2高达0.999。据此预测北井在相同的回灌条件下需要回灌11d,其水质才能由最初Ⅳ类水质提升为Ⅱ类水质。本研究的水质预测方法能够有效提高地下水回灌的效率,对于地下水的精准回灌具有重要的指导意义。
        Groundwater recharge can not only cover the deficit of groundwater resources,but also dilute and purify contaminated groundwater.The recharge experiments at Beijing Water Source No.4 Plant and the PHREEQC simulation software were used in this study for water quality mixing simulations and water quality prediction.The results showed that the recharge has a great impact on the water quality of South Well,but limited impacts on that of North Well and East Well.The water quality of South Well was upgraded from ClassⅢto ClassⅡ.The chloride,sulfate,nitrate and bicarbonate were recharged and their the concentration.at the end were very close to those of the recharge wells.The final concentrations of potassium,calcium and magnesium were slightly lower than those of the recharge wells,probably due to cation exchanges.The simulated water quality of mixed water had a good correlation with the observations,and a linear equation of the simulation mixing ratio and recharge time of South Well were obtained.Its coefficient of determination(R2)was as high as 0.999.It predicted that the groundwater in Beijing needed 11 days to be recharged under the same conditions for the water quality being upgraded from the ClassⅣto ClassⅡ.The water quality prediction method of this study can effectively improve the efficiency of groundwater recharge and has useful guideline for groundwater recharge prediction.
引文
[1]方生,陈秀玲.地下水开发引起的环境问题与治理[J].地下水,2001,23(1):8-11.(FANG S,CHEN X L.Environmental problems and treatment caused by groundwater development[J].Groundwater,2001,23(1):8-11.(in Chinese))DOI:10.3969/j.issn.1004-1184.2001.01.004.
    [2]李会安,窦艳兵.南水北调水进京后北京市地下水利用与保护[J].水利规划与设计,2006(5):19-21.(LI HA,DOU Y B.Groundwater utilization and protection in Beijing after Water Diversion from Beijing to South China[J].Water Resources Planning and Design,2006(5):19-21.(in Chinese))DOI:10.3969/j.issn.1672-2469.2006.05.006.
    [3]潘莉,李玉仙,王体明,等.南水北调来水对北京市供水的影响[J].南水北调与水利科技,2016(A01):205-208.(PAN L,LI Y X,WANG T M,et al.Impact of South-to-North Water Transfer on water supply in Beijing[J].South-to-North Water Transfer and Water Science and Technology,2016(A01):205-208.(in Chinese))
    [4]郑凡东,刘立才,杨牧骑,等.南水北调水源北京西郊回灌的水岩相互作用模拟[J].水文地质工程地质,2012,39(6):22-28.(ZHENG F D,LIU L C,YANG M Q,et al.Simulation of water-rock interaction in the western suburbs of the South-to-North Water Transfer Project in Beijing[J].Hydrogeology and Engineering Geology,2012,39(6):22-28.(in Chinese))DOI:10.16030/j.cnki.issn.1000-3665.2012.06.005.
    [5]刘立才,郑凡东,张春义.南水北调水源与北京地下水混合的水质变化特征[J].水文地质工程地质,2012,39(1):1-7.(LIU L C,ZHENG F D,ZHANG C Y.Variation characteristics of water quality mixed with water source from South-to-North Water Transfer Project and Beijing groundwater[J].Hydrogeology and Engineering Geology,2012,39(1):1-7.(in Chinese))DOI:10.16030/j.cnki.issn.1000-3665.2012.01.025.
    [6]林学钰,张文静,何海洋,等.人工回灌对地下水水质影响的室内模拟实验[J].吉林大学学报(地球科学版),2012,42(5):1404-1409.(LIN X Y,ZHANG W J,HEH Y,et al.Indoor simulation experiments on the influence of artificial recharge on groundwater quality[J].Journal of Jilin University(Earth Science Edition),2012,42(5):1404-1409.(in Chinese))DOI:10.13278/j.cnki.jjuese.2012.05.026.
    [7]杜新强,齐素文,廖资生,等.人工补给对含水层水质的影响[J].吉林大学学报(地球科学版),2007,37(2):293-297.(DU X Q,QI S W,LIAO Z S,et al.Effects of artificial recharge on aquifer water quality[J].Journal of Jilin University(Earth Science Edition),2007,37(2):293-297.(in Chinese))DOI:10.3969/j.issn.1671-5888.2007.02.017.
    [8]杜新强,冶雪艳,路莹,等.地下水人工回灌堵塞问题研究进展[J].地球科学进展,2009,24(9):973-980.(DUX Q,YE X Y,LU Y,et al.Research progress on artificial recharge blockage of groundwater[J].Advances in Earth Science,2009,24(9):973-980.(in Chinese))DOI:10.3321/j.issn:1001-8166.2009.09.003.
    [9]黄修东,束龙仓,刘佩贵,等,注水井回灌过程中堵塞问题的试验研究[J].水利学报,2009,40(4):430-434.(HUANG X D,SHU L C,LIU P G,et al.Experimental study on clogging problems in recharged water injection wells[J].Journal of Hydraulic Engineering,2009,40(4):430-434.(in Chinese))DOI:10.13243/j.cnki.slxb.2009.04.015.
    [10]束龙仓,张永杰,许杨,等.地下水人工回灌气相堵塞特征的试验研究[J].水科学进展,2017,28(5):756-762(SHU L C,ZHANG Y J,XU Y,et al.Experimental study on gas clogging characteristics of groundwater artificial recharge[J].Advances in Water Science,2017,28(5):756-762.(in Chinese))DOI:10.14042/j.cnki.32.1309.2017.05.013.
    [11]张永杰,束龙仓,温忠辉,等,人工回灌对地下水年龄分布规律的影响[J].水文地质工程地质,2018,45(1):8-14,44(ZHANG Y J,SHU L C,WEN Z H,et al.Effects of artificial recharge on the age distribution of groundwater[J].Hydrogeology and Engineering Geology,2018,45(1):8-14,44.(in Chinese))DOI:10.16030/j.cnki.Issn.1000-3665.2018.01.02.
    [12]刘东,张健,付强.三江平原井灌区地下水人工回灌量测算[J].水土保持研究,2012,19(2):240-243.(LIUD,ZHANG J,FU Q.Calculation of groundwater artificial recharge in well irrigation area of Sanjiang Plain[J].Soil and Water Conservation Research,2012,19(2):240-243.(in Chinese))
    [13]周建军,虎维岳,张壮路.废弃矿井地下水回灌模拟分析研究[J].西安科技大学学报,2008,28(3):434-438.(ZHOU J J,HU W Y,ZHANG Z L.Simulation analysis of groundwater recharge in abandoned mines[J].Journal of Xi′an University of Science and Technology,2008,28(3):434-438.(in Chinese))DOI:10.3969/j.issn.1672-9315.2008.03.008.
    [14]刘青勇,潘世兵,武晓峰,等.地下水回灌补源防治咸水入侵技术研究---以山东省广绕县为例[J].自然灾害学报,2006,15(3):100-104.(LIU Q Y,PAN SB,WU X F,et al.Study on the prevention and control of saltwater intrusion by recharge of groundwater-Acase study of Guanghuan County,Shandong Province[J].Journal of Natural Disasters,2006,15(3):100-104.(in Chinese))DOI:10.3969/j.issn.1004-4574.2006.03.017.
    [15]陆建生,潘伟强.上海某枢纽基坑工程浅层承压水回灌试验分析[J].地下空间与工程学报,2014,10(4):810-817.(LU J S,PAN W Q.Experimental analysis of shallow confined water recharge in foundation pit engineering of a certain hub in Shanghai[J].Chinese Journal of Underground Space and Engineering,2014,10(4):810-817.(in Chinese))
    [16]瞿成松.上海陆家嘴地区回灌试验分析[J].地下空间与工程学报,2014,10(2):295-298.(QU C S.Analysis of recharged test in Lujiazui Area of Shanghai[J].Chinese Journal of Underground Space and Engineering,2014,10(2):295-298.(in Chinese))
    [17]牛磊,张春福,孟祥玉,等.天津地区浅层地下水回灌试验分析[J].施工技术,2016,45(19):46-48.(NIUL,ZHANG C F,MENG X Y,et al.Experimental analysis of shallow groundwater recharge in Tianjin area[J].Construction Technology,2016,45(19):46-48.(in Chinese))DOI:10.7672/sgjs2016190046.
    [18]章丽萍,温晓东,张剑,等.南水北调工程北京段地下水回灌对含水层水质影响[J].水资源保护,2014,(4):7-9.(ZHANG L P,WEN X D,ZHANG J,et al.Influence of groundwater recharge on aquifer water quality in Beijing section of South-to-North Water Transfer Project[J].Water Resources Protection,2014,(4):7-9.(in Chinese))DOI:10.3969/j.issn.1004-6933.2014.04.002.
    [19]刘立才,郑凡东,李炳华,等.南水北调水源在密怀顺水源地回灌的地下水水质变化试验[J].水文地质工程地质,2015,42(4):18-22.(LIU L C,ZHENG F D,LI B H,et al.Experimental study on groundwater quality change of the South-to-North Water Transfer Project in the water source of Mishunshun[J].Hydrogeology and Engineering Geology,2015,42(4):18-22.(in Chinese))DOI:10.16030/j.cnki.issn.1000-3665.2015.04.04.
    [20]程东会,陈鸿汉,何江涛,等.北京城近郊区地下水人为影响和水-岩作用指示性指标研究[J].水文地质工程地质,2007,34(5):37-42.(CHENG D H,CHEN HH,HE J T,et al.Anthropogenic impacts of groundwater and indicators of water-rock interaction in the suburbs of Beijing City[J].Hydrogeology and Engineering Geology,2007,34(5):37-42.(in Chinese))DOI:10.3969/j.issn.1000-3665.2007.05.010.
    [21]杨维,陈曦,李晨霞.回灌条件下地下水质模拟与预测[J].工程勘察,2002(4):23-25.(YANG W,CHENX,LI C X.Simulation and prediction of groundwater quality under recirculation conditions[J].Engineering Investigation,2002(4):23-25.(in Chinese))
    [22]贾文飞,杨洋,赵阳,等.潮白河地下水调蓄区水岩作用过程模拟[J].南水北调与水利科技,2016,14(1):143-148.(JIA W F,YANG Y,ZHAO Y,et al.Simulation of water-rock process in the groundwater storage area of Chaobai River[J].South-to-North Water Transfer and Water Science and Technology,2016,14(1):143-148.(in Chinese))DOI:10.13476/j.cnki.nsbdqk.2016.01.024.
    [23]ONG"OR B T I,LONG-CANG S.Groundwater overdraft and the impact of artificial recharge on groundwater quality in a cone of depression,Jining,China[J].Water International,2009,34(4):468-483.DOI:10.1080/02508060903377619.
    [24]QIN D,QIAN Y,HAN L,et al.Assessing impact of irrigation water on groundwater recharge and quality in arid environment using CFCs,tritium and stable isotopes,in the Zhangye Basin,Northwest China[J].Journal of Hydrology,2011,405(1):194-208.DOI:10.1016/j.jhydrol.2011.05.023.
    [25]MILLER C J,MILLER C J.Impact of artificial recharge on Tucson area groundwater quality[J].1990.
    [26]KUMAR S,GHOSH N C,SINGH R P,et al.Impact of canal recharge on groundwater quality of Kolayat Area,District Bikaner,India[J].2016.DOI:10.1007/978-3-319-18663-4_52.
    [27]黄修东,束龙仓,刘佩贵,等,渗滤池砂样对回灌水中污染物去除的研究[J].水电能源科学,2009,27(1):62-65.(HUANG X D,SHU L C,LIU P G,et al,Study on the removal of pollutants in recirculating water by percolating sand samples[J].Hydropower Science,2009,27(1):62-65(in Chinese))DOI:10.3969/j.issn.1000-7709.2009.01.017.
    [28]王恩,束龙仓,黄修东,等,松散砂层及其有效粒径对回灌水水质影响的实验研究[J].水电能源科学,2009,27(4):37-40.(WANG E,SHU L C,HUANGX D et al.Experimental study on the effect of loose sand layer and its effective particle size on the quality of recharged water[J].Hydropower Energy Science,2009,27(4):37-40.(in Chinese))DOI:10.3969/j.issn.1000-7709.2009.04.013.
    [29]武显仓,赵琪,桓颖,等.深层承压含水层人工回灌条件下地下水中硝酸根的衰减[J].科技导报,2015,33(4):28-32.(WU X C,ZHAO Q,HUAN Y,et al.Attenuation of nitrate in groundwater under artificial recharge conditions of deep confined aquifer[J].Science&Technology Review,2015,33(4):28-32.(in Chinese))DOI:10.3981/j.issn.1000-7857.2015.04.004.
    [30]李学礼,孙占学,刘金辉.水文地球化学.第3版[M].北京:原子能出版社,2010.(LI X L,SUN Z X,LIU JH.Hydrogeochemistry.3rd edition[M].Beijing:A-tomic Energy Press,2010.(in Chinese))
    [31]BIAN C,CAI W T,LIU J W,et al.In Situ determination of nitrite in water and its application in groundwater contamination investigation[J].Environmental Engineering,2016,39(9):130-133.)DOI:10.13205/j.hjgc.201609028.

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