用户名: 密码: 验证码:
地表水与地下水联动关系研究综述
详细信息    查看全文 | 推荐本文 |
  • 英文篇名:Review of the Interactive Relation between Surface Water and Groundwater
  • 作者:雷晓辉 ; 刘柏君 ; 权锦 ; 王浩
  • 英文作者:LEI Xiao-hui;LIU Bo-jun;QUAN Jin;WANG Hao;State Key Laboratory of Simulation and Regulation of Water Cycle in River Basin,China Institute of Water Resources and Hydropower Research;Yellow River Engineering Consulting Co., Ltd;
  • 关键词:地表水 ; 地下水 ; 联动关系 ; 综述
  • 英文关键词:surface water;;groundwater;;interactive relation;;review
  • 中文刊名:中国农村水利水电
  • 英文刊名:China Rural Water and Hydropower
  • 机构:中国水利水电科学研究院流域水循环模拟与调控国家重点实验室;黄河勘测规划设计研究院有限公司;
  • 出版日期:2019-05-15
  • 出版单位:中国农村水利水电
  • 年:2019
  • 期:05
  • 基金:“十三五”国家重点研发计划课题(2018YFC1508706);; 国家自然科学基金项目(51569025)
  • 语种:中文;
  • 页:6-10+16
  • 页数:6
  • CN:42-1419/TV
  • ISSN:1007-2284
  • 分类号:X52
摘要
地表水与地下水均是重要的取用水水源,两者水量的不同会影响到区域水资源开发利用程度,同时,地表水与地下水间存在着水量交换,时而呈现平衡,时而出现此消彼长。如何获知两者间的联动关系,准确评估两者间的转换水量,是合理开发水资源、高效利用水资源、有效保护水资源的重要途径之一,也是众多学者研究的热点。基于此,从地下水模拟、地表水与地下水联合模拟、地表水与地下水联合调控、地下水位响应关系等4个方面论述了具有代表性的地表水与地下水联动关系研究成果,通过总结与分析,探究了研究现状,并对未来的研究方向进行了阐述。
        Surface water and groundwater are both the important sources of water utilization; the difference in water amount between surface water and groundwater will affect the development and utilization of regional water resources. And meanwhile, there is a water exchange between surface water and groundwater, which sometimes shows the balance, and sometimes shows a fluctuant process. It is one of the important ways to rationally develop water resources, efficiently utilize water resources and effectively protect water resources to study the linkage relationship between surface water and groundwater, and accurately evaluate the water conversion amount between the two, which is also the hot issue deserving a further research. Thus, the representative researches are discussed from the four aspects including groundwater simulation, joint simulation of surface water and groundwater, joint regulation of surface water and groundwater, response of groundwater level in this paper. Through summary and analysis, the current development is introduced and also the directions of future research on the interactive relation between surface water and groundwater are discussed.
引文
[1] 徐海量,樊自立,禹朴家,等.新疆玛纳斯河流域生态补偿研究[J],干旱区地理,2010,33(5):776-783.
    [2] 文力.西北典型内陆河流域地下水开发利用与生态环境保护模式——以玛纳斯河流域为例[D].北京:中国地址科学院,2006.
    [3] 董新光,邓铭江.新疆地下水资源[M].乌鲁木齐:新疆科技出版社,2005.
    [4] Wada Y,Wisser D,Bierkens M F P.Global modeling of withdrawal,allocation and consumptive use of surface water and groundwater resources[J].Earth System Dynamics,5,1(2014-01-14),2014,4(1):355-392.
    [5] Brunner P,Cook P G,Simmons C T.Hydrogeologic controls on disconnection between surface water and groundwater.[J].Water Resources Research,2009,45(1):1 422.
    [6] Banks E W,Simmons C T,Love A J,et al.Assessing spatial and temporal connectivity between surface water and groundwater in a regional catchment:Implications for regional scale water quantity and quality[J].Journal of Hydrology,2011,404(1):30-49.
    [7] Chen C W,Wei C C,Liu H J,et al.Application of Neural Networks and Optimization Model in Conjunctive Use of Surface Water and Groundwater[J].Water Resources Management,2014,28(10):2 813-2 832.
    [8] Change I P O C.Climate Change 2007:Synthesis Report[J].Environmental Policy Collection,2007,27(2):408.
    [9] Zende A M,Nagarajan R,Atal K R.Assessment of Groundwater Potential Zones by using GIS Techniques in Yerala River Basin,Western Maharashtra,India[J].2012,2:9-17.
    [10] 杨林山.气候变化与人类活动对洮河流域水文过程的影响[D].兰州:兰州大学,2015.
    [11] 徐翔宇.气候变化下典型流域的水文响应研究[D].北京:清华大学,2012.
    [12] Brown G O.Henry Darcy and the making of a law[J].Water Resources Research,2002,38(7):11-11.
    [13] Wooding R A,Chapman T G.Groundwater flow over a sloping impermeable layer:1.Application of the Dupuit-Forchheimer assumption[J].Journal of Geophysical Research,1966,71(12):2 895-2 902.
    [14] 严明疆,申建梅,张光辉,等.人类活动影响下的地下水脆弱性演变特征及其演变机理[J].干旱区资源与环境,2009,23(2):3-7.
    [15] Hantush M S,Jacob C E.Non‐steady radial flow in an infinite leaky aquifer[J].Eos Transactions American Geophysical Union,2011,36(1):95-100.
    [16] 刘建霞,袁西龙.青岛大沽河水源地地下水水质的数值模型预测[J].海洋地质动态,2006,22(2):9-14.
    [17] 尹大凯,胡和平,惠士博.宁夏银北灌区井渠结合灌溉三维数值模拟与分析[J].灌溉排水学报,2003,22(1):53-57.
    [18] 张祥伟,竹内邦良.大区域地下水模拟的理论和方法[J].水利学报,2004(6):7-13.
    [19] 李向国,李敏,叶晋岩,等.岩溶地下水水资源评价方法及应用实例[J].西部探矿工程,2005,17(3):79-80..
    [20] Pinder G F,Bredehoeft J D.Application of the Digital Computer for Aquifer Evaluation[J].Water Resources Research,1968,4(5):1 069-1 093.
    [21] 魏林宏,束龙仓,郝振纯.地下水流数值模拟的研究现状和发展趋势[J].重庆大学学报:自然科学版,2000,23(S1):50-52.
    [22] Bakker M,Post V,Langevin C D,et al.Scripting MODFLOW Model Development Using Python and FloPy[J].Ground Water,2016,54(5):733.
    [23] 童少青,董艳辉,王礼恒.非结构化网格MODFLOW模拟方法与应用[J].水文地质工程地质,2016,43(2):9-16.
    [24] 薛禹群,叶淑君,谢春红,等.多尺度有限元法在地下水模拟中的应用[J].水利学报,2004,35(7):7-13.
    [25] 谢春红,张勤,丁家平.稳定渗流的有限元计算新方法[J].水利学报,1995(12):29-38.
    [26] Wang Q Y,Jia Z H,Liu X F,et al.Visual MODFLOW and its application to groundwater simulation[J].Journal of Water Resources & Water Engineering,2007.
    [27] Li W,Zhang B,Hong M.Application of Visual MODFLOW in Assessment of Groundwater Resources in Longxi Area of Daqing[J].World Geology,2003.
    [28] Rajamanickam R,Nagan S.Groundwater quality modeling of Amaravathi River basin of Karur District,Tamil Nadu,using visual modflow.[J].International Journal of Environmental Sciences,2011,5(7):21-27.
    [29] 李文跃,张博,洪梅,等.Visual MODFLOW在大庆龙西地区地下水数值模拟中的应用[J].世界地质,2003,22(2):161-165.
    [30] 吴庆,郭永丽,滕彦国,等.基于过程模拟的李官堡水源地地下水污染预警[J].水文,2017,37(1):19-24.
    [31] Facchi A,Ortuani B,Maggi D,et al.Coupled SVAT-groundwater model for water resources simulation in irrigated alluvial plains[J].Environmental Modelling & Software,2004,19(11):1 053-1 063.
    [32] Seyed Reza Saghravani,Sa'ari b.Mustapha,Shaharin b.Ibrahim,et al.Phosphorus migration in an unconfined aquifer using MODFLOW and MT3DMS[J].Journal of Environmental Engineering & Landscape Management,2011,19(4):271-277.
    [33] Mondal N C,Singh V P.Evaluation of groundwater monitoring network of Kodaganar River basin from Southern India using entropy[J].Environmental Earth Sciences,2012,66(4):1 183-1 193.
    [34] Juan C S,Kolm K E.Conceptualization,characterization and numerical modeling of the Jackson Hole alluvial aquifer using ARC/INFO and MODFLOW[J].Engineering Geology,1996,42(2-3):119-137.
    [35] Baharuddin M F T,Tajudin S A A,Abidin M H Z,et al.Simulation of Sub-Drains Performance Using Visual MODFLOW for Slope Water Seepage Problem[J].2016,136(1):012 014.
    [36] 武强,董东林.水资源评价的可视化专业软件(VisualModflow)与应用潜力[J].水文地质工程地质,1999(5):21-23.
    [37] Shu L C,Chen X H.Simulation of water quantity exchange between groundwater and the Platte River water,central Nebraska[J].Journal of Central South University of Technology,2002,9(3):212-215.
    [38] 贾金生,田冰,刘昌明.Visual MODFLOW在地下水模拟中的应用——以河北省栾城县为例[J].河北农业大学学报,2003,26(2):71-78.
    [39] 尹大凯,胡和平,惠士博.宁夏银北灌区井渠结合灌溉三维数值模拟与分析[J].灌溉排水学报,2003,22(1):53-57.
    [40] 吴吉春,陆乐.地下水模拟不确定性分析[J].南京大学学报(自然科学),2011,47(3):227-234.
    [41] 陆垂裕,孙青言,李慧,等.基于水循环模拟的干旱半干旱地区地下水补给评价[J].水利学报,2014,45(6):701-711.
    [42] 粟晓玲,宋悦,刘俊民,等.耦合地下水模拟的渠井灌区水资源时空优化配置[J].农业工程学报,2016,32(13):43-51.
    [43] 魏光辉,马亮,WEIGuang-hui,等.基于自记忆方程的干旱区地下水水位动态模拟[J].节水灌溉,2016(3):58-60.
    [44] Coplen T.Stable Isotope Hydrology:Deuterium and Oxygen-18 in the Water Cycle[J].Eos Transactions American Geophysical Union,1982,63(45):861-862.
    [45] Henderson A C G,Holmes J A,Leng M J.Late Holocene isotope hydrology of Lake Qinghai,NE Tibetan Plateau:effective moisture variability and atmospheric circulation changes[J].Quaternary Science Reviews,2010,29(17-18):2 215-2 223.
    [46] Jasechko S,Wassenaar L I,Mayer B.Isotopic evidence for widespread cold-season-biased groundwater recharge and young streamflow across central Canada[J].Hydrological Processes,2017,31(12):2 196-2 209.
    [47] 陈建生,凡哲超,汪集旸,等.巴丹吉林沙漠湖泊及其下游地下水同位素分析[J].地球学报,2003,24(6):497-504.
    [48] Gat J R.Isotope hydrology:a study of the water cycle[J].Annals of the American Thoracic Society,2010,12(4):480-5.
    [49] Mccarthy K A,Mcfarland W D,Wilkinson J M,et al.The dynamic relationship between ground water and the Columbia River:using deuterium and oxygen-18 as tracers[J].Journal of Hydrology,1992,135(1-4):1-12.
    [50] Mathieu R,Bariac T.An Isotopic Study (2H and 18O) of Water Movements in Clayey Soils Under a Semiarid Climate[J].Water Resources Research,1996,32(4):779-790.
    [51] Maloszewski P,Stichler W,Zuber A,et al.Identifying the flow systems in a karstic-fissured-porous aquifer,the Schneealpe,Austria,by modelling of environmental 18 O and 3 H isotopes[J].Journal of Hydrology,2002,256(1-2):48-59.
    [52] Brown O R,Taylor K.Adsorbed alkyl radicals in the cathodic synthesis of mercury dialkyls[J].Journal of Electroanalytical Chemistry & Interfacial Electrochemistry,1974,50(2):211-220.
    [53] Payne B R,Quijano L,Latorre D C.Environmental isotopes in a study of the origin of salinity of groundwater in the Mexicali Valley[J].Journal of Hydrology,1979,41(3-4):201-215.
    [54] Yurtsever Y.Editor's Message:Hydrology,Isotopes,and the International Atomic Energy Agency[J].Hydrogeology Journal,1997,5(3):2-6.
    [55] Katz B G,Coplen T B,Bullen T D,et al.Use of Chemical and Isotopic Tracers to Characterize the Interactions Between Ground Water and Surface Water in Mantled Karst[J].Ground Water,2010,35(6):1 014-1 028.
    [56] Krabbenhoft D P,Bowser C J,Anderson M P,et al.Estimating groundwater exchange with lakes:1.The stable isotope mass balance method[J].Water Resources Research,1990,26(10):2 445-2 453.
    [57] 张应华,仵彦卿,丁建强,等.运用氧稳定同位素研究黑河中游盆地地下水与河水转化[J].冰川冻土,2005,27(1):106-110.
    [58] 王杰,王文科,田华,等.环境同位素在三水转化研究中的应用[J].工程勘察,2007(3):31-34.
    [59] 刘丹,刘世青.应用环境同位素方法研究塔里木河下游浅层地下水[J].成都理工大学学报(自科版),1997(3):89-95.
    [60] 钱云平,林学钰,秦大军,等.应用同位素研究黑河下游额济纳盆地地下水[J].干旱区地理(汉文版),2005,28(5):574-580.
    [61] 李健,王辉,魏丽琼.格尔木河流域平原区地下水同位素及水化学特征[J].西北地质,2007,40(4):94-100.
    [62] 朱谱成,苏小四,张世广,等.那陵郭勒河冲洪积扇地表水-地下水转化关系[J].人民黄河,2014,36(7):60-64.
    [63] 耿直,武中强,王小军,等.河北省农村地区水源地安全评价与分析[J].地下水,2016,38(5):97-101.
    [64] Oh H J,Kim Y S,Choi J K,et al.GIS mapping of regional probabilistic groundwater potential in the area of Pohang City,Korea[J].Journal of Hydrology,2011,399(3-4):158-172.
    [65] Khan S,Rana T,Hanjra M A.A cross disciplinary framework for linking farms with regional groundwater and salinity management targets[J].Agricultural Water Management,2008,95(1):35-47.
    [66] 倪付燕.小南海泉域地下水资源管理模型[D].南京:河海大学,2007.
    [67] Markstrom S L,Niswonger R G,Regan R S,et al.GSFLOW-Coupled ground-water and surface-water flow model based on the integration of the Precipitation-Runoff Modeling System (PRMS) and the Modular Ground-Water Flow Model (MODFLOW-2005)[J].2008.
    [68] Wong H S,Sun N Z,Yeh W W G.Optimization of conjunctive use of surface water and groundwater with water quality constraints[J].International Review of Hydrobiology,2014,97(97):526-541.
    [69] 陈雨孙,刘春平.地下水非稳定流优化模型(有限单元和线性规划相结合)[J].工程勘察,1986(5):27-32.
    [70] 谢新民,周之豪.地表-地下水资源系统多目标管理模型与模糊决策研究[J].大连理工大学学报,1994(2):240-248.
    [71] 马福昌,兰瑞,王才.基于MapX的地下水资源管理信息系统的设计与开发[J].图书情报导刊,2005(13):176-178.
    [72] 孙才志,刘立权,杨新岩,等.基于生态约束的辽阳首山地下水水源地管理模型[J].资源科学,2013,35(7):1 388-1 397.
    [73] 程卫国.变化条件下吉林西部地下水的模拟与管理[D].长春:吉林大学,2015.
    [74] 胡立堂,孙康宁,尹文杰,等.GRACE卫星在区域地下水管理中的应用潜力综述[J].地球科学与环境学报,2016,38(2):258-266.
    [75] 杨国强,孟婧莹,苏小四,等.地下水超采评价的指标体系与评价过程[J].节水灌溉,2012(8):34-38.
    [76] 张建友,张红,秦作栋.山西省地下水回灌前景分析[J].山西水利,2013(1):4-7.
    [77] Taormina R,Chau K W,Sethi R.Artificial neural network simulation of hourly groundwater levels in a coastal aquifer system of the Venice lagoon[J].Engineering Applications of Artificial Intelligence,2012,25(8):1 670-1 676.
    [78] 王蕊,王中根,夏军,等.气候变化及南水北调中线工程对白洋淀流域水文的影响[J].水力发电学报,2012,31(2):14-19.
    [79] Thorburn P J,Walker G R,Woods P H.Comparison of diffuse discharge from shallow water tables in soils and salt flats[J].Journal of Hydrology,1992,136(1-4):253-274.
    [80] Ali R,Elliott R L,Ayars J E,et al.Soil salinity modeling over shallow water tables.II:application of LEACHC.[J].Journal of Irrigation & Drainage Engineering,2000,126(4):234-242.
    [81] Benyamini Y,Mirlas V,Marish S,et al.A survey of soil salinity and groundwater level control systems in irrigated fields in the Jezre'el Valley,Israel[J].Agricultural Water Management,2005,76(3):181-194.
    [82] 张惠昌.干旱区地下水生态平衡埋深[J].勘察科学技术,1992(6):9-13.
    [83] 白永辉,张丽.河北省沧州市地质灾害与地下水关系研究[J].中国地质灾害与防治学报,2005,16(3):71-73.
    [84] 谢新民,柴福鑫,颜勇,等.地下水控制性关键水位研究初探[J].地下水,2007,29(6):47-50.

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700