西北干旱区间歇性河流与含水层水量交换研究进展与展望

doi:10.18306/dlkxjz.2018.02.002

摘要/Abstract

摘要：

本文依托国家自然科学基金青年项目“河水温度对干旱区宽浅型河床渗透系数影响的定量研究”,并梳理了其他相关研究,总结了中国西北干旱区间歇性河流与含水层水量交换研究所面临的基础科学问题及当前所取得的研究进展。主要结论为：以宽浅型沙质河床为基本特征的西北干旱区内陆河流域下游河流,其河床每年经历数次干湿交替与冻融过程。受河水温度与河流水动力条件的影响,河床作为河流与含水层相互作用的重要界面,其渗透性能具有高度时空变异性,已成为河水与地下水水量交换研究的难点与热点。分析指出,在环境变化和当前交叉学科迅猛发展的背景下,以河流与含水层相互作用为核心的潜流带水文学发展面临新的机遇与挑战。

关键词: 地表水—地下水转化;, 河床渗透系数, 水文过程, 干旱区

Abstract:

Incorporating the research results of the the National Natural Science Foundation supported project "Quantifying the effect of river water temperature on riverbed hydraulic conductivity of broad-shallow rivers in the arid area" (No. 41301025), this article summarizes the basic scientific issues and the current research progress in the field of water exchange between intermittent rivers and aquifers in arid areas of northwestern China. Riverbed at the lower reaches of rivers in the arid regions of northwestern China is shallow, wide, and sandy. Such riverbed experiences several dry/wet alternations and freezing-thawing process each year. Due to the influence of river temperature and river flow conditions, the riverbed as an important interface of river-aquifer systems exerts significant temporal and spatial variability, which has become a key issue in understanding surface water and groundwater exchange. Hyporheic zone hydrology, which focuses on river-aquifer interaction, is facing new opportunities and challenges under the current changing environment and rapidly developing interdisciplinary research.

Key words: surface water-groundwater transfer, riverbed hydraulic conductivity, hydrological process, arid area

王平. 西北干旱区间歇性河流与含水层水量交换研究进展与展望[J]. 地理科学进展, 2018, 37(2): 183-197.

Ping WANG. Progress and prospect of research on water exchange between intermittent rivers and aquifers in arid regions of northwestern China[J]. PROGRESS IN GEOGRAPHY, 2018, 37(2): 183-197.

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参考文献 138

[39]	Cheng G D.1983. The mechanism of repeated-segregation for the formation of thick layered ground ice[J]. Cold Regions Science and Technology, 8(1): 57-66. doi: 10.1016/0165-232X(83)90017-4
[40]	Cheng G D, Jin H J.2013. Permafrost and groundwater on the Qinghai-Tibet Plateau and in northeast China[J]. Hydrogeology Journal, 21(1): 5-23. doi: 10.1007/s10040-012-0927-2
[41]	Clapp R B, Hornberger G M.1978. Empirical equations for some soil hydraulic properties[J]. Water Resources Research, 14(4): 601-604. doi: 10.1029/WR014i004p00601
[42]	Constantz J.2008. Heat as a tracer to determine streambed water exchanges[J]. Water Resources Research, 44(4): W00D10. doi: 10.1029/2008WR006996
[43]	Constantz J.2016. Streambeds merit recognition as a scientific discipline[J]. Wiley Interdisciplinary Reviews: Water, 3(1): 13-18. doi: 10.1002/wat2.1119
[44]	Constantz J, Cox M H, Su G W.2003. Comparison of heat and bromide as ground water tracers near streams[J]. Ground Water, 41(5): 647-656. doi: 10.1111/j.1745-6584.2003.tb02403.x pmid: 13678119
[45]	Constantz J, Thomas C L, Zellweger G.1994. Influence of diurnal variations in stream temperature on streamflow loss and groundwater recharge[J]. Water Resources Research, 30(12): 3253-3264. doi: 10.1029/94WR01968
[46]	Cook P G.2015. Quantifying river gain and loss at regional scales[J]. Journal of Hydrology, 531: 749-758. doi: 10.1016/j.jhydrol.2015.10.052
[47]	Cuthbert M O, Mackay R, Durand V, et al.2010. Impacts of river bed gas on the hydraulic and thermal dynamics of the hyporheic zone[J]. Advances in Water Resources, 33(11): 1347-1358. doi: 10.1016/j.advwatres.2010.09.014
[48]	Dahan O, Tatarsky B, Enzel Y, et al.2008. Dynamics of flood water infiltration and ground water recharge in hyperarid desert[J]. Ground Water, 46(3): 450-461. doi: 10.1111/j.1745-6584.2007.00414.x pmid: 18194313
[49]	Datry T, Larned S T, Tockner K.2014. Intermittent rivers: A challenge for freshwater ecology[J]. BioScience, 64(3): 229-235. doi: 10.1093/biosci/bit027
[50]	de Vries J, Simmers I.2002. Groundwater recharge: An overview of processes and challenges[J]. Hydrogeology Journal, 10(1): 5-17. doi: 10.1007/s10040-001-0171-7
[51]	Doble R C, Crosbie R S, Smerdon B D, et al.2012. Groundwater recharge from overbank floods[J]. Water Resources Research, 48(9): W09522. doi: 10.1029/2011WR011441
[52]	Doppler T, Franssen H-J H, Kaiser H-P, et al.2007. Field evidence of a dynamic leakage coefficient for modelling river-aquifer interactions[J]. Journal of Hydrology, 347(1-2): 177-187. doi: 10.1016/j.jhydrol.2007.09.017
[1]	程国栋, 肖洪浪, 傅伯杰, 等. 2014. 黑河流域生态—水文过程集成研究进展[J]. 地球科学进展, 29(4): 431-437. doi: 10.11867/j.issn.1001-8166.2014.04.0431
	[Cheng G D, Xiao H L, Fu B J, et al.2014. Advances in synthetic research on the eco-hydrological process of the Heihe River Basin[J]. Advances in Earth Science, 29(4): 431-437.] doi: 10.11867/j.issn.1001-8166.2014.04.0431
[53]	Du C Y, Yu J J, Wang P, et al.2016. Reference evapotranspiration changes: Sensitivities to and contributions of meteorological factors in the Heihe River basin of northwestern China (1961-2014)[J]. Advances in Meteorology, 2016: 4143580. doi: 10.1155/2016/4143580
[54]	Duque C, Calvache M L, Engesgaard P.2010. Investigating river-aquifer relations using water temperature in an anthropized environment (Motril-Salobreña aquifer)[J]. Journal of Hydrology, 381(1-2): 121-133. doi: 10.1016/j.jhydrol.2009.11.032
[2]	杜尧, 马腾, 邓娅敏, 等. 2017. 潜流带水文—生物地球化学: 原理、方法及其生态意义[J]. 地球科学, 42(5): 661-673. doi: 10.3799/dqkx.2017.054
	[Du Y, Ma T, Deng Y M, et al.2017. Hydro-biogeochemistry of hyporheic zone: Principles, methods and ecological significance[J]. Earth Science, 42(5): 661-673.] doi: 10.3799/dqkx.2017.054
[55]	Essaid H I, Zamora C M, McCarthy K A, et al.2008. Using heat to characterize streambed water flux variability in four stream reaches[J]. Journal of Environmental Quality, 37(3): 1010-1023. doi: 10.2134/jeq2006.0448 pmid: 18453424
[56]	Fleckenstein J H, Krause S, Hannah D M, et al.2010. Groundwater-surface water interactions: New methods and models to improve understanding of processes and dynamics[J]. Advances in Water Resources, 33(11): 1291-1295. doi: 10.1016/j.advwatres.2010.09.011
[3]	冯斯美, 宋进喜, 来文立, 等. 2013. 河流潜流带渗透系数变化研究进展[J]. 南水北调与水利科技, 11(3): 123-126.
	[Feng S M, Song J X, Lai W L, et al.2013. An overview of the effects of hyporheic processes on the streambed hydraulic conductivity in the hyporheic zone of a river[J]. South-to-North Water Transfers and Water Science & Technology, 11(3): 123-126.]
[57]	Fox G A, Durnford D S.2003. Unsaturated hyporheic zone flow in stream/aquifer conjunctive systems[J]. Advances in Water Resources, 26(9): 989-1000. doi: 10.1016/S0309-1708(03)00087-3
[58]	Frey K E, McClelland J W.2009. Impacts of permafrost degradation on arctic river biogeochemistry[J]. Hydrological Processes, 23(1): 169-182. doi: 10.1002/hyp.7196
[59]	Gao T G, Zhang T J, Cao L, et al.2016. Reduced winter runoff in a mountainous permafrost region in the northern Tibetan Plateau[J]. Cold Regions Science and Technology, 126: 36-43. doi: 10.1016/j.coldregions.2016.03.007
[60]	Gerecht K E, Cardenas M B, Guswa A J, et al.2011. Dynamics of hyporheic flow and heat transport across a bed-to-bank continuum in a large regulated river[J]. Water Resources Research, 47(3): W03524. doi: 10.1029/2010WR009794
[4]	何志斌, 赵文智. 2007. 河床水力传导度及其各向异性的测定[J]. 水科学进展, 18(3): 351-355. doi: 10.3321/j.issn:1001-6791.2007.03.007
	[He Z B, Zhao W Z.2007. Measurement of streambed hydraulic conductivity and anisotropy analysis[J]. Advances in Water Science, 18(3): 351-355.] doi: 10.3321/j.issn:1001-6791.2007.03.007
[61]	Gibson S, Heath R, Abraham D, et al.2011. Visualization and analysis of temporal trends of sand infiltration into a gravel bed[J]. Water Resources Research, 47(12): W12601. doi: 10.1029/2011WR010486
[62]	Halloran L J S, Rau G C, Andersen M S.2016. Heat as a tracer to quantify processes and properties in the vadose zone: A review[J]. Earth-Science Reviews, 159: 358-373. doi: 10.1016/j.earscirev.2016.06.009
[5]	胡立堂, 王忠静, 赵建世, 等. 2007. 地表水和地下水相互作用及集成模型研究[J]. 水利学报, 38(1): 54-59.
	[Hu L T, Wang Z J, Zhao J S, et al.2007. Advances in the interactions and integrated model between surface water and groundwater[J]. Journal of Hydraulic Engineering, 38(1): 54-59.]
[63]	Hantush M S.1965. Wells near streams with semipervious beds[J]. Journal of Geophysical Research, 70(12): 2829-2838. doi: 10.1029/JZ070i012p02829
[64]	Hatch C E, Fisher A T, Revenaugh J S, et al.2006. Quantifying surface water-groundwater interactions using time series analysis of streambed thermal records: Method development[J]. Water Resources Research, 42(10): W10410. doi: 10.1029/2005WR004787
[6]	黄丽, 郑春苗, 刘杰, 等. 2012. 分布式光纤测温技术在黑河中游地表水与地下水转换研究中的应用[J]. 水文地质工程地质, 39(2): 1-6.
	[Huang L, Zheng C M, Liu J, et al.2012. Application of distributed temperature sensing to study groundwater-surface water interactions in the Heihe River Basin[J]. Hydrogeology and Engineering Geology, 39(2): 1-6.]
[7]	靳孟贵, 鲜阳, 刘延锋. 2017. 脱节型河流与地下水相互作用研究进展[J]. 水科学进展, 28(1): 149-160. doi: 10.14042/j.cnki.32.1309.2017.01.017
	[Jin M G, Xian Y, Liu Y F.2017. Disconnected stream and groundwater interaction: A review[J]. Advances in Water Science, 28(1): 149-160.] doi: 10.14042/j.cnki.32.1309.2017.01.017
[65]	Hatch C E, Fisher A T, Ruehl C R, et al.2010. Spatial and temporal variations in streambed hydraulic conductivity quantified with time-series thermal methods[J]. Journal of Hydrology, 389(3-4): 276-288. doi: 10.1016/j.jhydrol.2010.05.046 pmid: 15373905
[66]	Healy R W, Essaid H I.2012. VS2DI: Model use, calibration, and validation[J]. Transactions of the ASABE, 55(4): 1249-1260. doi: 10.13031/2013.42238
[8]	刘传琨, 胡玥, 刘杰, 等. 2014. 基于温度信息的地表—地下水交互机制研究进展[J]. 水文地质工程地质, 41(5): 5-10, 18.
	[Liu C K, Hu Y, Liu J, et al.2014. Advances in using temperature to study surface water-groundwater interactions[J]. Hydrogeology and Engineering Geology, 41(5): 5-10, 18.]
[67]	Healy R W, Ronan A D.1996. Documentation of computer program VS2DH for simulation of energy transport in variably saturated porous media—Modification of the U.S. Geological Survey's computer program VS2DT[R]. Water resources investigation report 96-4230. Denver, Colorado: U.S. Geological Survey.
[68]	Hinkel K M, Arp C D, Townsend-Small A, et al.2017. Can deep groundwater influx be detected from the geochemistry of thermokarst lakes in arctic Alaska[J]. Permafrost and Periglacial Processes, 28(3): 552-557. doi: 10.1002/ppp.1895
[9]	刘登峰, 田富强, 林木, 等. 2014. 基于生态水文耦合模型的塔里木河下游人工输水优化方案研究[J]. 水力发电学报, 33(4): 51-59.
	[Liu D F, Tian F Q, Lin M, et al.2014. Study on optimal scheme of water transfer in the lower Tarim river based on ecohydrological evolution model[J]. Journal of Hydroelectric Engineering, 33(4): 51-59.]
[69]	Hoffmann J P, Ripich M A, Ellett K M.2002. Characteristics of shallow deposits beneath Rillito Creek, Pima County, Arizona[R]. Water-resources investigations report 01-4257. Tucson, AZ: US Geological Survey: 42.
[70]	Huang X, Andrews C B, Liu J, et al.2016. Assimilation of temperature and hydraulic gradients for quantifying the spatial variability of streambed hydraulics[J]. Water Resources Research, 52(8): 6419-6439. doi: 10.1002/2015WR018408
[10]	马瑞, 董启明, 孙自永, 等. 2013. 地表水与地下水相互作用的温度示踪与模拟研究进展[J]. 地质科技情报, 32(2): 131-137.
	[Ma R, Dong Q M, Sun Z Y, et al.2013. Using heat to trace and model the surface water-groundwater interactions: A review[J]. Geological Science and Technology Information, 32(2): 131-137.]
[71]	Hunt B.1999. Unsteady stream depletion from ground water pumping[J]. Ground Water, 37(1): 98-102. doi: 10.1111/j.1745-6584.1999.tb00962.x
[72]	Hvorslev M J.1951. Time lag and soil permeability in groundwater observations[R]. Waterways experiment station bulletin 36. Vicksburg, MS: US Army Corps of Engineers.
[73]	Hyun Y, Kim H, Lee S-S, et al.2011. Characterizing streambed water fluxes using temperature and head data on multiple spatial scales in Munsan stream, South Korea[J]. Journal of Hydrology, 402(3-4): 377-387. doi: 10.1016/j.jhydrol.2011.03.032
[74]	Jolly I D, McEwan K L, Holland K L.2008. A review of groundwater-surface water interactions in arid/semi-arid wetlands and the consequences of salinity for wetland ecology[J]. Ecohydrology, 1(1): 43-58. doi: 10.1002/eco.6
[11]	庞忠和. 2014. 新疆水循环变化机理与水资源调蓄[J]. 第四纪研究, 34(5): 907-917. doi: 10.3969/j.issn.1001-7410.2014.05.01
	[Pang Z H.2014. Mechanism of water cycle changes and implications on water resources regulation in Xinjiang Uygur autonomous region[J]. Quaternary Sciences, 34(5): 907-917.] doi: 10.3969/j.issn.1001-7410.2014.05.01
[75]	Kalbus E, Reinstorf F, Schirmer M.2006. Measuring methods for groundwater-surface water interactions: A review[J]. Hydrology and Earth System Sciences, 10(6): 873-887. doi: 10.5194/hess-10-873-2006
[76]	Landon M K, Rus D L, Harvey F E.2001. Comparison of instream methods for measuring hydraulic conductivity in sandy streambeds[J]. Ground Water, 39(6): 870-885. doi: 10.1111/j.1745-6584.2001.tb02475.x pmid: 11708453
[12]	束龙仓, Chen X H.2002. 美国内布拉斯加州普拉特河河床沉积物渗透系数的现场测定[J]. 水科学进展, 13(5): 629-633. doi: 10.3321/j.issn:1001-6791.2002.05.017
	[Shu L C, Chen X H.2002. Measurement in situ of streambed hydraulic conductivities in the Platte River, Nebraska[J]. Advances in Water Science, 13(5): 629-633.] doi: 10.3321/j.issn:1001-6791.2002.05.017
[77]	Lapham W W.1989. Use of temperature profiles beneath streams to determine rates of vertical ground-water flow and vertical hydraulic conductivity[R]. US Geological Survey water-supply paper 2337. Denver, Colorado: USGS Numbered Series: 35.
[78]	Liao C, Zhuang Q H.2017. Quantifying the role of permafrost distribution in groundwater and surface water interactions using a three-dimensional hydrological model[J]. Arctic, Antarctic, and Alpine Research, 49(1): 81-100. doi: 10.1657/AAAR0016-022
[13]	束龙仓, Chen X H.2003. 河流—含水层系统中水文要素的变化过程分析[J]. 河海大学学报: 自然科学版, 31(3): 251-254.
	[Shu L C, Chen X H.2003. Variation process of hydrologic elements of river-aquifer system[J]. Journal of Hohai University: Natural Sciences, 31(3): 251-254.]
[79]	Liu X, Yu J J, Wang P, et al.2016. Lake evaporation in a hyper-arid environment, northwest of China—measurement and estimation[J]. Water, 8(11): 527. doi: 10.3390/w8110527
[80]	Lundquist J D, Lott F.2008. Using inexpensive temperature sensors to monitor the duration and heterogeneity of snow-covered areas[J]. Water Resources Research, 44(4): W00D16. doi: 10.1029/2008wr007035
[14]	束龙仓, 鲁程鹏, 李伟. 2008. 考虑参数不确定性的地表水与地下水交换量的计算方法[J]. 水文地质工程地质, 35(5): 68-71. doi: 10.3969/j.issn.1000-3665.2008.05.016
	[Shu L C, Lu C P, Li W.2008. Calculation method of the exchange volume between surface water and groundwater based on uncertainty of parameters[J]. Hydrogeology and Engineering Geology, 35(5): 68-71.] doi: 10.3969/j.issn.1000-3665.2008.05.016
[15]	宋进喜, Chen X H, Cheng C, 等. 2009. 美国内布拉斯加州埃尔克霍恩河河床沉积物渗透系数深度变化特征[J]. 科学通报, 54(24): 3892-3899.
	[Song J X, Chen X H, Cheng C, et al.2009. Variability of streambed vertical hydraulic conductivity with depth along the Elkhorn River, Nebraska, USA[J]. Chinese Science Bulletin, 54(24): 3892-3899.]
[81]	McCallum A M, Andersen M S, Rau G C, et al.2014. River-aquifer interactions in a semiarid environment investigated using point and reach measurements[J]. Water Resources Research, 50(4): 2815-2829. doi: 10.1002/2012WR012922
[82]	Min L L, Yu J J, Liu C M, et al.2013. The spatial variability of streambed vertical hydraulic conductivity in an intermittent river, northwestern China[J]. Environmental Earth Sciences, 69(3): 873-883. doi: 10.1007/s12665-012-1973-8
[16]	宋进喜, 任朝亮, 李梦洁, 等. 2014. 河流潜流带颤蚓生物扰动对沉积物渗透性的影响研究[J]. 环境科学学报, 34(8): 2062-2069. doi: 10.13671/j.hjkxxb.2014.0586
	[Song J X, Ren C L, Li M J, et al.2014. Effects of Tubificid bioturbations on vertical hydraulic conductivity of the hyporheic streambed sediments[J]. Acta Scientiae Circumstantiae, 34(8): 2062-2069.] doi: 10.13671/j.hjkxxb.2014.0586
[83]	Morin E, Grodek T, Dahan O, et al.2009. Flood routing and alluvial aquifer recharge along the ephemeral arid Kuiseb River, Namibia[J]. Journal of Hydrology, 368(1-4): 262-275. doi: 10.1016/j.jhydrol.2009.02.015
[84]	Mutiti S, Levy J.2010. Using temperature modeling to investigate the temporal variability of riverbed hydraulic conductivity during storm events[J]. Journal of Hydrology, 388(3-4): 321-334. doi: 10.1016/j.jhydrol.2010.05.011
[85]	Niswonger R G, Prudic D E.2005. Documentation of the Streamflow-Routing (SFR2) Package to include unsaturated flow beneath streams—A modification to SFR1[R]. U.S. Geological Survey techniques and methods 6-A13. Denver, Colorado: U.S. Geological Survey.
[86]	Noorduijn S L, Shanafield M, Trigg M A, et al.2014. Estimating seepage flux from ephemeral stream channels using surface water and groundwater level data[J]. Water Resources Research, 50(2): 1474-1489. doi: 10.1002/2012WR013424
[17]	王根绪, 李元寿, 王一博, 等. 2007. 长江源区高寒生态与气候变化对河流径流过程的影响分析[J]. 冰川冻土, 29(2): 159-168. doi: 10.3969/j.issn.1000-0240.2007.02.001
	[Wang G X, Li Y S, Wang Y B, et al.2007. Impacts of alpine ecosystem and climate changes on surface runoff in the headwaters of the Yangtze River[J]. Journal of Glaciology and Geocryology, 29(2): 159-168.] doi: 10.3969/j.issn.1000-0240.2007.02.001
[87]	Partington D, Therrien R, Simmons C T, et al.2017. Blueprint for a coupled model of sedimentology, hydrology, and hydrogeology in streambeds[J]. Reviews of Geophysics, 55(2): 287-309. doi: 10.1002/2016RG000530
[88]	Pekel J-F, Cottam A, Gorelick N, et al.2016. High-resolution mapping of global surface water and its long-term changes[J]. Nature, 540: 418-422. doi: 10.1038/nature20584 pmid: 27926733
[18]	王平, 于静洁, 闵雷雷, 等. 2014. 额济纳绿洲浅层地下水动态监测研究及其进展[J]. 第四纪研究, 34(5): 982-993. doi: 10.3969/j.issn.1001-7410.2014.05.08
	[Wang P, Yu J J, Min L L, et al.2014. Shallow groundwater regime and its driving forces in the Ejina Oasis[J]. Quaternary Sciences, 34(5): 982-993.] doi: 10.3969/j.issn.1001-7410.2014.05.08
[89]	Pozdniakov S P, Wang P, Lekhov M V.2016. A semi-analytical generalized Hvorslev formula for estimating riverbed hydraulic conductivity with an open-ended standpipe permeameter[J]. Journal of Hydrology, 540: 736-743. doi: 10.1016/j.jhydrol.2016.06.061
[90]	Prudic D E, Konikow L F, Banta E R.2004. A new streamflow-routing (SFR1) package to simulate stream-aquifer interaction with MODFLOW-2000[R]. U.S. Geological Survey, open-file report 2004-1042. Carson, Nevada: U.S. Department of the Interior, U.S. Geological Survey.
[19]	吴志伟, 宋汉周. 2011. 地下水温度示踪理论与方法研究进展[J]. 水科学进展, 22(5): 733-740.
	[Wu Z W, Song H Z.2011. Temperature as a groundwater tracer: Advances in theory and methodology[J]. Advances in Water Science, 22(5): 733-740.]
[20]	徐斅祖, 王家澄, 张立新. 2001. 冻土物理学[M]. 北京: 科学出版社.
	[Xu X Z, Wang J C, Zhang L X.2001. Physics of frozen soil[M]. Beijing, China: Science Press.]
[21]	薛禹群. 1997. 地下水动力学[M]. 北京: 地质出版社.
	[Xue Y Q.1997. Dixia shuidonglixue[M]. Beijing, China: Geological Publishing House.]
[91]	Rau G C, Halloran L J S, Cuthbert M O, et al.2017. Characterising the dynamics of surface water-groundwater interactions in intermittent and ephemeral streams using streambed thermal signatures[J]. Advances in Water Resources, 107: 354-369. doi: 10.1016/j.advwatres.2017.07.005
[92]	Reid M E, Dreiss S J.1990. Modeling the effects of unsaturated, stratified sediments on groundwater recharge from intermittent streams[J]. Journal of Hydrology, 114(1-2): 149-174. doi: 10.1016/0022-1694(90)90079-D
[93]	Rimon Y, Nativ R, Dahan O.2011. Vadose zone water pressure variation during infiltration events[J]. Vadose Zone Journal, 10(3): 1105-1112. doi: 10.2136/vzj2010.0061
[94]	Rivière A, Gonçalvès J, Jost A, et al.2014. Experimental and numerical assessment of transient stream-aquifer exchange during disconnection[J]. Journal of Hydrology, 517: 574-583. doi: 10.1016/j.jhydrol.2014.05.040
[22]	中国科学院地学部. 1996. 西北干旱区水资源考察报告: 关于黑河、石羊河流域合理用水和拯救生态问题的建议[J]. 地球科学进展, 11(1): 1-4.
	[Earth Science Division of Chinese Academy of Sciences.1996. Xibei ganhanqu shuiziyuan kaocha baogao: Guanyu HeiHe, ShiYangHe liuyu heli yongshui he zhengjiu shengtai wenti de jianyi[J]. Advances in Earth Sciences, 11(1): 1-4.]
[95]	Ronan A D, Prudic D E, Thodal C E, et al.1998. Field study and simulation of diurnal temperature effects on infiltration and variably saturated flow beneath an ephemeral stream[J]. Water Resources Research, 34(9): 2137-2153. doi: 10.1029/98WR01572
[96]	Rosenberry D O.2008. A seepage meter designed for use in flowing water[J]. Journal of Hydrology, 359(1-2): 118-130. doi: 10.1016/j.jhydrol.2008.06.029
[23]	周幼吾, 郭东信, 程国栋, 等. 2000. 中国冻土[M]. 北京: 科学出版社.
	[Zhou Y W, Guo D X, Cheng G D, et al.2000. Geocryology in China[M]. Beijing, China: Science Press.]
[97]	Rosenberry D O, LaBaugh J W.2008. Field techniques for estimating water fluxes between surface water and ground water[R]. Techniques and methods chapter 4-D2. Reston, VA: U.S. Department of the Interior, U.S. Geological Survey.
[98]	Rosenberry D O, Pitlick J.2009. Local-scale variability of seepage and hydraulic conductivity in a shallow gravel-bed river[J]. Hydrological Processes, 23(23): 3306-3318. doi: 10.1002/hyp.7433
[24]	朱金峰, 刘悦忆, 章树安, 等. 2017. 地表水与地下水相互作用研究进展[J]. 中国环境科学, 37(8): 3002-3010.
	[Zhu J J, Liu Y Y, Zhang S A, et al.2017. Review on the research of surface water and groundwater interactions[J]. China Environmental Science, 37(8): 3002-3010.]
[99]	Roshan H, Rau G C, Andersen M S, et al.2012. Use of heat as tracer to quantify vertical streambed flow in a two-dimensional flow field[J]. Water Resources Research, 48(10): W10508. doi: 10.1029/2012WR011918
[100]	Scanlon B R, Healy R W, Cook P G.2002. Choosing appropriate techniques for quantifying groundwater recharge[J]. Hydrogeology Journal, 10(1): 18-39. doi: 10.1007/s10040-001-0176-2
[25]	Alyamani M S, Şen Z.1993. Determination of hydraulic conductivity from complete grain-size distribution curves[J]. Ground Water, 31(4): 551-555. doi: 10.1111/j.1745-6584.1993.tb00587.x
[26]	Anderson M P.2005. Heat as a ground water tracer[J]. Ground Water, 43(6): 951-968. doi: 10.1111/j.1745-6584.2005.00052.x pmid: 16324018
[101]	Schmidt C, Conant Jr B, Bayer-Raich M, et al.2007. Evaluation and field-scale application of an analytical method to quantify groundwater discharge using mapped streambed temperatures[J]. Journal of Hydrology, 347(3-4): 292-307. doi: 10.1016/j.jhydrol.2007.08.022
[102]	Selker J S, Thévenaz L, Huwald H, et al.2006. Distributed fiber-optic temperature sensing for hydrologic systems[J]. Water Resources Research, 42(12): W12202. doi: 10.1029/2006WR005326
[27]	Anibas C, Buis K, Verhoeven R, et al.2011. A simple thermal mapping method for seasonal spatial patterns of groundwater-surface water interaction[J]. Journal of Hydrology, 397(1-2): 93-104. doi: 10.1016/j.jhydrol.2010.11.036
[28]	Anibas C, Fleckenstein J H, Volze N, et al.2009. Transient or steady-state? Using vertical temperature profiles to quantify groundwater-surface water exchange[J]. Hydrological Processes, 23(15): 2165-2177. doi: 10.1002/hyp.7289
[103]	Simpson S C, Meixner T.2012. Modeling effects of floods on streambed hydraulic conductivity and groundwater-surface water interactions[J]. Water Resources Research, 48(2): W02515.
[104]	Šimůnek J, van Genuchten M T.2008. Modeling nonequilibrium flow and transport processes using HYDRUS[J]. Vadose Zone Journal, 7(2): 782-797. doi: 10.2136/vzj2007.0074
[29]	Anibas C, Schneidewind U, Vandersteen G, et al.2016. From streambed temperature measurements to spatial-temporal flux quantification: Using the LPML method to study groundwater-surface water interaction[J]. Hydrological Processes, 30(2): 203-216. doi: 10.1002/hyp.10588
[30]	Brooks R H, Corey A T.1964. Hydraulic properties of porous media[R]. Hydrology papers. Fort Collins, Colorado: Colorado State University: 25.
[105]	Šimůnek J, van Genuchten M T, Šejna M.2008. Development and applications of the HYDRUS and STANMOD software packages and related codes[J]. Vadose Zone Journal, 7(2): 587-600. doi: 10.2136/vzj2007.0077
[106]	Šimůnek J, van Genuchten M T, Šejna M.2016. Recent developments and applications of the HYDRUS computer software packages[J]. Vadose Zone Journal, 15(7): 25. doi: 10.2136/vzj2016.04.0033
[31]	Brunner P, Cook P G, Simmons C T.2009. Hydrogeologic controls on disconnection between surface water and groundwater[J]. Water Resources Research, 45(1): W01422. doi: 10.1029/2008WR006953
[32]	Brunner P, Cook P G, Simmons C T.2011. Disconnected surface water and groundwater: From theory to practice[J]. Ground Water, 49(4): 460-467. doi: 10.1111/j.1745-6584.2010.00752.x pmid: 20849421
[107]	Song J X, Chen X H, Cheng C, et al.2009. Feasibility of grain-size analysis methods for determination of vertical hydraulic conductivity of streambeds[J]. Journal of Hydrology, 375(3-4): 428-437. doi: 10.1016/j.jhydrol.2009.06.043
[108]	Song J X, Chen X H, Cheng C.2010. Observation of bioturbation and hyporheic flux in streambeds[J]. Frontiers of Environmental Science & Engineering in China, 4(3): 340-348. doi: 10.1007/s11783-010-0233-y
[33]	Brunner P, Therrien R, Renard P, et al.2017. Advances in understanding river-groundwater interactions[J]. Reviews of Geophysics, 55(3): 818-854. doi: 10.1002/2017RG000556
[34]	Caissie D, Luce C H.2017. Quantifying streambed advection and conduction heat fluxes[J]. Water Resources Research, 53(2): 1595-1624. doi: 10.1002/2016WR019813
[109]	Tang Q, Kurtz W, Schilling O S, et al.2017. The influence of riverbed heterogeneity patterns on river-aquifer exchange fluxes under different connection regimes[J]. Journal of Hydrology, 554: 383-396. doi: 10.1016/j.jhydrol.2017.09.031
[110]	Tian Y, Zheng Y, Wu B, et al.2015. Modeling surface water-groundwater interaction in arid and semi-arid regions with intensive agriculture[J]. Environmental Modelling & Software, 63: 170-184. doi: 10.1016/j.envsoft.2014.10.011
[35]	Calver A.2001. Riverbed permeabilities: Information from pooled data[J]. Ground Water, 39(4): 546-553. doi: 10.1111/j.1745-6584.2001.tb02343.x pmid: 11447855
[36]	Chen W F, Huang C, Chang M, et al.2013. The impact of floods on infiltration rates in a disconnected stream[J]. Water Resources Research, 49(12): 7887-7899. doi: 10.1002/2013WR013762
[111]	Tian Y, Zheng Y, Zheng C M, et al.2015. Exploring scale-dependent ecohydrological responses in a large endorheic river basin through integrated surface water-groundwater modeling[J]. Water Resources Research, 51(6): 4065-4085. doi: 10.1002/2015WR016881
[112]	Tooth S.2000. Process, form and change in dryland rivers: A review of recent research[J]. Earth-Science Reviews, 51(1-4): 67-107. doi: 10.1016/S0012-8252(00)00014-3
[37]	Chen X H.2000. Measurement of streambed hydraulic conductivity and its anisotropy[J]. Environmental Geology, 39(12): 1317-1324. doi: 10.1007/s002540000172
[38]	Chen X H.2004. Streambed hydraulic conductivity for rivers in south-central Nebraska[J]. Journal of the American Water Resources Association, 40(3): 561-573. doi: 10.1111/j.1752-1688.2004.tb04443.x
[113]	Turner K W, Edwards T W D, Wolfe B B.2014. Characterising runoff generation processes in a lake-rich thermokarst landscape (Old Crow Flats, Yukon, Canada) using δ18O, δ2H and d-excess measurements[J]. Permafrost and Periglacial Processes, 25(1): 53-59. doi: 10.1002/ppp.v25.1
[114]	van Genuchten M T.1980. A closed-form equation for predicting the hydraulic conductivity of unsaturated soils[J]. Soil Science Society of America Journal, 44(5): 892-898. doi: 10.2136/sssaj1980.03615995004400050002x
[115]	Vandersteen G, Schneidewind U, Anibas C, et al.2015. Determining groundwater-surface water exchange from temperature-time series: Combining a local polynomial method with a maximum likelihood estimator[J]. Water Resources Research, 51(2): 922-939. doi: 10.1002/2014WR015994
[116]	Villeneuve S, Cook P G, Shanafield M, et al.2015. Groundwater recharge via infiltration through an ephemeral riverbed, central Australia[J]. Journal of Arid Environments, 117: 47-58. doi: 10.1016/j.jaridenv.2015.02.009
[117]	Vogt T, Schirmer M, Cirpka O A.2012. Investigating riparian groundwater flow close to a losing river using diurnal temperature oscillations at high vertical resolution[J]. Hydrology and Earth System Sciences, 16(2): 473-487. doi: 10.5194/hess-16-473-2012
[118]	Vogt T, Schneider P, Hahn-Woernle L, et al.2010. Estimation of seepage rates in a losing stream by means of fiber-optic high-resolution vertical temperature profiling[J]. Journal of Hydrology, 380(1-2): 154-164. doi: 10.1016/j.jhydrol.2009.10.033
[119]	Walvoord M A, Striegl R G.2007. Increased groundwater to stream discharge from permafrost thawing in the Yukon River basin: Potential impacts on lateral export of carbon and nitrogen[J]. Geophysical Research Letters, 34(12): L12402. doi: 10.1029/2007GL030216
[120]	Wang G X, Hu H C, Li T B.2009. The influence of freeze-thaw cycles of active soil layer on surface runoff in a permafrost watershed[J]. Journal of Hydrology, 375(3-4): 438-449. doi: 10.1016/j.jhydrol.2009.06.046
[121]	Wang P, Pozdniakov S P, Shestakov V M.2015. Optimum experimental design of a monitoring network for parameter identification at riverbank well fields[J]. Journal of Hydrology, 523: 531-541. doi: 10.1016/j.jhydrol.2015.02.004
[122]	Wang P, Pozdniakov S P, Vasilevskiy P Y.2017. Estimating groundwater-ephemeral stream exchange in hyper-arid environments: Field experiments and numerical simulations[J]. Journal of Hydrology, 555: 68-79. doi: 10.1016/j.jhydrol.2017.10.004
[123]	Wang P, Yu J J, Pozdniakov S P, et al.2014. Shallow groundwater dynamics and its driving forces in extremely arid areas: A case study of the lower Heihe River in northwestern China[J]. Hydrological Processes, 28(3): 1539-1553. doi: 10.1002/hyp.9682
[124]	Wang P, Yu J J, Zhang Y C, et al.2011. Impacts of environmental flow controls on the water table and groundwater chemistry in the Ejina Delta, northwestern China[J]. Environmental Earth Sciences, 64(1): 15-24. doi: 10.1007/s12665-010-0811-0
[125]	Wang P, Zhang Y C, Yu J J, et al.2011. Vegetation dynamics induced by groundwater fluctuations in the lower Heihe River Basin, northwestern China[J]. Journal of Plant Ecology, 4(1-2): 77-90. doi: 10.1093/jpe/rtr002
[126]	Wang W K, Dai Z X, Zhao Y Q, et al.2016. A quantitative analysis of hydraulic interaction processes in stream-aquifer systems[J]. Scientific Reports, 6: 19876. doi: 10.1038/srep19876 pmid: 4730216
[127]	Weber M D, Booth E G, Loheide S P.2013. Dynamic ice formation in channels as a driver for stream-aquifer interactions[J]. Geophysical Research Letters, 40(13): 3408-3412. doi: 10.1002/grl.50620
[128]	Wheater H S, Mathias S A, Li X.2010. Groundwater modelling in arid and semi-arid areas[M]. Cambridge, UK: Cambridge University Press.
[129]	Winter T C.1995. Recent advances in understanding the interaction of groundwater and surface water[J]. Reviews of Geophysics, 33(S2): 985-994. doi: 10.1029/95RG00115
[130]	Wu B, Zheng Y, Wu X, et al.2015. Optimizing water resources management in large river basins with integrated surface water-groundwater modeling: A surrogate-based approach[J]. Water Resources Research, 51(4): 2153-2173. doi: 10.1002/2014WR016653
[131]	Wu G D, Shu L C, Lu C P, et al.2015. Variations of streambed vertical hydraulic conductivity before and after a flood season[J]. Hydrogeology Journal, 23(7): 1603-1615. doi: 10.1007/s10040-015-1275-9
[132]	Xi H Y, Zhang L, Feng Q, et al.2015. The spatial heterogeneity of riverbed saturated permeability coefficient in the lower reaches of the Heihe River Basin, Northwest China[J]. Hydrological Processes, 29(23): 4891-4907. doi: 10.1002/hyp.10544
[133]	Xie Y Q, Cook P G, Brunner P, et al.2014. When can inverted water tables occur beneath streams[J]. Groundwater, 52(5): 769-774. doi: 10.1111/gwat.12109 pmid: 24032399
[134]	Yager R M.1993. Estimation of hydraulic conductivity of a riverbed and aquifer system on the Susquehanna River in Broome County, New York[R]. USGS water supply paper 2387. New York: U.S. Geological Survey.
[135]	Yao Y Y, Huang X, Liu J, et al.2015. Spatiotemporal variation of river temperature as a predictor of groundwater/surface-water interactions in an arid watershed in China[J]. Hydrogeology Journal, 23(5): 999-1007. doi: 10.1007/s10040-015-1265-y
[136]	Yao Y Y, Zheng C M, Liu J, et al.2015. Conceptual and numerical models for groundwater flow in an arid inland river basin[J]. Hydrological Processes, 29(6): 1480-1492. doi: 10.1002/hyp.10276
[137]	Yao Y Y, Zheng C M, Tian Y, et al.2015. Numerical modeling of regional groundwater flow in the Heihe River Basin, China: Advances and new insights[J]. Science China Earth Sciences, 58(1): 3-15. doi: 10.1007/s11430-014-5033-y
[138]	Zhang Y C, Yu J J, Wang P, et al.2011. Vegetation responses to integrated water management in the Ejina basin, northwest China[J]. Hydrological Processes, 25(22): 3448-3461. doi: 10.1002/hyp.8073