[1] CRUZ VJ, FIGUEIRAC, PRADAS. Using stable isotopes to characterize groundwater recharge sources in the volcanic island of Madeira, Portugal[J]. Journal of Hydrology, 536, 409-425(2016).
[2] WOESSNER WW. Stream and fluvial plain ground water interactions: Rescaling hydrogeologic thought[J]. Ground Water, 38, 423-429(2000).
[3] HARVEY JW, KRUPA SL, NEWLIN JT. Modeling decadal timescale interactions between surface water and ground water in the Central Everglades, Florida, USA[J]. Journal of Hydrology, 320, 400-420(2006).
[4] WINTER TC. Relation of streams, lakes, and wetlands to groundwater flow systems[J]. Hydrogeology Journal, 7, 28-45(1999).
[5] MONTOYA AM, OBEVSEKERAJ, RESTREPO JI. A wetland simulation module for the MODFLOW ground water model[J]. Ground Water, 36, 764-770(1998).
[6] BRUEN MP, OSMAN YZ. Modelling stream-aquifer seepage in an alluvial aquifer: An improved loosing-stream package for modflow[J]. Journal of Hydrology, 264, 69-86(2002).
[7] KALBUSE, MOLSON JW, SCHMIDTC et al. Influence of aquifer and streambed heterogeneity on the distribution of groundwater discharge[J]. Hydrology and Earth System Sciences, 13, 69-77(2009).
[8] CARDENAS MB, WILSON JL, ZLONTNIK VA. Impact of heterogeneity, bed forms, and stream curvature on subchannel hyporheic exchange[J]. Water Resources Research, 40, W08307(2004).
[9] CARDENAS MB. Stream-aquifer interactions and hyporheic exchange in gaining and losing sinuous streams[J]. Water Resources Research, 45, W06429(2009).
[10] BLASCHKE AP, BLOSCHLG, DERXJ. Three-dimensional flow patterns at the river-aquifer interface: A case study at the Danube[J]. Advances in Water Resources, 33, 1375-1387(2010).
[11] CHENL, WANG GX, YANG LY et al. Impacts of land use changes on groundwater resources in the Heihe River Basin[J]. Journal of Geographical Sciences, 15, 405-414(2005).
[12] 刘悦忆, 章树安, 朱金峰, LIU YY, ZHANG SA, ZHU JF et al. Review on the research of surface water and groundwater interactions[J]. China Environmental Science, 37, 3002-3010(2017).
[13] KALBUSE, RENINSTORFF, SCHIRMERM. Measuring methods for groundwater-surface water interactions: A review[J]. Hydrology and Earth System Sciences, 10, 873-887(2006).
[14] BAYER-RAICHM, SCHINMERM, SCHMIDTC. Characterization of spatial heterogeneity of groundwater-stream water interactions using multiple depth streambed temperature measurements at the reach scale[J]. Hydrology and Earth System Sciences Discussions, 3, 1419-1446(2006).
[15] 李广, 姚天次, 章新平, LIG, YAO TC, ZHANG XP et al. Characteristics of the stable isotopes in different water bodies and relationships in surrounding areas of Yuelu Mountain in the Xiangjiang River Basin[J]. Journal of Natural Resources, 31, 1198-1210(2016).
[16] LIAOF, WANG GC, ZHAOD et al. Groundwater-surface water interactions derived by hydrochemical and isotopic (222Rn, deuterium, oxygen-18) tracers in the Nomhon Area, Qaidam Basin, NW China[J]. Journal of Hydrology, 565, 650-661(2018).
[17] 迟宝明, 谷洪彪, 王贺, CHI BM, GU HB, WANGH et al. Relationship between surface water and groundwater in the Liujiang Basin hydrochemical constrains[J]. Progress in Geography, 32, 789-799(2017).
[18] CUI BL, LIX Y. Stable isotopes reveal sources of precipitation in the Qinghai Lake Basin of the Northeastern Tibetan Plateau[J]. Science of the Total Environment, 527-528, 26-37(2015).
[19] 曹广超, 曹生奎, 陈克龙, CAO GC, CAO SK, CHEN KL et al. Characteristics of soil carbon density distribution of the Kobresia humilis meadow in the Qinghai Lake Basin[J]. Acta Ecologica Sinica, 34, 482-490(2014).
[20] 金章东, 石岳威, 张飞, JIN ZD, SHI YW, ZHANGF. Sources of shallow groundwater recharge and changes of water level in Qinghai Lake Basin[J]. Journal of Earth Environment, 1, 169-174(2010).
[21] JIN ZD, XIAOJ, ZHANGF. Geochemical and isotopic characteristics of shallow groundwater within the Lake Qinghai Catchment, NE Tibetan Plateau[J]. Quaternary International, 313-314, 62-67(2013).
[22] 崔步礼, CUI BL. Study on the relationship between water cycle and water quantity conversion in Qinghai Lake Basin based on hydrogen and oxygen stable isotope[J]. Beijing: Beijing Normal University, 16-18(2011).
[23] 曹生奎, 冯起, 杨羽帆, CAO SK, FENGQ, YANG YF et al. Spatial distribution characteristics of composition of stable hydrogen and oxygen isotopes of shallow groundwater in Shaliu River Basin of Qinghai Lake[J]. Journal of Desert Research, 1-9(2019).
[24] CUI BL, LIX Y. Runoff processes in the Qinghai Lake Basin, Northeast Qinghai-Tibet Plateau, China: Insights from stable isotope and hydrochemistry[J]. Quaternary International, 380-381, 123-132(2015).
[25] . Gangcha County, 95-97(1998).
[26] GUO QL, HAN YY, YANG YS et al. Assessment of surface-groundwater interactions using hydrochemical and isotopictechniques in a coalmine watershed, NW China[J]. Environmental Earth Sciences, 3, 78-91(2019).
[27] LIU ZH, RAO WB, TAN HB et al. Stable isotopes of soil water: Implications for soil water and shallow groundwater recharge in hill and gully regions of the Loess Plateau, China[J]. Agriculture, Ecosystems and Environment, 243, 1-9(2017).
[28] 顾慰祖, GUW Z. Isotope Hydrology, 145-147(2011).
[29] WANGW, WUT, ZHAOL et al. Exploring the ground ice recharge near permafrost table on the Central Qinghai-Tibet Plateau using chemical and isotopic data[J]. Journal of Hydrology, 560, 220-229(2018).
[30] 李小雁, 吴华武, 赵国琴, LI XY, WU HW, ZHAO GQ et al. Variation characteristics of δ18O and δD in precipitation and river water of Qinghai Lake Basin[J]. Journal of Natural Resources, 29, 1552-1564(2014).
