[1] PRADAS, FIGUEIRAC, CRUZ VJ. 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, NEWLIN JT, KRUPA SL. 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] RESTREPO JI, OBEVSEKERAJ, MONTOYA AM. 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] MOLSON JW, SCHMIDTC, KALBUSE 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] DERXJ, BLOSCHLG, BLASCHKE AP. 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, YANG LY, WANG GX 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] 朱金峰, LIU YY, ZHU JF, ZHANG SA, 章树安, 刘悦忆 et al. Review on the research of surface water and groundwater interactions[J]. China Environmental Science, 37, 3002-3010(2017).
[13] KALBUSE, SCHIRMERM, RENINSTORFF. 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] 章新平, YAO TC, ZHANG XP, 姚天次, LIG, 李广 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] ZHAOD, LIAOF, WANG GC 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] 谷洪彪, 迟宝明, CHI BM, GU HB, WANGH, 王贺 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] CAO GC, 曹生奎, CAO SK, 曹广超, CHEN KL, 陈克龙 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] 石岳威, 张飞, SHI YW, JIN ZD, ZHANGF, 金章东. 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] CAO SK, 杨羽帆, 冯起, FENGQ, 曹生奎, 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] LIX Y, CUI BL. 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] YANG YS, HAN YY, GUO QL 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] TAN HB, RAO WB, LIU ZH 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] WUT, ZHAOL, WANGW 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, LI XY, 赵国琴, 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).
