[1] 张应华,仵彦卿,温小虎,等.环境同位素在水循环研究中的应用[J].水科学进展,2006,17(5):738-747. [2] Sophocleous M.Interactions between groundwater and surface water:the state of the science[J].Hydrogeology Journal,2002,10(1):52-67. [3] 宋献方,夏军,于静洁,等.应用环境同位素技术研究华北典型流域水循环机理的展望[J].地理科学进展,2002,21(6):527-537. [4] Intaraprasong T,Zhan H.A general framework of stream-aquifer interaction caused by variable stream stages[J].Journal of Hydrology,2009,373(1/2):112-121. [5] Chen J Y,Tang C Y,Sakura Y,et al.Groundwater flow and geochemistry in the lower reaches of the Yellow River:a case study in Shandang Province,China[J].Hydrogeology Journal,2002,10(6):674-674. [6] Chen Z Y,Nie Z L,Zhang G H,et el.Environmental isotopic study on the recharge and residence time of groundwater in the Heihe River Basin,northwestern China[J].Hydrogeology Journal,2006,14(8):1635-1651. [7] Zhang J,Letolle R,Martin J M,et al.Stable oxygen isotope distribution in the Huanghe (Yellow River) and the Changjiang (Yangtze River) estuarine systems[J].Continental Shelf Research,1990,10(4):369-384. [8] Liu Y H,An S Q,Xu Z,et al.Spatio-temporal variation of stable isotopes of river waters,water source identification and water security in the Heishui Valley (China) during the dry-season[J].Hydrogeology Journal,2008,16(2):311-319. [9] Yao T D,Valerie M,Gao J,et al.A review of climatic controls on δ18O in precipitation over the Tibetan Plateau:Observations and simulations[J].Reviews of Geophysics,2013,51:525-548. [10] 张兵,宋献方,张应华,等.第二松花江流域地表水与地下水相互关系[J].水科学进展,2014,25(3):336-347. [11] Huang T M,Pang Z H.Changes in groundwater induced by water diversion in the Lower Tarim River,Xinjiang Uygur,NW China:evidence from environmental isotopes and water chemistry[J].Journal of Hydrology,2010,387(3/4):188-201. [12] Pang Z H,Huang T M,Chen Y N.Diminished groundwater recharge and circulation relative to degrading riparian vegetation in the middle Tarim River,Xinjiang Uygur,Western China[J].Hydrological Processes,2010,24(2):147-159. [13] Pang Z H,Kong Y L,Froehlich K,et al.Processes affecting isotopes in precipitation of an arid region[J].Tellus Series B:Chemical and Physical Meteorology,2011,63(3):352-359. [14] Wang Y,Chen Y N,Li W H.Temporal and spatial variation of water stable isotopes (18O and 2H) in the Kaidu River basin,Northwestern China[J].Hydrology Process,2014,28:653-661. [15] Wang P,Yu J J,Zhang Y C,et al.Groundwater recharge and hydrogeochemical evolution in the Ejina Basin,northwest China[J].Journal of Hydrology,2013,476:72-86. [16] 陈亚宁.中国西北干旱区水资源研究[M].北京:科学出版社,2014. [17] 范煜婷.塔里木河流域径流组分及特征研究[D].北京:中国科学院大学,2014. [18] 王荣军.基于环境同位素的融雪期径流分割——以天山北坡军塘湖流域为例[D].乌鲁木齐:新疆大学,2013. [19] 周海,郑新军,唐立松,等.盐生荒漠土壤水氧、氢同位素组成季节动态[J].中国沙漠,2014,34(1):162-169. [20] 姚俊强.干旱内陆河流域水资源供需平衡与管理[D].乌鲁木齐:新疆大学,2015. [21] Yuan F,Miyamoto S.Characteristics of oxygen-18 and deuterium composition in waters from the Pecos River in American Southwest[J].Chemical Geology,2008,255:220-230. |