[1] 德罗斯特W, 莫泽尔H, 诺伊迈尔F, 等. 同位素方法在地下水水文学中的应用[M]. 张人权, 编译. 北京:地质出版社, 1983:4-80. Derluost W, Mozer H, Nowimair F, et al. Application of isotopes in groundwater hydrology[M]. Zhang Renquan, trans. Beijing:Geological Publishing House, 1983:4-80
[2] Clark I, Fritz P. Environmental isotopes in hydrogeology[M]. Boca Raton:CRC Press, 1997.
[3] Craig H. Isotopic variations in meteoric waters[J]. Science, 1961, 133:1702-1073.
[4] 吴华武, 章新平, 关华德, 等. 不同水汽来源对湖南长沙地区降水中δD,δ18O的影响[J]. 自然资源学报, 2012, 27(8):1404-1414. Wu Huawu, Zhang Xinping, Guan Huade, et al. Influences of different moisture sources on δD and δ18O in precipitation in Changsha, Hunan Province[J]. Journal of Natural Resources, 2012, 27(8):1404-1414.
[5] Kong Yanlong, Pang Zhonghe. Statistical analysis of stream discharge in response to climate change for Urumqi River catchment, Tianshan Mountains, central Asia[J]. Quaternary International, 2014:336:44-51
[6] 苏小四, 万玉玉, 董维红, 等. 马莲河河水与地下水的相互关系:水化学和同位素证据[J]. 吉林大学学报:地球科学版, 2009, 39(6):1087-1094. Su Xiaosi, Wan Yuyu, Dong Weihong, et al. Hydraulic relationship between Malianhe River and groundwater:hydrogeocheical and isotopic evidences[J]. Journal of Jinlin University:Earth Science Edition, 2009, 39(6):1087-1094.
[7] 马金珠, 黄天明, 丁贞玉, 等. 同位素指示的巴丹吉林沙漠南缘地下水补给来源[J]. 地球科学进展, 2007, 22(9):922-930. Ma Jinzhu, Huang Tianming, Ding Zhenyu, et al. Environmental isotopes as the indicators of the groundwater recharge in the South Badain Jaran Desert[J]. Advances in Earth Science, 2007, 22(9):922-930.
[8] 陈宗宇, 万力, 聂振龙, 等. 利用稳定同位素识别黑河流域地下水的补给来源[J]. 水文地质工程地质, 2006, 33(6):9-14. Chen Zongyu, Wan Li, Nie Zhenlong, et al. Indentification of groundwater recharge in the Heihe Basin using envrionmetal isotopes[J]. Hydrogeology & Engineering Geology, 2006, 33(6):9-14.
[9] Li Jie, Pang Zhonghe, Kong Yanlong, et al. Contrasting seasonal distribution of stable isotopes and deuterium excess in precipitation over China[J]. Fresenius Environmental Bulletin, 2014, 23(9):2074-2085.
[10] Kong Yanlong, Pang Zhonghe, Froehlich K. Quantifying recycled moisture fraction in precipitation of an arid region using deuterium excess[J/OL]. Tellus Series B-Chemical and Physical Meteorology, 2013, 65:19251, doi:10.3402/tellusb.v65i0.19251.
[11] Dansgaard W. Stable isotopes in precipitation[J]. Tellus, 1964, 16(4):436-468.
[12] Froehlich K, Gibson J, Aggarwal P. Deuterium excess in precipitation and its climatological significance[C]//Proceedings of Study of Environmental Change Using Isotope Techniques, Vienna:IAEA, 2002:54-65.
[13] Merlivat L, Jouzel J. Global climatic interpretation of the deuteriumoxygen 18 relationship for precipitation[J]. Journal of Geophysical Research, 1979, 84(C8):5029-5033.
[14] 庞忠和. 新疆水循环变化机理与水资源调蓄[J]. 第四纪研究, 2014, 34(5):907-917. Pang Zhonghe. Mechanism of water cycle changes and implications on water resources regulation in Xinjiang Uygur Autonomous Region[J]. Quaternary Sciences, 2014, 34(5):907-917.
[15] 刘斌, 陈旭光, 程强, 等. 准噶尔盆地天山北麓水文地质条件变化特征[J]. 新疆地质, 2011, 29(1):90-94. Liu Bin, Chen Xuguang, Cheng Qiang, et al. The changing charcteristic of hydrogeologicc condition in the southern areas of Junggar Basin (The northern piedont areas of the Tianshan Mountains)[J]. Xinjiang Geology, 2011, 29(1):90-94.
[16] Pang Zhonghe, Kong Yanlong, Froehlich K, et al. Processes affecting isotopes in precipitation of an arid region[J]. Tellus, 2011, 63B:352-359.
[17] Tian Lide, Yao tandong, MacClune K, et al. Stable isotopic variations in west China:A consideration of moisture sources[J/OL]. Journal of Geophysical Research-Atmospheres, 2007, 112(D10):doi:10.1029/2006JD007718.
[18] Li Jie, Pang Zhonghe, Froehlich K, et al. Paleo-environment from isotopes and hydrochemistry of groundwater in East Junggar Basin, Northwest China[J]. Journal of Hydrology, 2015, 529:650-661.
[19] Draxler R, Rolph G. 2003:HYSPLIT (HYBRID Single-Particle Lagrangian Integrated Trajectory) model[J/OL]. NOAA Air Resources Laboratory, 2013:www.arl.noaa.gov/ready/hysplit4.html.
[20] Breitenbach S F M, Adkins J F, Meyer H, et al. Strong influence of water vapor source dynamics on stable isotopes in precipitation observed in Southern Meghalaya, NE India[J]. Earth and Planetary Science Letters, 2010, 292:212-220.
[21] 李小飞, 张明军, 李亚举, 等. 西北干旱区降水中δ18O变化特征及其水汽输送[J]. 环境科学, 2012, 33(3):711-719 Li Xiaofei, Zhang Mingjun, Li Yaju, et al. Characteristic ofδ18O in precipitation and moisture transports over the arid region in Northwest China[J]. Environmental Science, 2012, 33(3):711-719.
[22] 柳鉴容, 宋献方, 袁国富, 等. 西北地区大气降水δ18O的特征及水汽来源[J]. 地理学报, 2008, 63(1):12-22. Liu Jianrong, Song Xianfang, Yuan Guofu, et al. Characteristics of δ18O in Precipitation over Northwest China and its water vapor sources[J]. Acta Geographica Sinica, 2008, 63(1):12-22.
[23] Aizen V B, Aizen E, Fujita K, et al. Stable-isotope time series and precipitation origin from firn-core and snow samples, Altai glaciers, Siberia[J]. Journal of Glaciology, 2005, 51(175):637-654.
[24] Kreutz K J, Wake C P, Aizen V B, et al. Seasonal deuterium excess in a Tien Shan ice core:Influence of moisture transport and recycling in Central Asia[J]. Geophysical Research Letters, 2003, 30(18):1922.
[25] Schotterer U, Fröhlich K, Gäggeler H, et al. Isotope records from Mongolian and Alpine ice cores as climate indicators[J]. Climatic Change, 1997, 36:519-530.
[26] Gonfiantini R. Environmental isotopes in lake studies[M]//Fritz P, Fontes J C, ed. Handbook of Environmental Isotope Geochemistry[M]. New York:Elsevier, 1986(3):113-168.
[27] Edmunds W, Ma J, Aeschbach-Hertig W, et al. Groundwater recharge history and hydrogeochemical evolution in the Minqin Basin, North West China[J]. Applied Geochemistry, 2006, 21(12):2148-2170.
[28] Chen Zongyu, Qi Jixiang, Xu Jianming, et al. Paleoclimatic interpretation of the past 30 ka from isotopic studies of the deep confined aquifer of the North China plain[J]. Applied Geochemistry, 2003, 18(7):997-1009.