Application of D and 18O stable isotopes in analyzing the water sources of different ages of Populus euphratica in the lower reaches of the Hei River
LIU Shu-bao1,3,CHEN Ya-ning2,LI Wei-hong2,CHEN Ya-peng2,REN Zhi-guo2
1 College of Pratacultural and Environmental Science Xinjiang Agricultural University, Urumqi 830052, Xinjiang, China; 2 State Key Laboratory of Desert and Oasis Ecology, Xinjiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, Xinjiang, China;3 Xinjiang Academy of Environmental Protection Science Research, Urumqi 830011, Xinjiang, China
LIU Shu-bao,CHEN Ya-ning,LI Wei-hong,CHEN Ya-peng,REN Zhi-guo. Application of D and 18O stable isotopes in analyzing the water sources of different ages of Populus euphratica in the lower reaches of the Hei River[J]., 2014, 37(5): 988-995.
[1] 冯起,司建华,李建林,等. 胡杨根系分布特征与根系吸水模型建立[J]. 地球科学进展,2008,23(7):765-772.[2] 杨玉海,陈亚宁,蔡柏岩,等. 极端干旱区胡杨根围丛枝菌根真菌的分离与鉴定[J]. 干旱区地理,2012,35(2):260-266.[3] 陈亚宁,李卫红,陈亚鹏,等. 新疆塔里木河下游断流河道输水与生态恢复[J]. 生态学报,2007,27(2):538-545.[4] 陈亚鹏,陈亚宁,徐长春,等. 塔里木河下游地下水埋深对胡杨气体交换和叶绿素荧光的影响[J]. 生态学报,2011,31(2):344-353.[5] 李建林,冯起,司建华. 极端干旱区胡杨吸水根系的分布与模拟研究[J]. 干旱区地理,2008,31(1):97-101.[6] 周辰昕,孙自永,余绍文. 黑河中游临泽地区沙丘植物水分来源的D、18O同位素示踪[J]. 地质科技情报,2011,30(9):102- 109.[7] 余绍文,孙自永,周爱国,等. D、18O同位素确定黑河中游戈壁地区植物水分来源[J]. 中国沙漠,2012,32(3):717-723.[8] 赵良菊,肖洪浪,程国栋,等. 黑河下游河岸林植物水分来源初步研究[J]. 地球学报,2008,29(6):709-718.[9] 陈亚宁,叶朝霞,毛晓辉,等. 新疆塔里木河断流趋势分析与减缓对策[J]. 干旱区地理,2009,32(6):813-819.[10] 陈亚宁,李卫红,陈亚鹏,等. 塔里木河下游断流河道输水的生态响应与生态修复[J]. 干旱区研究, 2006,23(4):521-530.[11] PHILLIPS D L,GREGG J W. Source partitioning using stable isotopes:coping with too many sources[J]. Oecologia, 2003,136,261-269.[12] DAWSON T E,EHLERINGER J R. Streamside trees that do not use steam water[J]. Nature,1991,350:335-337.[13] 章光新,何岩,邓伟. 同位素D与O在水环境中的应用研究进展[J]. 干旱区研究, 2004,21(3):225-229.[14] DAWSON T E,EHLERINGER J R. Isotopic enrichment of water in the “woody” tissues of plants:Implications for plant water sou- rce,water uptake, and other studies which use the stable isotopic composition of cellulose[J]. Geochimica et Cosmochimica Acta,1993,57(14):3487-3492.[15] 张应华,仵彦卿. 黑河流域大气降水水汽来源分析[J]. 干旱区地理,2008,31(3):403-408.[16] PHILLIPS D L. Mixing models in analysis of diet using multiple stable isotopes:a critique[J]. Oecologia, 2001,127:166-170.[17] ASBJORNSEN H,MORA G,HELMERS M J. Variation in water uptake dynamics among contrasting agricultural and native plant communities in the Midwestern US[J]. Agriculture,ecosystems & environment,2007,121(4):343-356.[18] BUSCH D E,INGRAHAM N L,SMITH S D. Water uptake in woody riparian phreaophytes of the southwestern United States:A stable isotope study[J]. Ecological Application,1992,2:450-459.[19] 朱雅娟,贾志清,卢琦,等. 乌兰布和沙漠5种灌木的水分利用策略[J]. 林业科学,2010,46(4):15-21.[20] 郜银梁,陈军锋,张成才,等. 黑河中游灌区水化学空间变异特征[J]. 干旱区地理,2011,34(6):575-582.[21] 苏永红,朱高峰,冯起,等. 额济纳盆地浅层地下水演化特征与滞留时间研究[J]. 干旱区地理,2009,32(4):544-551.[22] 赵文智,刘鹄. 荒漠区植被对地下水埋深响应研究进展[J]. 生态学报,2006,26(8):2702-2708.[23] 李晖,周宏飞. 稳定性同位素在干旱区生态水文过程中的应用特征及机理研究[J]. 干旱区地理,2006,29(6):800-816.[24] ZHAO Y,ZHAO C Y,XU Z L,et al. Physiological responses of Populus euphratica Oliv. to groundwater table variations in the lower reaches of Heihe River,Northwest China[J]. Journal of Arid Land,2012,4(3):281-291.[25] 李红寿,汪万福,柳本立,等. 用隔绝法对极干旱区土壤水分来源的分析[J]. 干旱区地理,2013,36(1):92-100.[26] NIE Y,CHEN H,WANG K,et al. Water source utilization by woody plants growing on dolomite outcrops and nearby soils during dry seasons in karst region of Southwest China[J]. Journal of Hydrology,2012,420:264-274.[27] MA Z G,CHEN X, WANG Q,et al. Retrieval of leaf biochemical properties by inversed PROSPECT model and hyperspectral indices:an aplication to [Populus euphratica] polymorphic leaves[J]. Journal of Arid Land,2012,4(1):52-62.[28] OVERDIECK D,ZICHE D,YU R D. Gas exchange of Populus euphratica leaves in a riparian zone[J]. Journal of Arid Land,2013:1-11.[29] LIU Y,XU Z,DUFFY R. Analyzing relationships among water uptake patterns,rootlet biomass distribution and soil water content profile in a subalpine shrubland using water isotopes[J]. European Journal of Soil Biology,2011,47(6):380-386.