基金
准噶尔盆地南缘荒漠植被斑块状格局对土壤水分运移过程的响应机理
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参考文献
[1] 贾志清,卢琦,郭保贵,等.沙生植物-梭梭研究进展[J].林业科学研究,2004,17(1):125-132.
[2] 柴成武,徐先英,唐卫东,等.石羊河流域荒漠区主要固沙植物根系研究[J].西北林学院学报,2009,24(4):21-26.
[3] Xu G Q.Root distribution of three co-occurring desert shrubs and their physiological response to precipitation[J].寒旱区科学(SCIENCES IN COLD AND ARID REGIONS),2009,1(2):120-127.
[4] 杨文新,何新林,杨广,等.荒漠区柽柳液流特征及其与环境因子的关系研究[J].节水灌溉,2012(12):26-29.
[5] 曹晓明,陈曦,王卷乐,等.古尔班通古特沙漠南缘非灌溉条件下梭梭(Haloxylon ammodendron)蒸腾耗水特征[J].干旱区地理(汉文版),2013,36(2):292-302.
[6] Chai C W,Xian-Ying X U,Tang W D,et al.Root System of the Main Sand Fixing Plants in Desert Zone of Shiyanghe River Basin[J].Journal of Northwest Forestry University,2009,24(4):21-26.
[7] Manasi river basin management office.Manasi river water conservancy department in the Xinjiang Uygur Autonomous Region basin[R].Shihezi:Xinjiang records management everywhere in Manasi River Basin Management Office,2006.
[8] 容丽.喀斯特石漠化区植物水分适应机制的稳定同位素研究[D].北京:中国科学院地球化学研究所,2006,1-5.
[9] 伊力,赵良菊,等.黑河下游典型生态系统水分补给源及优势植物水分来源研究[J].冰川冻土,2012,24(6):1478-1486.
[10] 邓文平,余新晓,等.利用稳定氢氧同位素定量区分栓皮栎旱季水分来源的方法比较[J].应用基础与工程科学学报,2013,21(3):412-422.
[11] 龙翔,孙自永,等.黑河中游河岸带柽柳水分来源的18O同位素示踪研究[J].干旱区资源与环境,2014,28(7):150-155.
[12] Yang Q,Xiao H L,Zhao L J,et al.Stable isotope techniques in plant water sources:a review[J].寒旱区科学(SCIENCES IN COLD AND ARID REGIONS),2010,2(2):112-122.
[13] Benstead J P,March J G,Fry B,et al.Testing Isosource:Stable Isotope Analysis of a Tropical Fishery with Diverse Organic Matter Sources[J].Ecology,2008,87(2):326.
[14] 段德玉, 欧阳华.稳定氢氧同位素在定量区分植物水分利用来源中的应用[J].生态环境学报,2007,16(2):655-660.
[15] Ellsworth P Z,Williams D G. Hydrogen isotope fractionation during water uptake by wood xerophytes[J].Plant and Soil,2007,291(1):93-107.