[1]WANG Yixin,FENG Tianjiao,XIAO Huijie,et al.Characteristics of Sap Flow Rate of Nitraria tangutorum Under Drought Stress and Different Plant Height and Basal Diameter[J].Research of Soil and Water Conservation,2023,30(05):234-240,249.[doi:10.13869/j.cnki.rswc.2023.05.039.]
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Characteristics of Sap Flow Rate of Nitraria tangutorum Under Drought Stress and Different Plant Height and Basal Diameter

References:
[1] 赵晨光, 庞德胜. 阿拉善白刺生长季需水量估算[J]. 防护林科技, 2018(4):24-27.
[2] 袁得润,徐先英.民勤沙区6种防护树种液流特征及其生态需水量估算[J].甘肃科技,2010,26(17):172-175,150.
[3] 李清河,刘建锋,张景波,等.乌兰布和沙漠东北部8种沙生灌木生长季末期的光合生理特性[J].西北植物学报,2006,26(11):2318-2323.
[4] 孙慧珍,李夷平,王翠,等.不同木材结构树干液流对比研究[J].生态学杂志,2005,24(12):1434-1439.
[5] 乌日娜,丁国栋,吴斌,等.沙木蓼蒸腾耗水特性及环境影响因子研究[J].水土保持通报,2012,32(3):68-72.
[6] 姚小英,蒲金涌,王澄海,等.甘肃黄土高原40 a来土壤水分蒸散量变化特征[J].冰川冻土,2007(1):126-130.
[7] 于界芬.树木蒸腾耗水特点及解剖结构的研究[D].南京:南京林业大学,2003.
[8] 吕金林.黄土丘陵区两典型森林群落及主要建群种蒸腾耗水特征研究[D].陕西杨凌:中国科学院大学(中国科学院教育部水土保持与生态环境研究中心),2021.
[9] 温杰,陈云明,唐亚坤,等.黄土丘陵区油松、沙棘生长旺盛期树干液流密度特征及其影响因素[J].应用生态学报,2017,28(3):763-771.
[10] 徐军亮,马履一.土壤温度对油松(Pinustabulaeformis)树干液流活动的影响[J].生态学报,2008,28(12):6107-6112.
[11] 杨洁,吕金林,何秋月,等.黄土丘陵区辽东栎和刺槐树干液流时滞效应与蒸腾特征的关联性[J].应用生态学报,2019,30(8):2607-2613.
[12] 孙慧珍.东北东部山区主要树种树干液流动态及与环境因子关系[D].哈尔滨:东北林业大学,2002.
[13] 王慧梅,孙伟,祖元刚,等.不同环境因子对兴安落叶松树干液流的时滞效应复杂性及其综合影响[J].应用生态学报,2011,22(12):3109-3116.
[14] 孙鹏飞,周宏飞,李彦,等.古尔班通古特沙漠原生梭梭树干液流及耗水量[J].生态学报,2010,30(24):6901-6909.
[15] 徐利岗,杜历,汤英,等.干旱区枸杞蒸腾耗水变化特征及其影响因子响应分析[J].干旱区地理,2016,39(6):1282-1290.
[16] 罗凤敏,辛智鸣,高君亮,等.沙棘液流动态变化及影响因素分析[J].草业科学,2015,32(11):1871-1877.
[17] 夏永辉,梁凤超,师庆东,等.准噶尔西部人工碳汇林原生荒漠植被梭梭蒸腾耗水研究[J].安徽农业科学,2014,42(33):11755-11759.
[18] 岳广阳,张铜会,赵哈林,等.科尔沁沙地黄柳和小叶锦鸡儿茎流及蒸腾特征[J].生态学报,2006,26(10):3205-3213.
[19] 单立山,李毅,张希明,等.灌溉对3种荒漠植物蒸腾耗水特性的影响[J].生态学报,2012,32(18):5692-5702.
[20] 杨强.降雨对毛乌素沙地油蒿和沙柳蒸腾特性的影响[D].北京:北京林业大学,2016.
[21] 郝少荣,裴志永,段广东,等.不同时间尺度下环境因子与沙柳茎流关系的差异研究[J].干旱区资源与环境,2020,34(3):152-158.
[22] 李吉跃. 植物耐旱性及其机理[J]. 北京林业大学学报, 1991, 13(3): 92-100.
[23] Du S, Wang Y L, Kume T, et al. Sapflow characteristics and climatic responses in three forest species in the semiarid Loess Plateau region of China[J]. Agricultural and Forest Meteorology,2011,151(1):1-10.
[24] Ford C R, Goranson C E, Mitchell R J, et al. Diurnal and seasonal variability in the radial distribution of sap flow:predicting total stem flow in Pinus taeda trees[J]. Tree Physiology,2004,24(9):951-960.
[25] Meinzer F C, James S A, Goldstein G. Dynamics of transpiration, sap flow and use of stored water in tropical forest canopy trees[J]. Tree Physiology,2004,24(8):901-909.
[26] Campbell G S, Norman J M. An introduction to environmental biophysics(Second Edition)[M]. New York: Springer,1998.
[27] Granier A. Evaluation of transpiration in a Douglas-fir stand by means of sap flow measurements[J]. Tree Physiology,1987,3(4):309-320.
[28] 种培芳.荒漠植物红砂、白刺和沙拐枣抗旱指标及抗旱性综合评价研究[D].兰州:甘肃农业大学,2010.
[29] Kozlowski T T. Water deficit and plant growth. Vol. 1. Development, control and measurement[M]. New York, London: Academic Press,1968.
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