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[1]ZHANG Yongwang,WAN Shanshan,WANG Jun,et al.Soil Water Deficit During Vegetation Succession on the Loess Plateau[J].Research of Soil and Water Conservation,2020,27(05):120-125,132.
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Soil Water Deficit During Vegetation Succession on the Loess Plateau

References:
[1]Legates D R, Mahmood R, Levia D, et al. Soil Moisture:A central and unifying theme in physical geography[J]. Progress in Physical Geography, 2011,35(1):65-86.
[2]邵明安,贾小旭,王云强,等.黄土高原土壤干层研究进展与展望[J].地球科学进展,2016,31(1):14-22.
[3]李小英,段争虎.黄土高原土壤水分与植被相互作用研究进展[J].土壤通报,2013,43(6):1508-1514.
[4]赵景波,祁子云,魏君平,等.青海湖北土壤水分分布与土壤干层恢复[J].地理科学进展,2012,31(7):853-858.
[5]王力,卫三平,吴发启.黄土丘陵沟壑区土壤水分环境及植被生长响应:以燕沟流域为例[J].生态学报,2009,29(3):1543-1553.
[6]卞莹莹,宋乃平,王兴,等.荒漠草原区不同土地利用方式下土壤水分相对亏缺[J].水土保持学报,2015,29(1):201-207.
[7]刘庚,牛俊杰,朱炜歆,等.晋西北黄土丘陵区人工林地土壤水分亏缺评价[J].水土保持通报,2015,35(5):309-314.
[8]Li Yan, Yehezkel C, Roni W, et al. On quantifying soil water deficit of a partially wetted root zone by the response of canopy or leaf conductnce[J]. Agricultural Water Management, 2004,65(1):21-38.
[9]Michelot A, Nathalie Breda, Damesin C, et al. Differing growth responses to climatic variations and soil water deficits of FagussylvatIca, Quercus petraea and Pinus sylvestris in a temperate forest[J]. Forest Ecology & Management, 2012,265(1):161-171.
[10]Raiio G, Provenzano G. Modelling eco-physiological response of table olive trees to soil water deficit conditions[J]. Agricultural Water Management, 2012,120(2):79-88.
[11]Mengistu D K. The influence of soil water deficit imposed during various developmental phases on physiological processes of tef[J]. Agriculture, Ecosystems & Environment, 2009,132(3/4):283-289.
[12]李军,陈兵,李小芳,等.黄土高原不同干旱类型区苜蓿地深层土壤干燥化效应[J].生态学报,2007,27(1):75-89.
[13]朱炜歆,牛俊杰,刘庚,等.植被类型对生长季黄土区土壤含水量的影响[J].干旱区资源与环境,2016,30(1):152-156.
[14]韦红波,李锐,杨勤科.我国植被水土保持功能研究进展[J].植物生态学报,2002,26(4):489-496.
[15]张平仓,郑粉莉.土壤侵蚀与生态环境演变[J].中国科学院水利部西北水土保持研究所集刊,1993,1(3):11-16.
[16]Wang Y, ming'an Shao, Shao H. A preliminary investigation of the dynamic characteristics of dried soil layers on the Loess Plateau of China[J]. Journal of Hydrology, 2010,381(1/2):9-17.
[17]杨磊,卫伟,莫保儒,等.半干旱黄土丘陵区不同人工植被恢复土壤水分的相对亏缺[J].生态学报,2011,31(11):3060-3068.
[18]高宇,樊军,彭小平,等.水蚀风蚀交错区典型植被土壤水分消耗和补充深度对比研究[J].生态学报,2013,34(23):7038-7046.
[19]Wang Y, Shao M, Liu Z, et al. Regional spatial pattern of deep soil water content and its influencing factors[J]. Hydrological Sciences Journal, 2012,57(2):265-281.
[20]Wang, Y, Liu, et al.. Vertical distribution and influencing factors of soil water content within 21-m profile on the Chinese Loess Plateau[J]. Geoderma, 2013,193:300-310.
[21]郭忠升.半干旱区柠条林利用土壤水分深度和耗水量[J].水土保持通报,2009,29(5):69-72.
[22]程积民,万惠娥,王静,等.黄土丘陵半干旱区天然草地土壤水分调控研究[J].草地学报,2003,11(4):296-300.
[23]陈洪松,邵明安,王克林.黄土区荒草地和裸地土壤水分的循环特征[J].应用生态学报,2005,16(10):1853-1857.
[24]王力,邵明安,王全九,等.黄土区土壤干化研究进展[J].农业工程学报,2004,20(5):27-31.
[25]Yang L, Wei W, Chen L, et al. Response of temporal variation of soil moisture to vegetation restoration in semi-arid Loess Plateau, China[J]. Catena, 2014,115:123-133.
[26]Yang L, Wei W, Chen L, et al. Response of deep soil moisture to land use and afforestation in the semi-arid Loess Plateau, China[J]. Journal of Hydrology, 2012,475:111-122.
[27]Satyanaga A, Rahardjo H, Leong E C, et al. Water characteristic curve of soil with bimodal grain-size distribution[J]. Computers & Geotechnics, 2013,48(3):51-61.
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