[1] 邓世宗,韦炳式.不同森林类型林冠对大气降雨量再分配的研究[J].林业科学,1990,26(3):271-276.
[2] 梁文俊,丁国栋,臧荫桐,等.华北土石山区油松林对降雨再分配的影响[J].水土保持研究,2012,19(4):77-80.
[3] 余新晓,张志强,陈丽华,等.森林生态水文[M].北京:中国林业出版社,2004.
[4] 周彬,韩海荣,康峰峰,等.太岳山不同郁闭度油松人工林降水分配特征[J].生态学报,2013,33(5):1645-1653.
[5] 何常清,薛建辉,吴永波,等.岷江上游亚高山川滇高山栎林的降雨再分配[J].应用生态学报,2008,19(9):1871-1876.
[6] 孙忠林,王传宽,王兴昌,等.两种温带落叶阔叶林降雨再分配格局及其影响因子[J].生态学报,2014,34(14):3978-3986.
[7] 石磊,盛后财,满秀玲,等.兴安落叶松林降雨再分配及其穿透雨的空间异质性[J].南京林业大学学报:自然科学版,2017,41(2):90-96.
[8] 赵明扬,孙长忠,康磊.黄土高原油松人工林水文效应的人工神经网络模型[J].西南林业大学学报,2013,33(3):52-55,86.
[9] 高国龙,杜华强,韩凝,等.基于特征优选的面向对象毛竹林分布信息提取[J].林业科学,2016,52(9):77-85.
[10] 肖丽霞,萧江华,胡小松,等.中国竹产业现状和发展研究[J].世界竹藤通讯,2005,3(3):29-32.
[11] 陈双林,萧江华,薛建辉.竹林水文生态效应研究综述[J].林业科学研究,2004,17(3):399-404.
[12] 周本智,傅懋毅.庙山坞自然保护区毛竹林细根生产和周转研究[J].江西农业大学学报,2008,30(2):239-245.
[13] 王艳萍,王力,卫三平. Gash模型在黄土区人工刺槐林冠降雨截留研究中的应用[J].生态学报,2012,32(17):5445-5453.
[14] 张一平,王馨,王玉杰,等.西双版纳地区热带季节雨林与橡胶林林冠水文效应比较研究[J].生态学报,2003,23(12):2653-2665.
[15] 孙忠林,王传宽,王兴昌,等.两种温带落叶阔叶林降雨再分配格局及其影响因子[J].生态学报,2014,34(14):3978-3986.
[16] 刘章文,陈仁升,宋耀选,等.祁连山典型灌丛降雨截留特征[J].生态学报,2012,32(4):333-342.
[17] 胡珊珊,于静洁,胡堃,等.华北石质山区油松林对降水再分配过程的影响[J].生态学报,2010,30(7):1751-1757.
[18] Zhang Y, Wang X, Hu R, et al. Rainfall partitioning into throughfall, stemflow and interception loss by two xerophytic shrubs within a rain-fed re-vegetated desert ecosystem, northwestern China[J]. Journal of Hydrology, 2015,527:1084-1095.
[19] 王晓燕,毕华兴,高路博,等.晋西黄土区刺槐人工林林冠截留模拟[J].中国水土保持科学,2012,10(2):44-49.
[20] Zimmermann A, Germer S, Neill C, et al. Spatio-temporal patterns of throughfall and solute deposition in an open tropical rain forest[J]. Journal of Hydrology, 2008,360(1/4):87-102.
[21] Keim R F, Skaugset A E, Weiler M. Temporal persistence of spatial patterns in throughfall[J]. Journal of Hydrology, 2005,314(1/4):263-274.
[22] 盛后财,蔡体久,俞正祥.大兴安岭北部兴安落叶松(Larix gmelinii)林下穿透雨空间分布特征[J].生态学报,2016,36(19):6266-6273.
[23] Nanko K, Onda Y, Ito A, et al. Spatial variability of throughfall under a single tree:Experimental study of rainfall amount, raindrops, and kinetic energy[J]. Agricultural and Forest Meteorology, 2011,151(9):0-1182.
[24] Marin C T, Bouten W, Sevink J. Gross rainfall and its partitioning into throughfall, stemflow and evaporation of intercepted water in four forest ecosystems in western Amazonia[J]. Journal of Hydrology, 2000,237(1/2):40-57.
[25] 李道宁.江西省大岗山主要森林类型水源涵养功能研究[D].哈尔滨:东北林业大学,2014.
[26] 巩合德,王开运,杨万勤,等.川西亚高山原始云杉林内降雨分配研究[J].林业科学,2005,41(1):198-201.
[27] McJannet D, Vertessy R. Effects of thinning on wood production, leaf area index, transpiration and canopy interception of a plantation subject to drought[J]. Tree Physiology, 2001,21(12/13):1001-1008.
[28] Bulcock H H, Jewitt G P W. Spatial mapping of leaf area index using hyperspectral remote sensing for hydrological applications with a particular focus on canopy interception[J]. Hydrology and Earth System Sciences, 2010,14(2):383-392.
[1]李海防,史梅容,王金叶,等.广西猫儿山毛竹林不同层次土壤含水量的降雨响应[J].水土保持研究,2016,23(05):120.
LI Haifang,SHI Meirong,WANG Jinye,et al.Response of Soil Water Contents in Different Layers to Rainfall Under Phyllostachys pubescens Forest in Mao’ershan Mountain, Guangxi[J].Research of Soil and Water Conservation,2016,23(03):120.
[2]张锦娟,王冉,陆芳春,等.不同配置模式毛竹林水土流失特征[J].水土保持研究,2017,24(03):92.
ZHANG Jinjuan,WANG Ran,LU Fangchun,et al.Characteristics of Soil and Water Loss on Bamboo Forest Lands[J].Research of Soil and Water Conservation,2017,24(03):92.
[3]王意锟,金爱武,方升佐,等.浙西南不同经营强度下毛竹林土壤渗透性研究[J].水土保持研究,2015,22(02):41.
WANG Yikun,JIN Aiwu,FANG Shengzuo,et al.Soil Infiltration Characteristics of Phyllostachys edulis Forests with Different Management Intensities in Southwest Zhejiang[J].Research of Soil and Water Conservation,2015,22(03):41.
收稿日期:2019-07-08 修回日期:2019-07-22资助项目:国家重点研发计划项目“低效人工林增效与生态服务提升综合集成与示范”(2017YFC0505506)第一作者:杜妍(1995—),女(蒙古族),内蒙赤峰人,硕士研究生,从事森林水文与水土保持研究E-mail:1807814130@qq.com通信作者:庄家尧(1969—),男,安徽凤阳人,副教授,研究生导师,从事森林水文与水土保持研究E-mail:nlzjiayao@njfu.edu.cn