文献类型：期刊文献

中文题名：六盘山华北落叶松林和红桦林枯落物持水特征及其截持降雨过程

英文题名：The water-holding capacity of litter layers in the forests of Larix principis-rupprechtii and Betula albo-sinensis in Liupan Mountain and their rainfall interception process

作者：莫菲[1] 于澎涛[1] 王彦辉[1] 王晶[2] 熊伟[1] 徐丽宏[1]

第一作者：莫菲

机构：[1]中国林业科学研究院森林生态环境与保护研究所,国家林业局森林生态环境重点实验室,北京100091;[2]东北林业大学林学院,黑龙江哈尔滨150040

年份：2009

卷号：29

期号：6

起止页码：2868-2876

中文期刊名：生态学报

外文期刊名：Acta Ecologica Sinica

收录：CSTPCD;;Scopus;北大核心:【北大核心2008】；CSCD:【CSCD2011_2012】；

基金：国家自然科学基金资助项目(40730631,40671038,30671677);国家科技部“十一五”科技支撑计划资助项目(2006BAD03A1803);国家科技部科研院所社会公益研究专项资助项目(2004DIB3J102);国家林业局技术引进资助项目(2003-4-43)

语种：中文

中文关键词：六盘山;华北落叶松;红桦;枯落物;截持降雨;最大持水量

外文关键词：Liupan Mountain ; Larix principis-rupprechtii ; Betula albo-sinensis ; litter layer; rainfall interception ; water- holding capacity

分类号：Q142;Q948

摘要：在六盘山南坡野外调查了华北落叶松(Larixprincipis-rupprechtii)和红桦(Betula albo-sinensis)两个林分的枯落物数量特征,其厚度分别是3.6cm和4.0cm,储量为16.83t/hm2和9.04t/hm2。浸泡测定了单位重量(1.0kg/m2)枯落物的持水能力,华北落叶松林和红桦林的最大持水深分别是1.8mm和2.7mm。在六盘山地区自然雨强范围内(<30mm/h),利用模拟降雨研究了枯落物的截持降雨过程,表明枯落物持水能力随雨强增大而提高;在雨强为30mm/h时,华北落叶松林和红桦林枯落物(1.0kg/m2)的最大截持雨量为1.5mm和2.6mm,分别是浸泡测定持水能力的83.3%和96.2%,两种实验吸持水分的过程基本一致。分析表明,枯落物截持过程的吸水速率受其本身含水量大小的影响,同时构建了具有较好截持机制的枯落物截持降雨过程模型,并基于枯落物浸泡实验和模拟降雨截持实验的数据拟合了模型参数。
The quantitative characters of litter layer were investigated in the south side of Liupan Mountains of Northwest China for a larch （Larix principis-rupprechtii） and birch （Betula albo-sinensis） stand. The thickness of litter layer of the larch and birch forest was 3.6 cm and 4.0 cm, and their corresponding weight was 16.83 t/hm^2 and 9.04 t/hm^2 respectively. The water-holding capacity of unit weight of litter （1.0 kg/m^2） measured by a soaking method was 1.8 mm for larch and 2.7 mm for birch. The rainfall interception process was studied under simulated rainfall within the normal rainfall intensity range of this region （〈 30 mm/h）. It showed that the interception capacity of litter increased with rainfall intensity. The maximum depth of interception of unit weight of litter （1.0 kg/m^2） under the rainfall intensity of 30 mm/h was 1.5 mm for larch and 2.6 mm for birch, accounting for only 83.3% and 96.2% of the water-holding capacity determined by soaking method. However, the water soak-up processes in the two different experiments were essentially consistent with each other. The water absorption rate of litter was influenced by its moisture condition. A mechanism based model for describing the rainfall interception process of litter of the two tree species was developed, and the model parameters were fitted based on the measured data both from the soaking experiment and simulated rainfall interception experiments.