文献类型：期刊文献

中文题名：宁夏六盘山水源区华山松次生林的生长季水量平衡与产流特征

英文题名：The characteristics of water budget and water yield of the Pinus armandii secondary forest in the waterhead area of Liupan Mountains,Northwest China

作者：杨丽丽[1,2] 邢元军[3] 王彦辉[2] 文仕知[1] 李振华[2]

第一作者：杨丽丽

机构：[1]中南林业科技大学林学院,长沙 410004;[2]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;[3]国家林业局中南林业调查规划设计院,长沙 410004

年份：2016

卷号：0

期号：8

起止页码：152-158

中文期刊名：干旱区资源与环境

外文期刊名：Journal of Arid Land Resources and Environment

收录：北大核心:【北大核心2014】；CSSCI:【CSSCI2014_2016】；CSCD:【CSCD_E2015_2016】；

基金：国家自然科学基金项目(41390461,41230852,41471029);中挪合作项目"Forest in south China:An important sink for reactive nitrogen and a regional hotspot for N2O?(209696/E10)";中南林业科技大学引进人才项目"六盘山典型森林的水文循环及其对碳,氮通量的影响";国家林业局宁夏六盘山森林生态站和宁夏回族自治区生态修复与多功能林业综合研究中心资助

语种：中文

中文关键词：森林水文;华山松林;水文过程;水量平衡;六盘山;产流特征

外文关键词：forest hydrology; Pinus armandii secondary forest; hydrologic process; water budget; Liupan Mountains ; water yield

分类号：S715

摘要：为揭示典型森林生态系统对水文过程和产流功能的调控机制,文中在宁夏六盘山区,选择了华山松次生林样地,观测了2011年生长季(5月24日至10月20日)的水文过程,分析了水量平衡与产流特征。结果表明:2011生长季总降水量为724.3mm;华山松林分冠层截留量(率)为102.3mm(14.13%);林下降水量(率)为622.0mm(85.87%);枯落物层渗漏水量(率)为424.3mm(58.59%);0-30cm土层渗漏水量(率)为275.9mm(38.09%)。华山松林的生长季总蒸散为477.1mm,各蒸散分量(mm)对总蒸散的贡献表现为林木蒸腾(222.9)>林下蒸散(151.9)>植被截持(102.3)。水量平衡计算表明,该年生长季降水量可充分满足华山松林蒸散耗水需要,林地产水量(0-30cm土层的净流出量)为252.7mm。
In order to reveal the regulatory mechanism of hydrological process and water yield in typical forest ecosystem, the representative stand of Pinus armandii secondary forest were selected in the Liupan Mountains, Ningxia in Northwest China. The observation of hydrological processes was carried out in the growing season of 2011 （May 24 to October 20）. The main characteristics of the water budget and water yield of the forest stands were analyzed. The main conclusions are described below. The gross precipitation in the growing season of 2011 amounted to 724.3mm. The canopy interception depth （rate） in the Pinus armandii secondary forest was 102. 3mm（14. 13% ）. The depth （rate） of rainfall under canopy was 622.0ram（85.87% ）. The leakage depth （rate） under humus layer was 424.3mm （58.59%）. The leakage depth （rate） under the 0 -30cm soil layer was 275.9mm（38.09% ）. According to the measurement, the evapotranspiration of Pinus armandii secondary forest was 477. lmm in growing season, the contribution of evapotranspiration components was in the order of： tree transpiration（222.9mm） 〉 floor evapotranspiration（151.9mm） 〉 canopy interception（102.3mm）. The calculation of water budget in growing season of 2011 indicated that the rainfall was sufficient to meet the demand of evapotranspiration in the Pinus armandii secondary forest stands studied. The water yield （i. e. , the net out- put from soil layer of 0 -30cm） performed as 252.7mm.