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黑河上游山区土壤非饱和导水率测定及其估算——以排露沟流域为例
引用本文:唐振兴,何志斌,刘鹄. 黑河上游山区土壤非饱和导水率测定及其估算——以排露沟流域为例[J]. 生态学杂志, 2011, 30(1): 177-182
作者姓名:唐振兴  何志斌  刘鹄
作者单位:中国科学院寒区旱区环境与工程研究所中国生态系统研究网络临泽内陆河流域研究站,兰州,730000
基金项目:国家自然科学基金项目(30800147); 中国科学院“优秀博士学位论文、院长奖获得者科研启动专项资金”(Y020B41001)资助
摘    要:黑河上游山区土壤水分表现为非饱和特征,准确估算该区域表层土壤非饱和导水率(K10)可提高山区生态水文模型的可靠性.本研究野外测定了黑河上游排露沟流域的K10,并利用土壤传递函数(PTFs)以土壤机械组成、容重及土壤平均粒径作为分析因子进行模拟估算,结果表明:排露沟流域森林、草地、退耕裸地的K10均值分别为(0.21±0...

关 键 词:黑河上游山区  非饱和导水率  土壤传递函数

Observation and simulation of soil unsaturated hydraulic conductivity in mountain region of upper Heihe River: A case study of Pailugou catchment
TANG Zhen-xing,HE Zhi-bin,LIU Hu. Observation and simulation of soil unsaturated hydraulic conductivity in mountain region of upper Heihe River: A case study of Pailugou catchment[J]. Chinese Journal of Ecology, 2011, 30(1): 177-182
Authors:TANG Zhen-xing  HE Zhi-bin  LIU Hu
Affiliation:TANG Zhen-xing,HE Zhi-bin,LIU Hu(Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences,Linze Inland River Research Station,Chinese Ecosystem Network Research,Lanzhou 730000,China)
Abstract:In mountain region of upper Heihe River,the characteristic of soil water regime is of unsaturated,and thus,to accurately estimate the values of its topsoil unsaturated hydraulic conductivity (K10) is essential for eco-hydrological modeling. Taking the Pailugou catchment in upper Heihe River as a case,its topsoil K10 values were measured,and simulated by the pedotransfer functions (PTFs) integrating with factors-soil mechanical composition,bulk density,and average particle size. The observed K10 in forestlan...
Keywords:Upper Heihe River  hydraulic conductivity  pedotransfer function.  
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