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作 者:岳燕杰 杨坤[2] 张泽光 杨新兵[2] 高琛[2]
机构地区:[1]张家口市林业调查规划院,河北张家口075000 [2]河北农业大学,河北保定071000 [3]河北省塞罕坝机械林场总场,河北围场068466
出 处:《河北林果研究》2016年第1期13-16,共4页Hebei Journal of Forestry and Orchard Research
基 金:河北省林业厅科技项目"冀北山区森林生态系统健康评价技术研究"(1403451);林业公益性行业科研专项子课题"冀北山区典型森林生态系统健康经营技术研究与示范"(200804022F)
摘 要:以华北落叶松桦木混交林、山杨桦木混交林和油松蒙古栎混交林为研究对象,分别对其6~9月间的土壤含水量动态变化实时监测,结果表明:华北落叶松桦木混交林、山杨桦木混交林和油松蒙古栎混交林土壤含水量变动范围分别为5.67%~15.43%、7.10%~24.23%、2.25%~14.57%,土壤水分调节层分别在50cm、20cm、30cm,土壤蒸发总量分别为43.1cm、38.1cm、50.2cm;3种林地7月份土壤蒸发量最大,导致土壤含水量最低。The Larix principis-rupprechtii and Betula spp.,the Populus davidiana and Betulaspp.mix-forest,the Pinus tabulae formis and Quercus mongolia mix-forest were used as the research object,and their dynamic changes of soil moisture content were monitored respectively during June to September.The results showed that for the Larix principis-rupprechtii and Betula mix-forest,the Populus davidiana and Betulaspp.mix-forest,the Pinus tabulaeformis and Quercus mongolia mix-forest,their moisture contents in soil were5.67%to 15.43%,7.10%to 24.23% and 2.25%to 14.57%;the soil moisture adjustment layer were 50 cm,20cm,30 cm respectively;total soil evaporation were 43.1cm,38.1cm,50.2cm respectively.The three types of woodland had the largest soil evaporation in July,leading to the lowest soil moisture content.
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