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作 者:赵东宁 姜洪源 徐生田 贾同飞 范春楠[3] 任飞燕[3] ZHAO Dongning;JIANG Hongyuan;XU Shengtian;JIA Tongfei;FAN Chunnan;REN Feiyan(Helong Forestry Bureau,Yanbian 133500,China;Changbai Mountains Forest Industry Group,Yanbian 133000,China;Forestry College of Beihua University,Jilin 132000,China)
机构地区:[1]和龙林业局,吉林延边133500 [2]长白山森工集团,吉林延边133000 [3]北华大学林学院,吉林吉林132000
出 处:《吉林林业科技》2021年第6期26-28,共3页Journal of Jilin Forestry Science and Technology
摘 要:通过观测我国东北东部天然次生林对降水的分配效应,结果表明:降雨量在1.69~24.36 mm时,森林各水文分配效应总体表现为穿透雨量>地表径流量>树干茎流量>林冠截留量。随降雨量和降雨强度的增加,穿透雨量、地表径流量和树干茎流量随之增大。当降雨量较小(1.69~4.91 mm)时,穿透雨量、地表径流量和树干茎流量随降雨量的增加呈低速增加趋势;当降雨量较大(4.91~24.36 mm)时,其增加速度随降雨量的增加而加快。The distribution effect of natural secondary forest on precipitation in the eastern part of Northeast China was observed.The hydrological distribution effect of the forest was generally showed that through fall>surface flow>stem flow>canopy interception with the rainfall in the range of 1.69-24.36 mm.The through fall,surface flow and stem flow increased with the increase of rainfall and rainfall intensity.With the rainfall in the range of 1.69-4.91 mm,they increased at the low speed with the increase of rainfall.With the rainfall in the range of 4.91-24.36 mm,the increase accelerated with the increase of rainfall.
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