详细信息
六盘山南侧华北落叶松人工林蒸腾对土壤水分和潜在蒸散的响应 被引量:14
Responses of transpiration to variation in evaporative demands and soil water in a larch plantation at the south side of Liupan Mountains,China
文献类型:期刊文献
中文题名:六盘山南侧华北落叶松人工林蒸腾对土壤水分和潜在蒸散的响应
英文题名:Responses of transpiration to variation in evaporative demands and soil water in a larch plantation at the south side of Liupan Mountains,China
作者:曹恭祥[1,2] 王云霓[1,2] 郭中[1] 季蒙[1] 王彦辉[2] 徐丽宏[2]
第一作者:曹恭祥
机构:[1]内蒙古自治区林业科学研究院,呼和浩特010010;[2]中国林业科学研究院森林生态环境与保护研究所,北京100091
年份:2020
卷号:31
期号:10
起止页码:3376-3384
中文期刊名:应用生态学报
外文期刊名:Chinese Journal of Applied Ecology
收录:CSTPCD;;Scopus;北大核心:【北大核心2017】;CSCD:【CSCD2019_2020】;PubMed;
基金:国家重点研发计划重点专项(2017YFC0506604);国家自然科学基金项目(41471029)资助。
语种:中文
中文关键词:林分蒸腾;液流;土壤水分;潜在蒸散
外文关键词:forest transpiration;sap flow;soil water content;potential evapotranspiration
分类号:S791.22
摘要:量化林分蒸腾对大气蒸发需求和土壤供水变化的响应能更好预测林分水分利用和水分循环特征并深化对林水关系的认识。本研究以六盘山南侧的香水河小流域的华北落叶松人工林为研究对象,采用热扩散探针法监测树干液流,同步测定环境因子,分析林分蒸腾对潜在蒸散和土壤体积含水率变化的响应关系。结果表明:林分蒸腾对土壤体积含水率变化响应的曲线在不同潜在蒸散水平下基本相似,即随土壤体积含水率增大,林分蒸腾先快速后缓慢增大,达到阈值后趋于平稳,该过程可用饱和指数增长函数得到较好的拟合;但土壤水分阈值存在差异,且阈值随潜在蒸散的升高而增大。林分日蒸腾量随潜在蒸散增加的变化遵循抛物线曲线,也存在阈值效应。采用连乘方式耦合了生长季中期林分蒸腾响应土壤体积含水率和潜在蒸散的关系,形成了同时考虑土壤供水能力和大气蒸发潜力影响的林分蒸腾模型,该模型能很好地估测蒸腾的日变化,可为人工林水分调控管理提供指导。
Quantifying the response of tree transpiration(T)to the variation of soil water supply capability and atmospheric evaporative demand is beneficial for a better prediction of water use and hydrological cycles in forests and deepen the understanding of the relationship between forest and water.Larix principis-rupprechtii in the Xiangshuihe watershed at the south side of Liupan Mountains was used as the research object.We simultaneously monitored sap flow density by thermal diffusion probe and the environmental factors.The response of the T to the soil volumetric water content(VWC)and potential evapotranspiration(PET)was analyzed.The results showed the response curve of T to VWC was quite similar under any different PET levels.With increasing VWC,T increased rapidly and then slowly,and began to be stable when VWC reached a threshold.This process could be well fitted by the saturated exponential function.However,the VWC threshold was different,and its value increased with rising PET.The relationship of daily T to PET was a quadra-tic equation,and PET also had a threshold effect.A stand transpiration model considering the effect of soil water supply capacity and atmospheric evaporative potential was founded which coupled the response relationship of T to PET and VWC in the rapid growth season.This model could well estimate the diurnal variation of transpiration,and provide guidance for the management of plantation water control.
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