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作 者:彭舜磊[1,2] 由文辉[1] 王强[1] 蒋跃[1] 余华光[1]
机构地区:[1]平顶山学院低山丘陵区生态修复重点实验室,河南平顶山467000 [2]华东师范大学生态与环境科学学院,上海200241
出 处:《水土保持研究》2016年第3期274-277,共4页Research of Soil and Water Conservation
基 金:高等学校博士学科点科研专项基金"台风暴雨对我国东部沿海常绿阔叶林水文过程的影响"(20090076110021);中国博士后科学基金"台风对天童常绿阔叶林养分迁移的影响"(2014M561043)
摘 要:植物冠层叶片存在稳定性碳同位素贫化效应,反映了冠层光合能力的异质性。通过测试不同月份栲树冠层冠顶至冠下8m叶片δ^(13) C及叶片最大光合速率(A_(max))和单位质量叶片氮含量(N_(mass)),分析了冠层叶片δ^(13) C的时空分布特征及其与A_(max)和N_(mass)的相关关系,验证树高极限的水力限制假说。结果表明:不同月份和冠层高度对冠层叶片δ^(13) C存在极为显著的影响(p<0.01),从冠顶到冠下8m叶片δ^(13) C平均值的变化范围为-28.61‰^-31.67‰,冠层叶片δ^(13) C随冠层高度降低呈线性极为显著减小(R^2=0.727,p<0.001);冠层叶片δ^(13) C随A_(max)和N_(mass)的增大而增大,呈极为显著的对数曲线关系(R^2=0.514,R^2=0.610,p<0.000 1),不支持树高极限的水力限制假说。Leaf carbon isotopic depletion exists in plant canopy,which indicates the photosynthetic heterogeneity of canopy.In order to study the temporal and spatial changes of leafδ-(13) C along canopy vertical gradient,and test whether the hypothesis of tree height limit from hydraulic limitation is true in the Castanopsis fargesii,the values of leafδ-(13)C,maximum assimilation rate(A_(max)),and leaf nitrogen content per unit mass(N_(mass))were measured from crown to 8mcrown below in different months.The results showed that the different months and canopy heights significantly affected on canopy leafδ-(13) C(p0.01).The mean value of leafδ-(13)C ranged from-28.61‰to-31.67‰ along canopy vertical gradients from crown to 8mcrown below,and significantly linearly decreased with the decrease of canopy heights(R-2=0.727,p0.001).Canopy leafδ-(13)C significantly increased with the increase of A_(max)and N_(mass)(p0.000 1),and their relationship followed the logarithmic curve very well(R-2=0.514 for A_(max),and R-2=0.610 for N_(mass)),which proved that the hypothesis of tree height limit from hydraulic limitation seems to be unlikely in the Castanopsis fargesii.
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