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控制华北地区油松人工林穿透雨的因素。

Factors controlling throughfall in a Pinus tabulaeformis forest in North China.

机构信息

School of Soil and Water Conservation, Beijing Forestry University, Beijing, 100083, China.

Key Laboratory of State Forestry Administration on Soil and Water Conservation (Beijing Forestry University), 100083, Beijing, China.

出版信息

Sci Rep. 2017 Oct 25;7(1):14060. doi: 10.1038/s41598-017-14464-z.

Abstract

The factors that control throughfall in Pinus tabulaeformis plantations were investigated using linear and curve analyses based on direct measurements of rainfall, throughfall and stemflow from 36 rainfall events. The results showed the following: (1) there was significant spatial heterogeneity in throughfall rates in P. tabulaeformis plots; (2) the throughfall rate increased with increasing rainfall; and (3) the rate of increase gradually decreased. When rainfall reached approximately 25 mm, the throughfall rate stabilized. The coefficient of variation of the throughfall rate decreased with increasing rainfall, with a peak at approximately 10 mm of rainfall. The coefficient of variation of throughfall stabilized at 20%, and the coefficient of variation of the throughfall rate stabilized at 17%. A linear regression equation (R = 0.76) was derived by fitting the P. tabulaeformis average diameter at breast height (DBH), average tree height, average branch height, stand density, canopy thickness, canopy density, and the rainfall and throughfall rate. A highly positive correlation was found between the throughfall rate, canopy density, rainfall class and tree height (P < 0.01). By establishing a quadratic response surface model of the stand structure indicators and the throughfall rate, R was increased to 0.85 (P < 0.01). The quadratic regression analysis demonstrated a highly positive correlation between throughfall rate, canopy density and rainfall class.

摘要

利用 36 次降雨事件的直接降雨量、穿透雨和树干流测量数据,采用线性和曲线分析方法,研究了控制油松人工林穿透雨的因素。结果表明:(1)油松林分穿透雨率存在显著的空间异质性;(2)穿透雨率随降雨量的增加而增加;(3)增加速率逐渐减小。当降雨量达到约 25mm 时,穿透雨率趋于稳定。穿透雨率的变异系数随降雨量的增加而减小,在降雨量约 10mm 时达到峰值。穿透雨率的变异系数稳定在 20%,穿透雨率的变异系数稳定在 17%。通过拟合油松林平均胸径(DBH)、平均树高、平均枝高、林分密度、冠层厚度、冠层密度、降雨量和穿透雨率,得出了一个线性回归方程(R=0.76)。穿透雨率与冠层密度、降雨量等级和树高呈高度正相关(P<0.01)。通过建立林分结构指标与穿透雨率的二次响应面模型,R 提高到 0.85(P<0.01)。二次回归分析表明,穿透雨率、冠层密度和降雨量等级之间呈高度正相关。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/6edb/5656610/e47bbb9d8b3d/41598_2017_14464_Fig1_HTML.jpg

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