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天然杨桦次生林表层土壤水分与枯落物的空间异质性

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枯落物作为水分调节的作用层,对森林生态系统的水分循环起着重要作用。采用地统计理论和方法对天然杨桦次生林的表层土壤水分和不同分解程度的枯落物空间异质性进行分析。结果表明,表层土壤水分、枯落物未分解层、半分解层和已分解层的空间变异均以指数理论模型的拟合效果较好,其结构比分别为88.3%,66.6%,89.2%和57.79%,未分解层和已分解层具有中等强度的空间相关性,表层土壤水分与半分解层具有强烈的空间相关性。分形维数显示表层土壤水分和枯落物层的空间分布格局无显著的各向异质性结构特征。从全方位的分形维数来看,表层土壤水分的分形维数为1.918;枯落物半分解层的分形维数最大,为1.967,明显与其他枯落物层不同;未分解和已分解层分形维数相对较小,分别为1.925和1.928。从空间分布格局来看,半分解层呈明显的斑块状分布,东-西和南-北方向均无明显差异;表层土壤水分、未分解层和已分解层空间分布较为连续,且具有相似性,空间分布在东-西方向上差异明显,南-北方向上差异较小。
Spatial Heterogeneity of Topsoil Moisture and Litter Lay in Natural Populus davidiana-Betula platyphylla Secondary Forests
Litter layer was an active layer of humidity control in forest ecosystem,it was important to hydrologic cycle of forest ecosystems.In the study,semivariance analysis of geostatistics was employed to quantify the spatial heterogeneity of topsoil moisture and litter layers of different degree of decomposition in natural Populus davidiana-Betula platyphylla secondary forests.The results showed that,the semivariograms of topsoil moisture,undecomposed,intermediate decomposed and decomposed litter layers were best described by exponential model,their structure ratio were 88.3 %,66.6%,89.2% and 57.79%.Undecomposed and decomposed litter layers had moderate spatial autocorrelation,while topsoil moisture and intermediate decomposed litter layer had strong spatial autocorrelation.Analyzing of fractal dimension of the 4 measured variables revealed that,spatial distribution pattern of topsoil moisture content and depth of litter layers had no remarkably anisotropic.From fractal dimension values,topsoil moisture was 1.981;intermediate decomposed litter layer had the highest value,which was 1.967.It was clearly apart from the other two litter lays.Fractal dimension of undecomposed and decomposed litter layers was 1.925 and 1.928.For spatial distribution pattern,intermediate decomposed layer was obviously fragmentized distributed,there were no remarkable differences in east-west and south-north directions.Topsoil moisture,undecomposed and decomposed litter layers had continuous spatial distribution.From different direction of distribution patterns,there were remarkable differences in east-west direction,while not obvious in north-south direction.

topsoil moisturelitter layerspatial heterogeneitygeostatistics

邵方丽、余新晓、杨志坚、王贺年

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北京林业大学水土保持与荒漠化防治教育部重点实验室,北京100083

表层土壤水分 枯落物 空间异质性 地统计学

林业公益性行业科研专项国家“十二五”科技支撑项目

2011040052011BAD38B05

2012

水土保持学报
中国土壤学会 中国科学院水利部水土保持研究所

水土保持学报

CSTPCDCSCD北大核心
影响因子:1.226
ISSN:1009-2242
年,卷(期):2012.26(3)
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