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黑河中游绿洲区不同土地利用类型表层土壤水分空间变异的尺度效应
引用本文:郭德亮,樊军,米美霞.黑河中游绿洲区不同土地利用类型表层土壤水分空间变异的尺度效应[J].应用生态学报,2013,24(5):1199-1208.
作者姓名:郭德亮  樊军  米美霞
作者单位:(;1.西北农林科技大学资源环境学院, 陕西杨凌 712100; ;2.中国科学院/水利部水土保持研究所黄土高原土壤侵蚀与旱地农业国家重点实验室, 陕西杨凌 712100)
基金项目:国家自然科学基金项目(项目编号:91025018)
摘    要:了解表层土壤水分空间变异及其尺度效应,可获取土壤水分真实变异,并可为客观揭示土壤水分空间变异制定合理采样方案提供参考.用“再采样”方法对黑河中游张掖绿洲区林地和农地表层土壤水分空间变异的尺度性进行研究.结果表明: 研究区林地和农地表层土壤水分变异程度随土壤水分含量的增加而增加;变异系数随采样尺度的增大而更接近真实变异值.在干旱和湿润条件下,当采样幅度在一定范围内增大时,林地和农地土壤水分的变异系数、Moran I指数、块金值、基台值及林地变程均不断变大,而农地在干旱条件下的变程无固定变化规律.当采样密度在一定范围内增大时,块金值、变程不断增大,但变异系数、Moran I指数、基台值均不受影响.


关 键 词:表层土壤水分  尺度  采样幅度  采样密度  空间变异

Scale-dependency of spatial variability of surface soil moisture under different land use types in Heihe Oasis, China
GUO De-liang,FAN Jun,MI Mei-xia.Scale-dependency of spatial variability of surface soil moisture under different land use types in Heihe Oasis, China[J].Chinese Journal of Applied Ecology,2013,24(5):1199-1208.
Authors:GUO De-liang  FAN Jun  MI Mei-xia
Institution:(;1.College of Resources and Environment, Northwest A&F University, Yangling 712100, Shaanxi, China; ;State Key Laboratory of Soil Erosion and Dry land Farming on the Loess Plateau, Institute of Soil and Water Conservation, Chinese Academy of Sciences/Ministry of Water Resources, Yangling 712100, Shaanxi, China)
Abstract:To study the surface soil moisture spatial variability and its scale effect is of significance to understand the real variability of soil moisture and to objectively provide a reference for constructing a logical sampling scheme. By using “re-sampling” method, this paper studied the scale-dependency of the spatial variability of soil surface moisture in the woodland and farmland in the oasis ecological system in the middle reaches of Heihe River. The results showed that the variation degree of the surface soil moisture in the test woodland and farmland increased with increasing soil moisture content, and the coefficient of variation (CV) became closer to the true value when the sampling scale increased. Under both dry and moist conditions, and when the sampling amplitude increased within a definite range, the CV, Moran’s I index, nugget, and sill of soil moisture in the woodland and farmland as well as the variation range in the woodland all increased, while the variation range in the farmland under arid condition did not show a stable regular pattern. When the sampling density increased within a definite range, the nugget and variation range increased, but the CV, Moran’s I index, and sill showed less change.
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