科尔沁沙地流动沙丘土壤水分空间变化特征分析

Spatial Variation of Soil Water Storage(SWS) on Active Dune in Horqin Sandy Land

应用地统计学原理，分析了科尔沁沙地流动沙丘不同部位和深度土壤水分的空间变化特点。结果表明，流动沙丘土壤水分空间分布呈现明显的空间异质性，土壤水分在流动沙丘的不同坡面和同坡面的不同区域呈现明显的不均匀分布特征，表层（0-40cm）和浅层（40-100cm）土壤水分是此空间差异的主要米源，其空间分布变异性明显高于深层（100—200cm）土壤：半方差分析结果也显示出表层和浅层土壤水分的空间异质性组成主要由随机因素引起，具有相对较小的变程，而深层土壤水分主要受到其自身土壤物理组成性质的影响，具有较强的空间白相关性，具有较大的变程，二者空间分布特点存在明显差异。流动沙丘土壤水分空间分布特点的明确，对阐述固沙先锋植物的侵入和定居格局具有现实的指导意义，也为人工同沙植被的建立提供理论指导。

A typical active dune in Horqin sandy land was selected as the study target and the spatial variation of soil water storage （SWS） at different depths was analyzed by semi-variograms analysis method on the base of full-scale sampling method. The research showed that SWS showed obvious spatial variation characteristics not only between different slops but also within the same slop, which could be attributed to the spatial variation of SWS of surface layer （0-40 cm） and shallow layer （40-100 cm）, which were significantly higher than the deep layer （100-200 cm）. The ranges of spatial heterogeneity of SWS of surface layer and shallow layers were lessee and were mainly resulted from stochastic factor, while SWS of deep layer was mainly affected by its physical structure, which had strong spatial dependence and higher variation range. It is practically significant to determine the pattern of SWS spatial variety of active dune in explaining the incursion and establishment pattern of pioneer plants for the establishment of manual sand stabilization.