黑土区典型小流域土壤物理特性空间分异及其与水土保持措施的关系

Spatial differentiation of soil physical properties and its relationship to soil and water conservation measures in the typical watershed of Mollisol region

  • 摘要: 土壤物理性质是评价土壤结构及功能的重要指标,探究水土保持措施对小流域土壤物理性质的影响,有助于为生态环境建设和防蚀措施布设提供理论依据。本研究以黑龙江省拜泉县通双小流域为对象,通过田间采样,选取土壤容重、土壤田间持水量、土壤饱和含水量、土壤水稳定性大团聚体含量(WR0.25)和平均重量直径(MWD)5种土壤物理性质,运用经典统计学、地统计学和信息熵等方法,分析土壤物理性质的空间分异特征,研究水土保持措施(梯田、等高垄作、乔木林、草地和灌木林)与土壤物理性质的相关性。研究结果表明:通双小流域表层土壤容重、田间持水量、饱和含水量和MWD属于中等变异,而土壤WR0.25属弱变异。各土壤物理性质具有中等强度的空间自相关性,在空间上呈斑块状或带状分布。信息熵结果表明,各土壤物理性质与水土保持措施间存在空间相关性,排序依次为土壤容重、土壤田间持水量/土壤饱和含水量、MWD和WR0.25。不同水土保持措施间土壤物理性质存在显著差异,乔木林的土壤容重显著高于梯田、等高垄作和灌木林,而土壤水分含量显著低于梯田、等高垄作和灌木林;草地的土壤WR0.25含量和MWD显著高于梯田和等高垄作。

     

    Abstract: Soil physical properties are the important indicators for evaluating soil structure and function. Exploring the effects of soil and water conservation measures on soil physical properties in small watersheds will be beneficial to provide a theoretical basis for the ecological environment construction and anti-erosion measures. In this study, Tongshuang small watershed in Baiquan County, Heilongjiang Province was selected as the research object. Five soil physical properties, including soil bulk density, soil field capacity, soil saturated water content, soil water stable macroaggregate content (WR0.25) and mean weight diameter (MWD), were selected through field sampling. The spatial differentiation characteristics of soil physical properties were analyzed by classical statistics, geostatistics and information entropy, and the correlation between soil and water conservation measures (terrace, contour ridge, forestland, grassland and shrubland) and soil physical properties was studied. The results showed that the surface soil bulk density, field capacity, saturated water content and MWD in Tongshuang small watershed were moderately variated, while soil WR0.25 was weakly variated. The soil physical properties were spatial autocorrelated moderately and exhibited patchy or banded distribution in space. The information entropy showed that there was a spatial correlation between soil physical properties and soil and water conservation measures, with the order of soil bulk density, soil field capacity / soil saturated water content, MWD and WR0.25. There were significant differences in soil physical properties among different soil and water conservation measures. The soil bulk density of arbor forest was significantly higher than that of terrace, contour ridge and shrubland; the soil moisture characteristics were significantly lower than that of terrace, contour ridge and shrubland; and the soil WR0.25 content and MWD of grassland were significantly higher than those of terrace and contour ridge.

     

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