安徽六安市表层土壤有机碳的空间分布及尺度变异分析

    Spatial Distribution and Variability of Topsoil Organic Carbon Content at Different Scales in Lu′an City,Anhui Province,China

    • 摘要: 利用第2次全国土壤普查所获得的8236个实测样本资料,分析了安徽六安市不同空间尺度水平表土有机碳含量及其变异。结果表明,供试市域表土有机碳含量在不同空间尺度水平存在明显差异,总体范围4.58~60.38 g·kg-1,其变化基本符合正态分布。空间变异性表现为县级尺度最大,而乡镇尺度、市域尺度相对较小,说明空间尺度对表层土壤有机碳含量及其估算有重要影响。在不同土地利用类型中,表土有机碳含量均为非耕地土壤(13.99±2.19)g·kg-1>水田土壤(10.39±1.58)g·kg-1>旱地土壤(8.44±0.92)g·kg-1,其中非耕地土壤的空间变异性最大,变异系数达45.15%,水田土壤变异系数最小,为17.19%。在不同的地貌类型上表土有机碳平均含量表现为山地>丘陵>岗地>平原,变异系数表现为丘陵>山地>平原>岗地,显示出人类扰动对表土有机碳含量的明显影响。

       

      Abstract: Based on the field survey of 8 236 samples collected from Lu′an City for the Second National Soil Survey,different variation of spatial distribution of topsoil organic carbon content at different scales was studied.It turns out that organic carbon content varies in the tested soils dimensionally ranging from 4.58 to 60.38 g·kg-1,which basically conforms to normal distribution.Comparatively,this dimensional variability is more obvious at county scale than at village scale,town scale and city scale,which means the dimensional scale has a significant impact on organic carbon content in topsoil and its estimation.In terms of different land use patterns,organic carbon content in non-cultivated soil (13.99 ± 2.19) g·kg-1is notably higher than that in paddy soil (10.39 ± 1.58) g·kg-1which is then remarkably higher than that in dry soil (8.44 ± 0.92)g·kg-1.Moreover,non-cultivated soil boasts of the greatest dimensional variability with a variability index of 45.15%,much higher than that of paddy soil 17.19%,which is the lowest amongst the three land use patterns.In terms of different geomorphic types,the average content of organic carbon shows a tendency of mountainous region>hilly area>upland area>plain,the variability indexes displaying a tendency of hilly area>mountainous region>plain>upland area.These data suggest that human disturbance has exerted tangible influence on the topsoil organic carbon content.

       

    /

    返回文章
    返回