• ISSN 1008-505X
  • CN 11-3996/S
李子忠, 龚元石. 不同尺度下田间土壤水分和混合电导率空间变异性与套合结构模型[J]. 植物营养与肥料学报, 2001, 7(3): 255-261. DOI: 10.11674/zwyf.2001.0303
引用本文: 李子忠, 龚元石. 不同尺度下田间土壤水分和混合电导率空间变异性与套合结构模型[J]. 植物营养与肥料学报, 2001, 7(3): 255-261. DOI: 10.11674/zwyf.2001.0303
LI Zi zhong, GONG Yuan shi. Spatial variability of soil water content and electrical conductivity in field for different sampling scales and their nested models[J]. Journal of Plant Nutrition and Fertilizers, 2001, 7(3): 255-261. DOI: 10.11674/zwyf.2001.0303
Citation: LI Zi zhong, GONG Yuan shi. Spatial variability of soil water content and electrical conductivity in field for different sampling scales and their nested models[J]. Journal of Plant Nutrition and Fertilizers, 2001, 7(3): 255-261. DOI: 10.11674/zwyf.2001.0303

不同尺度下田间土壤水分和混合电导率空间变异性与套合结构模型

Spatial variability of soil water content and electrical conductivity in field for different sampling scales and their nested models

  • 摘要: 应用地统计学原理和方法 ,分析了夏玉米田间 90m90m(L区 ) ,内套一个 30m 30m(M区) ,再内套一个 10m 10m(S区 ) 3个尺度下土壤含水量和电导率的空间变异性。结果表明 ,各尺度间土壤含水量的标准差和变异系数比较接近而电导率的差别较大。在L和M尺度下土壤含水量在 3个置信度下呈正态或对数正态分布 ,在S尺度下只在 0.01置信度下呈对数正态分布 ;在L尺度下土壤电导率仅在信度为 0.05和0.01时呈对数正态分布 ,在M尺度下仅在信度为 0.01时正态或对数正态分布 ,较高信度时呈对数正态分布 ,在S尺度下不呈正态或对数正态分布。各尺度下它们的空间结构可用球状模型描述 ,其变程分别约为 2.2~19.8m(土壤含水量 )和 2.5~17.2m(电导率 ) ,不同尺度间土壤含水量和电导率的空间变异结构函数差别较大 ,用套合结构模型能更好地描述不同尺度下土壤含水量和电导率的空间变异性。

     

    Abstract: Using geostatistics, spatial variability of soil water content and bulk soil electrical conductivity was analyzed in the L (90m90m), M(30m30m, nested in the L ) and S(10m10m, nested in the M ) area of summer maize fields The results indicated that, no significant differences were in the standard error and coefficient of variation (CV%) of soil water content among the different scales, but such differences were in bulk soil electrical conductivity Water content was distributed normally or log normally in L and M, but it was only distributed log normally for 0.01 confidence level in S area Electrical conductivity was not distributed normally or log normally in S, but it was distributed normally or log normally for 0.01 confidence level, log normally for higher confidence levels in M, and log normally for 0.05 and 0.01 confidence levels in L area Semivariograms showed spherical models with the range of 2.2~19.8m and 2.5~17.2m for water content and electrical conductivity among different scales And it was suggested that nested models should be created when significant differences were showed among the models of different scales In addition, nested models were used to describe the spatial variability of soil water content and electrical conductivity among the different scales

     

/

返回文章
返回