陕西省水蚀土壤因子指标插值方法比较研究
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国家重点基础研究发展计划(2007CB407203)


Comparison of Spatial Interpolation Methods for Soil Variables of Regional Water Erosion Assessment in Shaanxi Province
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    摘要:

    基于地统计学原理和半变异理论,采用地理信息系统技术定量研究了陕西省水蚀土壤因子指标的空间变异特征。分析比较了反距离权重法、样条函数法与普通克吕格法对陕西省土壤因子指标空间插值的精度。结果表明,研究区土壤抗冲系数具有中等强度的空间相关性,块金系数为32.29%,而稳渗速率、崩解速率、抗剪强度均表现为强烈的空间相关性,块金系数分别为13.19%,11.61%和12.98%。综合考虑平均相对误差、均方差及插值效果,认为普通克吕格法最好,更能反映土壤参数的空间特征并符合区域水土流失模型对数据的要求。对于普通克吕格法,稳渗速率的Lag步长为30 000 m,半方差理论模型为指数模型;抗冲系数、崩解速率、抗剪强度的Lag步长为55 000,半方差理论模型均为高斯模型。在空间分布上,各指标随土壤类型由北到南呈现明显的地带性规律。

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    Based on geo-statistical principle and semi-variability theory, this paper quantificationally studied the spatial variability of soil factor for modeling of soil erosion by water in GIS, comparing the accuracy of different interpolation methods, including IDW,Spline and Ordinary Kriging. The results showed that the spatial correlation of regional soil coefficient of soil anti-scourability was moderately, the nugget-to-sill ratio was 32. 29%,while the spatial correlation of steady infiltration rate,collapse velocity and shear strength was very strongly correlated,the nugget-to-sill ratio was 13. 19%,11. 61 % and 12. 98%respectively. In a word,taking account of MRE, RMSE and interpolation results, Ordinary Kriging interpolation was the best one,which represented the spatial characteristics of soil factors well and can be better used in regional soil erosion model in view of data requirement. To Ordinary Kriging, the lag step of the steady infiltration rate was 30000 meters, and the semi-variance theory model was exponential model whereas the soil coefficient of restitution,collapse velocity and shear strength was 50 000 meters respectively, and the semivariance theory was Gaussian Model. Besides, owing to the spatial distribution of soil type ranging from north to south, each index showed clear zonation differentiation character.

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庞国伟,杨勤科,张爱国,李锐.陕西省水蚀土壤因子指标插值方法比较研究[J].水土保持通报,2009,(2):176-182

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  • 在线发布日期: 2014-11-26
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