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Improved Prediction and Reduction of Sampling Density for Soil Salinity by Different Geostatistical Methods

机译:不同地统计方法改进对土壤盐分采样密度的预测和降低

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The spatial estimation for soil properties was improved and sampling intensities also decreased in terms of incorporated auxiliary data. In this study, kriging and two interpolation methods were proven well to estimate auxiliary variables: cokriging and regression-kriging, and using the salinity data from the first two stages as auxiliary variables, the methods both improved the interpolation of soil salinity in coastal saline land. The prediction accuracy of the three methods was observed under different sampling density of the target variable by comparison with another group of 80 validation sample points, from which the root-mean-square error (RMSE) and correlation coefficient (r) between the predicted and measured values were calculated. The results showed, with the help of auxiliary data, whatever the sample size of the target variable may be, cokriging and regression-kriging performed better than ordinary kriging. Moreover, regression-kriging produced on average more accurate predictions than cokriging. Compared with the kriging results, cokriging improved the estimations by reducing RMSE from 23.3 to 29% and increasing r from 16.6 to 25.5%, regression-kriging improved the estimations by reducing RMSE from 25 to 41.5% and increasing r from 16.8 to 27.2%. Therefore, regression-kriging shows promise for improved prediction for soil salinity and reduction of soil sampling intensity considerably while maintaining high prediction accuracy. Moreover, in regression-kriging, the regression model can have any form, such as generalized linear models, non-linear models or tree-based models, which provide a possibility to include more ancillary variables.
机译:土壤条件的空间估计得到了改善,采样强度也随着合并的辅助数据而降低。在这项研究中,克里格法和两种插值方法被证明可以很好地估计辅助变量:cokriging和回归克里格法,并且使用前两个阶段的盐度数据作为辅助变量,这两种方法都改善了沿海盐碱地土壤盐分的插值。通过与另一组80个验证样本点进行比较,观察了三种方法在目标变量的不同采样密度下的预测准确性,由此得出预测值与预测值之间的均方根误差(RMSE)和相关系数(r)。计算出测量值。结果表明,借助辅助数据,无论目标变量的样本大小如何,协同克里金法和回归克里金法的性能均优于普通克里金法。此外,回归克里金法产生的平均预测比共同克里金法更准确。与克里金法结果相比,共克里金法将RMSE从23.3%降低至29%,将r从16.6增至25.5%,从而将估计值提高了;回归克里金法将RMSE从25%降低至41.5%,将r从16.8%增至27.2%,从而提高了估计值。因此,回归克里格法显示出有望改善土壤盐分的预测并降低土壤采样强度的同时保持较高的预测精度。此外,在回归克里金法中,回归模型可以具有任何形式,例如广义线性模型,非线性模型或基于树的模型,这提供了包含更多辅助变量的可能性。

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