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Three dimensional spatial distribution modeling of soil texture under agricultural systems using a sequence indicator simulation algorithm

机译:基于序列指标模拟算法的农业系统土壤三维空间分布建模。

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Understanding the distribution of alluvial soil textures on a large scale is crucial for agricultural and environmental management. In our study an indicator variogram and a sequence indicator simulation (SIS) algorithm were used to analyze and simulate the spatial distribution of soil textures based on observations of 139 soil profiles in a 15 km2 region in the Huabei alluvial plain in China. The nugget-to-sill ratio value (SH) of the indicator variograms for all textures in a vertical direction (Z)was equal to 1. This suggests that spatial auto-correlation dominates in the direction of sedimentary deposition with 0.05 m sampling intervals. In contrast, SH ratios from 0.48 to 0.81 show that the soil textures have a degree of randomness in the horizontal direction (X, Y) where the sampling distance was about 300 m. Using the indicator variograms in 3 directions (X, Y and Z) as outlined above, a 3D SIS algorithm was used to simulate textures. Finally, the simulation results were evaluated by the reproduction of a histogram, variogram and the mean absolute error (MAE) of prediction. The mean absolute percentage error (MAPE) of the histogram reproduction showed that the main textures (sand, sandy loam and clay) were described well, whereas the lessprevalent textures were underestimated. The MAPE of the indicator variograms reproduction were reasonable although some deviation existed as less prevalent textures in the vertical direction. The mean absolute error (MAE) of the SIS prediction was 0.47.This result is considered acceptable for a category variable because of the stochastic nature of soil textures in a horizontal direction, and hence may provide useful data for other agricultural research.
机译:大规模了解冲积土壤质地的分布对于农业和环境管理至关重要。在我们的研究中,基于对中国华北冲积平原15 km2区域中139个土壤剖面的观测,使用了指示变量图和序列指示符模拟(SIS)算法来分析和模拟土壤质地的空间分布。所有纹理在垂直方向(Z)上的指标变异函数的块金比值(SH)等于1。这表明空间自相关在以0.05 m采样间隔的沉积沉积方向上占主导地位。相比之下,SH比率从0.48到0.81表明,土壤质地在采样距离约为300 m的水平方向(X,Y)上具有随机度。使用上面概述的3个方向(X,Y和Z)上的指标变异函数,使用3D SIS算法模拟纹理。最后,通过复制直方图,方差图和预测的平均绝对误差(MAE)来评估仿真结果。直方图再现的平均绝对百分比误差(MAPE)表明,主要纹理(沙,沙壤土和粘土)的描述很好,而不太普遍的纹理被低估了。指标变异函数再现的MAPE是合理的,尽管由于垂直方向上较少的普遍存在纹理而存在一些偏差。 SIS预测的平均绝对误差(MAE)为0.47。由于土壤质地在水平方向上具有随机性,因此该结果对于类别变量而言是可以接受的,因此可以为其他农业研究提供有用的数据。

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