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Applying Spatial Geostatistical Analysis Models for Evaluating Variability of Soil Properties in Eastern Shiraz, Iran

机译:应用空间地统计学分析模型评估伊朗东部设拉子土壤性质的变异性

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The information on the spatial properties of soil is vital to improve soil management and to increase the crop productivity. Geostatistical analysis technique is one of the most important methods for determining the spatial properties of soil. The aim of this study was to investigate spatial variability of soil chemical and physical attributes for field management in eastern Shiraz, Iran, in 2010. In the study area, for applying geostatistical analysis, eighty soil samples were taken randomly. The variability of saturation percentage (SP), electrical conductivity (EC), soil pH, sand%, silt%, clay%, nitrogen (N), phosphorus (P) and potassium content (K) of the soil used to determine the spatial properties of soil by geostatistical analysis techniques. Soil properties were analyzed both geostatistically and statistically on the basis of the Semivariogram models. Thus, each soil parameter was used for different Semivariogram models such as spherical, circular and exponential because of their different spatial structures. The results showed that the best model to generate soil properties map was ordinary kriging with spherical and exponential Semivariogram models. The best model for soil pH, SP, K and N was the spherical model whereas for sand%, silt%, clay%, EC and P, the best model was the exponential model. Based on the models, the range of spatial dependency was found to vary within soil parameters. EC had the longest (134 meter) and pH had the shortest (19.1 meter) range of spatial dependency. Additionally, spatial patterns may vary among soil parameters in the study area. Therefore, Semivariogram models can be useful tools to determine spatial variability of parameters, preparing soil map and field management strategy.
机译:有关土壤空间特性的信息对于改善土壤管理和提高农作物生产力至关重要。地统计分析技术是确定土壤空间特性的最重要方法之一。这项研究的目的是在2010年调查伊朗东部设拉子的土壤化学和物理属性的空间变异性,以便进行田间管理。在研究区域,为进行地统计分析,随机抽取了80个土壤样本。用于确定空间空间的土壤饱和度百分比(SP),电导率(EC),土壤pH,沙%,淤泥%,粘土%,氮(N),磷(P)和钾含量(K)的变异性地统计学方法分析土壤的性质。在半变异函数模型的基础上,对土壤性质进行了地统计学和统计学分析。因此,每个土壤参数因其不同的空间结构而用于不同的半变异函数模型,例如球形,圆形和指数型。结果表明,生成土壤特性图的最佳模型是采用球面和指数半变异函数模型的普通克里金法。土壤pH,SP,K和N的最佳模型是球形模型,而对于沙%,淤泥%,粘土%,EC和P而言,最佳模型是指数模型。基于这些模型,发现空间相关性的范围在土壤参数内变化。 EC的空间依赖性范围最长(134米),pH值的范围最短(19.1米)。此外,研究区域中土壤参数的空间格局可能会有所不同。因此,半变异函数模型可以用作确定参数的空间变异性,准备土壤图和田间管理策略的有用工具。

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