Using Geostatistics for Spatial Analysis of Soil Moisture Content, Electrical Conductivity, and pH at Paddy Fields

Y. Wijayanto, Muhammad Aldian Dwi Kustianto, S. A. Budiman, Ika Purnamasari
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Abstract

Soil is dynamic due to various internal and external processes exerted on the soil, resulting in unique soil characteristics in space in short and long distances. Geostatistics (kriging) is the method of quantifying the spatial variation of soil properties. This research was mainly aimed at applying geostatistics to quantify and interpolate the spatial dependence and structure of three soil properties, namely pH, EC, and Soil Moisture Content (SMC) in a small area. This research was conducted on paddy fields in Mlandingan Kulon Village, Situbondo Regency. Sampling was conducted on an area of   9.2 ha with 31 sample points. Normal data distribution was found for pH and EC, whereas this was not the case for SMC. The results of the analysis showed that most of the pH values   were alkaline (>8), EC values were non-saline (<2 mm/cm), and SMC was in the low category (<20%). The results show that for three soil properties, weak dependencies were observed. The values of Root Mean Square Error (RMSE)  confirmed that kriging with exponential was better compared to the spherical model, resulting in the RMSE of 0.546 (pH), 0.041 (EC), and 1.512 (SMC).
稻田土壤含水量、电导率和pH值空间分析的地质统计学方法
土壤是动态的,由于各种内外作用作用于土壤,导致土壤在短距离和长距离上具有独特的空间特征。地质统计学(kriging)是一种量化土壤性质空间变化的方法。本研究主要是利用地质统计学方法对小区域内pH、EC、SMC三种土壤性质的空间依赖关系和结构进行量化插值。本研究在斯图邦多县Mlandingan Kulon村的稻田进行。采样面积9.2 ha,采样点31个。pH和EC呈正态分布,而SMC并非如此。分析结果表明,大部分pH值为碱性(bbb8), EC值为非盐水(<2 mm/cm), SMC处于低类别(<20%)。结果表明,3种土壤性质之间存在较弱的相关性。均方根误差(RMSE)值证实指数克里格模型优于球形模型,其RMSE分别为0.546 (pH)、0.041 (EC)和1.512 (SMC)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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