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Characterizing the spatial variability of soil salinity in Lake Urmia Basin by applying geo-statistical methods

机译:应用地统计学方法表征乌尔米亚湖盆地土壤盐分的空间变异性

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Land degradation by salinity is one of the main environmental hazards threatening soil sustainability especially in arid and semi-arid regions of the world characterized by low precipitation and high evaporation. Geo-statistical approaches and remote sensing (RS) techniques have provided fast, accurate and economic prediction and mapping of soil salinity within the last two decades. Obtaining multi-temporal data via satellite images in different spatial domains with various scales is one of the key developments of monitoring spatial variability of soil salinity. In addition, geo-statistical methods have the capability of producing prediction surfaces from limited sample data. This study aims to map spatial distribution of soil salinity in the selected pilot area which is located in the western part of Urmia Lake Basin, Iran, by applying geo-statistical methods. A kriging based map and three different co-kriging based maps were produced using electrical conductivity (EC) measurements as primary variable and three different soil salinity index values as secondary variable. Three soil salinity indices were created by using Sentinel-2A image that were acquired in the same date of field measurements to generate 3 various soil salinity prediction maps. Salinity maps obtained from geo-statistical methods were compared and validated to understand the performance of these approaches for soil salinity prediction. The results of this study demonstrated that co-kriging can provide promising estimation of spatial variability of soil salinity especially when there is relevant and abundant set of secondary data derived from satellite images.
机译:盐碱化土地退化是威胁土壤可持续性的主要环境危害之一,特别是在世界上降水量少,蒸发量高的干旱和半干旱地区。地统计学方法和遥感(RS)技术在过去的二十年中提供了快速,准确和经济的土壤盐分预测和绘图。通过不同尺度的不同空间域的卫星图像获得多时相数据是监测土壤盐分空间变异性的重要进展之一。另外,地统计学方法具有从有限的样本数据中生成预测面的能力。本研究旨在通过应用地统计学方法绘制伊朗乌尔米亚湖盆地西部选定试点地区土壤盐分的空间分布图。使用电导率(EC)测量作为主要变量,使用三个不同的土壤盐度指数值作为次要变量,生成了基于克里格图的地图和三个不同的基于共同克里格图的地图。通过使用Sentinel-2A图像创建了三个土壤盐度指数,这些图像是在现场测量的同一日期获取的,以生成3个不同的土壤盐度预测图。比较并验证了从地统计学方法获得的盐度图,以了解这些方法在土壤盐分预测中的性能。这项研究的结果表明,协同克里格法可以为土壤盐分的空间变异性提供有希望的估计,特别是当有大量相关的从卫星图像中获得的辅助数据时。

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