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Spatial assessment of soil salinity in the Harran Plain using multiple kriging techniques

机译:利用多种克里金法对哈兰平原土壤盐分进行空间评估

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The Harran Plain is located in the southeastern part of Turkey and has recently been developed for irrigation agriculture. It already faces soil salinity problems causing major yield losses. Management of the problem is hindered by the lack of information on the extent and geography of the salinization problem. A survey was carried out to delineate the spatial distribution of salt-affected areas by randomly selecting 140 locations that were sampled at two depths (0 to 30 and 30 to 60 cm) and analyzed for soil salinity variables: soil electrical conductivity (EC), soluble cations (Ca~(2+) Mg~(2+), Na~+, and K~+), soluble anions (SO_4~(2-), Cl~-), exchangeable Na~+ (me 100 g~(-1)) and exchangeable sodium percentage. Terrain attributes (slope, topographical wetness index) were extracted from the digital elevation model of the study area. Variogram analyses after log transformation and ordinary kriging (OK) were applied to map spatial patterns of soil salinity variables. Multivariate geostatistical methods-regression kriging (RK) and kriging with external drift (KED)-were used using elevation and soil electrical conductivity data as covariates. Performances of the three estimation methods (OK, RK, and KED) were compared using independent validation samples randomly selected from the main dataset. Soils were categorized into salinity classes using disjunctive kriging (DK) and ArcGIS, and classification accuracy was tested using the kappa statistic. Results showed that soil salinity variables all have skewed distribution and are poorly correlated with terrain indices but have strong correlations among each other. Up to 65 % improvement was obtained in the estimations of soil salinity variables using hybrid methods over OK with the best estimations obtained with RK using EC_(0-30) as covariate. DK-ArcGIS successfully classified soil samples into different salinity groups with overall accuracy of 75 % and kappa of 0.55 (p<0.001).
机译:哈兰平原位于土耳其的东南部,最近被开发用于灌溉农业。它已经面临着土壤盐分问题,导致大量的产量损失。由于缺乏有关盐碱化问题的范围和地理位置的信息,因此无法管理该问题。通过随机选择在两个深度(0至30和30至60厘米)采样的140个位置并分析土壤盐度变量:土壤电导率(EC),可溶性阳离子(Ca〜(2+)Mg〜(2 +),Na〜+和K〜+),可溶性阴离子(SO_4〜(2-),Cl〜-),可交换的Na〜+(me 100 g〜 (-1))和可交换的钠百分比。从研究区域的数字高程模型中提取地形属性(坡度,地形湿度指数)。对数转换和普通克里金法(OK)后的变异函数分析用于绘制土壤盐分变量的空间格局。使用高程和土壤电导率数据作为协变量,使用多元地统计方法-回归克里格(RK)和带外部漂移的克里格(KED)-。使用从主数据集中随机选择的独立验证样本比较了三种估计方法(OK,RK和KED)的性能。使用分离Kriging(DK)和ArcGIS将土壤分类为盐度类别,并使用kappa统计量测试分类准确性。结果表明,土壤盐度变量均具有偏斜分布,与地形指数相关性不强,但相互之间具有很强的相关性。与OK相比,使用混合方法对土壤盐度变量的估计最多可提高65%,而使用EC_(0-30)作为协变量的RK可获得的最佳估计值。 DK-ArcGIS成功地将土壤样品分类为不同的盐度组,总精度为75%,kappa为0.55(p <0.001)。

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