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Exploring Spatial Variation of Soil Salinity in the Yellow River Delta

机译:黄河三角洲土壤盐分的空间变化研究

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In this paper, spatial autocorrelation analysis, ordinary least square (OLS) and spatial regression model are applied to explore spatial variation of soil salinity based on samples collected from the Yellow River Delta. Generally, spatial data, like soil salinity, elevation etc., are characterized by spatial effects such as spatial dependence and spatial structure. Inasmuch as these effects exist, the utilization of OLS model may lead to inaccurate inference about predictor variable. Moreover, the traditional regression models used to analyze spatial data often have autocorrelated residuals which violate the assumption of Guess-Markov Theorem. This indicates that conventional regression models cannot be used in analyzing spatial variation of soil salinity directly. To overcome this limitation, spatial regression model is introduced to explore the relationship between soil salinity and environmental factors (including elevation, pH and organic matter concentration, etc.). By verifying Moran's I scatterplot of regression residuals, we find no autocorrelation in spatial regression model compared with high positive autocorrelation in the OLS model;besides, the spatial regression model has a significant (p < 0.01) estimations and good-fit-it in our study. Finally, an approach of specifying suitable spatial weight matrix is put forward.
机译:本文运用空间自相关分析,普通最小二乘(OLS)和空间回归模型,基于黄河三角洲地区的样本,探讨了土壤盐分的空间变化。通常,空间数据(例如土壤盐分,海拔等)的特征在于空间效应,例如空间依赖性和空间结构。由于存在这些影响,OLS模型的使用可能导致对预测变量的推断不准确。此外,用于分析空间数据的传统回归模型通常具有自相关残差,这违反了Guess-Markov定理的假设。这表明常规回归模型不能直接用于分析土壤盐分的空间变化。为了克服这个限制,引入了空间回归模型来探索土壤盐分与环境因素(包括海拔,pH和有机物浓度等)之间的关系。通过验证回归残差的Moran I散点图,我们发现与OLS模型中的高正自相关相比,空间回归模型中没有自相关;此外,空间回归模型在我们的研究中具有显着的(p <0.01)估计和良好拟合研究。最后,提出了一种确定合适的空间权重矩阵的方法。

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