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A linear mixed model, with non-stationary mean and covariance,for soil potassium based on gamma radiometry

机译:基于伽玛射线法的土壤钾含量具有非平稳均值和协方差的线性混合模型

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摘要

In this paper we present a linear mixed model for the potassium content of soil across a large region of eastern England in which the mean is modelled as a linear function of the passive gamma-ray emissions of the earth surface in the energy interval commonly associated with potassium decay. Non-stationary models are proposed for the random effect, which is the variation not captured by this regression. Specif-ically, we assume that the local spectrum of the standardized random effect can be obtained by tempering a common (sta-tionary) spectrum, that is to say raising its values to a power, the tempering parameter, which is itself modelled as a linear function of the radiometric data. This allows the "smooth-ness" of the random effect to vary locally. In addition the lo-cal spatially correlated variance and "nugget" variance (ap-parently uncorrelated given the resolution of the sampling) can also be modelled as a function of the radiometric data. Using the radiometric signal as a covariate gave some im-provement in the precision of predictions of soil potassium at validation sites. In addition, there was evidence that non-stationary models for the random effect fitted the data better than stationary models, and this difference was statistically significant. Non-stationary models also appeared to describe the error variance of predictions at the validation sites better. Further work is needed on selection among alternative non-stationary models, since simple procedures used here, based on comparing log-likelihood ratios of nested models and the Akaike information criterion for non-nested models, did not identify the model which gave the best account of the predic-tion error variances at validation sites.
机译:在本文中,我们提出了英格兰东部大部分地区土壤钾含量的线性混合模型,该模型的均值被建模为在通常与能量相关的能量间隔内,地表的被动伽马射线发射的线性函数。钾衰变。对于随机效应,提出了非平稳模型,即该回归未捕获的变化。具体而言,我们假设可以通过对公共(静态)频谱进行调和来获得标准化随机效应的局部频谱,也就是说,将其值提高为幂,即调和参数,其本身可以建模为辐射数据的线性函数。这允许随机效应的“平滑度”局部变化。此外,局部空间相关方差和“块”方差(在给定采样分辨率的情况下显然不相关)也可以根据辐射数据建模。使用辐射信号作为协变量可以提高验证点土壤钾的预测精度。另外,有证据表明,随机效应的非平稳模型比平稳模型更适合数据,并且这种差异具有统计学意义。非平稳模型似乎也可以更好地描述验证站点上预测的误差方差。在替代的非平稳模型中进行选择还需要进一步的工作,因为此处使用的简单程序基于比较嵌套模型的对数似然比和非嵌套模型的Akaike信息准则,因此无法确定给出最佳解释的模型验证点的预测误差方差。

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