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Mapping of soil properties at high resolution in Switzerland using boosted geoadditive models

机译:使用增强的地理添加模型在瑞士高分辨率绘制土壤特性

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High-resolution maps of soil properties are a prerequisite for assessing soil threats and soil functions and for fostering the sustainable use of soil resources. For many regions in the world, accurate maps of soil properties are missing, but often sparsely sampled (legacy) soil data are available. Soil property data (response) can then be related by digital soil mapping (DSM) to spatially exhaustive environmental data that describe soil-forming factors (covariates) to create spatially continuous maps. With airborne and space-borne remote sensing and multi-scale terrain analysis, large sets of covariates have become common. Building parsimonious models amenable to pedological interpretation is then a challenging task. We propose a new boosted geoadditive modelling framework (geoGAM) for DSM. The geoGAM models smooth non-linear relations between responses and single covariates and combines these model terms additively. Residual spatial autocorrelation is captured by a smooth function of spatial coordinates, and non-stationary effects are included through interactions between covariates and smooth spatial functions. The core of fully automated model building for geoGAM is component-wise gradient boosting. We illustrate the application of the geoGAM framework by using soil data from the Canton of Zurich, Switzerland. We modelled effective cation exchange capacity (ECEC) in forest topsoils as a continuous response. For agricultural land we predicted the presence of waterlogged horizons in given soil depths as binary and drainage classes as ordinal responses. For the latter we used proportional odds geoGAM, taking the ordering of the response properly into account. Fitted geoGAM contained only a few covariates (7 to 17) selected from large sets (333 covariates for forests, 498 for agricultural land). Model sparsity allowed for covariate interpretation through partial effects plots. Prediction intervals were computed by model-based bootstrapping for ECEC. The predictive performance of the fitted geoGAM, tested with independent validation data and specific skill scores for continuous, binary and ordinal responses, compared well with other studies that modelled similar soil properties. Skill score (SS) values of 0.23 to 0.53 (with SS?=?1 for perfect predictions and SS?=?0 for zero explained variance) were achieved depending on the response and type of score. GeoGAM combines efficient model building from large sets of covariates with effects that are easy to interpret and therefore likely raises the acceptance of DSM products by end-users.
机译:高分辨率的土壤特性图是评估土壤威胁和土壤功能以及促进土壤资源可持续利用的先决条件。对于世界上许多地区,缺少准确的土壤特性图,但通常可获得稀疏采样(遗留)的土壤数据。然后可以通过数字土壤制图(DSM)将土壤属性数据(响应)与描述土壤形成因子(协变量)的空间详尽的环境数据相关联,以创建空间连续图。随着机载和星载遥感以及多尺度地形分析,大的协变量集变得很普遍。因此,建立适合儿童学解释的简约模型是一项艰巨的任务。我们为DSM提出了一个新的增强型地理添加剂建模框架(geoGAM)。 geoGAM模型可平滑响应和单个协变量之间的非线性关系,并将这些模型项相加组合。剩余空间自相关由空间坐标的平滑函数捕获,并且通过协变量和平滑空间函数之间的相互作用包括非平稳效应。 geoGAM的全自动模型构建的核心是逐分量梯度提升。我们通过使用来自瑞士苏黎世州的土壤数据来说明geoGAM框架的应用。我们将森林表层土壤中的有效阳离子交换容量(ECEC)建模为连续响应。对于农业用地,我们以给定的土壤深度预测了淹水层位的存在,以二元级和排水级作为序数响应。对于后者,我们使用了比例赔率geoGAM,并适当考虑了响应的顺序。拟合的geoGAM仅包含从大集合中选择的几个协变量(7到17)(森林为333个协变量,农业用地为498个协变量)。模型稀疏性允许通过局部效应图进行协变量解释。预测间隔是通过基于模型的ECEC自举计算的。与独立的验证数据和针对连续,二元和序数响应的特定技能评分相比较,拟合出的geoGAM的预测性能与模拟相似土壤特性的其他研究进行了比较。技能得分(SS)值在0.23到0.53之间(对于完美的预测,SS?=?1,对于零解释方差,SS?=?0)取决于得分的响应和类型。 GeoGAM将大量协变量的有效模型构建与易于解释的效果结合在一起,因此可能会提高最终用户对DSM产品的接受度。

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