首页> 外文期刊>Earth Surface Processes and Landforms: The journal of the British Geomorphological Research Group >Determinants of sediment properties and organic matter in beach and dune environments based on boosted regression trees
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Determinants of sediment properties and organic matter in beach and dune environments based on boosted regression trees

机译:基于增强回归树的海滩和沙丘环境中沉积物性质和有机质的决定因素

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摘要

Grain size properties and the variation of organic matter in coastal beach and dune environments are assumed to be controlled by the intensity of aeolian processes, time and the sediment source. However, assumptions are based on relatively limited empirical studies. In this study, we examined which environmental variables are the main predictors of multiple topsoil properties. To achieve this, we analysed an extensive dataset systematically collected across all beach zones and a large geographical area at the Finnish Baltic Sea coast characterized by post-glacial land uplift. We included a comprehensive set of predictors in the analysis and applied boosted regression trees, a modern modelling technique particularly suited for analysis without prior assumptions of the data model. The results suggest that mean grain size and sorting are mainly determined by northing and fetch. Northing, disturbance and fetch predicted the variation of soil organic matter while litter cover was strongly related to disturbance. Based on the analyses, we were able to identify the main drivers of multiple topsoil properties on land uplift beaches. Parent material is suggested to determine sediment textural properties, which largely masks the effects of transient processes. Mean grain size and sorting are highly interdependent: grains become finer and sorting improves with increasing shore exposure. The intensity of momentary geomorphic processes controls the accumulation of litter whereas the slower accumulation of organic matter in the soil is influenced also by the static exposure setting. Skewness and kurtosis of the grain size distribution are mainly influenced by unmeasured processes, potentially relating to the geomorphological origin of the sediment. Copyright (c) 2014 John Wiley & Sons, Ltd.
机译:假定沿海海滩和沙丘环境中的粒度特征和有机物的变化受风化过程的强度,时间和沉积物来源的控制。但是,假设是基于相对有限的经验研究。在这项研究中,我们检查了哪些环境变量是多种表土特性的主要预测因子。为了实现这一目标,我们分析了在芬兰波罗的海沿岸的所有海滩区域和大地理区域中系统收集的大量数据集,其特征是冰川后土地隆升。我们在分析中包括了一组全面的预测变量,并应用了增强的回归树,这是一种现代建模技术,特别适合在没有数据模型事先假设的情况下进行分析。结果表明,平均晶粒度和排序主要由北向和取回决定。北向,扰动和取水预测土壤有机质的变化,而凋落物覆盖与扰动密切相关。基于分析,我们能够确定陆地隆升海滩上多种表层土属性的主要驱动因素。建议使用母体材料来确定沉积物的质地特性,这在很大程度上掩盖了瞬态过程的影响。平均粒度和分类高度相关:谷物变得更细,分类随着海岸暴露量的增加而改善。瞬时地貌过程的强度控制了枯枝落叶的积累,而土壤中有机物较慢的积累也受到静态暴露设置的影响。粒度分布的偏度和峰度主要受不可测过程的影响,这可能与沉积物的地貌起源有关。版权所有(c)2014 John Wiley&Sons,Ltd.

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