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了解控制欧洲土壤表土有机碳含量的因素的空间分布。

Understanding the spatial distribution of factors controlling topsoil organic carbon content in European soils.

机构信息

Departamento de Edafoloxía e Química Agrícola, Facultade de Bioloxía, Universidade de Santiago de Compostela, 15782 Santiago de Compostela, Spain.

Departamento de Edafoloxía e Química Agrícola, Facultade de Bioloxía, Universidade de Santiago de Compostela, 15782 Santiago de Compostela, Spain.

出版信息

Sci Total Environ. 2017 Dec 31;609:1411-1422. doi: 10.1016/j.scitotenv.2017.08.012. Epub 2017 Aug 6.

Abstract

Soil Organic Carbon (SOC) constitutes the largest terrestrial carbon pool. The understanding of its dynamics and the environmental factors that influence its behaviour as sink or source of atmospheric CO is crucial to quantify the carbon budget at the global scale. At the European scale, most of the existing studies to account for SOC stocks are centred in the fitting of predictive model to ascertain the distribution of SOC. However, the development of methodologies for monitoring and identifying the environmental factors that control SOC storage in Europe remains a key research challenge. Here we present a modelling procedure for mapping and monitoring SOC contents that uses Visible-Near Infrared (VNIR) spectroscopic measurements and a series of environmental covariates to ascertain the key environmental processes that have a major contribution into SOC sequestration processes. Our results show that it follows a geographically non-stationary process in which the influencing environmental factors have different weights depending on the spatial location. This implies that SOC stock modelling should not rely on a single model but on a combination of different statistical models depending on the environmental characteristics of each area. A cluster classification of European soils in relation to those factors resulted in the determination of four groups for which specific models have been obtained. Differences in climate, soil pH, content of coarse fragments or land cover type are the main factors explaining the differences in SOC in topsoil from Europe. We found that climatic conditions are the main driver of SOC storage at the continental scale, but we also found that parameters like land cover type influence SOC content found at the local scales in certain areas. Our methodology developed at continental scale could be used in future research aimed to improve the predictive performance of SOC assessments at European scale.

摘要

土壤有机碳(SOC)构成了最大的陆地碳库。了解其动态以及影响其作为大气 CO 汇或源的行为的环境因素,对于在全球范围内量化碳预算至关重要。在欧洲范围内,大多数现有的 SOC 储量研究都集中在拟合预测模型以确定 SOC 的分布上。然而,开发用于监测和识别控制欧洲 SOC 储存的环境因素的方法仍然是一个关键的研究挑战。在这里,我们提出了一种用于绘制和监测 SOC 含量的建模程序,该程序使用可见近红外(VNIR)光谱测量和一系列环境协变量来确定对 SOC 固存过程有重大贡献的关键环境过程。我们的结果表明,它遵循一种地理上非平稳的过程,其中影响环境因素的权重因空间位置而异。这意味着 SOC 储量建模不应依赖于单个模型,而应根据每个区域的环境特征,结合使用不同的统计模型。根据这些因素对欧洲土壤进行聚类分类,确定了四个组,并为每个组获得了特定的模型。气候、土壤 pH 值、粗粒物质含量或土地覆盖类型的差异是解释欧洲表土 SOC 差异的主要因素。我们发现,气候条件是大陆尺度 SOC 储存的主要驱动因素,但我们也发现,像土地覆盖类型这样的参数会影响某些地区的局部 SOC 含量。我们在大陆尺度上开发的方法可用于未来的研究,旨在提高欧洲尺度 SOC 评估的预测性能。

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