首页> 外文期刊>The Science of the Total Environment >Agricultural soil organic carbon stocks in the north-eastern Iberian Peninsula: Drivers and spatial variability
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Agricultural soil organic carbon stocks in the north-eastern Iberian Peninsula: Drivers and spatial variability

机译:伊比利亚东北半岛的农业土壤有机碳储量:驱动力和空间变异性

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Estimating soil organic carbon (SOC) stocks under agriculture, assessing the importance of their drivers and understanding the spatial distribution of SOC stocks are crucial to predicting possible future SOC stocks scenarios under climate change conditions and to designing appropriate mitigation and adaptation strategies. This study characterized and modelled SOC stocks at two soil depth intervals, topsoil (0-30 an) and subsoil (30-100 cm), based on both legacy and recent data from 7245 agricultural soil profiles and using environmental drivers (climate, agricultural practices and soil properties) for agricultural soils in Catalonia (NE Spain). Generalized Least Square (GLS) and Geographical Weighted Regression (GWR) were used as modelling approaches to: (i) assess the main SOC stock drivers and their effects on SOC stocks; (ii) analyse spatial variability of SOC stocks and their relationships with the main drivers; and (iii) predict and map SOC stocks at the regional scale. While topsoil variation of SOC stocks depended mainly on climate, soil texture and agricultural variables, subsoil SOC stocks changes depended mainly on soil attributes such us soil texture, clay content, soil type or depth to bedrock. The GWR model revealed that the relationship between SOC stocks and drivers varied spatially. Finally, the study was only able to predict and map topsoil SOC stocks at the regional scale, because controlling factors of SOC stocks at the subsoil level were largely unavailable for digital mapping. According to the resulting map, the mean SOC stock value for Catalan agriculture at the topsoil level was 4.88 +/- 0.89 kg/m(2) and the total magnitude of the carbon pool in agricultural soils of Catalonia up to 30 cm reached 47.9 Tg. The present study findings are useful for defining carbon sequestration strategies at the regional scale related with agricultural land use changes and agricultural management practices in a context of climate change. (C) 2019 Elsevier B.V. All rights reserved.
机译:估算农业下的土壤有机碳(SOC)储量,评估其驱动力的重要性以及了解SOC储量的空间分布对于预测气候变化条件下未来可能的SOC储量情景以及设计适当的缓解和适应策略至关重要。这项研究基于来自7245个农业土壤剖面的遗留数据和最新数据,并使用环境驱动因素(气候,农业实践)对两个土壤深度区间表层土壤(0-30 an)和下层土壤(30-100 cm)的SOC储量进行了表征和建模和土壤特性)用于加泰罗尼亚(西班牙东北部)的农业土壤。广义最小二乘(GLS)和地理加权回归(GWR)作为建模方法用于:(i)评估主要SOC存量驱动因素及其对SOC存量的影响; (ii)分析SOC存量的空间变异性及其与主要驱动因素的关系; (iii)在区域范围内预测和绘制SOC存量。 SOC储量的表土变化主要取决于气候,土壤质地和农业变量,而土壤下SOC储量的变化主要取决于土壤属性,例如土壤质地,粘土含量,土壤类型或基岩深度。 GWR模型显示,SOC存量与驱动因素之间的关系在空间上变化。最后,该研究只能在区域规模上预测和绘制表土SOC存量,因为在地下土壤中,SOC存量的控制因素在很大程度上无法用于数字制图。根据结果​​图,加泰罗尼亚农业在表层土壤中的平均SOC储量值为4.88 +/- 0.89 kg / m(2),加泰罗尼亚30厘米以下的农业土壤中碳库的总量达到47.9 Tg 。本研究结果有助于在气候变化的背景下,在与农业土地使用变化和农业管理实践相关的区域范围内确定碳固存策略。 (C)2019 Elsevier B.V.保留所有权利。

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