Soil organic carbon and total nitrogen stocks related to land use and basic environmental properties − assessment of soil carbon sequestration potential in different ecosystems

IF 5.4 1区 农林科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY
Cristian Paltineanu , Sorina Dumitru , Olga Vizitiu , Victoria Mocanu , Anca-Rovena Lăcătusu , Stelian Ion , Horia Domnariu
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Abstract

Soil organic carbon (SOC) and total nitrogen (TN) stocks are crucial for the development of wild plants and crops. This paper examines the current SOC and TN stocks and their variability within land uses under different environments, assessing the relationships between SOC and TN stocks with basic environmental properties and quantifying the magnitude of SOC sequestration potential for a better land use management. We studied 991 soil profiles, from steppe to wet mountain-soils. The land use was essential in influencing soil organic C and total N stocking, with the forestland showing the significantly highest SOC stocks specifically in mountain soils, followed by grassland and cropland. Altitude, clay content, pH and plant available phosphorous and potassium were other influencers of SOC and TN stocks. The best predictive multiple linear regression model explained 68 % of the 0.5 m depth SOC stock variability for forest, 61 % for grassland and 37 % for cropland, while Random Forest model explained 70 %, 65 %, and 28 % for the same land uses. The obtained models rank factors contribution and may be useful in management. Lands having the highest C sequestration potential occurred within fine-textured soils, mainly in croplands. The most favorable soil depth for further C sequestration is below C-saturated topsoil and this could be achieved by deep-rooting crops and conservative technologies. Additionally, changing some low-fertile soils of cropland into forestland or grassland would improve SOC sequestration. These measures might contribute to sequester additional C amounts in soils, in order to bolster initiatives for climate-change mitigation and adaptation.
与土地利用和基本环境属性相关的土壤有机碳和全氮储量 - 不同生态系统的土壤固碳潜力评估
土壤有机碳(SOC)和总氮(TN)储量对野生植物和农作物的生长至关重要。本文研究了当前土壤有机碳(SOC)和全氮(TN)的储量及其在不同环境下土地利用中的变化,评估了土壤有机碳(SOC)和全氮(TN)储量与基本环境属性之间的关系,并量化了土壤有机碳(SOC)固存潜力的大小,以便更好地进行土地利用管理。我们研究了从草原到潮湿山地土壤的 991 个土壤剖面。土地利用对土壤有机碳和全氮储量的影响至关重要,特别是在山区土壤中,林地的有机碳储量明显最高,其次是草地和耕地。海拔、粘土含量、pH 值以及植物可利用的磷和钾是影响 SOC 和 TN 储量的其他因素。最佳预测多元线性回归模型对森林、草地和耕地 0.5 米深度 SOC 储量变化的解释率分别为 68%、61% 和 37%,而随机森林模型对相同土地用途的解释率分别为 70%、65% 和 28%。所获得的模型对各因素的贡献进行了排序,可能有助于管理。固碳潜力最大的土地是细粒土壤,主要是耕地。最有利于进一步固碳的土壤深度低于碳饱和表土,这可以通过深根作物和保守技术来实现。此外,将一些耕地中的低肥力土壤改为林地或草地也会提高 SOC 固存。这些措施可能有助于在土壤中螯合更多的碳,以支持减缓和适应气候变化的举措。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Catena
Catena 环境科学-地球科学综合
CiteScore
10.50
自引率
9.70%
发文量
816
审稿时长
54 days
期刊介绍: Catena publishes papers describing original field and laboratory investigations and reviews on geoecology and landscape evolution with emphasis on interdisciplinary aspects of soil science, hydrology and geomorphology. It aims to disseminate new knowledge and foster better understanding of the physical environment, of evolutionary sequences that have resulted in past and current landscapes, and of the natural processes that are likely to determine the fate of our terrestrial environment. Papers within any one of the above topics are welcome provided they are of sufficiently wide interest and relevance.
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