旱地生态系统中的浅层土壤:碳积累的驱动因素和对土地管理的影响

IF 3.1 2区 农林科学 Q2 SOIL SCIENCE
C. Roberto Pinheiro Junior , Tiago Osório Ferreira , José de Souza Oliveira Filho , Hermano Melo Queiroz , Lucas Pecci Canisares , Lucas T. Greschuk , Carlos Eduardo Pellegrino Cerri , Marcos Gervasio Pereira , Gonçalo Amarante Guimarães Pereira , Maurício Roberto Cherubin
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引用次数: 0

摘要

浅层土壤(即石质 Entisols)约占巴西旱地面积的 20%。固有的土壤特性(即深度较浅)和缺水限制了这些土壤中植物的生长和碳(C)的输入。在这样一个敏感的生态系统中,可持续的土地管理方案是促进社会经济发展和确保粮食安全的关键。在此,我们利用分布在巴西旱地(东北部地区)的 50 个石质 Entisol 剖面数据集,以便(i) 研究土地利用(耕地、草地和原始森林)、气候(半干旱和亚湿润干旱)和坡度等级(0-3%、3-8%、8-20% 和 20-45%)对土壤碳积累的影响;以及 (ii) 评估了解碳积累的多重驱动因素如何有助于确定可持续的土地管理方案。结果表明,土地利用并不影响碳储量和碳/氮比,但它们受到气候的影响。在亚湿润干旱气候条件下,碳储量为 41.7 兆克/公顷-1,比半干旱气候条件下(28.9 兆克/公顷-1)高出 44%,这一结果反映了较湿润环境中生物量生产较高的影响。在 20-45% 的坡度下,碳储量为 54.3 兆克/公顷-1,比 0-3% 的坡度下(19.9 兆克/公顷-1)高出 172%,这是因为在较陡的坡度下,海拔较高,环境较潮湿。我们的研究结果表明,坡度较低的地区碳储量较低,干旱指数也较低。这些较干旱的条件降低了一年生作物和草地的生产潜力,但却有利于种植高产的草酸代谢(CAM)作物,如龙舌兰属植物,它们具有生产生物燃料的巨大潜力。此外,从乙醇生产中重新引入有机残留物的可能性可以促进碳储量的增加,从而有助于减缓气候变化。归根结底,我们的研究从整体上提供了 SOC 积累驱动因素的见解,为全球热带干旱地区高度敏感环境的土地利用规划提供了支持。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Shallow soils in dryland ecosystems: Drivers of C accumulation and land management implications

Shallow soils in dryland ecosystems: Drivers of C accumulation and land management implications

Shallow soils (i.e., Lithic Entisols) cover about 20% of Brazilian drylands. Inherent soil characteristics (i.e., shallow depths) and water scarcity restrict plant growth and carbon (C) inputs in these soils. In such a sensitive ecosystem, sustainable land management options are key to promoting socio-economic development and ensuring food security. Here, we use a dataset of 50 Lithic Entisol profiles distributed within the Brazilian drylands (northeastern region) to: (i) investigate the effects of land-use (cropland, grassland, and native forest), climate (semi-arid and dry sub-humid), and slope classes (0–3%, 3–8%, 8–20% and 20–45%) on soil C accumulation; and (ii) evaluate how understanding multiple drivers C accumulation can support the identification of sustainable land management options. The results suggested that land use does not affect C stock and C/N ratio, nevertheless, they were affected by climate. Under dry sub-humid climate conditions, C stocks were 41.7 Mg ha−1, 44% higher than under semi-arid climate (28.9 Mg ha−1), a result that reflects the effect of higher biomass production in wetter environments. Under slopes of 20–45%, C stocks were 54.3 Mg ha−1, 172% higher than under slopes of 0–3% (19.9 Mg ha−1), because of the higher altitudes and wetter conditions under steeper slopes. Our results showed that areas under lower slopes have lower C stocks and lower aridity index. These drier conditions reduce the productive potential of annual crops and grasslands but enable the cultivation of high-yielding Crassulacean Acid Metabolism (CAM) crops, such as Agave spp, which have a high potential for biofuel production. Furthermore, the possibility of reintroducing organic residues from ethanol production can promote an increase in C stocks, contributing to climate change mitigation. Ultimately, our study provides insights from a holistic view of SOC accumulation drivers, supporting land use planning of highly sensitive environments in tropical drylands around the world.

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来源期刊
Geoderma Regional
Geoderma Regional Agricultural and Biological Sciences-Soil Science
CiteScore
6.10
自引率
7.30%
发文量
122
审稿时长
76 days
期刊介绍: Global issues require studies and solutions on national and regional levels. Geoderma Regional focuses on studies that increase understanding and advance our scientific knowledge of soils in all regions of the world. The journal embraces every aspect of soil science and welcomes reviews of regional progress.
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