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能否通过在热带和亚热带环境中采用保护性农业来恢复自然资本的 C 预算?

Can C-budget of natural capital be restored through conservation agriculture in a tropical and subtropical environment?

机构信息

Graduate Program in Agronomy, State University of Maringá, Av. Colombo, 5790 - Zona 7, 87020-900, Maringá, PR, Brazil; Researcher Fellowship, Level 1D - Conselho Nacional de Desenvolvimento Científico e Tecnológico - CNPq, 71605-170, Brasilia, DF, Brazil.

Carbon Management and Sequestration Center, School of Environment and Natural Resources, Distinguished Professor, The Ohio State University, 2021 Coffey Rd, Columbus, OH, 43210, USA.

出版信息

Environ Pollut. 2022 Apr 1;298:118817. doi: 10.1016/j.envpol.2022.118817. Epub 2022 Jan 8.

Abstract

Conservation agriculture through no-till based on cropping systems with high biomass-C input, is a strategy to restoring the carbon (C) lost from natural capital by conversion to agricultural land. We hypothesize that cropping systems based on quantity, diversity and frequency of biomass-C input above soil C dynamic equilibrium level can recover the natural capital. The objectives of this study were to: i) assess the C-budget of land use change for two contrasting climatic environments, ii) estimate the C turnover time of the natural capital through no-till cropping systems, and iii) determine the C pathway since soil under native vegetation to no-till cropping systems. In a subtropical and tropical environment, three types of land use were used: a) undisturbed soil under native vegetation as the reference of pristine level; b) degraded soil through continuous tillage; and c) soil under continuous no-till cropping system with high biomass-C input. At the subtropical environment, the soil under continuous tillage caused loss of 25.4 Mg C ha in the 0-40 cm layer over 29 years. Of this, 17 Mg C ha was transferred into the 40-100 cm layers, resulting in the net negative C balance for 0-100 cm layer of 8.4 Mg C ha with an environmental cost of USD 1968 ha. The 0.59 Mg C ha yr sequestration rate by no-till cropping system promote the C turnover time (soil and vegetation) of 77 years. For tropical environment, the soil C losses reached 27.0 Mg C ha in the 0-100 cm layer over 8 years, with the environmental cost of USD 6155 ha, and the natural capital turnover time through C sequestration rate of 2.15 Mg C ha yr was 49 years. The results indicated that the particulate organic C and mineral associate organic C fractions are the indicators of losses and restoration of C and leading C pathway to recover natural capital through no-till cropping systems.

摘要

基于高生物量-C 投入的种植制度的免耕农业是一种从农业用地转化中恢复自然资本损失的碳 (C) 的策略。我们假设,基于高于土壤 C 动态平衡水平的生物量-C 投入的数量、多样性和频率的种植制度可以恢复自然资本。本研究的目的是:i)评估两种对比气候环境下土地利用变化的 C 预算,ii)通过免耕种植制度估算自然资本的 C 周转时间,iii)确定从原生植被下的土壤到免耕种植制度的 C 途径。在亚热带和热带环境中,使用了三种类型的土地利用:a)未受干扰的原生植被下的土壤作为原始水平的参考;b)通过连续耕作退化的土壤;c)连续免耕种植制度下具有高生物量-C 投入的土壤。在亚热带环境中,连续耕作导致 29 年内 0-40cm 土层损失 25.4 Mg C ha。其中,17 Mg C ha 转移到 40-100cm 层,导致 0-100cm 层的净负 C 平衡为 8.4 Mg C ha,环境成本为 1968 美元 ha。免耕种植制度每年固碳 0.59 Mg C ha,促进了 77 年的 C 周转时间(土壤和植被)。在热带环境中,8 年内 0-100cm 土层的土壤 C 损失达到 27.0 Mg C ha,环境成本为 6155 美元 ha,通过固碳速率 2.15 Mg C ha yr 的自然资本周转时间为 49 年。结果表明,颗粒有机 C 和矿物结合有机 C 分数是 C 损失和恢复的指标,是通过免耕种植制度恢复自然资本的主要 C 途径。

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