天然草地转为农业或松树种植园:对土壤甲烷吸收的影响

IF 5 3区 农林科学 Q1 SOIL SCIENCE Soil Use and Management Pub Date : 2024-01-30 DOI:10.1111/sum.13017
María De Bernardi, Maria Eugenia Priano, Maria Elena Fernández, Javier Gyenge, Maria Paula Juliarena
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引用次数: 0

摘要

高地土壤是甲烷(CH4)被甲烷营养细菌消耗的唯一已知生物汇。这一过程主要受限于与土壤物理特性相关的扩散过程,而土壤物理特性会因土地用途的改变而改变,这取决于土壤类型、原有系统和转换后的新土地用途。我们的研究重点是确定土地利用的变化(从天然草地到农田和两种辐射松造林,在疏伐管理上有所不同)导致的土壤甲烷吸收量的差异,以及确定哪些是控制所研究土壤类型(Hapludoll)甲烷吸收量的主要驱动因素,重点是扩散过程。2015 年 10 月至 2019 年 4 月期间,采用静态室技术对 CH4 通量进行了 12 次测量。此外,还在相同日期测量了土壤剖面中的 CH4 梯度浓度以及物理和化学变量。所研究的所有土地利用方式都是CH4的净吸收汇。从草地到农业的土地利用变化减少了土壤对CH4的吸收(约37%±19),而植树造林则增加了(约85%±73)这一与天然草地相关的环境服务。我们发现,控制这种土壤对甲烷吸收的主要驱动因素是水和充满空气的孔隙空间,它们是控制土壤甲烷扩散的变量;它们主要与土地利用之间的容重差异(压实度)有关。有机质也是一个重要的驱动因素,主要与土壤结构有关。土地利用的变化影响了所有这些驱动因素。只有在管理不同(修剪和疏伐与无管理)的两个造林地中,较深土层的 CH4 浓度才存在差异。然而,两者对 CH4 的吸收量并无显著差异,这表明不需要很高的树木覆盖率来增加土壤的 CH4 吸收汇。这种树木和草本植物的混合覆盖可能会产生类似的环境服务产出,从而增加土地用途的选择性。
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Natural grassland conversion to agriculture or pine plantations: Effects on soil methane uptake
Upland soils are the only known biological sink for methane (CH4) by methanotrophic bacteria consumption. This process is mainly limited by the diffusion processes related to the soil's physical characteristics, which can be modified because of changes in land use depending on the soil type, the original system and the new land use converted. Our study focused on determining the differences in soil CH4 uptake because of changes in land use (from natural grassland to agricultural land and two Pinus radiata afforestation, differing in thinning management) and on determining which are the main drivers that control CH4 uptake in the studied soil type (Hapludoll), with focus on the diffusion process. CH4 fluxes were measured 12 times with the static chamber technique between October 2015 and April 2019. Also, CH4 gradient concentration in the soil profile and physical and chemical variables were measured on the same dates. All land uses studied acted as net CH4 sinks. Land-use change from grassland to agriculture decreased soil CH4 uptake (~37% ± 19), whereas afforestation increased (~85% ± 73) this environmental service related to natural grassland. We found that the main drivers that control CH4 uptake in this soil are water and air-filled pore space, variables that govern soil CH4 diffusion; they are mostly related to differences in bulk density (compaction) among land uses. Organic matter was also an important driver, mainly related to soil structure. Land-use change affected all of these drivers. CH4 concentration presented differences at deeper soil layers only in the two afforestations, which differed in management (pruning and thinning vs. no management). However, CH4 uptake did not present significant differences between them, suggesting that there is no need for a high tree cover to increase the CH4 sink of the soil. This mixed tree and herbaceous cover may result in a similar environmental service output, increasing the options of land uses.
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来源期刊
Soil Use and Management
Soil Use and Management 农林科学-土壤科学
CiteScore
7.70
自引率
13.20%
发文量
78
审稿时长
3 months
期刊介绍: Soil Use and Management publishes in soil science, earth and environmental science, agricultural science, and engineering fields. The submitted papers should consider the underlying mechanisms governing the natural and anthropogenic processes which affect soil systems, and should inform policy makers and/or practitioners on the sustainable use and management of soil resources. Interdisciplinary studies, e.g. linking soil with climate change, biodiversity, global health, and the UN’s sustainable development goals, with strong novelty, wide implications, and unexpected outcomes are welcomed.
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