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Effects of Afforestation Restoration on Soil Potential N2O Emission and Denitrifying Bacteria After Farmland Abandonment in the Chinese Loess Plateau

机译:黄土高原地区退耕后造林恢复对土壤潜在N2O排放和反硝化细菌的影响

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摘要

Denitrification is a critical component of soil nitrogen (N) cycling, including its role in the production and loss of nitrous oxide (N2O) from the soil system. However, restoration effects on the contribution of denitrification to soil N2O emissions, the abundance and diversity of denitrifying bacteria, and relationships among N2O emissions, soil properties, and denitrifying bacterial community composition remains poorly known. This is particularly true for fragile semiarid ecosystems. In order to address this knowledge gap, we utilized 42-year chronosequence of Robinia pseudoacacia plantations in the Chinese hilly gullied Loess Plateau. Soil potential N2O emission rates were measured using anaerobic incubation experiments. Quantitative polymerase chain reaction (Q-PCR) and Illumina MiSeq high-throughput sequencing were used to reveal the abundance and community composition of denitrifying bacteria. In this study, the afforestation practices following farmland abandonment had a strong negative effect on soil potential N2O emission rates during the first 33 years. However, potential N2O emission rates steadily increased in 42 years of restoration, leading to enhanced potential risk of greenhouse gas emissions. Furthermore, active afforestation increased the abundance of denitrifying functional genes, and enhanced microbial biomass. Actinobacteria and Proteobacteria were the dominant denitrifying bacterial phyla in the 0 to 33-years old sites, while the 42-years sites were dominated by Planctomycetes and Actinobacteria, implying that the restoration performed at these sites promoted soil microbial succession. Finally, correlation analyses revealed that soil organic carbon concentrations had the strongest relationship with potential N2O emission rates, followed by the abundance of the nosZ functional gene, bulk density, and the abundance of Bradyrhizobium and Variovorax across restoration stages. Taken together, our data suggest above-ground restoration of plant communities results in microbial community succession, improved soil quality, and significantly altered N2O emissions.
机译:反硝化是土壤氮(N)循环的关键组成部分,包括其在土壤系统中产生和损失一氧化二氮(N2O)的作用。然而,恢复作用对反硝化对土壤N2O排放的贡献,反硝化细菌的丰度和多样性以及N2O排放,土壤性质和反硝化细菌群落组成之间的关系的影响仍然知之甚少。对于脆弱的半干旱生态系统尤其如此。为了解决这一知识鸿沟,我们利用了中国黄土丘陵黄土高原刺槐人工林的42年时间序列。使用厌氧培养实验测量土壤潜在的N2O排放速率。定量聚合酶链反应(Q-PCR)和Illumina MiSeq高通量测序用于揭示反硝化细菌的丰度和群落组成。在这项研究中,弃耕后的造林措施在头33年中对土壤潜在N2O排放速率产生了强烈的负面影响。但是,在恢复后的42年中,潜在的N2O排放率稳步上升,导致温室气体排放的潜在风险增加。此外,积极的植树造林增加了反硝化功能基因的数量,并增强了微生物的生物量。放线菌和变形杆菌是0到33岁年龄段的主要反硝化细菌门,而42年的位点由浮游菌和放线菌占主导地位,这意味着在这些位置进行的恢复促进了土壤微生物的演替。最后,相关分析表明,土壤有机碳浓度与潜在的N2O排放速率之间存在最强的关系,其次是nosZ功能基因的丰度,堆积密度,以及整个恢复期的Bradyrhizobium和Variovorax的丰度。综上所述,我们的数据表明植物群落的地上恢复可导致微生物群落演替,改善土壤质量并显着改变N2O排放。

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