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生物炭如何影响土壤硝化作用和硝化诱导的 NO 排放?

How does biochar influence soil nitrification and nitrification-induced NO emissions?

机构信息

Co-Innovation Center for Sustainable Forestry in Southern China, Nanjing Forestry University, No. 159, Longpan Road, Nanjing 210037, China.

Co-Innovation Center for Sustainable Forestry in Southern China, Nanjing Forestry University, No. 159, Longpan Road, Nanjing 210037, China.

出版信息

Sci Total Environ. 2024 Jan 15;908:168530. doi: 10.1016/j.scitotenv.2023.168530. Epub 2023 Nov 13.

Abstract

Nitrification is a major pathway of NO production, especially in aerobic soils. The amendment of soils with biochar has been suggested as a promising solution to regulate soil N cycle and reduce NO emissions. However, there is a lack of comprehensive and quantitative understanding of biochar impacts on soil nitrification and nitrification-induced NO emissions. In this study, a meta-analysis was conducted using data compiled across 95 peer-reviewed studies. Results showed that biochar in general significantly increased soil nitrification rate by 56 %, with overall no significant effect on nitrification-induced NO emissions, suggesting that biochar likely restricted the fraction of nitrified N emitted as NO emissions. The abundance of ammonia-oxidizing bacteria (AOB) was significantly increased by 37 % following biochar addition, but that of ammonia-oxidizing archaea (AOA) did not change significantly, indicating that the impact of biochar on AOB rather than AOA may play an important role in soil nitrification. The impacts of biochar on soil nitrification processes were heterogeneous depending on soil properties. Biochar increased soil nitrification rate and AOB abundance to a larger extent in poorly pH-buffered soils such as those with acidic pH (<5), low organic carbon (<10 g kg), or poor texture (rich in either sand or clay), which may be attributed to the liming and structural effects of biochar that regulate soil pH and water-air status. The overall no significant effect of biochar on nitrification-induced NO emissions was due to a positive effect in acidic soils, a negative effect in alkaline soils, and little effect in neutral soils. This study provides a comprehensive insight into how different factors mediate the response of soil nitrification processes to biochar amendment, which contributes to a new understanding of biochar function in regulating soil NO emissions, and can assist in designing biochar projects that would benefit soil N cycle while minimizing undesirable side effects.

摘要

硝化作用是氮素产生的主要途径,特别是在有氧土壤中。有人建议用生物炭来改良土壤,以调节土壤氮循环并减少一氧化二氮排放,这是一种很有前途的方法。然而,我们对生物炭对土壤硝化作用和硝化作用诱导的一氧化二氮排放的影响缺乏全面和定量的认识。在这项研究中,我们使用了 95 篇同行评议研究的综合数据进行了荟萃分析。结果表明,生物炭通常会使土壤硝化速率显著提高 56%,但对硝化作用诱导的一氧化二氮排放没有显著影响,这表明生物炭可能限制了作为一氧化二氮排放的硝化氮的比例。生物炭添加后,氨氧化细菌(AOB)的丰度显著增加了 37%,而氨氧化古菌(AOA)的丰度没有显著变化,这表明生物炭对 AOB 的影响而不是 AOA 的影响可能在土壤硝化作用中发挥重要作用。生物炭对土壤硝化过程的影响因土壤特性而异。生物炭在 pH 值较低(<5)、有机碳含量较低(<10 g kg)或质地较差(富含砂或粘土)的缓冲能力较差的土壤中,更能显著提高土壤硝化速率和 AOB 的丰度,这可能归因于生物炭的石灰化和结构效应,这些效应调节了土壤 pH 值和水-气状况。生物炭对硝化作用诱导的一氧化二氮排放的整体无显著影响是由于在酸性土壤中存在正效应,在碱性土壤中存在负效应,而在中性土壤中几乎没有影响。本研究全面了解了不同因素如何调节土壤硝化过程对生物炭添加的响应,这有助于更好地理解生物炭在调节土壤一氧化二氮排放方面的功能,并有助于设计有利于土壤氮循环而最小化不良副作用的生物炭项目。

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