Potential of biochar to mitigate methane production in paddy soils—application of a new incubation and modelling approach

IF 3.7 3区 环境科学与生态学 Q2 ENVIRONMENTAL SCIENCES Biogeochemistry Pub Date : 2024-12-23 DOI:10.1007/s10533-024-01200-9
Thomas Middelanis, Dana Looschelders, Peter Mueller, Klaus-Holger Knorr
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Abstract

Paddy soils are a significant source of methane (CH4) affecting the global climate. Therefore, it is important to investigate both emission mitigation strategies and the underlying biogeochemical processes. The application of biochar into paddy soils has emerged as a promising measure to mitigate CH4 emissions. However, it has not yet been clarified why such effects are usually weaker in field studies than in laboratory incubations and which properties of biochar specifically decrease the production of CH4. We conducted two incubation experiments, one with 1.5% addition of untreated biochars and one with same amounts, but pH-levelled, rinsed biochars. According to the common experimental design of existing incubation studies (experiment 1) biochar addition induced a mean soil pH increase of 0.28 after anaerobic incubation compared to the contro. In these treatments, biochar significantly extended the pre-methanogenic stage (mean 24.23%). However, this effect was weakened or even reversed when pH-levelled, rinsed biochars were amended in experiment 2, which was intended to mimic the persistent long-term effects in the field. This indicated that the provision of electron accepting capacities to suppress methanogenesis may be less important than previously thought. The addition of biochar significantly lowered CH4 production rates m in both experiments with no significant influence of the pH (mean 25.89%), though. Our study demonstrated that incubation studies on CH4 production in paddy soils can be improved by separating the pre-methanogenic and the methanogenic stage. This facilitates future research to compare characteristics of biochar, but also combinations of measures to optimise CH4 mitigation strategies.

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生物炭在水稻土中减少甲烷产生的潜力——一种新的孵化和建模方法的应用
水稻土是影响全球气候的重要甲烷(CH4)来源。因此,研究减排战略和潜在的生物地球化学过程十分重要。在水稻土中应用生物炭是一种很有希望减少甲烷排放的措施。然而,目前尚不清楚为什么这种效应在实地研究中通常比在实验室孵育中弱,以及生物炭的哪些特性会特异性地减少CH4的产生。我们进行了两项培养实验,一项是添加1.5%未经处理的生物炭,另一项是添加相同数量但ph水平的漂洗生物炭。根据现有培养研究的常见实验设计(实验1),添加生物炭诱导厌氧培养后土壤pH比对照平均增加0.28。在这些处理中,生物炭显著延长了产甲烷前阶段(平均24.23%)。然而,在实验2中,当ph水平的漂洗生物炭被修正时,这种效果被削弱甚至逆转,这是为了模拟田间持续的长期影响。这表明提供电子接受能力来抑制甲烷生成可能没有以前认为的那么重要。在两个实验中,生物炭的添加均显著降低了CH4产率m,但对pH的影响不显著(平均为25.89%)。本研究表明,通过分离产甲烷前阶段和产甲烷阶段,可以提高水稻土CH4产气量的培养研究。这有利于未来比较生物炭特性的研究,也有利于优化CH4减缓策略的措施组合。
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来源期刊
Biogeochemistry
Biogeochemistry 环境科学-地球科学综合
CiteScore
7.10
自引率
5.00%
发文量
112
审稿时长
3.2 months
期刊介绍: Biogeochemistry publishes original and synthetic papers dealing with biotic controls on the chemistry of the environment, or with the geochemical control of the structure and function of ecosystems. Cycles are considered, either of individual elements or of specific classes of natural or anthropogenic compounds in ecosystems. Particular emphasis is given to coupled interactions of element cycles. The journal spans from the molecular to global scales to elucidate the mechanisms driving patterns in biogeochemical cycles through space and time. Studies on both natural and artificial ecosystems are published when they contribute to a general understanding of biogeochemistry.
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