Methanogenesis and Methane Oxidation in Paddy Fields under Organic Fertilization

C. Kim, Denver I. Walitang, T. Sa
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引用次数: 3

Abstract

BACKGROUND: Global warming is one of the most pressing environmental issues which concomitantly complicates global climate change. Methane emission is a balance between methanogenesis and methane consumption, both of which are driven by microbial actions in different ecosystems producing methane, one of the major greenhouse gases. Paddy fields are major sources of anthropogenic methane emissions and could be compounded by organic fertilization. METHODS AND RESULTS: Literature reviews were conducted to give an overview of the global warming conditions and to present the relationship of carbon and methane to greenhouse gas emissions, and the need to understand the underlying processes of methane emission. A more extensive review was done from studies on methane emission in paddy fields under organic fertilization with greater emphasis on long term amendments. Changes in paddy soils due to organic fertilization include alterations of the physicochemical properties and changes in biological components. There are diverse phylogenetic groups of methanogens and methane oxidizing bacteria involved in methane emission. Also, multiple factors influence methanogenesis and methane oxidation in rice paddy fields under organic fertilization and they should be greatly considered when developing mitigating steps in methane emission in paddy fields especially under long term organic fertilization. CONCLUSION(S): This review showed that organic fertilization, particularly for long term management practices, influenced both physicochemical and biological components of the paddy fields which could ultimately affect methanogenesis, methane oxidation, and methane emission. Understanding interrelated factors affecting methane emission helps create ways to mitigate their impact on global warming and climate change.
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有机施肥对稻田产甲烷和甲烷氧化的影响
背景:全球变暖是最紧迫的环境问题之一,它伴随着全球气候变化的复杂化。甲烷排放是甲烷生成和甲烷消耗之间的平衡,两者都是由不同生态系统中产生甲烷(主要温室气体之一)的微生物活动驱动的。水田是人为甲烷排放的主要来源,可通过有机施肥加以补充。方法与结果:通过文献综述,概述了全球变暖状况,提出了碳和甲烷与温室气体排放的关系,以及了解甲烷排放潜在过程的必要性。从有机施肥对稻田甲烷排放的研究中进行了更广泛的回顾,更侧重于长期修正。有机施肥对水稻土的影响包括理化性质的改变和生物成分的变化。产甲烷菌和甲烷氧化菌参与甲烷排放的系统发育类群不同。此外,有机施肥对稻田甲烷生成和氧化的影响是多方面的,在制定减少稻田甲烷排放的措施时应充分考虑这些因素,特别是在长期有机施肥条件下。结论:有机施肥,特别是长期施用,会影响稻田的物理化学和生物成分,最终影响甲烷生成、甲烷氧化和甲烷排放。了解影响甲烷排放的相关因素有助于找到减轻其对全球变暖和气候变化影响的方法。
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