连续13年不同麦秆施用量的稻田土壤甲烷排放效应与微生物机制[*]
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土壤与农业可持续发展全国重点实验室中国科学院南京土壤研究所

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Soil methane emission effects and microbial mechanisms of rice field soils with different rice straw application rates over 13 consecutive years
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State Key Laboratory of Soil and Sustainable Agriculture,Institute of Soil Science,Chinese Academy of Sciences

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    摘要:

    探究长期秸秆还田对稻田甲烷(CH4)排放的影响及其微生物驱动机制,可为优化长期秸秆还田管理、协同实现“固碳减排”提供理论依据。基于连续13年(2006~2018)的稻麦轮作定位试验,设置4个秸秆还田梯度处理:S0(对照,0 t·hm-2)、S1(1.6 t·hm-2)、S2(3.2 t·hm-2)、S3(4.8 t·hm-2),观测2017~2018年间稻季CH4排放及相关土壤环境因子变化。研究结果表明,秸秆还田量与CH4累积排放量呈显著正相关,S1、S2和S3处理的累积排放量相较于S0处理分别增加166%~219%、420%~527%和660%~785%。这可能是由于秸秆输入提升土壤有机碳和可溶性有机碳含量,并降低土壤氧化还原电位,形成强厌氧环境,从而显著提高产甲烷菌功能基因(mcrA)丰度(S1、S2和S3处理较S0处理分别增加2.5、3.8和3.6倍)并富集多底物代谢的甲烷八叠球菌科(Methanosarcinaceae),导致CH4产生潜力大幅增加(S1、S2和S3处理较S0提升45%、103%和246%)。尽管甲烷氧化菌功能基因(pmoA)丰度及氧化潜力亦有所增加,但氧化潜力增幅远低于产生潜力增幅,造成“产生多氧化少”的代谢失衡,进一步加剧了CH4净排放。此外,S3虽能提升土壤固碳速率,但其减缓效益抵消率最高(12.93),而中低量还田(S1、S2)在减缓效益抵消率无显著差异的条件下,S1处理CH4排放系数最低(5.05%),S2处理固碳速率最高(2.27 t CO2-eq t·hm-2·a-1),说明中低量秸秆还田可实现固碳与减排的协同。因此,适度秸秆还田可能是协调稻田“增汇”与“减排”矛盾的关键措施。

    Abstract:

    【Objective】Investigating the long-term effects of straw returning on methane (CH4) emissions in rice paddies and their microbial driving mechanisms can provide a theoretical basis for optimizing long-term straw returning management and synergistically achieving "carbon sequestration and emission reduction".【Method】Based on a continuous 13-year (2006~2018) field experiment with rice-wheat rotation, four straw returning gradients were established: S0 (control at 0 t·hm-2), S1 (1.6 t·hm-2), S2 (3.2 t·hm-2), and S3 (4.8 t·hm-2). The changes in CH4 emissions during the rice season (2017~2018) and related soil environmental factors were observed.【Result】The results showed a significant positive correlation between straw returning amount and cumulative CH4 emissions, with the cumulative emissions in S1, S2, and S3 treatments increasing by166%~219%、420%~527% and 660%~785% compared to S0, respectively. The microbial mechanism lies in the fact that straw input enhances soil organic carbon and dissolved organic carbon content while reducing soil redox potential, creating a strongly anaerobic environment. This significantly increases the abundance of methanogenic functional genes (mcrA) (with average increases of 2.5, 3.8, and 3.6 times compared to S0 for S1, S2, and S3, respectively) and enriches the Methanosarcinaceae family, which metabolizes multiple substrates, leading to a substantial increase in CH4 production potential (S3 increased by 246% compared to S0). Although the abundance and oxidation potential of methanotrophic functional genes (pmoA) also increased, the growth was far lower than the production potential, resulting in a metabolic imbalance of "more production than oxidation", further exacerbating net CH4 emissions.【Conclusion】Additionally, although S3 could enhance soil carbon sequestration rates, it had the highest mitigation benefit offset rate (12.93). In contrast, under conditions where there was no significant difference in mitigation benefit offset rates, S1 achieved the lowest CH4 emission coefficient (5.05%), while S2 achieved the highest carbon sequestration rate (2.27 t CO2-eq t·hm-2·a-1), indicating that moderate straw returning optimally synergizes carbon sequestration and emission reduction. Therefore, moderate straw returning is a key measure to reconcile the contradiction between "carbon sequestration" and "emission reduction" in rice paddies.

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李毓莹,黄琼,金柯达,张广斌,马静,徐华[†].连续13年不同麦秆施用量的稻田土壤甲烷排放效应与微生物机制[*][J].土壤学报,,[待发表]
LI Yuying, HUANG Qiong, JIN Keda, ZHANG Guangbin, MA Jing, XU Hua†. Soil methane emission effects and microbial mechanisms of rice field soils with different rice straw application rates over 13 consecutive years[J]. Acta Pedologica Sinica,,[In Press]

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  • 收稿日期:2025-11-10
  • 最后修改日期:2026-04-20
  • 录用日期:2026-06-10
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