Wanyu Shen , Yang Ji , Zhongjun Jia , Qiong Huang , Xiaoli Zhu , Jing Ma , Zhenke Zhu , Tida Ge , Guangbin Zhang , Hua Xu
{"title":"两种水稻土中秸秆通过不同产甲烷途径产生甲烷的研究","authors":"Wanyu Shen , Yang Ji , Zhongjun Jia , Qiong Huang , Xiaoli Zhu , Jing Ma , Zhenke Zhu , Tida Ge , Guangbin Zhang , Hua Xu","doi":"10.1016/j.apsoil.2025.106524","DOIUrl":null,"url":null,"abstract":"<div><div>Straw returning provides large carbon sources to paddy soils, stimulating CH<sub>4</sub> production and emissions. However, the effects of straw types (rice and maize, corresponding to C3 and C4 plants) on the methanogenic pathway and microbial mechanisms are still unknown. Here, two paddy soils [rice-wheat rotation soil (RW) and permanently flooded soil (PF)] were anaerobically incubated with rice straw (RS) and maize straw (MS) additions to investigate the response of methanogenic pathways and archaeal communities to straw addition. Our results showed that the produced CH<sub>4</sub> with MS addition was significantly enriched in <sup>13</sup>C than that of others, with δ<sup>13</sup>CH<sub>4</sub>-values ranging from −39.22 ‰ to −44.99 ‰ and − 48.31 ‰ to −53.19 ‰, respectively. Moreover, CH<sub>4</sub> production potential was increased by 95 %–100 % in RW soil and 161 %–207 % in PF soil with straw addition, compared with no straw addition (13.1–16.6 μg CH<sub>4</sub> g<sup>−1</sup> d<sup>−1</sup>). This stimulation in RW soil was probably associated with the increase in hydrogenotrophic methanogenesis by straw addition. Indeed, the contribution of hydrogenotrophic methanogenesis to total CH<sub>4</sub> production (1– <em>f</em><sub>ac</sub>) increased from 55 % in control (CK) to 75 % in RS addition, and to 85 % in MS addition. Meanwhile, the relative abundance of hydrogenotrophic <em>Methanobacterium</em> increased from 10 % to 20 % (RS) and 25 % (MS), respectively. Straw addition significantly increased acetate consumption in RW soil, indicating that acetate might first transfer to CO<sub>2</sub>/H<sub>2</sub> and then to CH<sub>4</sub> rather than directly to CH<sub>4</sub>. For PF soil, the significant increase in CH<sub>4</sub> production by RS addition was also likely ascribed to the rise of 1– <em>f</em><sub>ac</sub> and hydrogenotrophic <em>Methanobacterium</em>. In contrast, MS addition mainly promoted acetoclastic methanogenesis to stimulate CH<sub>4</sub> production, with <em>f</em><sub><em>ac</em></sub>-values increased from 70 % to 80 % and relative abundance of acetoclastic <em>Methanosarcina</em> increased from 60 % to 70 %. The findings show that the differences in methanogens and carbon isotopic caused by straw types are key factors affecting methanogenic pathways, and further provide valuable insights into the methanogenic mechanisms under straw addition in different paddy soils.</div></div>","PeriodicalId":8099,"journal":{"name":"Applied Soil Ecology","volume":"216 ","pages":"Article 106524"},"PeriodicalIF":5.0000,"publicationDate":"2025-10-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Straw-mediated CH4 production via distinct methanogenic pathways in two paddy soils\",\"authors\":\"Wanyu Shen , Yang Ji , Zhongjun Jia , Qiong Huang , Xiaoli Zhu , Jing Ma , Zhenke Zhu , Tida Ge , Guangbin Zhang , Hua Xu\",\"doi\":\"10.1016/j.apsoil.2025.106524\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Straw returning provides large carbon sources to paddy soils, stimulating CH<sub>4</sub> production and emissions. However, the effects of straw types (rice and maize, corresponding to C3 and C4 plants) on the methanogenic pathway and microbial mechanisms are still unknown. Here, two paddy soils [rice-wheat rotation soil (RW) and permanently flooded soil (PF)] were anaerobically incubated with rice straw (RS) and maize straw (MS) additions to investigate the response of methanogenic pathways and archaeal communities to straw addition. Our results showed that the produced CH<sub>4</sub> with MS addition was significantly enriched in <sup>13</sup>C than that of others, with δ<sup>13</sup>CH<sub>4</sub>-values ranging from −39.22 ‰ to −44.99 ‰ and − 48.31 ‰ to −53.19 ‰, respectively. Moreover, CH<sub>4</sub> production potential was increased by 95 %–100 % in RW soil and 161 %–207 % in PF soil with straw addition, compared with no straw addition (13.1–16.6 μg CH<sub>4</sub> g<sup>−1</sup> d<sup>−1</sup>). This stimulation in RW soil was probably associated with the increase in hydrogenotrophic methanogenesis by straw addition. Indeed, the contribution of hydrogenotrophic methanogenesis to total CH<sub>4</sub> production (1– <em>f</em><sub>ac</sub>) increased from 55 % in control (CK) to 75 % in RS addition, and to 85 % in MS addition. Meanwhile, the relative abundance of hydrogenotrophic <em>Methanobacterium</em> increased from 10 % to 20 % (RS) and 25 % (MS), respectively. Straw addition significantly increased acetate consumption in RW soil, indicating that acetate might first transfer to CO<sub>2</sub>/H<sub>2</sub> and then to CH<sub>4</sub> rather than directly to CH<sub>4</sub>. For PF soil, the significant increase in CH<sub>4</sub> production by RS addition was also likely ascribed to the rise of 1– <em>f</em><sub>ac</sub> and hydrogenotrophic <em>Methanobacterium</em>. In contrast, MS addition mainly promoted acetoclastic methanogenesis to stimulate CH<sub>4</sub> production, with <em>f</em><sub><em>ac</em></sub>-values increased from 70 % to 80 % and relative abundance of acetoclastic <em>Methanosarcina</em> increased from 60 % to 70 %. The findings show that the differences in methanogens and carbon isotopic caused by straw types are key factors affecting methanogenic pathways, and further provide valuable insights into the methanogenic mechanisms under straw addition in different paddy soils.</div></div>\",\"PeriodicalId\":8099,\"journal\":{\"name\":\"Applied Soil Ecology\",\"volume\":\"216 \",\"pages\":\"Article 106524\"},\"PeriodicalIF\":5.0000,\"publicationDate\":\"2025-10-10\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Applied Soil Ecology\",\"FirstCategoryId\":\"97\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0929139325006626\",\"RegionNum\":2,\"RegionCategory\":\"农林科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"SOIL SCIENCE\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Applied Soil Ecology","FirstCategoryId":"97","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0929139325006626","RegionNum":2,"RegionCategory":"农林科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"SOIL SCIENCE","Score":null,"Total":0}
Straw-mediated CH4 production via distinct methanogenic pathways in two paddy soils
Straw returning provides large carbon sources to paddy soils, stimulating CH4 production and emissions. However, the effects of straw types (rice and maize, corresponding to C3 and C4 plants) on the methanogenic pathway and microbial mechanisms are still unknown. Here, two paddy soils [rice-wheat rotation soil (RW) and permanently flooded soil (PF)] were anaerobically incubated with rice straw (RS) and maize straw (MS) additions to investigate the response of methanogenic pathways and archaeal communities to straw addition. Our results showed that the produced CH4 with MS addition was significantly enriched in 13C than that of others, with δ13CH4-values ranging from −39.22 ‰ to −44.99 ‰ and − 48.31 ‰ to −53.19 ‰, respectively. Moreover, CH4 production potential was increased by 95 %–100 % in RW soil and 161 %–207 % in PF soil with straw addition, compared with no straw addition (13.1–16.6 μg CH4 g−1 d−1). This stimulation in RW soil was probably associated with the increase in hydrogenotrophic methanogenesis by straw addition. Indeed, the contribution of hydrogenotrophic methanogenesis to total CH4 production (1– fac) increased from 55 % in control (CK) to 75 % in RS addition, and to 85 % in MS addition. Meanwhile, the relative abundance of hydrogenotrophic Methanobacterium increased from 10 % to 20 % (RS) and 25 % (MS), respectively. Straw addition significantly increased acetate consumption in RW soil, indicating that acetate might first transfer to CO2/H2 and then to CH4 rather than directly to CH4. For PF soil, the significant increase in CH4 production by RS addition was also likely ascribed to the rise of 1– fac and hydrogenotrophic Methanobacterium. In contrast, MS addition mainly promoted acetoclastic methanogenesis to stimulate CH4 production, with fac-values increased from 70 % to 80 % and relative abundance of acetoclastic Methanosarcina increased from 60 % to 70 %. The findings show that the differences in methanogens and carbon isotopic caused by straw types are key factors affecting methanogenic pathways, and further provide valuable insights into the methanogenic mechanisms under straw addition in different paddy soils.
期刊介绍:
Applied Soil Ecology addresses the role of soil organisms and their interactions in relation to: sustainability and productivity, nutrient cycling and other soil processes, the maintenance of soil functions, the impact of human activities on soil ecosystems and bio(techno)logical control of soil-inhabiting pests, diseases and weeds.