{"title":"特定根长调节根瘤对不同大型植物反硝化作用的影响","authors":"","doi":"10.1016/j.geoderma.2024.117002","DOIUrl":null,"url":null,"abstract":"<div><p>Macrophytes influence nitrogen (N) removal from wetlands. However, the specific plant traits responsible for this effect and the related microbial mechanisms remain largely unknown, especially root traits. In a mesocosm experiment, we determined the rhizosphere effect (RE) on microbial N removal processes by incubating rhizosphere and bulk soils collected from 11 macrophyte species. In addition, we examined root traits (involved in chemistry and morphology), along with examining the diversity, compositions, and abundance of bacterial communities involved in denitrification (<em>nirS</em> and <em>nirK</em>) and anammox (<em>hzsB</em>). Across the 11 macrophyte species, the positive RE on denitrification ranged from 66% to 412%, with an average of 194.72%. RE on denitrification was significantly and positively correlated with the recruitment of <em>nir-type</em> denitrifiers in the rhizosphere. We found that higher specific root length (SRL) root promoted the stronger RE, by increasing the abundance of <em>nir</em>-type denitrifiers and further enhancing N removal. Net N removal from water in the wetlands increased with a higher positive RE on <em>nir-type</em> denitrifiers. In addition, SRL significantly influenced the compositions of denitrifiers in the rhizosphere soil. We further found that the enrichment of <em>Azospira</em>, <em>Bradyrhizobium</em>, <em>Sinorhizobium</em>, <em>Rhodopseudomonas</em>, Alcaligenaceae, Bradyrhizobiaceae, and <em>Pleomorphomonas</em> improved the denitrification rate. These findings highlight the potential of root morphology in regulating plant–microbe interactions, thereby improving water purification.</p></div>","PeriodicalId":12511,"journal":{"name":"Geoderma","volume":null,"pages":null},"PeriodicalIF":5.6000,"publicationDate":"2024-08-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S0016706124002313/pdfft?md5=ae5949ef90c62cb9919a6c981c1c1104&pid=1-s2.0-S0016706124002313-main.pdf","citationCount":"0","resultStr":"{\"title\":\"Specific root length regulated the rhizosphere effect on denitrification across distinct macrophytes\",\"authors\":\"\",\"doi\":\"10.1016/j.geoderma.2024.117002\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><p>Macrophytes influence nitrogen (N) removal from wetlands. However, the specific plant traits responsible for this effect and the related microbial mechanisms remain largely unknown, especially root traits. In a mesocosm experiment, we determined the rhizosphere effect (RE) on microbial N removal processes by incubating rhizosphere and bulk soils collected from 11 macrophyte species. In addition, we examined root traits (involved in chemistry and morphology), along with examining the diversity, compositions, and abundance of bacterial communities involved in denitrification (<em>nirS</em> and <em>nirK</em>) and anammox (<em>hzsB</em>). Across the 11 macrophyte species, the positive RE on denitrification ranged from 66% to 412%, with an average of 194.72%. RE on denitrification was significantly and positively correlated with the recruitment of <em>nir-type</em> denitrifiers in the rhizosphere. We found that higher specific root length (SRL) root promoted the stronger RE, by increasing the abundance of <em>nir</em>-type denitrifiers and further enhancing N removal. Net N removal from water in the wetlands increased with a higher positive RE on <em>nir-type</em> denitrifiers. In addition, SRL significantly influenced the compositions of denitrifiers in the rhizosphere soil. We further found that the enrichment of <em>Azospira</em>, <em>Bradyrhizobium</em>, <em>Sinorhizobium</em>, <em>Rhodopseudomonas</em>, Alcaligenaceae, Bradyrhizobiaceae, and <em>Pleomorphomonas</em> improved the denitrification rate. 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引用次数: 0
摘要
大型营养体会影响湿地对氮(N)的去除。然而,造成这种影响的具体植物特征以及相关的微生物机制在很大程度上仍不为人所知,尤其是根系特征。在一个中观宇宙实验中,我们通过培养从 11 种大型营养繁殖植物采集的根圈土壤和块状土壤,确定了根圈效应(RE)对微生物脱氮过程的影响。此外,我们还考察了根系特征(涉及化学和形态),以及参与反硝化作用(和)和氨氧化作用()的细菌群落的多样性、组成和丰度。在 11 种大型藻类中,反硝化的正 RE 值从 66% 到 412% 不等,平均为 194.72%。反硝化的 RE 与根瘤中反硝化物的增加呈显著正相关。我们发现,根系比长(SRL)越高,反硝化作用越强,因为它能增加-型反硝化细菌的数量,进一步提高对氮的去除率。反硝化细菌的正向 RE 越高,湿地水中的净氮去除率就越高。此外,SRL 对根瘤土壤中反硝化细菌的组成也有很大影响。我们进一步发现,富集Ⅴ、Ⅴ、Ⅴ、Alcaligenaceae、Bradyrhizobiaceae 和提高反硝化率。这些发现凸显了根系形态在调节植物与微生物相互作用方面的潜力,从而提高了水的净化能力。
Specific root length regulated the rhizosphere effect on denitrification across distinct macrophytes
Macrophytes influence nitrogen (N) removal from wetlands. However, the specific plant traits responsible for this effect and the related microbial mechanisms remain largely unknown, especially root traits. In a mesocosm experiment, we determined the rhizosphere effect (RE) on microbial N removal processes by incubating rhizosphere and bulk soils collected from 11 macrophyte species. In addition, we examined root traits (involved in chemistry and morphology), along with examining the diversity, compositions, and abundance of bacterial communities involved in denitrification (nirS and nirK) and anammox (hzsB). Across the 11 macrophyte species, the positive RE on denitrification ranged from 66% to 412%, with an average of 194.72%. RE on denitrification was significantly and positively correlated with the recruitment of nir-type denitrifiers in the rhizosphere. We found that higher specific root length (SRL) root promoted the stronger RE, by increasing the abundance of nir-type denitrifiers and further enhancing N removal. Net N removal from water in the wetlands increased with a higher positive RE on nir-type denitrifiers. In addition, SRL significantly influenced the compositions of denitrifiers in the rhizosphere soil. We further found that the enrichment of Azospira, Bradyrhizobium, Sinorhizobium, Rhodopseudomonas, Alcaligenaceae, Bradyrhizobiaceae, and Pleomorphomonas improved the denitrification rate. These findings highlight the potential of root morphology in regulating plant–microbe interactions, thereby improving water purification.
期刊介绍:
Geoderma - the global journal of soil science - welcomes authors, readers and soil research from all parts of the world, encourages worldwide soil studies, and embraces all aspects of soil science and its associated pedagogy. The journal particularly welcomes interdisciplinary work focusing on dynamic soil processes and functions across space and time.