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Comparison of methanotrophic community and methane oxidation between rhizospheric and non-rhizospheric soils

机译:根际土壤和非根际土壤的甲烷营养群落和甲烷氧化的比较

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Using particulate methane monooxygenase (pMMO) encoding gene, pmoA-based terminal-restrict fragment length polymorphism (T-RFLP), the methanotrophic communities between rhizospheric soils (RSs) and non-rhizospheric soil (NRSs) of landfill cover (LC), riparian wetland (RW) and rice paddy (RP) were compared before and after pre-incubation of 90 days. The ultimate potential ofmethane oxidation rate (UPMOR) and gene copy number of pmoA were evaluated in the soil samples after pre-incubation. Compared to the methanotrophic community in the soil samples before pre-incubation, type II methanotrophs, the Methylocystis- Methylosinus group, was mostly increased after pre-incubation, regardless of the soil type. The UPMOR (11.82 ± 0.27 μmol- CH4· g~(-1)soil-DW·h~(-1)) in the LC-RS was significantly higher than that (9.57 ± 0.14 μmol-CH4· g~(-1)soil-DW·h~(-1)) in the LC-NRS. However, no significant difference was found between RSs and NRSs in the RW (15.28 ± 0.91 and 13.23 ± 0.69 μmol-CH4· g~(-1)soil-DW·h~(-1), respectively) and RP (13.81 ± 1.04 and 12.81 ± 2.40 μmol-CH4· g~(-1)soil-DW·h~(-1), respectively) soils. There was no significantly difference in the gene copy numbers of pmoA in the RSs compared with those in the NRSs at all of the sampling sites. This study provides basic metagenomic information about both rhizospheric and nonrhizospheric methanotrophs, which will be helpful in developing a better strategy of biological methane removal from both natural and anthropogenic major methane sources.
机译:利用颗粒甲烷单加氧酶(pMMO)编码基因,基于pmoA的末端限制性片段长度多态性(T-RFLP),填埋覆盖物(LC),河岸带的根际土壤(RSs)和非根际土壤(NRSs)之间的甲烷营养群落在预培养90天之前和之后比较了湿地(RW)和水稻(RP)。预孵育后,评估土壤样品中甲烷氧化速率(UPMOR)和pmoA基因拷贝数的最终潜力。与预培养前土壤样品中的甲烷营养群落相比,无论土壤类型如何,II型甲烷营养菌(甲基囊藻-甲基肌苷组)在预孵育后大多增加。 LC-RS中的UPMOR(11.82±0.27μmol-CH4·g〜(-1)土壤-DW·h〜(-1))明显高于(9.57±0.14μmol-CH4·g〜(-1) LC-NRS中的(soil-DW·h〜(-1))。但是,RW中的RS和NRS之间没有显着差异(分别为15.28±0.91和13.23±0.69μmol-CH4·g〜(-1)土壤-DW·h〜(-1))和RP(13.81±分别为1.04和12.81±2.40μmol-CH4·g〜(-1)土壤-DW·h〜(-1)土壤。与所有采样位点的NRS相比,RS中pmoA的基因拷贝数没有显着差异。这项研究提供了有关根际和非根际甲烷营养生物的基本宏基因组学信息,这将有助于制定更好的从天然和人为主要甲烷源中去除生物甲烷的策略。

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