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Long-term sulfide input enhances chemoautotrophic denitrification rather than DNRA in freshwater lake sediments

机译:长期硫化物输入增强了淡水湖沉积物中的化学营养脱氮而不是DNRA

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摘要

Partitioning between nitrate reduction pathways, denitrification and dissimilatory nitrate reduction to ammonium (DNRA) determines the fate of nitrate removal and thus it is of great ecological importance. Sulfide (S2-) is a potentially important factor that influences the role of denitrification and DNRA. However, information on the impact of microbial mechanisms for S2- on the partitioning of nitrate reduction pathways in freshwater environments is still lacking. This study investigated the effects of long-term (108 d) S2- addition on nitrate reduction pathways and microbial communities in the sediments of two different freshwater lakes. The results show that the increasing S2- addition enhanced the coupling of S2- oxidation with denitrification instead of DNRA. The sulfide-oxidizing denitrifier, Thiobacillus, was significantly enriched in the incubations of both lake samples with S2- addition, which indicates that it may be the key genus driving sulfide-oxidizing denitrification in the lake sediments. During S2- incubation of the Hongze Lake sample, which had lower inherent organic carbon (C) and sulfate (SO42-), Thiobacillus was more enriched and played a dominant role in the microbial community; while during that of the Nansi Lake sample, which had higher inherent organic C and SO42-, Thiobacillus was less enriched, but increasing abundances of sulfate reducing bacteria (Desulfomicrobium, Desulfatitalea and Geothermobacter) were observed. Moreover, sulfide-oxidizing denitrifiers and sulfate reducers were enriched in the Nansi Lake control treatment without external S2- input, which suggests that internal sulfate release may promote the cooperation between sulfide-oxidizing denitrifiers and sulfate reducers. This study highlights the importance of sulfide-driven denitrification and the close coupling between the N and S cycles in freshwater environments, which are factors that have often been overlooked. (C) 2020 Elsevier Ltd. All rights reserved.
机译:硝酸盐还原途径之间的分区,硝酸硝化和硝酸盐还原对铵(DNRA)决定了硝酸盐去除的命运,因此它具有很大的生态重要性。硫化物(S2-)是影响反硝化和DNRA的作用的潜在重要因素。然而,关于微生物机制S2的影响的信息仍然缺乏淡水环境中硝酸盐还原途径的分配。本研究调查了长期(108d)S2-添加对两种不同淡水湖泊沉积物中的硝酸盐还原途径和微生物群落的影响。结果表明,增加的S2-添加增强了S2-氧化与反硝化而不是DNRA的偶联。硫化硫化物氧化反硝基硫杆菌在湖泊样品的培养中显着富集,表明它可能是在湖泊沉积物中排出硫化物氧化反硝化的关键属。在S2-孵育洪泽湖样品中,炎湖样品具有低固有的有机碳(C)和硫酸盐(SO 42-),硫嘧磺酸盐更富集并在微生物群落中发挥显着作用;虽然在纳西湖样品中,其具有较高的固有有机C和SO42-的,但硫胞嘧啶的富含富集,但观察到硫酸盐还原细菌(脱硫纤维素,脱硫和地热杆菌)的增加。此外,富含硫化硫化的脱氮剂和硫酸盐还原剂,在没有外部S2的情况下富集纳西湖控制处理,这表明内部硫酸盐释放可以促进硫化物氧化脱氮化和硫酸盐减速剂之间的合作。本研究突出了硫化物驱动脱氮的重要性,淡水环境中的N和S循环之间的紧密耦合,这是经常被忽视的因素。 (c)2020 elestvier有限公司保留所有权利。

著录项

  • 来源
    《Environmental Pollution》 |2021年第2期|116201.1-116201.10|共10页
  • 作者单位

    Peking Univ Dept Environm Engn Minist Educ Key Lab Water & Sediment Sci Beijing 100871 Peoples R China|Tsinghua Univ Lab Environm Technol INET Beijing 100084 Peoples R China;

    Tsinghua Univ Lab Environm Technol INET Beijing 100084 Peoples R China;

    Peking Univ Dept Environm Engn Minist Educ Key Lab Water & Sediment Sci Beijing 100871 Peoples R China;

    Peking Univ Dept Environm Engn Minist Educ Key Lab Water & Sediment Sci Beijing 100871 Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Denitrification; DNRA; Sulfide oxidation; Sulfate reduction; Thiobacillus;

    机译:脱氮;DNRA;硫化物氧化;硫酸盐减少;硫酸盐;

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