Soil HONO emissions at high moisture content are driven by microbial nitrate reduction to nitrite: tackling the HONO puzzle

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Autoren

  • Dianming Wu
  • Marcus A. Horn
  • Thomas Behrendt
  • Stefan Müller
  • Jingsong Li
  • Jeff A. Cole
  • Baohua Xie
  • Xiaotang Ju
  • Guo Li
  • Michael Ermel
  • Robert Oswald
  • Janine Fröhlich-Nowoisky
  • Peter Hoor
  • Chunsheng Hu
  • Min Liu
  • Meinrat O. Andreae
  • Ulrich Pöschl
  • Yafang Cheng
  • Hang Su
  • Ivonne Trebs
  • Bettina Weber
  • Matthias Sörgel

Organisationseinheiten

Externe Organisationen

  • East China Normal University
  • Max-Planck-Institut für Chemie (Otto-Hahn-Institut)
  • Chinese Academy of Sciences (CAS)
  • Universität Bayreuth
  • Johannes Gutenberg-Universität Mainz
  • Anhui University
  • University of Birmingham
  • China Agricultural University
  • King Saud University
  • Institute of Science and Technology, Luxembourg
Forschungs-netzwerk anzeigen

Details

OriginalspracheEnglisch
Seiten (von - bis)1688-1699
Seitenumfang12
FachzeitschriftThe ISME journal
Jahrgang13
Ausgabenummer7
Frühes Online-Datum4 März 2019
PublikationsstatusVeröffentlicht - Juli 2019

Abstract

Nitrous acid (HONO) is a precursor of the hydroxyl radical (OH), a key oxidant in the degradation of most air pollutants. Field measurements indicate a large unknown source of HONO during the day time. Release of nitrous acid (HONO) from soil has been suggested as a major source of atmospheric HONO. We hypothesize that nitrite produced by biological nitrate reduction in oxygen-limited microzones in wet soils is a source of such HONO. Indeed, we found that various contrasting soil samples emitted HONO at high water-holding capacity (75–140%), demonstrating this to be a widespread phenomenon. Supplemental nitrate stimulated HONO emissions, whereas ethanol (70% v/v) treatment to minimize microbial activities reduced HONO emissions by 80%, suggesting that nitrate-dependent biotic processes are the sources of HONO. High-throughput Illumina sequencing of 16S rRNA as well as functional gene transcripts associated with nitrate and nitrite reduction indicated that HONO emissions from soil samples were associated with nitrate reduction activities of diverse Proteobacteria. Incubation of pure cultures of bacterial nitrate reducers and gene-expression analyses, as well as the analyses of mutant strains deficient in nitrite reductases, showed positive correlations of HONO emissions with the capability of microbes to reduce nitrate to nitrite. Thus, we suggest biological nitrate reduction in oxygen-limited microzones as a hitherto unknown source of atmospheric HONO, affecting biogeochemical nitrogen cycling, atmospheric chemistry, and global modeling.

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Soil HONO emissions at high moisture content are driven by microbial nitrate reduction to nitrite: tackling the HONO puzzle. / Wu, Dianming; Horn, Marcus A.; Behrendt, Thomas et al.
in: The ISME journal, Jahrgang 13, Nr. 7, 07.2019, S. 1688-1699.

Publikation: Beitrag in FachzeitschriftArtikelForschungPeer-Review

Wu, D, Horn, MA, Behrendt, T, Müller, S, Li, J, Cole, JA, Xie, B, Ju, X, Li, G, Ermel, M, Oswald, R, Fröhlich-Nowoisky, J, Hoor, P, Hu, C, Liu, M, Andreae, MO, Pöschl, U, Cheng, Y, Su, H, Trebs, I, Weber, B & Sörgel, M 2019, 'Soil HONO emissions at high moisture content are driven by microbial nitrate reduction to nitrite: tackling the HONO puzzle', The ISME journal, Jg. 13, Nr. 7, S. 1688-1699. https://doi.org/10.15488/15944, https://doi.org/10.1038/s41396-019-0379-y
Wu, D., Horn, M. A., Behrendt, T., Müller, S., Li, J., Cole, J. A., Xie, B., Ju, X., Li, G., Ermel, M., Oswald, R., Fröhlich-Nowoisky, J., Hoor, P., Hu, C., Liu, M., Andreae, M. O., Pöschl, U., Cheng, Y., Su, H., ... Sörgel, M. (2019). Soil HONO emissions at high moisture content are driven by microbial nitrate reduction to nitrite: tackling the HONO puzzle. The ISME journal, 13(7), 1688-1699. https://doi.org/10.15488/15944, https://doi.org/10.1038/s41396-019-0379-y
Wu D, Horn MA, Behrendt T, Müller S, Li J, Cole JA et al. Soil HONO emissions at high moisture content are driven by microbial nitrate reduction to nitrite: tackling the HONO puzzle. The ISME journal. 2019 Jul;13(7):1688-1699. Epub 2019 Mär 4. doi: 10.15488/15944, 10.1038/s41396-019-0379-y
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@article{208d44512db84608bf6fb4a28c43de2d,
title = "Soil HONO emissions at high moisture content are driven by microbial nitrate reduction to nitrite: tackling the HONO puzzle",
abstract = "Nitrous acid (HONO) is a precursor of the hydroxyl radical (OH), a key oxidant in the degradation of most air pollutants. Field measurements indicate a large unknown source of HONO during the day time. Release of nitrous acid (HONO) from soil has been suggested as a major source of atmospheric HONO. We hypothesize that nitrite produced by biological nitrate reduction in oxygen-limited microzones in wet soils is a source of such HONO. Indeed, we found that various contrasting soil samples emitted HONO at high water-holding capacity (75–140%), demonstrating this to be a widespread phenomenon. Supplemental nitrate stimulated HONO emissions, whereas ethanol (70% v/v) treatment to minimize microbial activities reduced HONO emissions by 80%, suggesting that nitrate-dependent biotic processes are the sources of HONO. High-throughput Illumina sequencing of 16S rRNA as well as functional gene transcripts associated with nitrate and nitrite reduction indicated that HONO emissions from soil samples were associated with nitrate reduction activities of diverse Proteobacteria. Incubation of pure cultures of bacterial nitrate reducers and gene-expression analyses, as well as the analyses of mutant strains deficient in nitrite reductases, showed positive correlations of HONO emissions with the capability of microbes to reduce nitrate to nitrite. Thus, we suggest biological nitrate reduction in oxygen-limited microzones as a hitherto unknown source of atmospheric HONO, affecting biogeochemical nitrogen cycling, atmospheric chemistry, and global modeling.",
author = "Dianming Wu and Horn, {Marcus A.} and Thomas Behrendt and Stefan M{\"u}ller and Jingsong Li and Cole, {Jeff A.} and Baohua Xie and Xiaotang Ju and Guo Li and Michael Ermel and Robert Oswald and Janine Fr{\"o}hlich-Nowoisky and Peter Hoor and Chunsheng Hu and Min Liu and Andreae, {Meinrat O.} and Ulrich P{\"o}schl and Yafang Cheng and Hang Su and Ivonne Trebs and Bettina Weber and Matthias S{\"o}rgel",
note = "Funding information: We thank J. Cui and M. Badawy for helping to collect the soil samples. We also thank G. Braker and L.R. Bakken for providing pure bacteria cultures. We are grateful to J. Kesselmeier, F. X. Meixner, and H.L. Drake for allowing us to complete experiments in their laboratories. We are also grateful to M. Welling, D. Plake, U. Parchatka, A. Moravek, A. Dallinger, S. Hetz, M. Morawe, N. Ro{\ss}bach, R. Mertel, and A. Wieczorek for supporting techniques in our experiments. This work was supported by the Max Planck Society and the Chinese Academy of Sciences. D. Wu was sponsored by the National Natural Science Foundation of China (41807449), Shanghai Pujiang Program (18PJ1403500), and “the Fundamental Research Funds for the Central Universities”. M. Liu was supported by the National Natural Science Foundation of China (41761144062). B. Weber would like to thank Paul Crutzen for awarding her a Nobel Laureate Fellowship (2013–2015).",
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Download

TY - JOUR

T1 - Soil HONO emissions at high moisture content are driven by microbial nitrate reduction to nitrite: tackling the HONO puzzle

AU - Wu, Dianming

AU - Horn, Marcus A.

AU - Behrendt, Thomas

AU - Müller, Stefan

AU - Li, Jingsong

AU - Cole, Jeff A.

AU - Xie, Baohua

AU - Ju, Xiaotang

AU - Li, Guo

AU - Ermel, Michael

AU - Oswald, Robert

AU - Fröhlich-Nowoisky, Janine

AU - Hoor, Peter

AU - Hu, Chunsheng

AU - Liu, Min

AU - Andreae, Meinrat O.

AU - Pöschl, Ulrich

AU - Cheng, Yafang

AU - Su, Hang

AU - Trebs, Ivonne

AU - Weber, Bettina

AU - Sörgel, Matthias

N1 - Funding information: We thank J. Cui and M. Badawy for helping to collect the soil samples. We also thank G. Braker and L.R. Bakken for providing pure bacteria cultures. We are grateful to J. Kesselmeier, F. X. Meixner, and H.L. Drake for allowing us to complete experiments in their laboratories. We are also grateful to M. Welling, D. Plake, U. Parchatka, A. Moravek, A. Dallinger, S. Hetz, M. Morawe, N. Roßbach, R. Mertel, and A. Wieczorek for supporting techniques in our experiments. This work was supported by the Max Planck Society and the Chinese Academy of Sciences. D. Wu was sponsored by the National Natural Science Foundation of China (41807449), Shanghai Pujiang Program (18PJ1403500), and “the Fundamental Research Funds for the Central Universities”. M. Liu was supported by the National Natural Science Foundation of China (41761144062). B. Weber would like to thank Paul Crutzen for awarding her a Nobel Laureate Fellowship (2013–2015).

PY - 2019/7

Y1 - 2019/7

N2 - Nitrous acid (HONO) is a precursor of the hydroxyl radical (OH), a key oxidant in the degradation of most air pollutants. Field measurements indicate a large unknown source of HONO during the day time. Release of nitrous acid (HONO) from soil has been suggested as a major source of atmospheric HONO. We hypothesize that nitrite produced by biological nitrate reduction in oxygen-limited microzones in wet soils is a source of such HONO. Indeed, we found that various contrasting soil samples emitted HONO at high water-holding capacity (75–140%), demonstrating this to be a widespread phenomenon. Supplemental nitrate stimulated HONO emissions, whereas ethanol (70% v/v) treatment to minimize microbial activities reduced HONO emissions by 80%, suggesting that nitrate-dependent biotic processes are the sources of HONO. High-throughput Illumina sequencing of 16S rRNA as well as functional gene transcripts associated with nitrate and nitrite reduction indicated that HONO emissions from soil samples were associated with nitrate reduction activities of diverse Proteobacteria. Incubation of pure cultures of bacterial nitrate reducers and gene-expression analyses, as well as the analyses of mutant strains deficient in nitrite reductases, showed positive correlations of HONO emissions with the capability of microbes to reduce nitrate to nitrite. Thus, we suggest biological nitrate reduction in oxygen-limited microzones as a hitherto unknown source of atmospheric HONO, affecting biogeochemical nitrogen cycling, atmospheric chemistry, and global modeling.

AB - Nitrous acid (HONO) is a precursor of the hydroxyl radical (OH), a key oxidant in the degradation of most air pollutants. Field measurements indicate a large unknown source of HONO during the day time. Release of nitrous acid (HONO) from soil has been suggested as a major source of atmospheric HONO. We hypothesize that nitrite produced by biological nitrate reduction in oxygen-limited microzones in wet soils is a source of such HONO. Indeed, we found that various contrasting soil samples emitted HONO at high water-holding capacity (75–140%), demonstrating this to be a widespread phenomenon. Supplemental nitrate stimulated HONO emissions, whereas ethanol (70% v/v) treatment to minimize microbial activities reduced HONO emissions by 80%, suggesting that nitrate-dependent biotic processes are the sources of HONO. High-throughput Illumina sequencing of 16S rRNA as well as functional gene transcripts associated with nitrate and nitrite reduction indicated that HONO emissions from soil samples were associated with nitrate reduction activities of diverse Proteobacteria. Incubation of pure cultures of bacterial nitrate reducers and gene-expression analyses, as well as the analyses of mutant strains deficient in nitrite reductases, showed positive correlations of HONO emissions with the capability of microbes to reduce nitrate to nitrite. Thus, we suggest biological nitrate reduction in oxygen-limited microzones as a hitherto unknown source of atmospheric HONO, affecting biogeochemical nitrogen cycling, atmospheric chemistry, and global modeling.

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U2 - 10.15488/15944

DO - 10.15488/15944

M3 - Article

VL - 13

SP - 1688

EP - 1699

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JF - The ISME journal

SN - 1751-7362

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ER -

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