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Microbial nitrification, denitrification and respiration in the leached cinnamon soil of the upper basin of Miyun Reservoir
Leached cinnamon soil is the main agricultural soil distributed in the North China Plain. In this research, leached cinnamon soil samples were collected in the upper basin of Miyun Reservoir (northeast of Beijing, China). The BaPS method (Barometric Process Separation) was applied to measure nitrifi...
Autores principales: | , , , , |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group
2017
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5292740/ https://www.ncbi.nlm.nih.gov/pubmed/28165035 http://dx.doi.org/10.1038/srep42032 |
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author | Xu, Wen Cai, Yan-Peng Yang, Zhi-Feng Yin, Xin-An Tan, Qian |
author_facet | Xu, Wen Cai, Yan-Peng Yang, Zhi-Feng Yin, Xin-An Tan, Qian |
author_sort | Xu, Wen |
collection | PubMed |
description | Leached cinnamon soil is the main agricultural soil distributed in the North China Plain. In this research, leached cinnamon soil samples were collected in the upper basin of Miyun Reservoir (northeast of Beijing, China). The BaPS method (Barometric Process Separation) was applied to measure nitrification, denitrification and respiration rates. The rates of nitrification, denitrification and respiration were 0–120.35 μg N/kg SDW h, 0–246.86 μg N/kg SDW h and 0.17–225.85 μg C/kg SDW h (Soil Dry Weight, SDW), respectively. The emission rates of CO(2) and N(x)O(y) through nitrification, denitrification and respiration were 1.00–547.80 and 6.00–4850.65 μmol/h, respectively. The analysis of relationships between nitrification, denitrification and respiration rates indicated that these three microbial processes were interacted, which posed impacts on soil nitrogen availability. As indicated by the results, C:N ratio coupled with [Image: see text] content could be taken as the indicators of [Image: see text] content, which is usually the predominant form of N available to plants growing in soil. Results showed that [Image: see text] content was the highest (i.e., >62.4 mg/kg) when C:N ratio was 5.30–8.40, meanwhile [Image: see text] content was 3.71–4.39 mg/kg. Nevertheless, [Image: see text] content was the lowest (i.e., <6.40 mg/kg) when C:N ratio was 9.2–12.10, meanwhile [Image: see text] content was 3.41–4.35 mg/kg. |
format | Online Article Text |
id | pubmed-5292740 |
institution | National Center for Biotechnology Information |
language | English |
publishDate | 2017 |
publisher | Nature Publishing Group |
record_format | MEDLINE/PubMed |
spelling | pubmed-52927402017-02-10 Microbial nitrification, denitrification and respiration in the leached cinnamon soil of the upper basin of Miyun Reservoir Xu, Wen Cai, Yan-Peng Yang, Zhi-Feng Yin, Xin-An Tan, Qian Sci Rep Article Leached cinnamon soil is the main agricultural soil distributed in the North China Plain. In this research, leached cinnamon soil samples were collected in the upper basin of Miyun Reservoir (northeast of Beijing, China). The BaPS method (Barometric Process Separation) was applied to measure nitrification, denitrification and respiration rates. The rates of nitrification, denitrification and respiration were 0–120.35 μg N/kg SDW h, 0–246.86 μg N/kg SDW h and 0.17–225.85 μg C/kg SDW h (Soil Dry Weight, SDW), respectively. The emission rates of CO(2) and N(x)O(y) through nitrification, denitrification and respiration were 1.00–547.80 and 6.00–4850.65 μmol/h, respectively. The analysis of relationships between nitrification, denitrification and respiration rates indicated that these three microbial processes were interacted, which posed impacts on soil nitrogen availability. As indicated by the results, C:N ratio coupled with [Image: see text] content could be taken as the indicators of [Image: see text] content, which is usually the predominant form of N available to plants growing in soil. Results showed that [Image: see text] content was the highest (i.e., >62.4 mg/kg) when C:N ratio was 5.30–8.40, meanwhile [Image: see text] content was 3.71–4.39 mg/kg. Nevertheless, [Image: see text] content was the lowest (i.e., <6.40 mg/kg) when C:N ratio was 9.2–12.10, meanwhile [Image: see text] content was 3.41–4.35 mg/kg. Nature Publishing Group 2017-02-06 /pmc/articles/PMC5292740/ /pubmed/28165035 http://dx.doi.org/10.1038/srep42032 Text en Copyright © 2017, The Author(s) http://creativecommons.org/licenses/by/4.0/ This work is licensed under a Creative Commons Attribution 4.0 International License. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in the credit line; if the material is not included under the Creative Commons license, users will need to obtain permission from the license holder to reproduce the material. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/ |
spellingShingle | Article Xu, Wen Cai, Yan-Peng Yang, Zhi-Feng Yin, Xin-An Tan, Qian Microbial nitrification, denitrification and respiration in the leached cinnamon soil of the upper basin of Miyun Reservoir |
title | Microbial nitrification, denitrification and respiration in the leached cinnamon soil of the upper basin of Miyun Reservoir |
title_full | Microbial nitrification, denitrification and respiration in the leached cinnamon soil of the upper basin of Miyun Reservoir |
title_fullStr | Microbial nitrification, denitrification and respiration in the leached cinnamon soil of the upper basin of Miyun Reservoir |
title_full_unstemmed | Microbial nitrification, denitrification and respiration in the leached cinnamon soil of the upper basin of Miyun Reservoir |
title_short | Microbial nitrification, denitrification and respiration in the leached cinnamon soil of the upper basin of Miyun Reservoir |
title_sort | microbial nitrification, denitrification and respiration in the leached cinnamon soil of the upper basin of miyun reservoir |
topic | Article |
url | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5292740/ https://www.ncbi.nlm.nih.gov/pubmed/28165035 http://dx.doi.org/10.1038/srep42032 |
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