Effect of elevated tropospheric ozone on soil carbon and nitrogen: a meta-analysis

Elevated tropospheric ozone concentration ([O 3 ]) may substantially influence the belowground processes of the terrestrial ecosystem. Nevertheless, a comprehensive and quantitative understanding of the responses of soil C and N dynamics to elevated [O 3 ] remains elusive. In this study, the results...

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Published inEnvironmental research letters Vol. 17; no. 4; pp. 43001 - 43012
Main Authors Hu, Enzhu, Ren, Zhimin, Wang, Xiaoke, Zhang, Hongxing, Zhang, Weiwei
Format Journal Article
LanguageEnglish
Published Bristol IOP Publishing 01.04.2022
Subjects
Ammonia
Carbon dioxide
Carbon/nitrogen ratio
Denitrification
Dissolved organic carbon
elevated ozone
Fumigation
Meta-analysis
microbial biomass
Microorganisms
Nitrification
Nitrogen
Ozone
Plant growth
soil carbon
Soil chemistry
Soil dynamics
soil nitrogen
Soil pH
Soils
Terrestrial ecosystems
Troposphere
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Abstract Elevated tropospheric ozone concentration ([O 3 ]) may substantially influence the belowground processes of the terrestrial ecosystem. Nevertheless, a comprehensive and quantitative understanding of the responses of soil C and N dynamics to elevated [O 3 ] remains elusive. In this study, the results of 41 peer-reviewed studies were synthesized using meta-analytic techniques, to quantify the impact of O 3 on ten variables associated with soil C and N, i.e. total C (TC, including soil organic C), total N (TN), dissolved organic C (DOC), ammonia N (NH 4 + ), nitrate N (NO 3 − ), microbial biomass C (MBC) and N (MBN), rates of nitrification (NTF) and denitrification (DNF), as well as C/N ratio. The results depicted that all these variables showed significant changes ( P < 0.05) with [O 3 ] increased by 27.6 ± 18.7 nl l −1 (mean ± SD), including decreases in TC, DOC, TN, NH 4 + , MBC, MBN and NTF, and increases in C/N, NO 3 − and DNF. The effect sizes of TN, NTF, and DNF were significantly correlated with O 3 fumigation levels and experimental duration ( P < 0.05). Soil pH and climate were essential in analyses of O 3 impacts on soil C and N. However, the responses of most variables to elevated [O 3 ] were generally independent of the O 3 fumigation method, terrestrial ecosystem type, and additional [CO 2 ] exposure. The altered soil C and N dynamics under elevated [O 3 ] may reduce its C sink capacity, and change soil N availability and thus, impact plant growth and enhance soil N losses.
AbstractList Elevated tropospheric ozone concentration ([O _3 ]) may substantially influence the belowground processes of the terrestrial ecosystem. Nevertheless, a comprehensive and quantitative understanding of the responses of soil C and N dynamics to elevated [O _3 ] remains elusive. In this study, the results of 41 peer-reviewed studies were synthesized using meta-analytic techniques, to quantify the impact of O _3 on ten variables associated with soil C and N, i.e. total C (TC, including soil organic C), total N (TN), dissolved organic C (DOC), ammonia N (NH _4 ^+ ), nitrate N (NO _3 ^− ), microbial biomass C (MBC) and N (MBN), rates of nitrification (NTF) and denitrification (DNF), as well as C/N ratio. The results depicted that all these variables showed significant changes ( P < 0.05) with [O _3 ] increased by 27.6 ± 18.7 nl l ^−1 (mean ± SD), including decreases in TC, DOC, TN, NH _4 ^+ , MBC, MBN and NTF, and increases in C/N, NO _3 ^− and DNF. The effect sizes of TN, NTF, and DNF were significantly correlated with O _3 fumigation levels and experimental duration ( P < 0.05). Soil pH and climate were essential in analyses of O _3 impacts on soil C and N. However, the responses of most variables to elevated [O _3 ] were generally independent of the O _3 fumigation method, terrestrial ecosystem type, and additional [CO _2 ] exposure. The altered soil C and N dynamics under elevated [O _3 ] may reduce its C sink capacity, and change soil N availability and thus, impact plant growth and enhance soil N losses.
Elevated tropospheric ozone concentration ([O3]) may substantially influence the belowground processes of the terrestrial ecosystem. Nevertheless, a comprehensive and quantitative understanding of the responses of soil C and N dynamics to elevated [O3] remains elusive. In this study, the results of 41 peer-reviewed studies were synthesized using meta-analytic techniques, to quantify the impact of O3 on ten variables associated with soil C and N, i.e. total C (TC, including soil organic C), total N (TN), dissolved organic C (DOC), ammonia N (NH4+), nitrate N (NO3−), microbial biomass C (MBC) and N (MBN), rates of nitrification (NTF) and denitrification (DNF), as well as C/N ratio. The results depicted that all these variables showed significant changes (P < 0.05) with [O3] increased by 27.6 ± 18.7 nl l−1 (mean ± SD), including decreases in TC, DOC, TN, NH4+, MBC, MBN and NTF, and increases in C/N, NO3− and DNF. The effect sizes of TN, NTF, and DNF were significantly correlated with O3 fumigation levels and experimental duration (P < 0.05). Soil pH and climate were essential in analyses of O3 impacts on soil C and N. However, the responses of most variables to elevated [O3] were generally independent of the O3 fumigation method, terrestrial ecosystem type, and additional [CO2] exposure. The altered soil C and N dynamics under elevated [O3] may reduce its C sink capacity, and change soil N availability and thus, impact plant growth and enhance soil N losses.
Elevated tropospheric ozone concentration ([O 3 ]) may substantially influence the belowground processes of the terrestrial ecosystem. Nevertheless, a comprehensive and quantitative understanding of the responses of soil C and N dynamics to elevated [O 3 ] remains elusive. In this study, the results of 41 peer-reviewed studies were synthesized using meta-analytic techniques, to quantify the impact of O 3 on ten variables associated with soil C and N, i.e. total C (TC, including soil organic C), total N (TN), dissolved organic C (DOC), ammonia N (NH 4 + ), nitrate N (NO 3 − ), microbial biomass C (MBC) and N (MBN), rates of nitrification (NTF) and denitrification (DNF), as well as C/N ratio. The results depicted that all these variables showed significant changes ( P < 0.05) with [O 3 ] increased by 27.6 ± 18.7 nl l −1 (mean ± SD), including decreases in TC, DOC, TN, NH 4 + , MBC, MBN and NTF, and increases in C/N, NO 3 − and DNF. The effect sizes of TN, NTF, and DNF were significantly correlated with O 3 fumigation levels and experimental duration ( P < 0.05). Soil pH and climate were essential in analyses of O 3 impacts on soil C and N. However, the responses of most variables to elevated [O 3 ] were generally independent of the O 3 fumigation method, terrestrial ecosystem type, and additional [CO 2 ] exposure. The altered soil C and N dynamics under elevated [O 3 ] may reduce its C sink capacity, and change soil N availability and thus, impact plant growth and enhance soil N losses.
Author Zhang, Hongxing
Wang, Xiaoke
Ren, Zhimin
Hu, Enzhu
Zhang, Weiwei
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Snippet Elevated tropospheric ozone concentration ([O 3 ]) may substantially influence the belowground processes of the terrestrial ecosystem. Nevertheless, a...
Elevated tropospheric ozone concentration ([O3]) may substantially influence the belowground processes of the terrestrial ecosystem. Nevertheless, a...
Elevated tropospheric ozone concentration ([O _3 ]) may substantially influence the belowground processes of the terrestrial ecosystem. Nevertheless, a...
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SubjectTerms Ammonia
Carbon dioxide
Carbon/nitrogen ratio
Denitrification
Dissolved organic carbon
elevated ozone
Fumigation
Meta-analysis
microbial biomass
Microorganisms
Nitrification
Nitrogen
Ozone
Plant growth
soil carbon
Soil chemistry
Soil dynamics
soil nitrogen
Soil pH
Soils
Terrestrial ecosystems
Troposphere
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Title Effect of elevated tropospheric ozone on soil carbon and nitrogen: a meta-analysis
URI https://iopscience.iop.org/article/10.1088/1748-9326/ac49b9
https://www.proquest.com/docview/2640007247
https://doaj.org/article/5f6d0f5213a042c2bdb00399c3ff79ea
Volume 17
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