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

• Published in: Environmental research letters Vol. 17; no. 4; pp. 43001 - 43012
• Main Authors: Hu, Enzhu, Ren, Zhimin, Wang, Xiaoke, Zhang, Hongxing, Zhang, Weiwei
• Format: Journal Article
• Language: English
• 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
• ISSN: 1748-9326; 1748-9326
• DOI: 10.1088/1748-9326/ac49b9

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.