Oxygen isotope exchange between water and carbon dioxide in soils is controlled by pH, nitrate and microbial biomass through links to carbonic anhydrase activity

Oxygen isotope exchange between water and carbon dioxide in soils is controlled by pH, nitrate and microbial biomass through links to carbonic anhydrase activity

<p>The oxygen isotope composition of atmospheric carbon dioxide (<span class="inline-formula">CO<sub>2</sub></span>) is intimately linked to large-scale variations in the cycling of <span class="inline-formula">CO<sub>2</sub></sp...

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Bibliographic Details
Main Authors: S. P. Jones, A. Kaisermann, J. Ogée, S. Wohl, A. W. Cheesman, L. A. Cernusak, L. Wingate
Format: Article
Language:English
Published: Copernicus Publications 2021-06-01
Series:SOIL
Online Access:https://soil.copernicus.org/articles/7/145/2021/soil-7-145-2021.pdf

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https://soil.copernicus.org/articles/7/145/2021/soil-7-145-2021.pdf

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