The role of soils in the regulation of ocean acidification

Soils play an important role in mediating chemical weathering reactions and carbon transfer from the land to the ocean. Proposals to increase the contribution of alkalinity to the oceans through ‘enhanced weathering’ as a means to help prevent climate change are gaining increasing attention. This wo...

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Published in:Philosophical Transactions of the Royal Society B: Biological Sciences
Main Authors: Renforth, P., Campbell, J. S.
Other Authors: Natural Environment Research Council, European Commission
Format: Article in Journal/Newspaper
Language:English
Published: The Royal Society 2021
Subjects:
Online Access:http://dx.doi.org/10.1098/rstb.2020.0174
https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.2020.0174
https://royalsocietypublishing.org/doi/full-xml/10.1098/rstb.2020.0174
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spelling crroyalsociety:10.1098/rstb.2020.0174 2024-09-30T14:40:43+00:00 The role of soils in the regulation of ocean acidification Renforth, P. Campbell, J. S. Natural Environment Research Council European Commission 2021 http://dx.doi.org/10.1098/rstb.2020.0174 https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.2020.0174 https://royalsocietypublishing.org/doi/full-xml/10.1098/rstb.2020.0174 en eng The Royal Society https://royalsociety.org/journals/ethics-policies/data-sharing-mining/ Philosophical Transactions of the Royal Society B: Biological Sciences volume 376, issue 1834, page 20200174 ISSN 0962-8436 1471-2970 journal-article 2021 crroyalsociety https://doi.org/10.1098/rstb.2020.0174 2024-09-09T06:01:18Z Soils play an important role in mediating chemical weathering reactions and carbon transfer from the land to the ocean. Proposals to increase the contribution of alkalinity to the oceans through ‘enhanced weathering’ as a means to help prevent climate change are gaining increasing attention. This would augment the existing connection between the biogeochemical function of soils and alkalinity levels in the ocean. The feasibility of enhanced weathering depends on the combined influence of what minerals are added to soils, the formation of secondary minerals in soils and the drainage regime, and the partial pressure of respired CO 2 around the dissolving mineral. Increasing the alkalinity levels in the ocean through enhanced weathering could help to ameliorate the effects of ocean acidification in two ways. First, enhanced weathering would slightly elevate the pH of drainage waters, and the receiving coastal waters. The elevated pH would result in an increase in carbonate mineral saturation states, and a partial reversal in the effects of elevated CO 2 . Second, the increase in alkalinity would help to replenish the ocean's buffering capacity by maintaining the ‘Revelle Factor’, making the oceans more resilient to further CO 2 emissions. However, there is limited research on the downstream and oceanic impacts of enhanced weathering on which to base deployment decisions. This article is part of the theme issue ‘The role of soils in delivering Nature's Contributions to People’. Article in Journal/Newspaper Ocean acidification The Royal Society Philosophical Transactions of the Royal Society B: Biological Sciences 376 1834 20200174
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description Soils play an important role in mediating chemical weathering reactions and carbon transfer from the land to the ocean. Proposals to increase the contribution of alkalinity to the oceans through ‘enhanced weathering’ as a means to help prevent climate change are gaining increasing attention. This would augment the existing connection between the biogeochemical function of soils and alkalinity levels in the ocean. The feasibility of enhanced weathering depends on the combined influence of what minerals are added to soils, the formation of secondary minerals in soils and the drainage regime, and the partial pressure of respired CO 2 around the dissolving mineral. Increasing the alkalinity levels in the ocean through enhanced weathering could help to ameliorate the effects of ocean acidification in two ways. First, enhanced weathering would slightly elevate the pH of drainage waters, and the receiving coastal waters. The elevated pH would result in an increase in carbonate mineral saturation states, and a partial reversal in the effects of elevated CO 2 . Second, the increase in alkalinity would help to replenish the ocean's buffering capacity by maintaining the ‘Revelle Factor’, making the oceans more resilient to further CO 2 emissions. However, there is limited research on the downstream and oceanic impacts of enhanced weathering on which to base deployment decisions. This article is part of the theme issue ‘The role of soils in delivering Nature's Contributions to People’.
author2 Natural Environment Research Council
European Commission
format Article in Journal/Newspaper
author Renforth, P.
Campbell, J. S.
spellingShingle Renforth, P.
Campbell, J. S.
The role of soils in the regulation of ocean acidification
author_facet Renforth, P.
Campbell, J. S.
author_sort Renforth, P.
title The role of soils in the regulation of ocean acidification
title_short The role of soils in the regulation of ocean acidification
title_full The role of soils in the regulation of ocean acidification
title_fullStr The role of soils in the regulation of ocean acidification
title_full_unstemmed The role of soils in the regulation of ocean acidification
title_sort role of soils in the regulation of ocean acidification
publisher The Royal Society
publishDate 2021
url http://dx.doi.org/10.1098/rstb.2020.0174
https://royalsocietypublishing.org/doi/pdf/10.1098/rstb.2020.0174
https://royalsocietypublishing.org/doi/full-xml/10.1098/rstb.2020.0174
genre Ocean acidification
genre_facet Ocean acidification
op_source Philosophical Transactions of the Royal Society B: Biological Sciences
volume 376, issue 1834, page 20200174
ISSN 0962-8436 1471-2970
op_rights https://royalsociety.org/journals/ethics-policies/data-sharing-mining/
op_doi https://doi.org/10.1098/rstb.2020.0174
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