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Quantification of CO2 removal in a large-scale enhanced weathering field trial on an oil palm plantation in Sabah, Malaysia

Quantification of CO2 removal in a large-scale enhanced weathering field trial on an oil palm plantation in Sabah, Malaysia
Quantification of CO2 removal in a large-scale enhanced weathering field trial on an oil palm plantation in Sabah, Malaysia

Modeling studies show that large-scale deployment of enhanced rock weathering on croplands has the potential to reduce levels of atmospheric carbon dioxide by the end of the century. There is, however, a pressing need to verify model predictions through long-term field trials. Here we report results from the first 3 years of an ongoing enhanced weathering field trial, carried out on an oil palm plantation in Sabah, Malaysia. Crushed silicate rock was applied to three hydrologically isolated catchments, and three adjacent (paired) reference catchments were left untreated. The drawdown of atmospheric CO 2 was quantified via the export of alkalinity in stream waters and changes in soil carbonate content. The amended and reference catchments were found to have a similar extent of CO 2 drawdown via alkalinity export [respectively, 3.8 ± 0.8 (1 SD) and 3.7 ± 0.6 (1 SD) tCO 2 ha −1] when all catchments were averaged over the study period (October 2018 to July 2021). However, differences were observed between the different catchment pairs (plots): two of the plots displayed a similar extent of CO 2 removal for both the amended and reference catchments, but the third amended catchment had a higher extent of CO 2 removal of ~1 tCO 2 ha −1 relative to its adjacent reference catchment. The difference in CO 2 removal rates determined for this plot can likely be attributed to increased weathering of silicate minerals in the amended catchment. Soil carbonate concentrations were on average <0.2 wt% CaCO 3, but we report a small increase of ~0.03 wt% CaCO 3 in the top 30 cm of soil in the amended soils relative to the reference catchments. The magnitude of CO 2 drawdown via alkalinity export determined for these agricultural catchments is around an order of magnitude higher than in natural forested catchments in Sabah and similar to that of basaltic catchments. We show that these high weathering rates are primarily driven by weathering of carbonate fertilizers. The data presented from this field trial provide vital contextual information on the real-world efficacy and practicalities associated with the implementation of enhanced weathering for atmospheric CO 2 removal that will help to inform further trials as well as wider-scale deployment.

carbon dioxide removal, climate change mitigation, enhanced weathering, oil palm, tropical croplands
Larkin, Christina S.
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Andrews, M. Grace
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Pearce, Christopher R.
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Yeong, Kok L.
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Beerling, David J.
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Bellamy, Joshua
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Benedick, Suzan
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Freckleton, Robert P.
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Goring-harford, Heather
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Sadekar, Satyam
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James, Rachael H.
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Larkin, Christina S.
7e5477b9-0a3d-4580-ba78-2e6282f010cc
Andrews, M. Grace
61a71817-9828-48d4-bcff-04d5cd65b266
Pearce, Christopher R.
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Yeong, Kok L.
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Beerling, David J.
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Bellamy, Joshua
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Benedick, Suzan
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Freckleton, Robert P.
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Goring-harford, Heather
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Sadekar, Satyam
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James, Rachael H.
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Larkin, Christina S., Andrews, M. Grace, Pearce, Christopher R., Yeong, Kok L., Beerling, David J., Bellamy, Joshua, Benedick, Suzan, Freckleton, Robert P., Goring-harford, Heather, Sadekar, Satyam and James, Rachael H. (2022) Quantification of CO2 removal in a large-scale enhanced weathering field trial on an oil palm plantation in Sabah, Malaysia. Frontiers in Climate, 4, [959229]. (doi:10.3389/fclim.2022.959229).

Record type: Article

Abstract

Modeling studies show that large-scale deployment of enhanced rock weathering on croplands has the potential to reduce levels of atmospheric carbon dioxide by the end of the century. There is, however, a pressing need to verify model predictions through long-term field trials. Here we report results from the first 3 years of an ongoing enhanced weathering field trial, carried out on an oil palm plantation in Sabah, Malaysia. Crushed silicate rock was applied to three hydrologically isolated catchments, and three adjacent (paired) reference catchments were left untreated. The drawdown of atmospheric CO 2 was quantified via the export of alkalinity in stream waters and changes in soil carbonate content. The amended and reference catchments were found to have a similar extent of CO 2 drawdown via alkalinity export [respectively, 3.8 ± 0.8 (1 SD) and 3.7 ± 0.6 (1 SD) tCO 2 ha −1] when all catchments were averaged over the study period (October 2018 to July 2021). However, differences were observed between the different catchment pairs (plots): two of the plots displayed a similar extent of CO 2 removal for both the amended and reference catchments, but the third amended catchment had a higher extent of CO 2 removal of ~1 tCO 2 ha −1 relative to its adjacent reference catchment. The difference in CO 2 removal rates determined for this plot can likely be attributed to increased weathering of silicate minerals in the amended catchment. Soil carbonate concentrations were on average <0.2 wt% CaCO 3, but we report a small increase of ~0.03 wt% CaCO 3 in the top 30 cm of soil in the amended soils relative to the reference catchments. The magnitude of CO 2 drawdown via alkalinity export determined for these agricultural catchments is around an order of magnitude higher than in natural forested catchments in Sabah and similar to that of basaltic catchments. We show that these high weathering rates are primarily driven by weathering of carbonate fertilizers. The data presented from this field trial provide vital contextual information on the real-world efficacy and practicalities associated with the implementation of enhanced weathering for atmospheric CO 2 removal that will help to inform further trials as well as wider-scale deployment.

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Accepted/In Press date: 11 August 2022
e-pub ahead of print date: 30 August 2022
Published date: 30 August 2022
Additional Information: Funding Information: This research was funded through a Leverhulme Research Centre Award (RC-2015-029) from the Leverhulme Trust. Funding Information: We thank Cynthia Dumousseaud, Gabriella Jardine, and Matt Cooper for technical assistance at the University of Southampton. We thank Onika Quarry for donating the rock used in this experiment as well as Glen Reynolds (Director of SEARRP) who helped to make sure the project ran smoothly. We thank the Sabah Biodiversity Centre that provided approval for both accessing the experimental site and exporting samples. Publisher Copyright: Copyright © 2022 Larkin, Andrews, Pearce, Yeong, Beerling, Bellamy, Benedick, Freckleton, Goring-Harford, Sadekar and James.
Keywords: carbon dioxide removal, climate change mitigation, enhanced weathering, oil palm, tropical croplands

Identifiers

Local EPrints ID: 470294
URI: http://eprints.soton.ac.uk/id/eprint/470294
PURE UUID: 929820ad-c230-4a37-a518-238ce00ce57d
ORCID for Christina S. Larkin: ORCID iD orcid.org/0000-0002-6420-0461
ORCID for Rachael H. James: ORCID iD orcid.org/0000-0001-7402-2315

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Date deposited: 05 Oct 2022 16:55
Last modified: 17 Mar 2024 04:05

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Contributors

Author: Christina S. Larkin ORCID iD
Author: Christopher R. Pearce
Author: Kok L. Yeong
Author: David J. Beerling
Author: Joshua Bellamy
Author: Suzan Benedick
Author: Robert P. Freckleton
Author: Satyam Sadekar

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