Preprints
https://doi.org/10.5194/egusphere-2026-5968
https://doi.org/10.5194/egusphere-2026-5968
08 Oct 2026
 | 08 Oct 2026
Status: this preprint is open for discussion and under review for Biogeosciences (BG).

Alkalinity generation and trace metal dynamics during olivine-based marine enhanced rock weathering in bioturbated sediments

Benjamin Van Heurck, Francesc Montserrat, Astrid Hylén, Diana Vasquez Cardenas, Saïd De Wolf, Cedric Goossens, Greet Lembregts, Daniel A. Frick, Matthias Kreuzburg, and Filip J. R. Meysman

Abstract. Ocean alkalinity enhancement (OAE) via marine enhanced rock weathering (mERW) of olivine is a proposed strategy for atmospheric carbon dioxide removal (CDR). However, the potential co-release of trace metals to marine ecosystems, most notably nickel (Ni) and chromium (Cr), raises environmental concerns.

Here, we investigated total alkalinity (AT) release, trace metal dynamics and metal bioaccumulation during mERW using two complementary approaches. First, a 28-day microcosm experiment showed that bioturbation by the lugworm Arenicola marina in pure olivine sand enhanced AT release nearly fivefold and more than doubled the release of dissolved Ni (DNi). Second, in a long-term (> 1 year) mesocosm experiment, we added fine-grained olivine at sediment loading levels of 6% and 10%, and coarse-grained olivine at 10%, to natural intertidal sediments inhabited by A. marina. We quantified sediment–water fluxes and porewater concentrations of AT, DNi, and DCr, and assessed metal accumulation in lugworm tissues. Olivine amendment increased sediment–water AT fluxes approximately two- to threefold, without significant effects of grain size or loading level. Fine-grained olivine treatments resulted in the highest DNi fluxes and the greatest Ni bioaccumulation in lugworms. Lugworm Ni concentrations increased up to tenfold relative to controls. In contrast, olivine amendment did not increase DCr fluxes and Cr bioaccumulation was minor compared to Ni.

These results show that bioturbation can enhance olivine weathering and that olivine amendment can increase AT release from natural coastal sediments. However, finer grain size disproportionately increased Ni release and bioaccumulation without a detectable additional AT benefit. This decoupling suggests that AT generated by olivine weathering may have been partly offset by suppression of natural sedimentary AT generation. Under the conditions tested here, coarse olivine therefore provided a more favourable balance between net AT release and ecotoxicological risks from Ni exposure during mERW.

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Benjamin Van Heurck, Francesc Montserrat, Astrid Hylén, Diana Vasquez Cardenas, Saïd De Wolf, Cedric Goossens, Greet Lembregts, Daniel A. Frick, Matthias Kreuzburg, and Filip J. R. Meysman

Status: open (until 19 Nov 2026)

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Benjamin Van Heurck, Francesc Montserrat, Astrid Hylén, Diana Vasquez Cardenas, Saïd De Wolf, Cedric Goossens, Greet Lembregts, Daniel A. Frick, Matthias Kreuzburg, and Filip J. R. Meysman
Benjamin Van Heurck, Francesc Montserrat, Astrid Hylén, Diana Vasquez Cardenas, Saïd De Wolf, Cedric Goossens, Greet Lembregts, Daniel A. Frick, Matthias Kreuzburg, and Filip J. R. Meysman
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Latest update: 08 Oct 2026
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Short summary
Adding crushed olivine to coastal sediments could help seawater absorb carbon dioxide, but it may also release toxic metals. We studied olivine in experiments with burrowing marine worms. The worms accelerated the release of alkalinity, a property that helps seawater take up carbon dioxide. Finer olivine released more nickel, while coarse olivine produced a similar increase in alkalinity. Coarser grains may therefore offer a better balance between potential climate benefits and metal exposure.
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