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B(OH)4- and CO32- do not compete for incorporation into aragonite in synthetic precipitations at pHtotal 8.20 and 8.41 but do compete at pHtotal 8.59 (2024)

First Author: Castillo Alvarez C

Attributed to: Trace element and isotope partitioning in carbonates in simulated biological environments funded by NERC

Abstract

No abstract provided

Bibliographic Information

Digital Object Identifier: http://dx.doi.org/10.1016/j.gca.2024.06.036

Publication URI: http://dx.doi.org/10.1016/j.gca.2024.06.036

Type: Journal Article/Review

Parent Publication: Geochimica et Cosmochimica Acta