Laboratory study of iron isotope fractionation during dissolution of mineral dust and industrial ash in simulated cloud water

Autor:	Elena C, Maters, Daniel S, Mulholland, Pascal, Flament, Jeroen, de Jong, Nadine, Mattielli, Karine, Deboudt, Guillaume, Dhont, Eugène, Bychkov
Rok vydání:	2021
Předmět:	Minerals Solubility Water Dust Iron Isotopes
Zdroj:	Chemosphere. 299
ISSN:	1879-1298
Popis:	Atmospheric deposition is a key mode of iron (Fe) input to ocean regions where low concentrations of this micronutrient limit marine primary production. Various natural particles (e.g., mineral dust, volcanic ash) and anthropogenic particles (e.g., from industrial processes, biomass burning) can deliver Fe to the ocean, and assessment of their relative importance in supplying Fe to seawater requires knowledge of both their deposition flux and their Fe solubility (a proxy for Fe bioavailability). Iron isotope (
Databáze:	OpenAIRE
Externí odkaz:	https://explore.openaire.eu/search/publication?articleId=pmid________::0c3dbdf904cd3f0022bc87ae9da12a7e https://pubmed.ncbi.nlm.nih.gov/35367494 Zobrazit plný text záznamu Full Text from ScienceDirect