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Organic–mineral interfacial chemistry drives heterogeneous nucleation of Sr-rich (Ba(x), Sr(1−x))SO(4) from undersaturated solution
Sr-bearing marine barite [(Ba(x), Sr(1−x))SO(4)] cycling has been widely used to reconstruct geochemical evolutions of paleoenvironments. However, an understanding of barite precipitation in the ocean, which is globally undersaturated with respect to barite, is missing. Moreover, the reason for the...
Tallennettuna:
| Julkaisussa: | Proc Natl Acad Sci U S A |
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| Päätekijät: | , , , , , |
| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
National Academy of Sciences
2019
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| Aiheet: | |
| Linkit: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6612914/ https://ncbi.nlm.nih.gov/pubmed/31113880 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1821065116 |
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