Stability of dissolved and soluble Fe(II) in shelf sediment pore waters and release to an oxic water column

Shelf sediments underlying temperate and oxic waters of the Celtic Sea (NW European Shelf) were found to have shallow oxygen penetrations depths from late spring to late summer (2.2–5.8 mm below seafloor) with the shallowest during/after the spring-bloom (mid-April to mid-May) when the organic carbo...

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Detalles Bibliográficos
Autores principales: Klar, J. K., Homoky, W. B., Statham, P. J., Birchill, A. J., Harris, E. L., Woodward, E. M. S., Silburn, B., Cooper, M. J., James, R. H., Connelly, D. P., Chever, F., Lichtschlag, A., Graves, C.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Springer International Publishing 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6961528/
https://www.ncbi.nlm.nih.gov/pubmed/32009691
http://dx.doi.org/10.1007/s10533-017-0309-x

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6961528/
https://www.ncbi.nlm.nih.gov/pubmed/32009691
http://dx.doi.org/10.1007/s10533-017-0309-x

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