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English: Low-temperature processes controlling silicon dissolution in seawater
Schematic view of the low-temperature processes that control the dissolution of (either amorphous or crystallized) siliceous minerals in seawater in and to the coastal zone and in the deep ocean, feeding submarine groundwater (FGW) and dissolved silicon in seawater and sediments (FW). These processes correspond to both low and medium energy flux dissipated per volume of a given siliceous particle in the coastal zone, in the continental margins, and in the abysses and to high-energy flux dissipated in the surf zone.
Date
Source [1] doi:10.5194/bg-18-1269-2021
Author Paul J. Tréguer, Jill N. Sutton, Mark Brzezinski, Matthew A. Charette, Timothy Devries, Stephanie Dutkiewicz, Claudia Ehlert, Jon Hawkings, Aude Leynaert, Su Mei Liu, Natalia Llopis Monferrer, María López-Acosta, Manuel Maldonado, Shaily Rahman, Lihua Ran and Olivier Rouxel

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Low-temperature processes controlling silicon dissolution in seawater

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18 February 2021

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current00:00, 30 August 2021Thumbnail for version as of 00:00, 30 August 20213,010 × 1,787 (4.59 MB)EpipelagicUploaded a work by Paul J. Tréguer, Jill N. Sutton, Mark Brzezinski, Matthew A. Charette, Timothy Devries, Stephanie Dutkiewicz, Claudia Ehlert, Jon Hawkings, Aude Leynaert, Su Mei Liu, Natalia Llopis Monferrer, María López-Acosta, Manuel Maldonado, Shaily Rahman, Lihua Ran and Olivier Rouxel from [https://bg.copernicus.org/articles/18/1269/2021/] {{doi|10.5194/bg-18-1269-2021}} with UploadWizard

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