Chromium(III) — chromium(VI) interconversions in seawater
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The marine Cr cycle is mainly governed by inputs from oxidative weathering on land and by removal through authigenic burial in reducing margin sediments and anoxic basins.
“The marine Cr cycle is primarily controlled by dissolved/particulate inputs derived from oxidative weathering on the continents and removal of Cr via authigenic burial in reducing continental margin sediments and anoxic marine basins”
From The chromium isotope composition of reducing and oxic marine sediments (2016) · cites this paper as Van der Weijden and Reith, 1982
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- Authors
- Van Der Weijden, C. H., & Reith, M.
- Affiliations
- Utrecht University (NL)
- Venue
- Marine Chemistry
- Publisher
- Elsevier BV
- Published
- 1982-12
- Volume
- 11
- Issue
- 6
- Pages
- 565-572
- ISSN
- 0304-4203 (ISSN-L)
- OpenAlex
- W2030955013
- Cited by
- 76
- References
- 11
- Citations by year
- 2026: 1 · 2025: 1 · 2024: 3 · 2023: 5 · 2022: 1 · 2021: 5 · 2020: 2 · 2019: 1 · 2018: 1 · 2017: 1 · 2016: 4 · 2015: 3 · 2014: 1 · 2013: 2 · 2012: 1
- FWCI
- 1.31
- Type
- journal article
- Language
- en
- Open access
- Licence
- Locations
- Marine Chemistry (publishedVersion)
- Utrecht University Repository (Utrecht University) (submittedVersion, other-oa)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Geochemistry and Elemental Analysis
- Physical Sciences › Environmental Science › Health, Toxicology and Mutagenesis › Chromium effects and bioremediation
- Physical Sciences › Earth and Planetary Sciences › Oceanography › Marine and coastal ecosystems
- Keywords
- trivalent chromium, hexavalent chromium, redox interconversion, dissolved chromium, seawater, dissolved oxygen oxidation, manganese oxide, catalytic oxidation, kinetic control, manganese dioxide
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