Abstract
Measurements of chromium (Cr) stable-isotope fractionation in laboratory experiments and natural waters show that lighter isotopes reacted preferentially during CR(VI) reduction by magnetite and sediments. The 53Cr/52Cr ratio of the product was 3.4 ± 0.1 per mil less than that of the reactant.53Cr/52Cr shifts in water samples indicate the extent of reduction, a critical process that renders toxic CR(VI) in the environment immobile and less toxic.
Original language | English (US) |
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Pages (from-to) | 2060-2062 |
Number of pages | 3 |
Journal | Science |
Volume | 295 |
Issue number | 5562 |
DOIs | |
State | Published - Mar 15 2002 |
ASJC Scopus subject areas
- General