Connecticut (dissolved osmium)
Connecticut basin, United States
Rivers and surface water
- Type
- River or surface water
River quoted by Sharma et al. (1999, Table 1) as a comparison for Himalayan rivers. Sampled at Wells River (Vermont), basin of Paleozoic terranes (Sharma and Wasserburg, 1997).
187Os/188Os isotope ratio, no unit Values of the same system
Standard : Rapport absolu, sans standard de référence
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 1.05 | 1 | river water (dissolved load) Single analysis: measured 187Os/186Os 7.1 ± 0.4, 8.8 after a blank correction scaled on the Mississippi. Dissolved Os 13.6 ± 0.9 fmol/kg, the lowest content of the four rivers. With the normal 186Os/188Os ratio of Table 1 (0.11995), one would get 1.25, 1.73, 1.06 and 1.28 for the Mississippi, Columbia, Connecticut and Vistula. | Sharma & Wasserburg (1997), Osmium in the rivers, Geochimica et Cosmochimica Acta 61(24):… |
Deposits of the same type
- Ottawa River at Chenaux Canada
- Missouri at Columbia United States
- Mississippi (dissolved osmium) United States
- Rio Grande (upper basin) United States
- Rio Negro at Manaus Brazil
- Solimões at Manaus Brazil
- Amazon Brazil
- Amazon, lower course (Óbidos) Brazil
Cite this page
IsoFind Atlas (2026). Connecticut (dissolved osmium), isotope signatures. https://www.isofind.tech/isotopes/en/sites/connecticut-osmium-dissous/ (accessed 2026-10-20).
@misc{isofind2026connecticutdissolvedosmiumiso,
title = {Connecticut (dissolved osmium), isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/sites/connecticut-osmium-dissous/},
note = {Accessed 2026-10-20}
}Updated : 2026-10-20