Baltimore Harbor, sediment (site L)
Chesapeake Bay, Baltimore Harbor (Maryland), United States
Sediments
- Type
- Sediment
Sediment with 0.05 % Cr, about 6 km seaward of the former chromium works. Crustal Os (0.644) despite the highest content among crustal samples: industrial discharges do not carry anthropogenic Os according to the authors. Helz et al. (2000).
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 |
|---|---|---|---|---|
| 0.6441 | 1 | core sediment Single analysis (BH). BH Os 0.205 ng/g. | Helz et al. (2000), Osmium isotopes demonstrate distal transport of contaminated sediment… |
Deposits of the same type
- Pebble iron oxide precipitates United States
- Laohugou No. 12 Glacier cryoconite China
- Yuzhufeng Glacier cryoconite China
- Bayi Glacier cryoconite China
- Qiyi Glacier cryoconite China
- Yulong Snow Mountains glacier cryoconite China
- Hailuogou Glacier (Mount Gongga) cryoconite China
- Dangxiong Glacier cryoconite China
Cite this page
IsoFind Atlas (2026). Baltimore Harbor, sediment (site L), isotope signatures. https://www.isofind.tech/isotopes/en/sites/port-de-baltimore-sediment-site-l/ (accessed 2026-10-21).
@misc{isofind2026baltimoreharborsedimentsiteli,
title = {Baltimore Harbor, sediment (site L), isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/sites/port-de-baltimore-sediment-site-l/},
note = {Accessed 2026-10-21}
}Updated : 2026-10-21