Rhine at Bingen
Rhineland-Palatinate, Germany
Rivers and surface water
- Type
- River or surface water
River studied by Nielsen et al. (2005) for dissolved Tl, value taken from Table 13.3 of Nielsen and Rehkämper (2012). The riverine mean (-2.5 ± 1.0) is close to the continental crust (-2.0): continental weathering fractionates Tl little; the lightest rivers (Danube, Rhine at Rueun, Doubs, Eder: -6.7 to -4.2) are ascribed to marine carbonates in their catchments. Indicative coordinates (Bingen town).
ε205Tl in ε units (parts per 10,000) Values of the same system
Standard : NIST SRM 997
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| −2.9 ± 1 ε | 1 | Single analysis; ± 1.0 ε (typical uncertainty); 6.71 ng/kg dissolved Tl. | Nielsen et Rehkämper (2012), Thallium isotopes and their application to problems in earth… |
Deposits of the same type
- Rhine at Speyer Germany
- Rhine at Laufenburg Switzerland
- Birs, Switzerland Switzerland
- Saane (Sarine), Switzerland Switzerland
- Rhine at Rueun Switzerland
- Verzasca, Switzerland Switzerland
- Ticino, Switzerland Switzerland
- Elbe (German reach) Germany
Cite this page
IsoFind Atlas (2026). Rhine at Bingen, isotope signatures. https://www.isofind.tech/isotopes/en/sites/rhin-a-bingen/ (accessed 2026-10-16).
@misc{isofind2026rhineatbingenisotopesignature,
title = {Rhine at Bingen, isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/sites/rhin-a-bingen/},
note = {Accessed 2026-10-16}
}Updated : 2026-10-16