Da Qaidam Lake: cool spring (point 19)
Qinghai, northern Qaidam Basin, China
Groundwater
- Type
- Groundwater
Spring fed mainly by melting ice and snow from a 5263 m summit. Feeding water of the salt lake sampled in October 1989 by Xiao et al. (1992); position on the Figure 1 map, without coordinates.
δ11B in ‰ (per mil) Values of the same system
Standard : NIST SRM 951
| Value | Range | n | Mineral or matrix | Source |
|---|---|---|---|---|
| 13.33 ‰ | 1 | spring water (dissolved boron) Single analysis (19). 0.22 µg/mL B (Huang, 1974), pH 8.4. | Xiao et al. (1992), Boron isotopic compositions of brine, sediments, and source water in … |
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Cite this page
IsoFind Atlas (2026). Da Qaidam Lake: cool spring (point 19), isotope signatures. https://www.isofind.tech/isotopes/en/sites/lac-da-qaidam-source-froide-point-19/ (accessed 2026-10-19).
@misc{isofind2026daqaidamlakecoolspringpoint19,
title = {Da Qaidam Lake: cool spring (point 19), isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/sites/lac-da-qaidam-source-froide-point-19/},
note = {Accessed 2026-10-19}
}Updated : 2026-10-19