Da Qaidam Lake: west spring (point 25)
Qinghai, northern Qaidam Basin, China
Groundwater
- Type
- Groundwater
Spring without river input, of deep origin according to the authors; lowest δ11B of the feeding waters. 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 |
|---|---|---|---|---|
| −11.72 ‰ | 1 | spring water (dissolved boron) Single analysis (25). 4.00 µg/mL B, pH 8.2. | 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: west spring (point 25), isotope signatures. https://www.isofind.tech/isotopes/en/sites/lac-da-qaidam-source-ouest-point-25/ (accessed 2026-10-19).
@misc{isofind2026daqaidamlakewestspringpoint25,
title = {Da Qaidam Lake: west spring (point 25), isotope signatures},
author = {{IsoFind Atlas}},
year = {2026},
url = {https://www.isofind.tech/isotopes/en/sites/lac-da-qaidam-source-ouest-point-25/},
note = {Accessed 2026-10-19}
}Updated : 2026-10-19