Sub-10 Nanomole Perchlorate δ 37 Cl, δ 18 O, and Δ 17 O Measurements by ESI-Orbitrap-MS
Abstract
Perchlorate (ClO 4 – ) is found in both Earth and Martian surface environments, yet its formation mechanism remains enigmatic. ClO 4 – isotope composition can help to identify the formation mechanism/source, but the conventional gas-source isotope ratio mass spectrometry (IRMS) method requires micromole or larger sample sizes together with tedious mineral precipitation steps. Here, a capable method for measuring δ 37 Cl, δ 18 O, and Δ 17 O values of trace ClO 4 – (
Fields of Study & Subjects
Chemical Analysis and Environmental Impact
Planetary Science and Exploration
Atmospheric Ozone and Climate
Publication details
- Journal / source
- Analytical Chemistry
- Publisher
- American Chemical Society (ACS)
- Volume
- 98
- Issue
- 8
- Pages
- 6034–6044
- Publication date
- 29 January 2026
- Language
- EN