Sub-10 Nanomole Perchlorate δ 37 Cl, δ 18 O, and Δ 17 O Measurements by ESI-Orbitrap-MS

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Authors: Longchen Zhu, Yihang Hong, Shohei Hattori, Zhenfei Wang, Zhao Wei, Yongbo Peng, Nils Johannes Kuhlbusch, Bao Huiming
Cited by: 2
References: 40

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