Precise measurement of chlorine stable isotopic ratios by thermal ionization mass spectrometry
Masahiko Numata, Noboru Nakamura, Toshitaka Gamo
Geochemical Journal, Vol. 35, No. 2, P. 89-100, 2001
ABSTRACT
An improved method for chlorine isotopic analysis by thermal ionization mass spectrometry of Cs2Cl+ has been investigated for precise measurement of 37Cl/35Cl isotopic ratios for small amount of samples. Chlorine in organic and inorganic samples was recovered as AgCl and converted to CsCl with metallic Mg and Cs-form ion exchange resin. The CsCl (containing 2 μg of Cl) was loaded on a Ta filament together with graphite powder. The 37Cl/35Cl ratio measurement was carried out using Cs2Cl+ ions with multi Faraday cup (static mode) for 80–100 min each single run. Replicate analysis of ocean water and laboratory standard (CsCl reagent) yield the in-run precision of 0.1–0.2‰ (2σm) for 300–400 ratios and external precision of 0.1–0.2‰ (1σSD). This method has been tested on a variety of chemical reagents including metal chlorides, hydrochloric acid and chlorinated organic solvents. It was found that the artificial chlorine compound show large variations of 37Cl/35Cl ratio (total ranges from −5 to +3‰ relative to standard mean ocean chloride) depending upon manufacturing processes. We suggest that the high sensitivity and precision technique established in this work would allow us to detect small isotopic variations of chlorine in small amounts of natural samples such as terrestrial materials (minerals/rocks, sediments, groundwater, etc, as well as environmental materials), meteorites and other planetary materials.
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