Preprints
https://doi.org/10.5194/egusphere-2026-4091
https://doi.org/10.5194/egusphere-2026-4091
27 Jul 2026
 | 27 Jul 2026
Status: this preprint is open for discussion and under review for Geochronology (GChron).

Technical Note: Stable Chloride Measurements at CAMS

Tyler S. Anderson and Alan Hidy

Abstract. We present a new method for preparing silicate samples for stable chloride analysis using the low-energy injection components of an accelerator mass spectrometry (AMS) system. This method uses Nb over AgBr as a bulking agent during sample preparation which drastically reduces background Cl signals (ion source memory) by a factor of ~100 and allows for faster, cheaper, and more precise analyses on low-Cl samples (<10 μg Cl). We demonstrate this approach with measurements of stable chlorine isotope ratios (35Cl/37Cl) performed on silicates, prepared in both AgBr and Nb matrices, that characterize chlorine concentrations of samples containing ~1500 ppm Cl. While this method was developed primarily to interrogate silicates, it performs equally well on other commonly analyzed sample matrices including carbonates and water. This Nb-based method is now the standard procedure at the Center for Accelerator Mass Spectrometry (CAMS) for preparing all stable Cl targets, including those accompanying 36Cl analyses.

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Tyler S. Anderson and Alan Hidy

Status: open (until 07 Sep 2026)

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Tyler S. Anderson and Alan Hidy
Tyler S. Anderson and Alan Hidy
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Short summary
We have developed a new method to measure stable Cl isotope ratios in rocks, improving on the standard method by preparing our samples in niobium instead of a silver bromide. This technique improves signal to noise by a factor of ~100, reduces sample measurement time and cost, and makes isotopic analyses of as little as 1 microgram of Cl extracted from a rock possible. This improves measurement of 36Cl and makes small or chlorine-poor samples accessible for stable isotope analysis.
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