The new CLOCIT irradiation facility for 40Ar/39Ar geochronology: Characterization, comparison with CLICIT, and implications for high-precision geochronology

This is a Preprint and has not been peer reviewed. The published version of this Preprint is available: https://doi.org/10.1111/ggr.12217. This is version 2 of this Preprint.

Add a Comment

You must log in to post a comment.


Comments

There are no comments or no comments have been made public for this article.

Downloads

Download Preprint

Supplementary Files
Authors

Daniel Rutte, Tim A. Becker, Al Deino, Steven R. Reese, Paul R. Renne, Robert A. Schickler

Abstract

The Cadmium-Lined Outer-Core Irradiation Tube (CLOCIT) is a new irradiation facility for 40Ar/39Ar geochronology at the Oregon State University TRIGA® reactor. We report fluence parameters from the first four CLOCIT irradiations and compare them to the existing Cadmium-Lined Inner-Core Irradiation Tube (CLICIT). CLOCIT provides an average neutron flux equivalent of 1.45–1.53 ×10-4 J/h; about 55% of CLICIT. Radial fluence gradients are on the order of 0.2–2.4 %/cm. A planar fit of J-values results in residuals in the range of uncertainty in the J-value, but systematic deviations resolve a non-planar component of the neutron flux field which has also been observed in CLICIT. Axial neutron fluence gradients are 0.6–1 %/cm, compared to 0.7–1.6 %/cm for the CLICIT. Production rate ratios of interfering reactions are (40Ar/39Ar)K = (4±6) ×10-4 and (38Ar/39Ar)K = (1.208±0.002) ×10-2, (36Ar/37Ar)Ca = (2.649±0.014) ×10-4, (38Ar/37Ar)Ca = (3.33±0.12) ×10-5, and (39Ar/37Ar)Ca = (9.1±0.28) ×10-4, similar to the CLICIT values.

DOI

https://doi.org/10.31223/osf.io/2us4z

Subjects

Earth Sciences, Geochemistry, Physical Sciences and Mathematics

Keywords

Dates

Published: 2018-02-20 12:28

Last Updated: 2018-04-27 17:01

Older Versions
License

Academic Free License (AFL) 3.0