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These are scheduled events to help delegates test out the tools and platform we will be using for the Q&A and other events at the conference.
Our workshop program provides training and teaching in topics across geochemistry and related fields. We are currently liaising with the workshop organisers to ascertain if any workshops can become virtual. Any updates will be added to this page.
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An X-Ray Spectrometry Method for Estimating Diffusion and Ion-Exchange Properties of Rocks
Morfin S, Hafezian G, Kumahor S & Al T
Morfin S, Hafezian G, Kumahor S & Al T (2020) Goldschmidt Abstracts, 2020 1847
The author has not provided any additional details.
08b: Room 3, View in program
Listed below are questions that have been submitted by the community that the author will try and cover in their presentation. To submit a question, ensure you are signed in to the website. Authors or session conveners approve questions before they are displayed here.
In the context of the selected tracers, are there any limitations associated with sample mineralogy (i.e., are there special considerations on the tracer used with respect to the rock type/composition of the samples under investigation)? Based on the presentation, the rotation speed would be adjusted based on the core diameter/sample size in order to capture the full sample, over 360 degrees, in a given time interval, correct (i.e., it would require adjustment for different sample sizes to ensure full coverage and to eliminate the beam hardening artefacts; is that correct)?
Yes, one important consideration is the compatibility of the tracer with the rock composition. For example, we commonly choose iodide as our tracer because it has a relatively high X-ray attenuation coefficient, and in most cases we assume it is a conservative tracer. However, iodide sometimes behaves in a non-conservative manner in rocks that have elevated organic carbon content. The number of rotations is not critical as long as it is more than 1. The number of rotations is dictated by the acquisition time, which is optimized for total counts vs total acquisition time. Eliminating the beam hardening effect is achieved by selecting narrow energy ranges.
Is this based on synchrotron or lab-based CT? What type of tracer are you using? Niopam?
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