Abstract
A non-metallic flow-through reaction cell is described, designed for in situ time-resolved X-ray diffraction coupled with stable isotope analysis. The experimental setup allows the correlation of Cu isotope fractionation with changes in crystal structure during copper sulfide dissolution. This flow-through cell can be applied to many classes of fluid-mineral reactions that involve dissolution or ion exchange.
Original language | English (US) |
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Pages (from-to) | 429-432 |
Number of pages | 4 |
Journal | Journal of Applied Crystallography |
Volume | 44 |
Issue number | 2 |
DOIs | |
State | Published - Apr 2011 |
All Science Journal Classification (ASJC) codes
- General Biochemistry, Genetics and Molecular Biology