A slow-cooling-rate in situ cell for long-duration studies of mineral precipitation in cold aqueous environments on Earth and other planetary bodies

Thompson, S.P.; Kennedy, H.; Day, S.J.; Baker, A.R.; Butler, B.M.; Safi, E.; Kelly, J.; Male, A.; Potter, J.; Cobb, T.; Murray, C.A.; Tang, C.C.; Evans, A.; Mercado, R.

doi:10.1107/S1600576718008816

Journal of Applied Crystallography Journal of Applied
Crystallography

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Figure 4
Cell temperatures at various data-collection dates. Gaps are due to synchrotron shutdowns. Arrows A, B and C indicate 30, 70 and 184 days (T = −12.7, −23.3 and −27.7°C, respectively; 260.5, 249.9 and 245.5 K, respectively) for comparison with data shown in Figs. 6 and 7.

JOURNAL OF
APPLIED
CRYSTALLOGRAPHY

ISSN: 1600-5767

Volume 51| Part 4| August 2018| Pages 1197-1210

https://doi.org/10.1107/S1600576718008816

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