Abstract
It is generally believed that H2O and OH− are the key species stabilizing and controlling amorphous calcium carbonate “polyamorph” forms, and may in turn control the ultimate crystallization products during synthesis and in natural systems. Yet, the locations and hydrogen-bonding network of these species in ACC have never been measured directly using neutron diffraction. We report a synthesis route that overcomes the existing challenges with respect to yield quantities and deuteration, both of which are critically necessary for high quality neutron studies.
Original language | English |
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Pages (from-to) | 2942-2945 |
Number of pages | 4 |
Journal | Chemical Communications |
Volume | 53 |
Issue number | 20 |
DOIs | |
State | Published - 2017 |
Funding
This work was supported by the US Department of Energy (DOE), Office of Science (SC), Office of Basic Energy Sciences (BES), Chemical Sciences, Geosciences, and Biosciences Division. Efforts by KP, DO, and JL were supported in part by the DOE, SC, BES Early Career Research Program (KC040602), under contract number DE-AC05-00OR22725. The NOMAD instrument at ORNL’s SNS is sponsored by the DOE, SC, BES, Scientific User Facilities Division. 11-ID-B was supported by the DOE, SC, BES, under Contract No. DE-AC02-06CH11357. The monohydrocalcite sample (NMNH 135404 00) is from the mineral collection of the Department of Mineral Sciences, Smithsonian Institution.