Japan Geoscience Union Meeting 2022

Presentation information

[J] Oral

M (Multidisciplinary and Interdisciplinary) » M-IS Intersection

[M-IS12] Interface- and nano-phenomena on crystal growth and dissolution

Sun. May 22, 2022 3:30 PM - 5:00 PM 104 (International Conference Hall, Makuhari Messe)

convener:Yuki Kimura(Institute of Low Temperature Science, Hokkaido University), convener:Hitoshi Miura(Graduate School of Science, Department of Information and Basic Science, Nagoya City University), Hisao Satoh(Low-Level Radioactive Waste Disposal Center, Japan Nuclear Fuel Limited), convener:Katsuo Tsukamoto(Tohoku University), Chairperson:Kyoko Kitakami Tanaka(Tohoku University), Yuki Kimura(Institute of Low Temperature Science, Hokkaido University)

4:15 PM - 4:30 PM

[MIS12-09] Intercalated Molecule Exchange Process of Thiomalate Substituted Octacalcium Phosphate Crystals during Phase Conversion

*Yuki Sugiura1, Masanori Horie1 (1.National Institute of Advanced Industrial Science and Technology)

Keywords:Calcium phosphate, Ion exchange, phase conversion

Octacalcium phosphate (OCP) is a layered calcium phosphate compound that has attracted significant attention as a new biomaterial due to its excellent biocompatibility. Its interlayer structure, known as HPO4-OH layer, can be easily replaced by dicarboxylic acid. However, the ionic and/or molecular exchange process of substituted dicarboxylic acid into OCP interlayer is still unclear. Therefore, in this study, we evaluate the molecular exchange process for thiomalate (SH-malate)-substituted OCP (OCP-SH-malate) during the phase conversion process to other phases in disodium hydrogen phosphate solution (Na2HPO4). When the OCP-SH-malate is immersed in 1 mol/L Na2HPO4 at 40 °C while shaking at 200 rpm, SH-malate, first desorbed from the interlayer of OCP-SH-malate and the HPO4-OH layer structure, is formed at the interlayer where the SH-malate was dissolved. The HPO4-OH layer structure is unstable, making it easily convert to hydroxyapatite (HAp) via dehydration upon further immersion. During this reaction, besides the dissolution of marginal edges of the crystals, crystals morphology was no obvious changes, neither were there evidences of dissolution and collapsing of OCP crystals nor nucleation of newly created crystals.