Characteristic microstructure underlying the fast hydration- dehydration reaction of b-La2( SO4) 3: " fine platy joints" with " loose grain boundaries"
Characteristic microstructure underlying the fast hydration- dehydration reaction of b-La2( SO4) 3: " fine platy joints" with " loose grain boundaries"
复制标题
DOI:
10.1039/c8ta06721j
复制
发表时间:
2018-12-28
影响因子:
11.9
通讯作者:
Uda, Tetsuya
中科院分区:
文献类型:
--
作者:
Shizume, Kunihiko;Hatada, Naoyuki;Uda, Tetsuya
The fast hydration/dehydration (water insertion/deinsertion) reaction of beta-La-2(SO4)(3) is expected to be applied to thermochemical heat storage, but its kinetics have not been well understood. In this work, we investigated the microstructure of beta-La-2(SO4)(3) and its contribution to the hydration reaction rate. From specific surface area measurements and transmission electron microscopy, a unique fine microstructure that looks like platy joints in geology was found in beta-La-2(SO4)(3) particles with a plate thickness of several hundred nanometers. There are loose grain boundaries where even nitrogen gas can diffuse. This microstructure is formed when beta-La-2(SO4)(3) is synthesized through dehydration of La-2(SO4)(3)9H(2)O. The hydration reaction rate of beta-La-2(SO4)(3) was quantitatively evaluated by thermogravimetry. Based on these results, we established a reasonable mechanism for water diffusion in beta-La-2(SO4)(3): water diffuses preferentially through the loose grain boundaries in the platy joints and is taken in respective crystal grains. The surface reaction on the platy grains presumably determines the rate of the hydration reaction. It is suggested that if we can increase the total surface area of platy grains during the synthesis process of beta-La-2(SO4)(3), a faster rate for the hydration reaction can be expected.