Correlation between Hinckley index and stacking order-disorder in kaolinite

Author:

Rao Wenxiu12,Liu Xin12,Lv Guocheng1ORCID,Liu Meng1,Wang Lijuan1,Niu Jinan3,Li Zhaohui4,Liao Libing1

Affiliation:

1. Engineering Research Center of Ministry of Education for Geological Carbon Storage and Low Carbon Utilization of Resources, Beijing Key Laboratory of Materials Utilization of Nonmetallic Minerals and Solid Wastes, National Laboratory of Mineral Materials, School of Materials Science and Technology, China University of Geosciences, Beijing 100083, China

2. These authors contributed equally to this work and should be considered co-first.

3. School of Materials and Physics, China University of Mining and Technology, Xuzhou 221116, China

4. Geosciences Department, University of Wisconsin-Parkside, Kenosha, Wisconsin 53144, U.S.A.

Abstract

Abstract Hinckley index (Hi) can be used to characterize the crystallinity of kaolinite. Stacking order-disorder in kaolinite can considerably affect its crystallinity. However, the correlation between Hi and stacking order-disorder in kaolinite has not been reported thus far. Herein, the correlation between stacking order-disorder in kaolinite and Hi was investigated via experiments (XRD, IR spectroscopy, TG-DSC), molecular simulation, and structure refinement. First, we experimentally discovered that the stacking order-disorder in kaolinite changed the relative position between two adjacent structural layers, mainly affecting the interlayer forces. When the kaolinite layers are orderly stacked, the inter-layer force is higher and the stacking lattice energy is lower. The lattice energy of kaolinite in different stacking states was simulated and analyzed using first-principles calculation. It was determined that the kaolinite layers are orderly stacked when two kaolinite layers have zero shift and disorderly stacked otherwise. Finally, through structural refinements, we proposed a new crystallinity index based on stacking order-disorder in kaolinite (crystallinity index based on stacking, CIS). CIS was well fitted to Hi (R2 = 0.986), indicating that kaolinite crystallinity, characterized by Hi, is essentially the ratio of orderly stacking to total stacking (the sum of ordered and disordered stacks). Furthermore, measuring Hi is difficult when kaolinite crystallinity is poor; however, CIS can be used alternatively. This study of the crystallinity of kaolinite will have important significance for its industrial application.

Publisher

Mineralogical Society of America

Subject

Geochemistry and Petrology,Geophysics

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