Near-Infrared Spectroscopic Study of OH Stretching Modes in Kaolinite and Dickite
Kaolinite and dickite are differently ordered polytypes of kaolinite-group minerals, whose differences are in the stacking mode of layers and ion occupation. Fourier transform infrared spectroscopy was used to collect information about the differences between the two minerals. The common characteris...
Main Authors: | Shaokun Wu, Mingyue He, Mei Yang, Bijie Peng |
---|---|
Format: | Article |
Language: | English |
Published: |
MDPI AG
2022-06-01
|
Series: | Crystals |
Subjects: | |
Online Access: | https://www.mdpi.com/2073-4352/12/7/907 |
Similar Items
-
Geochemistry of Fe3+ in the hydrothermal dickite from Jedlina Zdroj (Lower Silesia, Poland)
by: NENAD S. KRSTIĆ, et al.
Published: (2009-12-01) -
Geochemistry of Fe3+ in the hydrothermal dickite from Jedlina Zdroj (Lower Silesia, Poland)
by: Premović Pavle I., et al.
Published: (2009-01-01) -
Near-Infrared Spectroscopy Study of OH Stretching Modes in Pyrophyllite and Talc
by: Haoyu Wu, et al.
Published: (2022-12-01) -
Near-Infrared Spectroscopy Study of Serpentine Minerals and Assignment of the OH Group
by: Shaokun Wu, et al.
Published: (2021-09-01) -
Preparation and Mechanism of Dickite-cesium Acetate Intercalated Complex
by: ZHONG Xiang-hua, et al.
Published: (2018-07-01)