Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
1695935 | Applied Clay Science | 2009 | 5 Pages |
Abstract
The technological characterization of kaolin from the Borborema–Seridó region has shown that it is predominantly kaolinitic, pseudoplastic and thixotropic; approximately 50% of its particles size is less than 2 μm. By using electronic paramagnetic resonance (EPR) and Mössbauer spectroscopy (ME), it was observed that Fe2+ and Fe3+ substitute Al3+ in octahedral sites of kaolinite. After magnetic separation followed by chemical bleaching, kaolin reached a brightness index of 87.72% ISO and an opacity index of 85.58% ISO, indicating that it can be used mainly as a filler and a coating in the paper industry, paint and pottery, among other industries.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Fernanda Arruda Nogueira Gomes Silva, Adão B. Luz, João Alves Sampaio, Luiz Carlos Bertolino, Rosa Bernstein Scorzelli, Mathieu Duttine, Flávio Teixeira da Silva,