2017
DOI: 10.1016/j.clay.2017.06.001
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Methodological reconstruction of dioctahedral 1:1 phyllosilicate polytypes

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Cited by 2 publications
(1 citation statement)
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“…Studies have been conducted to obtain atomic coordinates and to propose a model that describes the structure of the main components of clays such as dickite (Dera, Prewitt, Japel, Bish, Johnston, 2003;Yan, Wang, 2018), nacrite (Jaafar, Rhaiem, Ben, Amara, 2016), and kaolinite ( Teixeira, Brandão, Nunes, 2017). Our results show kaolinite as the main component of the studied pink clay, 1:1 layer (Figure 4), inner hydroxyl groups (red and light pink), a tetrahedron (dark blue), and octahedron (light blue), iron atoms replaces silicate and aluminum sites in kaolinite.…”
Section: Resultsmentioning
confidence: 99%
“…Studies have been conducted to obtain atomic coordinates and to propose a model that describes the structure of the main components of clays such as dickite (Dera, Prewitt, Japel, Bish, Johnston, 2003;Yan, Wang, 2018), nacrite (Jaafar, Rhaiem, Ben, Amara, 2016), and kaolinite ( Teixeira, Brandão, Nunes, 2017). Our results show kaolinite as the main component of the studied pink clay, 1:1 layer (Figure 4), inner hydroxyl groups (red and light pink), a tetrahedron (dark blue), and octahedron (light blue), iron atoms replaces silicate and aluminum sites in kaolinite.…”
Section: Resultsmentioning
confidence: 99%