2010
DOI: 10.3923/ajmskr.2010.121.136
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Diatomite: Its Characterization, Modifications and Applications

Abstract: The review tackles common diatomite, its characterization, modifications and its composites, heavy metal toxicity and its immobilization techniques using diatomite, other important applications of diatomite.

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Cited by 114 publications
(21 citation statements)
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“…The results of the chemical analysis of the materials (Table 2) indicate that the main compounds present in D and SCBA are silica and alumina, with low traces of CaO and MgO. Similar results were reported by Wen-Tien et al, 2004;Galal Morsy, 2010;Chargas-Cordeiro et al, 2009. The sum of major oxides is higher than 70%; therefore, the materials have pozzolanic potential (ASTM, 2012) and can react in an alkaline environment created by C (Malhotra and Ramezanianpour, 1994).…”
Section: Characterization Of the Materialssupporting
confidence: 61%
“…The results of the chemical analysis of the materials (Table 2) indicate that the main compounds present in D and SCBA are silica and alumina, with low traces of CaO and MgO. Similar results were reported by Wen-Tien et al, 2004;Galal Morsy, 2010;Chargas-Cordeiro et al, 2009. The sum of major oxides is higher than 70%; therefore, the materials have pozzolanic potential (ASTM, 2012) and can react in an alkaline environment created by C (Malhotra and Ramezanianpour, 1994).…”
Section: Characterization Of the Materialssupporting
confidence: 61%
“…On the other hand, diatomite promoted a significant increase in the CEC and availability of K and Mn contents. The increase in CEC may be due to the high porosity (35 -65%), high permeability, low density, small particle size, and high specific surface area of diatomite (Bakr, 2010). Therefore, it is capable of retaining water and cationic ions owing to its CEC > 50 cmol c kg -1 (Pati et al, 2016).…”
Section: Diatomite Effects On the Soil Chemical Characteristicsmentioning
confidence: 99%
“…La diatomita forma parte del grupo de rocas silíceas sedimentarias, que posee los siguientes rasgos característicos: (1) presencia de sílice amorfo activo SiO2, (2) estructura de finos poros, (3) ligereza y (4) baja conductividad térmica (Galal Mors, 2010; Ivanov y Belyakov, 2008; Loganina et al 2014). Las tierras diatomeas están constituidas por restos de esqueletos fosilizados de diatomeas, un tipo de algas unicelulares de origen acuático (Arik, 2003;Galal Mors, 2010;Loganina et al, 2014;Paschen, 1986). La diatomita se utiliza desde hace miles de años, pero en los últimos 200 años, se ha producido un incremento en su uso y una extracción a escala comercial (Flower, 2013).…”
Section: Método a Fundamento Teóricounclassified