Selenium and Molybdenum Adsorption on Kaolinite Clay Mineral Coated with Hydrous Oxides of Iron and Aluminum

2003 ◽  
pp. 237-249 ◽  
Author(s):  
D. K. Bhumbla ◽  
S. S. Dhaliwal ◽  
K. S. Sajwan ◽  
B. S. Sekhon
Keyword(s):  
Clay Mineral ◽  
Kaolinite Clay ◽  
Hydrous Oxides

scholarly journals Dataset of multiple methodology characterization of an illite-kaolinite clay mineral for the purpose of using it as ceramic membrane supports

Data in Brief ◽  
2020 ◽  
Vol 29 ◽  
pp. 105300 ◽  
Author(s):  
Abdelaziz Elgamouz ◽  
Najib Tijani ◽  
Ihsan Shehadi ◽  
Kamrul Hasan ◽  
Mohamad Al-Farooq Kawam
Keyword(s):  
Clay Mineral ◽  
Ceramic Membrane ◽  
Kaolinite Clay

scholarly journals Erratum to “Characterization of the firing behaviour of an illite-kaolinite clay mineral and its potential use as membrane support” [Heliyon 5, (8), (August 2019), e02281]

Heliyon ◽  
2019 ◽  
Vol 5 (12) ◽  
pp. e02714
Author(s):  
Abdelaziz Elgamouz ◽  
Najib Tijani ◽  
Ihsan Shehadi ◽  
Kamrul Hasan ◽  
Mohamad Al-Farooq Kawam
Keyword(s):  
Clay Mineral ◽  
Kaolinite Clay ◽  
Potential Use

scholarly journals Wetting Effects and Molecular Adsorption at Hydrated Kaolinite Clay Mineral Surfaces

2016 ◽  
Vol 120 (21) ◽  
pp. 11433-11449 ◽  
Author(s):  
Thomas Underwood ◽  
Valentina Erastova ◽  
H. Chris Greenwell
Keyword(s):  
Clay Mineral ◽  
Molecular Adsorption ◽  
Mineral Surfaces ◽  
Kaolinite Clay

scholarly journals Influence of Degree of Clay-Mineral Crystallization and Free Iron Oxide Content on the Cation Exchange Capacity of Catalina and Cialitos Soils

1969 ◽  
Vol 52 (2) ◽  
pp. 148-154
Author(s):  
Raúl Pérez Escolar ◽  
M. A. Lugo López
Keyword(s):  
Cation Exchange ◽  
Iron Oxides ◽  
Clay Mineral ◽  
Cation Exchange Capacity ◽  
Thermal Analyses ◽  
Clay Fraction ◽  
Exchange Capacity ◽  
Oxide Content ◽  
Kaolinite Clay ◽  
Free Iron

Catalina and Cialitos soils have different cation exchange capacities, even though their organic-matter and clay contents are similar. X-ray and differential thermal analyses were made on the clay fraction to determine whether this variation in exchange capacity could be attributed to differences in clay mineral composition. The analyses revealed that, in both cases, kaolinite is the predominant clay mineral. However, it was found that, in Cialitos clay the kaolinite is poorly crystallized, whereas crystals are well defined in Catalina clay. Since the poorer the crystallinity, the higher the exchange capacity, this could account for the higher cation exchange capacity of Cialitos clay. Another factor that may also partly account for the difference in cation exchange capacity is the higher content of free iron oxides in Catalina clay. It is well known that free iron oxides block exchange positions in kaolinite clay minerals.

scholarly journals Characterization of the firing behaviour of an illite-kaolinite clay mineral and its potential use as membrane support

Heliyon ◽  
2019 ◽  
Vol 5 (8) ◽  
pp. e02281 ◽  
Author(s):  
Abdelaziz Elgamouz ◽  
Najib Tijani ◽  
Ihsan Shehadi ◽  
Kamrul Hasan ◽  
Mohamad Al-Farooq Kawam
Keyword(s):  
Clay Mineral ◽  
Kaolinite Clay ◽  
Potential Use

High Resolution Replication of Organoclay Surfaces

1982 ◽  
Vol 40 ◽  
pp. 576-577
Author(s):  
W. W. Barker ◽  
W. E. Rigsby ◽  
V. J. Hurst ◽  
W. J. Humphreys
Keyword(s):  
Clay Mineral ◽  
Organic Molecule ◽  
Organic Molecules ◽  
X Ray Diffraction ◽  
Xrd Pattern ◽  
X Ray ◽  
Naturally Occurring ◽  
Silicate Layers ◽  
Mineral Identification

Experimental clay mineral-organic molecule complexes long have been known and some of them have been extensively studied by X-ray diffraction methods. The organic molecules are adsorbed onto the surfaces of the clay minerals, or intercalated between the silicate layers. Natural organo-clays also are widely recognized but generally have not been well characterized. Widely used techniques for clay mineral identification involve treatment of the sample with H2 O2 or other oxidant to destroy any associated organics. This generally simplifies and intensifies the XRD pattern of the clay residue, but helps little with the characterization of the original organoclay. Adequate techniques for the direct observation of synthetic and naturally occurring organoclays are yet to be developed.

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