scholarly journals CO2 Capture by Nickel Hydroxide Interstratified in the Nanolayered Space of a Synthetic Clay Mineral

2020 ◽  
Vol 124 (48) ◽  
pp. 26222-26231
Author(s):  
Kristoffer W. Bø Hunvik ◽  
Patrick Loch ◽  
Leide P. Cavalcanti ◽  
Konstanse Kvalem Seljelid ◽  
Paul Monceyron Røren ◽  
...  
Keyword(s):  
Clay Mineral ◽  
Co2 Capture ◽  
Nickel Hydroxide ◽  
Synthetic Clay

Synthetic clay mineral as nanocarrier of sulfamethoxazole and trimethoprim

2018 ◽  
Vol 161 ◽  
pp. 395-403 ◽  
Author(s):  
D. Hernández ◽  
L. Lazo ◽  
L. Valdés ◽  
L.C. de Ménorval ◽  
Z. Rozynek ◽  
...  
Keyword(s):  
Clay Mineral ◽  
Synthetic Clay

Reversible surface-sorption-induced electron-transfer oxidation of Fe(II) at reactive sites on a synthetic clay mineral

2007 ◽  
Vol 71 (4) ◽  
pp. 863-876 ◽  
Author(s):  
A. Géhin ◽  
J.-M. Grenèche ◽  
C. Tournassat ◽  
J. Brendlé ◽  
D.G. Rancourt ◽  
...  
Keyword(s):  
Electron Transfer ◽  
Clay Mineral ◽  
Synthetic Clay

Cation exchange dynamics confined in a synthetic clay mineral

2014 ◽  
Vol 223 (9) ◽  
pp. 1883-1893 ◽  
Author(s):  
G. Grassi ◽  
L. Michels ◽  
Z. Rozynek ◽  
M. A. S. Altoé ◽  
E. C. dos Santos ◽  
...  
Keyword(s):  
Cation Exchange ◽  
Clay Mineral ◽  
Synthetic Clay

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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