Kinetics of cadmium desorption from fibrous silicate clay minerals: Influence of organic ligands and aging

2007 ◽  
Vol 37 (1-2) ◽  
pp. 175-184 ◽  
Author(s):  
Mehran Shirvani ◽  
Hossein Shariatmadari ◽  
Mahmoud Kalbasi
2008 ◽  
Vol 72 (5) ◽  
pp. 1335-1349 ◽  
Author(s):  
Manabu Fujii ◽  
Andrew L. Rose ◽  
T. David Waite ◽  
Tatsuo Omura

Clay Minerals ◽  
1990 ◽  
Vol 25 (3) ◽  
pp. 313-327 ◽  
Author(s):  
A. P. W. Hodder ◽  
B. E. Green ◽  
D. J. Lowe

AbstractThe kinetics of clay formation in buried paleosols developed from late Quaternary rhyolitic tephra layers near Rotorua, New Zealand, can be described in terms of a combination of parabolic and linear kinetics, reflecting the hydration of glass, and the formation of clay minerals, respectively. Such a model is consistent with the formation of clay minerals showing an Arrhenian temperature dependence and suggests, on the basis of calculated activation energies, that the process of formation of Al-rich allophane (imogolite) is diffusion controlled, whereas the rate of formation of Si-rich allophane is controlled by the chemical processes at the site of reaction.


2018 ◽  
Vol 20 (25) ◽  
pp. 17226-17233 ◽  
Author(s):  
S. Jelavić ◽  
S. L. S. Stipp ◽  
N. Bovet

We show direct measurements of the composition in the interface between clay minerals and aqueous solutions containing organic ligands.


Fuel ◽  
2008 ◽  
Vol 87 (13-14) ◽  
pp. 3137-3146 ◽  
Author(s):  
C CHENG ◽  
Y HWANG ◽  
J LENHART ◽  
H WALKER

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