Role of clay minerals in controlling phosphorus availability in a subtropical Alfisol

Geoderma ◽  
2022 ◽  
Vol 409 ◽  
pp. 115592
Author(s):  
Juan Xiong ◽  
Zhaohui Liu ◽  
Yupeng Yan ◽  
Jinling Xu ◽  
Dong Liu ◽  
...  
1981 ◽  
pp. 15-30
Author(s):  
Cyril Ponnamperuma ◽  
Elaine Friebele ◽  
Akira Shimoyama

2020 ◽  
Vol 288 ◽  
pp. 83-100
Author(s):  
Silvan Wick ◽  
Bart Baeyens ◽  
Maria Marques Fernandes ◽  
Jörg Göttlicher ◽  
Marlene Fischer ◽  
...  

2019 ◽  
Vol 185 ◽  
pp. 149-161 ◽  
Author(s):  
Aref Alshameri ◽  
Hongping He ◽  
Chen Xin ◽  
Jianxi Zhu ◽  
Wei Xinghu ◽  
...  

2015 ◽  
Vol 118 ◽  
pp. 283-289 ◽  
Author(s):  
Lahcen Daoudi ◽  
Abdelouahab Knidiri ◽  
Hicham El Boudour El Idrissi ◽  
Benaissa Rhouta ◽  
Nathalie Fagel

Fuel ◽  
2012 ◽  
Vol 97 ◽  
pp. 344-351 ◽  
Author(s):  
P. Blanchart ◽  
P. Faure ◽  
M. De Craen ◽  
C. Bruggeman ◽  
R. Michels

1989 ◽  
Vol 7 (1) ◽  
pp. 33-55 ◽  
Author(s):  
A.M. Vassallo ◽  
S.A. McCarthy ◽  
M.A. Wilson ◽  
A. J. Palmisano ◽  
A.S. Campbell
Keyword(s):  

Clay Minerals ◽  
1994 ◽  
Vol 29 (1) ◽  
pp. 63-68 ◽  
Author(s):  
T. J. Primmer

AbstractMuch emphasis has been placed recently on the role of Ostwald-type processes (both ripening and the step rule) in the formation of interstratified illite-smectite clay minerals during diagenesis. Closer investigation of the relationships between illite particle thickness (as defined in terms of the fundamental particle theory) and particle chemistry show that simple Ostwald ripening is too simplistic a mechanism to describe observed changes in illite thickness and composition. In addition, available thermodynamic data on clay minerals suggest that the conventional notion of metastability associated with Ostwald's step rule is an inaccurate description of the relationship between illitic clay minerals and their macroscopic 2 : 1 phyllosilicate analogues.


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