Competitive Sorption between Imidacloprid and Imidacloprid-urea on Soil Clay Minerals and Humic Acids

2002 ◽  
Vol 50 (23) ◽  
pp. 6823-6827 ◽  
Author(s):  
Liu ◽  
Wei Zheng ◽  
Jianying Gan
Keyword(s):  
Clay Minerals ◽  
Humic Acids ◽  
Competitive Sorption ◽  
Soil Clay

Crystal structure model development for soil clay minerals – I. Hydroxy-interlayered smectite (HIS) synthesized from bentonite. A multi-analytical study

Geoderma ◽  
2019 ◽  
Vol 347 ◽  
pp. 135-149 ◽  
Author(s):  
Jan Dietel ◽  
Jens Gröger-Trampe ◽  
Marko Bertmer ◽  
Stephan Kaufhold ◽  
Kristian Ufer ◽  
...  
Keyword(s):  
Crystal Structure ◽  
Clay Minerals ◽  
Analytical Study ◽  
Model Development ◽  
Structure Model ◽  
Soil Clay

scholarly journals Microbial reduction of Fe(III)-bearing clay minerals in the presence of humic acids

2017 ◽  
Vol 7 (1) ◽  
Author(s):  
Guangfei Liu ◽  
Shuang Qiu ◽  
Baiqing Liu ◽  
Yiying Pu ◽  
Zhanming Gao ◽  
...  
Keyword(s):  
Clay Minerals ◽  
Humic Acids ◽  
Microbial Reduction

Effect of Cyclodextrins on Surface and Pore Properties of Soil Clay Minerals

2001 ◽  
Vol 35 (24) ◽  
pp. 4947-4952 ◽  
Author(s):  
Grzegorz Jozefaciuk ◽  
Attila Muranyi ◽  
Eva Fenyvesi
Keyword(s):  
Clay Minerals ◽  
Soil Clay ◽  
Pore Properties ◽  
Properties Of Soil

Trioctahedral minerals in the soil-clays of north-east Scotland

1950 ◽  
Vol 29 (208) ◽  
pp. 72-84 ◽  
Author(s):  
G. F. Walker
Keyword(s):  
Clay Minerals ◽  
Decomposition Products ◽  
Widespread Distribution ◽  
North East ◽  
The North ◽  
Soil Clays ◽  
The Subject ◽  
Soil Clay

This paper deals with a series of soil-clay minerals which have a widespread distribution in the north-east of Scotland. The original member is a biotite-like mica which breaks down readily in the soil into (i) a vermiculite or (ii) a montmorillonite, depending on the soil-forming conditions operating. Apart from this 'clay biotite' and its decomposition products, the main crystalline constituents of the Scottish soil-clays are a member of the kaolinite group and illite (' clay muscovite'). Iron and aluminium oxides are present in all the clays in the amorphous condition, but crystalline varieties are scarce. The distribution of the minerals and their relationship to the various soft-forming factors will form the subject of a separate communication; here, the nature of the clay minerals and their interrelationships are considered.

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