Positive permanent charge in oxisols

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Positive permanent charge in oxisols

The existences of a positive permanent charge can be inferred from charge characteristics of highly weathered tropical soils; it was found to be related to isomorphous substitution of Ti(IV) for Fe(III) in iron oxides. Comparable near‐constant values were found from anion adsorption at pH 7.0 to 9.0...

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Bibliographic Details
Main Authors:	Tessens, E., Zauyah, Siti
Format:	Article
Published:	Wiley 1982
Online Access:	http://psasir.upm.edu.my/id/eprint/112434/

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