Measurement of ion transport in soils by a radioabsorption method

The transport of ions was investigated in industrial bentonites, montmorillonites, in soils of different nature and in soils of original structure using radioactive isotopes by a radioabsorption method. The effective diffusion coefficient and activation energy characteristic of the transport process...

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Published inColloids and surfaces Vol. 54; no. 1-2; pp. 61 - 74
Main Author VARRO, T
Format Journal Article
LanguageEnglish
Published Amsterdam Elsevier B.V 1991
Elsevier
Subjects
Chemistry
Exact sciences and technology
General and physical chemistry
Ion-exchange
Surface physical chemistry
Clay
Montmorillonite
Ion transport
Experimental study
Alkaline earth metal Ions
Transition metal Ions
Bentonite
Alkali metal Ions
Ion exchanger
Diffusion coefficient
Ion exchange
Thermodynamic properties
Activation energy
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Abstract The transport of ions was investigated in industrial bentonites, montmorillonites, in soils of different nature and in soils of original structure using radioactive isotopes by a radioabsorption method. The effective diffusion coefficient and activation energy characteristic of the transport process were determined. The radioabsorption method sensitively follows the micromigration of radioactive ions in soils; it is rapid, applicable to the determination of diffusion coefficients in a wide range (10 −18-10 −9 m 2 s −1), gives results with good reproducibility (Sd 30%) and makes possible the comprehensive investigation of factors influencing transport processes in soils.
AbstractList The transport of ions was investigated in industrial bentonites, montmorillonites, in soils of different nature and in soils of original structure using radioactive isotopes by a radioabsorption method. The effective diffusion coefficient and activation energy characteristic of the transport process were determined. The radioabsorption method sensitively follows the micromigration of radioactive ions in soils; it is rapid, applicable to the determination of diffusion coefficients in a wide range (10 −18-10 −9 m 2 s −1), gives results with good reproducibility (Sd 30%) and makes possible the comprehensive investigation of factors influencing transport processes in soils.
Author Varró, Tibor
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10.2136/sssaj1978.03615995004200010009x
10.1039/jr9460000537
10.2136/sssaj1960.03615995002400060014x
10.1097/00010694-196502000-00007
10.1007/BF01340139
10.1016/S0065-2113(08)60141-8
10.3891/acta.chem.scand.04-0307
10.1021/j150500a014
10.2136/sssaj1961.03615995002500050014x
10.2136/sssaj1978.03615995004200020008x
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Issue 1-2
Keywords Clay
Montmorillonite
Ion transport
Experimental study
Alkaline earth metal Ions
Transition metal Ions
Bentonite
Alkali metal Ions
Ion exchanger
Diffusion coefficient
Ion exchange
Thermodynamic properties
Activation energy
Language English
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PublicationTitle Colloids and surfaces
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Elsevier
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Snippet The transport of ions was investigated in industrial bentonites, montmorillonites, in soils of different nature and in soils of original structure using...
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SubjectTerms Chemistry
Exact sciences and technology
General and physical chemistry
Ion-exchange
Surface physical chemistry
Title Measurement of ion transport in soils by a radioabsorption method
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