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Abstract

 

This article in SSSAJ

  1. Vol. 46 No. 1, p. 32-38
     
    Received: Sept 2, 1980
    Published: Jan, 1982


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doi:10.2136/sssaj1982.03615995004600010006x

Determination of the Charge Character of Selected Acid Soils1

  1. J. H. Grove,
  2. C. S. Fowler and
  3. M. E. Sumner2

Abstract

Abstract

The components of the exchangeable cation suite and its degree of domination by aluminum (Al) are prerequisites for lime requirement determinations based on percent Al saturation. The usefulness of these data is enhanced if the determinations are made under conditions which approximate those of the “field” environment.

Twenty acid soils were selected to evaluate several procedures using buffered and unbuffered electrolytes to determine soil charge characteristics. Soil pH values (1N KCl) and organic matter contents ranged from 3.4 to 5.2 and 0.4 to 6.6%, respectively. Exchangeable cations (Al, Ca, Mg, K, Na), cation exchange capacity (CEC), and anion exchange capacity (AEC) were determined by 0.2N NH4Cl saturation followed by 0.2N KNO3 saturation with correction for occluded salt. Extractable Al [1N KCl, 1N NH4OAc (pH 4.8)], exchangeable bases [1N NH4OAc (pH 7.0)], and buffered soil CEC [1N NH4OAc (pH 7.0) saturation, ethanol wash, 0.2N KNO3 saturation] were also measured. The effects of intervening ethanol and water washes on unbuffered electrolyte CEC values were determined.

Positive charge was detected in 16 samples. Buffered acetate extractions for soil Al and CEC generally gave much higher values than did unbuffered electrolyte procedures. Exchangeable bases and Al were similar whether extracted with 1N NH4OAc (pH 7.0) and 1N KCl or with 0.2N NH4Cl (bulked saturation extracts). “Net CEC,” calculated as CEC-AEC using the unbuffered electrolyte method without an intervening wash, gave generally closer agreement to the total sum of exchangeable cations than a simple CEC value.

A sum-of-cations calculation method utilizing an unbuffered electrolyte extraction for Al is recommended for soil testing facilities desiring the most unambiguous information regarding soil exchange character and the acidity associated with these exchange sites under field conditions.

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