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Published in Soil Sci Soc Am J 46:32-38 (1982)
© 1982 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Determination of the Charge Character of Selected Acid Soils1

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

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.

Key Words: cation exchange capacity • anion exchange capacity • pH-dependent charge • exchangeable Al


NOTES

1 Contribution from the Agron. Dep., College Stn., Univ. of Georgia, Athens, GA 30602. Presented in part before Div. S-2, Soil Sci. Soc. of Am., Chicago, Ill., 6 Dec. 1978.

2 Former Graduate Research Assistant, Graduate Research Assistant, and Professor, Agron. Dep., Univ. of Georgia, Athens, GA 30602, respectively. Senior Author is presently Assistant Professor, Agron. Dep., Univ. of Kentucky, Lexington, KY 40546.

Received for publication September 2, 1980. Accepted for publication August 5, 1981.




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