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Published in Soil Sci Soc Am J 62:136-141 (1998)
© 1998 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
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Proton Adsorption on an Aluminum Oxide in the Presence of Bicarbonate

C. P. Schulthess* and H. Wijnja

Dep. of Plant Sci., U-67, Univ. of Connecticut, Storrs, CT 06269

K. Swanson

99 Mill St., Glastonbury, CT 06033

*Corresponding author (cschulth{at}canrl.cag.uconn.edu).

ABSTRACT

The aqueous species of CO2 [CO2(aq), H2CO3, HCO3 and CO2–3] are often ignored in adsorption studies despite the fact that CO2 in soil air can be hundreds of times greater than in the atmosphere. Adsorption studies that do not account for CO2 species may be under-estimating proton adsorption in natural environments. The objective of this study was to discern the effect CO2 species have on proton adsorption to an Al oxide. The backtitration method was used to produce proton adsorption curves as a function of pH for samples of Al oxide with and without aqueous bicarbonate. Sodium chloride was used to vary the ionic strength. Proton adsorption increased in the presence of the bicarbonate below pH 9.7. The greater the concentration of bicarbonate, the greater the proton adsorption. The point of zero salt effect (PZSE = 8.30) was unaffected by the bicarbonate. The data presented show an approximate 1:1 stoichiometry for proton removal with inorganic-C (HCO3 plus all other species) adsorption data. That is, this research directly quantified that every inorganic C adsorbed (expressed as HCO3 adsorbed) is accompanied by the removal of one proton (more precisely, 1.10 ± 0.28) from the aqueous phase by the Al oxide. Thus, the net removed from the liquid phase is equivalent to one H2CO3 in mass-balanced terms. The use of traditional titration methods, rather than the backtitration method, resulted in a questionable pH-dependent pattern that reflects the impact of Al dissolution on these measurements.


NOTES

Storrs Agric. Exp. Stn. Scientific Contribution no. 1619.

Received for publication July 24, 1996.


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