SSSAJ Grow Your Career with SSSA
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 62:348-353 (1998)
© 1998 Soil Science Society of America
677 S. Segoe Rd., Madison, WI 53711 USA
This Article
Right arrow Full Text (PDF)
Right arrow Alert me when this article is cited
Right arrow Alert me if a correction is posted
Services
Right arrow Similar articles in this journal
Right arrow Alert me to new issues of the journal
Right arrow Download to citation manager
Right arrow reprints & permissions
Citing Articles
Right arrow Citing Articles via HighWire
Right arrow Citing Articles via Google Scholar
Google Scholar
Right arrow Articles by Schulthess, C. P.
Right arrow Articles by Belek, J. Z.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Schulthess, C. P.
Right arrow Articles by Belek, J. Z.
GeoRef
Right arrow GeoRef Citation
Agricola
Right arrow Articles by Schulthess, C. P.
Right arrow Articles by Belek, J. Z.

Proton Adsorption on a Titanium Oxide in the Presence of Bicarbonate

C. P. Schulthess* and J. Z. Belek

Department of Plant Science, U-67, Univ. of Connecticut, Storrs, CT 06269

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

ABSTRACT

The very high concentration of aqueous CO2 species below ground highlights a need to fully characterize the physicochemical behavior of this compound in the soil environment. This study focused on the adsorption of bicarbonates by a Ti oxide, and on its effects on the adsorption of protons, which was measured by the backtitration technique. The inorganic C adsorbed on the Ti oxide from pH 1.5 to 10 with a broad maximum at pH 4 to 6. For every molecule of inorganic C adsorbed (expressed as HCO3 adsorbed), an average of 2.3 protons were removed from the liquid phase (either by coadsorption or neutralization of the proton). The point of zero salt effect (PZSE) also increased from pH 5.7 to 6.2. The high stoichiometry of 2.3 suggests that the bicarbonate will also affect the desorption of cationic impurities; higher levels of Na, Ca, and Mg were measured in the liquid phase in the presence of inorganic C at pH 4. This study indirectly highlights that modeling the adsorption of protons by an oxide (even a "simple" one like Ti oxide) can be easily complicated by the presence of low levels of inorganic C or the presence of adsorbed cationic impurities.


NOTES

Storrs Agric. Exp. Stn. Scientific Contribution no. 1722.

Received for publication October 14, 1996.


This article has been cited by other articles:


Home page
Soil Sci.Home page
C.P. Schulthess and Z. Hu
Impact of Chloride Anions on Proton and Selenium Adsorption by an Aluminum Oxide
Soil Sci. Soc. Am. J., May 1, 2001; 65(3): 710 - 718.
[Abstract] [Full Text] [PDF]




HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
The SCI Journals Agronomy Journal Crop Science
Journal of Natural Resources
and Life Sciences Education
Vadose Zone Journal
Journal of Plant Registrations Journal of
Environmental Quality
The Plant Genome
Copyright © 1998 by the Soil Science Society of America.