SSSAJ Journal of Natural Resources and Life Sciences Education
HOME HELP FEEDBACK SUBSCRIPTIONS ARCHIVE SEARCH TABLE OF CONTENTS
 QUICK SEARCH:   [advanced]


     


Published in Soil Sci Soc Am J 60:1188-1196 (1996)
© 1996 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 Courchesne, F.
Right arrow Articles by Beauchemin, P.
Right arrow Search for Related Content
PubMed
Right arrow Articles by Courchesne, F.
Right arrow Articles by Beauchemin, P.
Agricola
Right arrow Articles by Courchesne, F.
Right arrow Articles by Beauchemin, P.

Magnesium and Potassium Release by Weathering in Spodosols: Grain Surface Coating Effects

François Courchesne*

Département de Géographie, Université de Montréal, Montréal, Canada H3C 3J7

Marie-Claude Turmel and Paul Beauchemin

Les Laboratoires Savoie-Dufresne, C.P. 927, Succ. Outremont, Montréal, H2V 4R8, Canada

*Corresponding author (courchef{at}ere.umontreal.ca).

ABSTRACT

The effect of coatings on the rate of Mg and K release by weathering were determined on four soil horizons (Croche, Sutton, and LaTuque B and Croche C), collected from three Spodosols in southern Quebec, Canada. Rates of Mg, K, Fe, and Al release from the <2-mm fraction of intact and treated (coatings removed with dithionite-citrate-bicarbonate [DCB] and H2O2) samples were measured in the laboratory using a continuous flow technique. The materials were leached with a 0.0005 M H2SO4 solution adjusted to pH 3.0 at a flow rate of 0.05 mL min–1 for 1080 h. Surface coatings were composed of Al, Fe, Si, and organic C with traces of Ca. Coating removal had no effect on cation release rates ({alpha} < 0.01) from the Croche C horizon, indicating that mineral surfaces were not altered by treatments with DCB and H2O2. Intact B horizons released Fe (3.04–4.87 µmol g–1 h–1/2) and Al (10.07–36.33 µmol g–1 h–1/2) at a faster rate than treated (Fe: 0.28–1.68 µmol g–1 h–1/2; Al: 1.21–27.34 µmol g–1 h–1/2) samples although effluent pH (pHf) was more acidic in the latter. Magnesium and K release rates were higher in treated (Mg: 0.35–2.03 µmol g–1 h–1/2; K: 0.052–0.073 µmol g–1 h–1/2) than in intact (Mg: 0.19–0.61 µmol g–1 h–1/2; K: 0.032–0.039 µmol g–1 h–1/2) samples for two of the three Spodic B horizons. In the Croche B horizon, the absence of rate differences ({alpha} < 0.01) was attributed to the incomplete removal of Al coatings from treated materials. Because differences in pHf levels could not be invoked to explain all of the observed rate variability, we suggest that the accumulation of coatings was an effective process isolating primary mineral surfaces, therefore reducing the extent of reactive surfaces available for Mg and K release.

Received for publication May 23, 1995.


This article has been cited by other articles:


Home page
Clays and Clay MineralsHome page
M. A. Velbel and W. W. Barker
PYROXENE WEATHERING TO SMECTITE: CONVENTIONAL AND CRYO-FIELD EMISSION SCANNING ELECTRON MICROSCOPY, KOUA BOCCA ULTRAMAFIC COMPLEX, IVORY COAST
Clays and Clay Minerals, February 1, 2008; 56(1): 112 - 127.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
C. Mikutta, F. Lang, and M. Kaupenjohann
Kinetics of Phosphate Sorption to Polygalacturonate-coated Goethite
Soil Sci. Soc. Am. J., February 27, 2006; 70(2): 541 - 549.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
E. Thiffault, D. Pare, N. Belanger, A. Munson, and F. Marquis
Harvesting Intensity at Clear-Felling in the Boreal Forest: Impact on Soil and Foliar Nutrient Status
Soil Sci. Soc. Am. J., February 27, 2006; 70(2): 691 - 701.
[Abstract] [Full Text] [PDF]


Home page
Soil Sci.Home page
C. Mikutta, F. Lang, and M. Kaupenjohann
Soil Organic Matter Clogs Mineral Pores: Evidence from 1H-NMR and N2 Adsorption
Soil Sci. Soc. Am. J., November 1, 2004; 68(6): 1853 - 1862.
[Abstract] [Full Text] [PDF]


Home page
J. Environ. Qual.Home page
B. U. Ugwuegbu, S. O. Prasher, D. Ahmad, and P. Dutilleul
Bioremediation of Residual Fertilizer Nitrate: II. Soil Redox Potential and Soluble Iron as Indicators of Soil Health During Treatment
J. Environ. Qual., January 1, 2001; 30(1): 11 - 18.
[Abstract] [Full Text]




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 © 1996 by the Soil Science Society of America.