My Account: Log In | Join | Renew
Search
Author
Title
Vol.
Issue
Year
1st Page

Abstract

 

This article in SSSAJ

  1. Vol. 60 No. 4, p. 1188-1196
     
    Received: May 23, 1995
    Published: July, 1996


    * Corresponding author(s): courchef@ere.umontreal.ca
 View
 Download
 Alerts
 Permissions
 Share

doi:10.2136/sssaj1996.03615995006000040033x

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

  1. François Courchesne ,
  2. Marie-Claude Turmel and
  3. Paul Beauchemin
  1. Département de Géographie, Université de Montréal, Montréal, Canada H3C 3J7
    Les Laboratoires Savoie-Dufresne, C.P. 927, Succ. Outremont, Montréal, H2V 4R8, Canada

Abstract

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 (α < 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 (α < 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.

  Please view the pdf by using the Full Text (PDF) link under 'View' to the left.

Copyright © . Soil Science Society of America