Canadian Forest Service Publications

Increased soil nitrate losses under mature sugar maple trees affected by experimentally induced deep frost. 1995. Boutin, R.; Robitaille, G. Canadian Journal of Forest Research 25: 588-602.

Year: 1995

Issued by: Laurentian Forestry Centre

Catalog ID: 16929

Language: English

Availability: PDF (request by e-mail)

Mark record

Abstract

This work reports and discusses data gathered during soil solution monitoring that was part of an experiment conducted in the Duchesnay Experimental Forest (Quebec, Canada) to study the effects of induced deep frost, superficial frost, and superficial frost plus drought on mature sugar maple trees (Acer saccharum Marsh.). Frost treatment was applied by preventing snow from accumulating under the canopy. Soil solution chemistry was modified when mature sugar maple trees declined after exposure to a severe deep frost. The first vegetation period after treatment showed that losses of NO3ˉ below the rooting zone were greatly increased under affected trees. The leaching rate of NO3ˉand basic cations was directly related to the level of change in canopy dieback and transparency. A mean NO3ˉ concentration of 630 µmolc•L-1 (53 times the controls; max. 4500 µmolc•L-1) was measured in soil solution under the deep frost treated trees. The leaching rate of K+ (18X, relative to the control) and Mn2+ (1lX) was higher than that of Mg2+ (5X) and Ca2+ (2.6X). Acidification of the soil solution (50% more H+) as a result of intense nitrification caused an increase in aluminum concentration (5X) and a decrease in SO42-. The acidification during the year after treatment was equivalent to decades of atmospheric acid deposition. The seasonal mean of SO42- did not differ between treatments, but there was evidence of a significant correlation between pH and SO42- in soil solution. Concentration of NH4+ was also enhanced but to a lesser degree (10X) than that of NO3-. Specific conductivity was a good predictor of NO3-, Ca2+., Mg2+, and total A1 in soil solution. The ion balance shifted from an anion deficit to a strong cation deficit when NO3- concentrations were high. Superficial frost with or without induced summer drought did not cause any significant change in soil solution chemistry compared with the controls. These results indicated the necessity to consider perturbations induced by extreme climate conditions, like deep soil frost, for the interpretation of soil solution chemistry data in the context of acid deposition studies and forest health.