EFFET DU DRAINAGE SOUTERRAIN SUR QUELQUES PROPRIETES DE SOLS ARGILEUX DU QUEBEC
Four series of agricultural soils of Quebec were sampled in the Lowlands on drained and undrained sites in order to investigate the effect of long-term internal drainage on the physical and chemical properties of the profiles. Change in structure was observed in the Ste-Rosalie soils. A massive layer found below 18 cm in the undrained profile was replaced by a more structured layer at greater depth in the drained profiles. Occurrence of mottles down to the Cg horizon reflected the better aeration conditions in the drained sites. Saturated hydraulic conductivity values were sometimes higher and sometimes lower than those measured in the undrained profiles. Below the plow layer, the two profiles drained for more than 50 yr had a cation exchange capacity 12–15% higher than the undrained profiles. Oxalate-extractable iron represented a high percentage of the dithionite-extractable iron and indicated a low rate of formation of crystalline pedogenic oxides. Mn accumulations were found in the more compact layers. The improvement of internal drainage requires a soil management that will enhance soil structure.