Pipeline construction on the Canadian boreal plain occurs on woodland and/o
r agricultural fields, but soil recovery from its impact is not well docume
nted. Therefore, we quantified changes over 3 yr (1992 to 1994) in the chem
ical properties of two Grey soils and the physical properties of a Grey soi
l that were subjected to pipeline burial and cropped to barley. The pipelin
e right-of-way (RoW) was divided into three zones: a road (or work) area us
ed for vehicular traffic, a trench area for burying pipeline, and a pile (o
r spoil) area where soil was stockpiled during excavation. Pipeline constru
ction resulted in mixing of subsoil material with topsoil, and the chemical
properties most affected were those that varied most with depth. The pH, e
lectrical conductivity, soluble sulphate, and exchangeable Ca and Na were i
ncreased in the surface 20 cm of soil, particularly the road and trench are
as. The affected properties moderated 2 or 3 yr after pipeline construction
as soluble components were dissolved or dispersed and translocated back to
lower soil depths. The RoW zones had increased soil strength and compactio
n, and reduced water retention and infiltration rates. However, the deterio
ration in soil physical condition was similar across the RoW zones, indicat
ing that it was due mainly to land clearing, a requirement to convert woodl
and to agricultural land. Improvement in bulk density, and water infiltrati
on and retention in 1993 and 1994 indicated that the RoW was undergoing reh
abilitation with time as a result of natural processes and annual cropping.