Many effects of forest management on northern soil environments are charact
eristic of other latitudes, as well. Nutrient removals in harvested timber
are substantial, and on some sites this may influence not only the amount b
ut also the balance of remaining plant-available nutrients in the long term
. Canopy removal during harvesting influences soil temperature and moisture
regimes. Physical effects of ground-based skidding may include soil struct
ural change, influencing water retention and flow, and reducing aeration an
d root penetration. Higher soil temperatures in the daytime and during the
growing season tend to result from the forest floor displacement and other
disturbances which may result from harvesting and site preparation activiti
es. Impairment of soil gas exchange, due to management activities, can resu
lt in increased leaching of nutrient cations where soil pH is not very low,
as a consequence of carbonic acid formation. Impaired gas exchange also re
sults in anoxic microenvironments and may result in denitrification and the
reduction of manganese, iron and sulfate. Prescribed fire results in subst
antial nutrient losses through volatilization (notably of N and S) and, in
some cases, fly-ash losses. Slashburning yields base oxides in the ash. Hyd
rolysis of these oxides results in increased soil pH and both, the magnitud
e and the duration of the pH change are influenced by soil-buffering capaci
ty. Many of the remaining ash nutrients are soluble, plant-available, and h
ighly susceptible to leaching. However, increased pH and sorption after bur
ning may limit availability of micronutrient metals and phosphorus in the s
oil. Hydrologic behavior can be influenced by fire effects on soil hydropho
bicity. Urea fertilizer use can increase soil pH in the short run and lead
to increased leaching of metals and biocides associated with dispersible or
ganic colloids. In the longer run, the soil acidification resulting from ni
trification of fertilizer N can result in leaching of some heavy metal cati
ons. (C) 2000 Elsevier Science B.V. All rights reserved.