Impacts of forest management on northern forest soils

Authors
Citation
Tm. Ballard, Impacts of forest management on northern forest soils, FOREST ECOL, 133(1-2), 2000, pp. 37-42
Citations number
43
Categorie Soggetti
Plant Sciences
Journal title
FOREST ECOLOGY AND MANAGEMENT
ISSN journal
03781127 → ACNP
Volume
133
Issue
1-2
Year of publication
2000
Pages
37 - 42
Database
ISI
SICI code
0378-1127(20000801)133:1-2<37:IOFMON>2.0.ZU;2-5
Abstract
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.