HR: 1340h
AN: H53A-1215    [Abstracts]
TI: Long-term Effects of Clearcutting on N Availability and Soil Solution Chemistry in the Fraser Experimental Forest, CO
AU: * Starr, B
EM: bstarr@fs.fed.us
AF: USDA Forest Service Rocky Mountain Research Station, 240 West Prospect, Fort Collins, CO 80526 United States
AU: Stottlemyer, R
EM: robert_stottlemyer@usgs.gov
AF: U.S. Department of the Interior U.S. Geological Survey, 2150 Centre Avenue, Bldg C , Fort Collins, CO 80526 United States
AU: Elder, K
EM: kelder@fs.fed.us
AF: USDA Forest Service Rocky Mountain Research Station, 240 West Prospect, Fort Collins, CO 80526 United States
AU: Rhoades, C
EM: crhoades@fs.fed.us
AF: USDA Forest Service Rocky Mountain Research Station, 240 West Prospect, Fort Collins, CO 80526 United States
AB: The effects of timber harvest on soil water ion chemistry and flux have been studied for more than two decades at the Fraser Experimental Forest in central Colorado. We examined the long-term effects of a clearcutting experiment, 18 years after harvesting of a high-elevation mixed conifer forest (2900 m). Early effects of harvesting included elevated concentrations and flux of NO3-N in soil water, and these increases continued through 18 years. In 2003, total N loss from the harvested plot (2.0 kg ha-1 yr-1) was four times greater than the control (0.5 kg ha-1 yr-1). The most pronounced differences in subsurface chemistry and flux were found for nitrate (NO3-N). The proportion of total N in subsurface discharge as NO3-N increased from < 1% in the control to greater than 50% in the clearcut. The annual loss of NO3-N equaled 1.2 kg ha-1 in the clearcut, about one-sixth the loss rate for the first 8 years after harvest. Total post harvest leaching losses of inorganic N were about 67 kg/ha. Nitrate losses from the control forest were negligible (< 0.001 kg ha-1 yr-1) for all periods. On an annual basis net N mineralization showed no effect of harvest after 18 years, but resin bags collected more N in the clearcut site than in the control. High current losses of nitrogen from the clearcut may result from the biological factors of lower plant uptake and increased microbial nitrification, and the physical factors of greater snow accumulation and snowmelt discharge.
DE: 1800 HYDROLOGY
DE: 1831 Groundwater quality
DE: 1860 Runoff and streamflow
DE: 0400 Biogeosciences
SC: Hydrology [H]
MN: 2004 AGU Fall Meeting