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Fire effects on infiltration rates after prescribed fire in northern Rocky Mountain forests, USA
Robichaud, P. R. 2000.
Fire effects on infiltration rates after prescribed fire in northern Rocky Mountain forests, USA.
Journal of Hydrology. 231-232(2000): 220-229.
Keywords: Water repellent, rainfall simulation, forest fire, hydraulic conductivity, water repellency, infiltration
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Abstract:
Infiltration rates in undisturbed forest environments are generally high. These high
infiltration rates may be reduced when forest management activities such as timber harvesting
and/or prescribed fires are used. Post-harvest residue burning is a common site preparation
treatment used in the Northern Rocky Mountains, USA, to reduce forest fuels and to prepare
sites for natural and artificial tree regeneration. Prescribed burn operations attempt to leave sites
with the surface condition of a low-severity burn. However, some of the areas often experience
surface conditions associated with a high-severity burn which may result in hydrophobic or
water repellent conditions. In this study, infiltration rates were measured after logging slash was
broadcast burned from two prescribed burns. The two sites were in Northern Rocky mountain coniferous
forests of Douglas-fir/lodgepole pine and ponderosa pine/Douglas-fir. Simulated rainfall was
applied to one-square meter plots in three, 30-minute applications at 94 mm h-1 within the three
surface conditions found after the burn: unburned-undisturbed areas, low-severity burn areas and
high-severity burn areas.
Runoff hydrographs from the rainfall simulations were relatively constant from the plots
that were in unburned-undisturbed areas and in areas subjected to a low-severity burn. These
constant runoff rates indicate constant hydraulic conductivity values for these surface conditions
even though there was variation between plots. Hydrographs from the rainfall simulation plots
located within areas of high-severity burn indicate greater runoff rates than the plots in low-severity
burn areas especially during the initial stages of the first rainfall event. These runoff
rates decreased to a constant rate for the last 10 minutes of the event. These results indicate
hydrophobic or water repellent soil conditions, which temporarily cause a 10 to 40 percent
reduction in hydraulic conductivity values when compared to a normal infiltrating soil condition.
Because variability was high for these forest conditions, cumulative distribution algorithms of
hydraulic conductivity provide a means to account for the inherent variability associated with
these hillslopes and different surface conditions caused by fire.
Moscow FSL publication no. 2000g
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