244 Geomorphology (Posters)
Wednesday, 21 October 2009
9:00 AM - 6:00 PM
Hall A
MEASURING POTENTIAL FLUVIAL AND AEOLIAN EROSION FROM A RANGELAND FIRE IN THE MOJAVE-GREAT BASIN TRANSITION ZONE
Paper number: 244-16
Program: Technical Sessions
Time: 9:00 AM – 6:00 PM
Authors
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Julianne J. MillerDesert Research Institute, Las Vegas, NV
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Dave DuBoisDesert Research Institute, Las Vegas, NV
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Vic EtyemezianDesert Research Institute, Las Vegas, NV
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Ilias KavourasDesert Research Institute, Las Vegas, NV
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George NikolichDesert Research Institute, Las Vegas, NV
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Stephen F. ZitzerDesert Research Institute, Las Vegas, NV
Abstract
Runoff potential increased for at least 3 months post-burn on burned shrub mounds in both channel and ridge top plots, but at 6 months, potential runoff began to decrease. Shrub interspaces within the burn showed runoff potential measurements comparable to unburned control plots. Analysis of runoff demonstrated that within 3 (?) months post-burn, a shift had occurred within the distribution of particles in the runoff from fine sands, silt, and clay to coarser particles. Measurement of aeolian transport potential 2 weeks post-burn clearly indicated that windblown particle suspension was higher in burned locations than in control plots. Within the burn site, emissions were highest from burned shrub mounds and much lower on shrub interspaces. Over a period of one year, the burn site soil has become somewhat more stable with respect to wind erosion. A important consideration in continued wind erodibility is the role of vegetation establishment which increases surface roughness.
The Jacobs site was dominated by blackbrush (Coleogyne ramosissima), an important species in shrub communities on slopes below pinyon pine-juniper forests in the