RESEARCH NOTES FROM SOUTHERN NEVADA Quarterly e-Newsletter
June 2005 Vol. 1, Issue 2 ![]() |
|
LAS VEGAS WASH—DYNAMICS OF WATER AND SEDIMENT IN SEVERE FLOODING
The Las Vegas Wash has experienced severe channel-bed degradation and bank erosion over the past 50 years, causing the channel planform, or pattern, to evolve; wetlands to diminish; and water quality to decline. Due to the short-term surges of floodwaters associated with storm events, the channel has undergone sudden and sharp erosion. DRI’s Jennifer Duan, specialist in computational hydroscience and engineering, is using a groundbreaking, advanced computational model, which she has previously developed, to simulate the hydrodynamic processes affecting the severely damaged Las Vegas Wash. This investigation was conducted under a Cooperative Agreement between the U.S. Army Corps of Engineers and DRI. The goal of this work was to understand flood paths running through the Las Vegas Valley, and with this knowledge, design bank-protection structures that could prevent future bank erosion and improve overall stability and function in the wash.
This initial analysis of the Las Vegas Wash was needed to measure the amount of sediment that is transported during base and storm flows and to evaluate the impact of high-volume turbulent storm flow on geomorphic processes in the wash. DRI scientists have conducted field measurements of flow and sediment transport monthly in the Las Vegas Wash, a gravel-bed stream, at three cross sections since 2003. These cross sections were selected because they were relatively stable, and it was possible to wade into the water at these areas. Because of the severe bed degradation and bank erosion, other locations were either inaccessible or too unstable. With Jennifer Duan’s model, the magnitude of a 100-year flood was simulated to visualize flow-field and bank-erosion processes, as well as sediment-transport processes expected to occur around dike structures. Because, significant sediment transport usually occurs during high flow, determining the extent of bed-load transport during storm events was necessary to assess properly the effect of storm flows on geomorphic processes. Investigations have shown that the banks of the Las Vegas Wash have suffered incredible degradation of approximately 4.9–5.9 feet during the 10 years between 1989 and 1999.
For additional information, |