June 20-21, 2005
Lynn Neakrase of Arizona State University's
Planetary Geology Group is shown above (left) conducting tests of dust devil
threshold wind speeds using the Tornado/Microburst Simulator in the WiST lab.
The photo on the right shows Neakrase and ISU Aerospace Engineering
senior Kevin Houstman readying a bed of fine sand for the test.
The ASU group also conducts such experimental
investigations of Martian dust devils using the Arizona State
University Vortex Generator in Earth-ambient and Martian-analog
pressures, using the Arizona State University Planetary Aeolian
facility and the Mars Surface Wind Tunnel facility at NASA Ames
Research Center in California. The large size of the ISU tornado simulator allowed researchers to test scales and Reynolds numbers not
previously possible.
Dust transport is believed to play an important
role in weather patterns on Mars. Since dust devils are one of
the primary means of delivering dust from the surface into the
atmosphere, gaining an understanding of these phenomena is an
important step in understanding the physics of the Martian
atmosphere.