Dust emission from wet and dry playas in the Mojave Desert, USA

Earth Surface Processes and Landforms
By: , and 



The interactions between playa hydrology and playa-surface sediments are important factors that control the type and amount of dust emitted from playas as a result of wind erosion. The production of evaporite minerals during evaporative loss of near-surface ground water results in both the creation and maintenance of several centimeters or more of loose sediment on and near the surfaces of wet playas. Observations that characterize the texture, mineralogic composition and hardness of playa surfaces at Franklin Lake, Soda Lake and West Cronese Lake playas in the Mojave Desert (California), along with imaging of dust emission using automated digital photography, indicate that these kinds of surface sediment are highly susceptible to dust emission. The surfaces of wet playas are dynamic - surface texture and sediment availability to wind erosion change rapidly, primarily in response to fluctuations in water-table depth, rainfall and rates of evaporation. In contrast, dry playas are characterized by ground water at depth. Consequently, dry playas commonly have hard surfaces that produce little or no dust if undisturbed except for transient silt and clay deposited on surfaces by wind and water. Although not the dominant type of global dust, salt-rich dusts from wet playas may be important with respect to radiative properties of dust plumes, atmospheric chemistry, windborne nutrients and human health.

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Publication type Article
Publication Subtype Journal Article
Title Dust emission from wet and dry playas in the Mojave Desert, USA
Series title Earth Surface Processes and Landforms
DOI 10.1002/esp.1515
Volume 32
Issue 12
Year Published 2007
Language English
Publisher Wiley
Contributing office(s) Toxic Substances Hydrology Program
Description 17 p.
First page 1811
Last page 1827
Country United States
State California
Other Geospatial Mojave Desert
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