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Evapotranspiration (ET) from saltcedar (Tamarix chinensis Lour) varies with weather factors as well as with stand density and water availability. In California, ET in July for a unit ground area of saltcedar in large drums varied from 2 millimeters per day in sparse stands, to 16 millimeters per day in dense stands; ET declined and diffusive resistance increased when saltcedar plants were subjected to stress brought on by low soil water availability and/or high evaporative demand. In a natural salt-cedar stand in New Mexico, ET in June varied from 3 millimeters to 11 millimeters per day, depending upon weather and plant density. Extrapolation of experimental transpiration data to field sites must, therefore, be done carefully when assessing irrecoverable ET losses.
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Davenport et al. (1982) studied this question.
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