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Seasonal Soil Moisture Patterns in Adjacent Greasewood and Sagebrush Stands
W. H. Rickard
Vol. 48, No. 6 (Nov., 1967), pp. 1034-1038
Stable URL: http://www.jstor.org/stable/1934561
Page Count: 5
You can always find the topics here!Topics: Soil water, Sodic soils, Soil water content, Soil salinity, Buried soils, Soil depth, Shrubs, Transpiration, Grasses, Soil profiles
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Soil moisture measurements were made over a 2-year period in adjacent greasewood (Sarcobatus vermiculatus) and sagebrush (Artemisia tridentata) stands in the desert steppe region of southeastern Washington. Soil moisture accumulated during fall and winter. The greater accumulation of moisture in the upper 4 dm of the greasewood stand appeared to be the result of decreased evaporation losses and the lack of transpiration from shrub species which are leafless during winter and early spring. The more luxuriant growth of cheatgrass in the greasewood stand was related to winter and spring retention of soil moisture.
Ecology © 1967 Wiley