1990
DOI: 10.1002/ldr.3400020202
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Field measurement of the sheltering effect of vegetation on erodible land surfaces

Abstract: Natural vegetation on erodible land surfaces, such as the loose sandy soils found in the southwestern United States and in Soviet Central Asia, absorbs part of the wind momentum flux (stress) and thus protects the erodible soil to a degree that depends on the geometry of plant distribution and profile. The sheltering effect of natural plants may be expressed as the ratio, R, of threshold friction velocity for the bare soil (determined in the laboratory or in specially prepared areas of bare soil in the field) … Show more

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Cited by 173 publications
(119 citation statements)
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“…This approach is inherently applicable to understanding the aerodynamics of a sparse vegetative canopy. Shear stress partitioning has been used to evaluate the role of vegetation in decreasing wind erosion in agricultural fields [Marshall, 1971] and rangelands [Stockton and Gillette, 1990;Wolfe and Nickling, 1996]. It has also been applied to examine the The purpose of this paper is to present drag coefficients derived from direct measurements of wind force on greasewood (Sarcobatus vermiculatus), a desert shrub that is widely distributed in the Great Basin region of the United States.…”
Section: Introductionmentioning
confidence: 99%
“…This approach is inherently applicable to understanding the aerodynamics of a sparse vegetative canopy. Shear stress partitioning has been used to evaluate the role of vegetation in decreasing wind erosion in agricultural fields [Marshall, 1971] and rangelands [Stockton and Gillette, 1990;Wolfe and Nickling, 1996]. It has also been applied to examine the The purpose of this paper is to present drag coefficients derived from direct measurements of wind force on greasewood (Sarcobatus vermiculatus), a desert shrub that is widely distributed in the Great Basin region of the United States.…”
Section: Introductionmentioning
confidence: 99%
“…The blown sand impact count as an index of the aeolian flux was measured at a height of 0.04 m above the ground (z = 0.04 m) using a ceramic sand flux sensor UD-101. The sensor counts piezoelectric signals generated by collisions between blown sand grains and the sensor surface, using the same principle of acoustic impact detection as the Sensit (Stockton and Gillette 1990) and Safires (Baas 2004). Significant difference between the UD-101 and the others is that the UD-101 is unidirectional while both the Sensit and Safires are omnidirectional.…”
Section: Methodsmentioning
confidence: 99%
“…Since the 1990s, high-frequency sampling instrumentation such as erodible mass sensors and high temporal resolution sediment traps have been employed to detect aeolian sand at frequencies of 1 Hz or greater, which has improved our understanding of the saltation systems in unsteady winds (Stockton and Gillette 1990;Jackson 1996;Stout and Zobeck 1997;Butterfield 1998;Davidson-Arnott et al 2008).…”
Section: Introductionmentioning
confidence: 99%
“…With the advance of sand fixation, large areas of sandy grassland mainly with psammophyte shrubs have been established in Mu Us sandy land based on their roles in reducing wind speed and soil erosion and improving ecological environments [6]. Since psammophyte shrubs have high biomass production [7] and also have been widely used as feedstuffs [8], they can play an important role in the nutrition of grazing animals during a withered season and a droughty year.…”
Section: Introductionmentioning
confidence: 99%