2021
DOI: 10.1007/s10035-021-01097-3
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Numerical analysis of the influence of the near ground turbulence on the wind-sand flow under the natural wind

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Cited by 6 publications
(2 citation statements)
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“…This in turn reduces the speeds of the horizontal dust flux particles, such that a steady state is reached when the speeds of the impacting particles are reduced to a value at which there is a single particle leaving the soil surface for each particle impacting it [ 52 ]. Because of the finite response time of dust flux particle speeds to the wind speed, the horizontal dust flux can “overshoot” the eventual steady-state mass flux [ 53 , 54 , 55 ].…”
Section: Discussionmentioning
confidence: 99%
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“…This in turn reduces the speeds of the horizontal dust flux particles, such that a steady state is reached when the speeds of the impacting particles are reduced to a value at which there is a single particle leaving the soil surface for each particle impacting it [ 52 ]. Because of the finite response time of dust flux particle speeds to the wind speed, the horizontal dust flux can “overshoot” the eventual steady-state mass flux [ 53 , 54 , 55 ].…”
Section: Discussionmentioning
confidence: 99%
“…Moreover, recent measurements indicated that the restitution coefficient is a declining function of the saltator impact speed [68]. Numerical simulations [50,53,69,70], laboratory experiments [71], and theory [57] have all indicated that the number of splashed particles scales with the impacting momentum. Experiments have also indicated that the fraction of the average impacting momentum spent on splashing surface particles is of the order of 15% for a bed of loose sand particles [56,57,59].…”
Section: Discussionmentioning
confidence: 99%