We present turbulent Schmidt number (Sct) estimations above three-dimensional urban canopies, where Sct is a property of the flow defined as the ratio of the eddy diffusivity of momentum (KM) to the eddy diffusivity of mass (Dt). Despite the fact that Sct modelling is of great interest, inter alia, for pollutant dispersion simulations conducted via computational fluid dynamics, no universal value is known. Simultaneous measurements of fluid velocity and mass concentration are carried out in a water channel for three staggered arrays of cubical obstacles corresponding to isolated flow, wake-interference, and skimming-flow regimes. A passive tracer is released from a continuous point source located at a height z= 1.67 H where H is the obstacle height. The results show an increase of Sct with height above the canopy for all three arrays, with values at z= 2 H (Sct≈ 0.6) about double compared to that at z= H. The observed Sct agrees well with that modelled by using a simple formulation for Sct based on expressions for KM and Dt published in previous studies. Comparisons with other Sct models found in the literature are also presented and discussed.
Turbulent Schmidt Number Measurements Over Three-Dimensional Cubic Arrays / Di Bernardino, Annalisa; Monti, Paolo; Leuzzi, Giovanni; Querzoli, Giorgio. - In: BOUNDARY-LAYER METEOROLOGY. - ISSN 0006-8314. - 174:2(2020), pp. 231-250. [10.1007/s10546-019-00482-z]
Turbulent Schmidt Number Measurements Over Three-Dimensional Cubic Arrays
Di Bernardino, Annalisa;Monti, Paolo
;Leuzzi, Giovanni;Querzoli,Giorgio
2020
Abstract
We present turbulent Schmidt number (Sct) estimations above three-dimensional urban canopies, where Sct is a property of the flow defined as the ratio of the eddy diffusivity of momentum (KM) to the eddy diffusivity of mass (Dt). Despite the fact that Sct modelling is of great interest, inter alia, for pollutant dispersion simulations conducted via computational fluid dynamics, no universal value is known. Simultaneous measurements of fluid velocity and mass concentration are carried out in a water channel for three staggered arrays of cubical obstacles corresponding to isolated flow, wake-interference, and skimming-flow regimes. A passive tracer is released from a continuous point source located at a height z= 1.67 H where H is the obstacle height. The results show an increase of Sct with height above the canopy for all three arrays, with values at z= 2 H (Sct≈ 0.6) about double compared to that at z= H. The observed Sct agrees well with that modelled by using a simple formulation for Sct based on expressions for KM and Dt published in previous studies. Comparisons with other Sct models found in the literature are also presented and discussed.File | Dimensione | Formato | |
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