Abstract
The power law and logarithmic law among others are the most commonly well-known theories for equilibrium mean profile of dust concentration in a neutral atmospheric surface layer. However, these theories are based on the assumption of homogeneity in horizontal (streamwise) direction, thereby the horizontal advection term in the transport equation is neglected. In this study, with the help of a self-similar analytical solution of the two-dimensional steady-state dust transport equation (Chamecki and Meneveau, J Fluid Mech 683:1–26, 2011), we examine the applicabilities of the assumption which the one-dimensional theories are based on. In addition, we also propose an empirical fit of the theory, and good agreements with reference data have been obtained. The new approximate profile can be used as an alternative of the one-dimensional theories in practical applications.
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Acknowledgements
The authors thank Dr. Jie Zhang and Prof. Feng Xu for helpful discussions and suggestions, as well as very insightful comments from the anonymous referees. Financial supports by Grants from the National Natural Science Foundation of China (11490553, 11502185 and 11362010), Natural Science Basic Research Plan in Shaanxi Province of China (2016JQ1004) and Key Laboratory of Mechanics on Disaster and Environment in Western China (Klmwde201501) are gratefully acknowledged.
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Zhu, Z., Hu, R., Zheng, X. et al. On dust concentration profile above an area source in a neutral atmospheric surface layer. Environ Fluid Mech 17, 1171–1188 (2017). https://doi.org/10.1007/s10652-017-9542-z
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DOI: https://doi.org/10.1007/s10652-017-9542-z