1987
DOI: 10.1007/bf00116118
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Turbulent dispersion in a stable layer with a quadratic exchange coefficient

Abstract: Dispersion from a line source into a stable boundary layer of thickness I is analysed through solution of the diffusion equation assuming an exchange coefficient K(z) cc (1 -z/l)2 and wind profiles u(z) cc z", with n = 0, 1. Estimates of ground-level concentrations are made by developing analytic formulae where this is possible. A general method of solution using Laplace transformation and Green's function techniques is developed as an alternative to the eigenftmction expansion method discussed previously (Rob… Show more

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Cited by 7 publications
(15 citation statements)
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“…Whereas in this model, the multiple Laplace transform inverted analytically this gives an exact solution. The solutions of this model verified with that of (Robson, 1987) by assuming no delayed removal (chemical reaction rate) and time independent case. It is interesting to note that the effect of chemical reaction rte has virtually no impact t the short travel time but has significant effect t large travel time.…”
Section: Resultssupporting
confidence: 57%
See 3 more Smart Citations
“…Whereas in this model, the multiple Laplace transform inverted analytically this gives an exact solution. The solutions of this model verified with that of (Robson, 1987) by assuming no delayed removal (chemical reaction rate) and time independent case. It is interesting to note that the effect of chemical reaction rte has virtually no impact t the short travel time but has significant effect t large travel time.…”
Section: Resultssupporting
confidence: 57%
“…In most of the previous models, numerical methods used either fully or partly. In model where the Laplace transform is generally inverted numerically (Robson, 1987). Whereas in this model, the multiple Laplace transform inverted analytically this gives an exact solution.…”
Section: Resultsmentioning
confidence: 99%
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“…The possibility of leakage of pollutants through inversion layer in negligibly less. Therefore, the diffusion coefficient of quadratic in nature considered which is best suited for the stable ABL (Robson [2]) in this model. The height of the atmospheric boundary layer is assumed to be z = H, from the surface.…”
Section: Formulation Of the Modelmentioning
confidence: 98%