Major hazard risk assessment over non-flat terrain. Part II. instantaneous release
Major hazard risk assessment over non-flat terrain. Part II. instantaneous release
This is the second part of a two-part paper which considers the risk of being exposed to accidentally released toxic gas; part one considered continuous releases and this part considers instantaneous releases. The risk estimated is RI; the probability at any point of receiving a non-zero dose given an instantaneous release (probability language is needed because wind direction is assumed to be a random variable).
On flat ground, simple analytical techniques show that for an instantaneous release of buoyancy B with a uniform windrose, RICð4=p5Þ1=4F1=2 r1=2 u1=2 B1=4 at radius r; where F is the front Froude number and u the windspeed.
In this paper RI is estimated over non-flat terrain using shallow layer modelling for a range of windspeeds and slopes. The source term is identical to that of Thorney Island Trial 08. In a windspeed of 1 m s1 a slope as little as 2% substantially affects the risk in the sense that the predicted risk contours are far from circularly symmetric; continuous releases showed similar trends.
The real terrain data used is from Little Barrier Island, New Zealand (latitude 36110 S; longitude 17540 E), chosen on account of its being uninhabited, and having steep slopes and complex topography. As the windspeed increases from 1 to 10 m s1; risk contours become less affected by terrain in both instantaneous and continuous releases.
Heavy gas dispersion, Major hazards, Risk assessment, Slopes, Complex terrain
707-714
Hankin, R.K.S.
296864a6-e423-44b6-ad0e-25422c913540
2004
Hankin, R.K.S.
296864a6-e423-44b6-ad0e-25422c913540
Hankin, R.K.S.
(2004)
Major hazard risk assessment over non-flat terrain. Part II. instantaneous release.
Atmospheric Environment, 38 (5), .
(doi:10.1016/j.atmosenv.2003.10.022).
Abstract
This is the second part of a two-part paper which considers the risk of being exposed to accidentally released toxic gas; part one considered continuous releases and this part considers instantaneous releases. The risk estimated is RI; the probability at any point of receiving a non-zero dose given an instantaneous release (probability language is needed because wind direction is assumed to be a random variable).
On flat ground, simple analytical techniques show that for an instantaneous release of buoyancy B with a uniform windrose, RICð4=p5Þ1=4F1=2 r1=2 u1=2 B1=4 at radius r; where F is the front Froude number and u the windspeed.
In this paper RI is estimated over non-flat terrain using shallow layer modelling for a range of windspeeds and slopes. The source term is identical to that of Thorney Island Trial 08. In a windspeed of 1 m s1 a slope as little as 2% substantially affects the risk in the sense that the predicted risk contours are far from circularly symmetric; continuous releases showed similar trends.
The real terrain data used is from Little Barrier Island, New Zealand (latitude 36110 S; longitude 17540 E), chosen on account of its being uninhabited, and having steep slopes and complex topography. As the windspeed increases from 1 to 10 m s1; risk contours become less affected by terrain in both instantaneous and continuous releases.
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Published date: 2004
Keywords:
Heavy gas dispersion, Major hazards, Risk assessment, Slopes, Complex terrain
Identifiers
Local EPrints ID: 9817
URI: http://eprints.soton.ac.uk/id/eprint/9817
ISSN: 1352-2310
PURE UUID: 112786de-0282-4fa7-b636-a31d98e058f8
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Date deposited: 19 Oct 2004
Last modified: 15 Mar 2024 04:57
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Author:
R.K.S. Hankin
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