Minimum ignition temperature of polyethylene dust: a theoretical model
โ Scribed by Manju Mittal; B. K. Guha
- Publisher
- John Wiley and Sons
- Year
- 1997
- Tongue
- English
- Weight
- 181 KB
- Volume
- 21
- Category
- Article
- ISSN
- 0308-0501
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โฆ Synopsis
Dust explosion hazard exists in plants and facilities handling combustible dusts. The minimum ignition temperature of dust clouds is an important parameter requiring special attention to designing the explosion preventive measures. This paper presents a model developed for determining the minimum ignition temperature for an organic dust cloud, polyethylene, simulating the conditions in the Godbert-Greenwald furnace. The model correlates the particle size, as well as the dust concentration with the minimum ignition temperature. It is based on the two-stage oxidation mechanism involving devolatilization/decomposition of the solid particle and homogeneous oxidation of volatile combustible products. In the case of polyethylene, the main combustible gas responsible for ignition and flame propagation has been confirmed to be butylene. The results of the computations were compared with the experimental values and those predicted by Mitsui and Tanaka. The predicted values by the model developed are in close agreement with the experimental data which confirm the proposed ignition mechanism. The model can be used for the prediction of minimum ignition temperature of organic dusts having an autoignition mechanism similar to polyethylene dust.
๐ SIMILAR VOLUMES
Dust explosion hazard exists in plants and facilities wherever combustible dusts are handled. The minimum ignition temperature of dust clouds is an important factor requiring special attention for the design of any explosion preventive measures. The present paper is confined to a study of the minimu
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## Abstract The original article to which this Erratum refers was published in International Journal of Climatology; 2007.
Criticality in the thermal explosion problem was defined as the attainment of an inflection in the temperature-time trajectories before the maximum temperature was reached by Rice et al. in 1935. The location of such a point was determined through numerical integration of the governing differential