Suppression of the Thermal Decomposition Reaction of Forest Combustible Materials in Large-Area Fires / R. S. Volkov, A. O. Zhdanova, G. V. Kuznetsov, P. A. Strizhak

Уровень набора: Journal of Engineering Physics and ThermophysicsАльтернативный автор-лицо: Volkov, R. S., specialist in the field of power engineering, Associate Professor of the Tomsk Polytechnic University, candidate of technical Sciences, 1987-, Roman Sergeevich;Zhdanova, A. O., specialist in the field of power engineering, engineer of Tomsk Polytechnic University, 1989-, Alena Olegovna;Kuznetsov, G. V., Specialist in the field of heat power energy, Professor of Tomsk Polytechnic University, Doctor of Physical and Mathematical Sciences, 1949-, Geny Vladimirovich;Strizhak, P. A., Specialist in the field of heat power energy, Doctor of Physical and Mathematical Sciences (DSc), Professor of Tomsk Polytechnic University (TPU), 1985-, Pavel AlexandrovichКоллективный автор (вторичный): Национальный исследовательский Томский политехнический университет, Исследовательская школа физики высокоэнергетических процессов, (2017- );Национальный исследовательский Томский политехнический университет, Инженерная школа энергетики, Научно-образовательный центр И. Н. Бутакова (НОЦ И. Н. Бутакова)Язык: английский.Страна: .Резюме или реферат: Experimental investigations on the characteristic time of suppression of the thermal decomposition reaction of typical forest combustible materials (aspen twigs, birch leaves, spruce needles, pine chips, and a mixture of these materials) and the volume of water required for this purpose have been performed for model fire hotbeds of different areas: SFCM=0.0003-0.007 m2 and SFCM=0.045-0.245 m2. In the experiments, aerosol water flows with droplets of size 0.01-0.25 mm were used for the spraying of model fire hotbeds, and the density of spraying was 0.02 L/(m2·s). It was established that the characteristics of suppression of a fire by an aerosol water flow are mainly determined by the sizes of the droplets in this flow. Prognostic estimates of changes in the dispersivity of a droplet cloud, formed from large (as large as 0.5 L) "drops" (water agglomerates) thrown down from a height, have been made. It is shown that these changes can influence the conditions and characteristics of suppression of a forest fire. Dependences, allowing one to forecast the characteristics of suppression of the thermal decomposition of forest combustible materials with the use of large water agglomerates thrown down from an aircraft and aerosol clouds formed from these agglomerates in the process of their movement to the earth, are presented..Примечания о наличии в документе библиографии/указателя: [References: 23 tit.].Аудитория: .Тематика: электронный ресурс | труды учёных ТПУ | forest combustible materials | thermal decomposition | hotbed of fire | aerosol flow | water mass | лесные материалы | горючие материалы | термическое разложение | аэрозоли | водные массы | пожары Ресурсы он-лайн:Щелкните здесь для доступа в онлайн
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[References: 23 tit.]

Experimental investigations on the characteristic time of suppression of the thermal decomposition reaction of typical forest combustible materials (aspen twigs, birch leaves, spruce needles, pine chips, and a mixture of these materials) and the volume of water required for this purpose have been performed for model fire hotbeds of different areas: SFCM=0.0003-0.007 m2 and SFCM=0.045-0.245 m2. In the experiments, aerosol water flows with droplets of size 0.01-0.25 mm were used for the spraying of model fire hotbeds, and the density of spraying was 0.02 L/(m2·s). It was established that the characteristics of suppression of a fire by an aerosol water flow are mainly determined by the sizes of the droplets in this flow. Prognostic estimates of changes in the dispersivity of a droplet cloud, formed from large (as large as 0.5 L) "drops" (water agglomerates) thrown down from a height, have been made. It is shown that these changes can influence the conditions and characteristics of suppression of a forest fire. Dependences, allowing one to forecast the characteristics of suppression of the thermal decomposition of forest combustible materials with the use of large water agglomerates thrown down from an aircraft and aerosol clouds formed from these agglomerates in the process of their movement to the earth, are presented.

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