{"title":"湍流脉冲气体-液滴涡流云传播的显著特征","authors":"M. A. Pakhomov, V. P. Terekhov","doi":"10.1134/S0015462824602870","DOIUrl":null,"url":null,"abstract":"<p>We present the results of the numerical modeling of the formation and motion of a blown solitary pulsed turbulent gas-droplet jet under the conditions approximately corresponding to human cough. The calculations are performed for the pulse duration <i>t</i> = 0.6 s and the greatest velocity of the gas phase of 20 m/s at the mass fraction of droplets <i>M</i><sub><i>L</i>1</sub> = 1%. The drop phase in the exit section is monodisperse, while the initial dimension of particles in the calculations varied in the range <i>D</i><sub>1</sub> = 5‒30 μm. Two zones of elevated vorticity are formed within the cloud in the initial period of motion. They are situated in the mixing layer and in the region of deceleration of two-phase pulsed jet. The greatest levels of the longitudinal velocity and the kinetic energy of turbulence are attained in the interval of pulse blow-on. At the subsequent moments of time the turbulence velocity and level monotonically decrease. The vortex cloud produced by the solitary pulse exists for a fairly long time (<i>t</i> ≈ 4 s) and has a time to penetrate into the surrounding space at a distance greater than 3 m.</p>","PeriodicalId":560,"journal":{"name":"Fluid Dynamics","volume":"59 4","pages":"687 - 699"},"PeriodicalIF":1.0000,"publicationDate":"2024-11-07","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Distinctive Features of Propagation of a Turbulent Pulsed Gas-Droplet Eddy Cloud\",\"authors\":\"M. A. Pakhomov, V. P. Terekhov\",\"doi\":\"10.1134/S0015462824602870\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>We present the results of the numerical modeling of the formation and motion of a blown solitary pulsed turbulent gas-droplet jet under the conditions approximately corresponding to human cough. The calculations are performed for the pulse duration <i>t</i> = 0.6 s and the greatest velocity of the gas phase of 20 m/s at the mass fraction of droplets <i>M</i><sub><i>L</i>1</sub> = 1%. The drop phase in the exit section is monodisperse, while the initial dimension of particles in the calculations varied in the range <i>D</i><sub>1</sub> = 5‒30 μm. Two zones of elevated vorticity are formed within the cloud in the initial period of motion. They are situated in the mixing layer and in the region of deceleration of two-phase pulsed jet. The greatest levels of the longitudinal velocity and the kinetic energy of turbulence are attained in the interval of pulse blow-on. At the subsequent moments of time the turbulence velocity and level monotonically decrease. The vortex cloud produced by the solitary pulse exists for a fairly long time (<i>t</i> ≈ 4 s) and has a time to penetrate into the surrounding space at a distance greater than 3 m.</p>\",\"PeriodicalId\":560,\"journal\":{\"name\":\"Fluid Dynamics\",\"volume\":\"59 4\",\"pages\":\"687 - 699\"},\"PeriodicalIF\":1.0000,\"publicationDate\":\"2024-11-07\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Fluid Dynamics\",\"FirstCategoryId\":\"5\",\"ListUrlMain\":\"https://link.springer.com/article/10.1134/S0015462824602870\",\"RegionNum\":4,\"RegionCategory\":\"工程技术\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q4\",\"JCRName\":\"MECHANICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Fluid Dynamics","FirstCategoryId":"5","ListUrlMain":"https://link.springer.com/article/10.1134/S0015462824602870","RegionNum":4,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q4","JCRName":"MECHANICS","Score":null,"Total":0}
Distinctive Features of Propagation of a Turbulent Pulsed Gas-Droplet Eddy Cloud
We present the results of the numerical modeling of the formation and motion of a blown solitary pulsed turbulent gas-droplet jet under the conditions approximately corresponding to human cough. The calculations are performed for the pulse duration t = 0.6 s and the greatest velocity of the gas phase of 20 m/s at the mass fraction of droplets ML1 = 1%. The drop phase in the exit section is monodisperse, while the initial dimension of particles in the calculations varied in the range D1 = 5‒30 μm. Two zones of elevated vorticity are formed within the cloud in the initial period of motion. They are situated in the mixing layer and in the region of deceleration of two-phase pulsed jet. The greatest levels of the longitudinal velocity and the kinetic energy of turbulence are attained in the interval of pulse blow-on. At the subsequent moments of time the turbulence velocity and level monotonically decrease. The vortex cloud produced by the solitary pulse exists for a fairly long time (t ≈ 4 s) and has a time to penetrate into the surrounding space at a distance greater than 3 m.
期刊介绍:
Fluid Dynamics is an international peer reviewed journal that publishes theoretical, computational, and experimental research on aeromechanics, hydrodynamics, plasma dynamics, underground hydrodynamics, and biomechanics of continuous media. Special attention is given to new trends developing at the leading edge of science, such as theory and application of multi-phase flows, chemically reactive flows, liquid and gas flows in electromagnetic fields, new hydrodynamical methods of increasing oil output, new approaches to the description of turbulent flows, etc.