Rupam Shankar Nath, Himangshu Kumar, Rudra Kanta Deka
{"title":"热分层和质量分层效应对具有周期性温度变化和可变质量扩散的垂直振荡板上非稳态流动的理论研究","authors":"Rupam Shankar Nath, Himangshu Kumar, Rudra Kanta Deka","doi":"10.1002/htj.23105","DOIUrl":null,"url":null,"abstract":"<p>This research paper examines the combined effects of thermal and mass stratification on unsteady flow past a vertical oscillating plate with periodic temperature variation and variable mass diffusion. The Laplace transform technique is introduced to deal with the linear coupled parabolic equations satisfying initial as well as boundary conditions and obtained solutions in closed form for concentration, temperature, and velocity. For example, to find the Laplace transform of an exponentially ordered piece wise continuous function <span></span><math>\n <semantics>\n <mrow>\n <mrow>\n <mi>n</mi>\n \n <mrow>\n <mo>(</mo>\n \n <mi>t</mi>\n \n <mo>)</mo>\n </mrow>\n </mrow>\n </mrow>\n <annotation> $n(t)$</annotation>\n </semantics></math>, one can uses the formula <span></span><math>\n <semantics>\n <mrow>\n <mrow>\n <mi>L</mi>\n \n <mrow>\n <mo>{</mo>\n \n <mrow>\n <mi>n</mi>\n \n <mrow>\n <mo>(</mo>\n \n <mi>t</mi>\n \n <mo>)</mo>\n </mrow>\n </mrow>\n \n <mo>}</mo>\n </mrow>\n \n <mo>=</mo>\n \n <msubsup>\n <mo>∫</mo>\n \n <mn>0</mn>\n \n <mi>∞</mi>\n </msubsup>\n \n <msup>\n <mi>e</mi>\n \n <mrow>\n <mo>−</mo>\n \n <mi>s</mi>\n \n <mi>t</mi>\n </mrow>\n </msup>\n \n <mi>n</mi>\n \n <mrow>\n <mo>(</mo>\n \n <mi>t</mi>\n \n <mo>)</mo>\n </mrow>\n \n <mi>d</mi>\n \n <mi>t</mi>\n \n <mo>=</mo>\n \n <mover>\n <mi>n</mi>\n \n <mo>¯</mo>\n </mover>\n \n <mrow>\n <mo>(</mo>\n \n <mi>s</mi>\n \n <mo>)</mo>\n </mrow>\n </mrow>\n </mrow>\n <annotation> $L\\{n(t)\\}={\\int }_{0}^{\\infty }{e}^{-st}n(t)dt=\\bar{n}(s)$</annotation>\n </semantics></math>, <i>t</i> being the time and <i>s</i> is a parameter. In this study, we explore the effects of different factors such as plate amplitude, plate frequency, thermal Grashof number, and the mass Grashof number on the concentration, velocity, and temperature profiles and shows them graphically. We see a decline in the fluid's velocity for thermal and mass stratification. Most interestingly, in presence of higher temperature gradient, as the frequency of the oscillations increases close to the plate surface, the fluid velocity declines. The reason behind this is that the flow system has a plate with very high fluctuations. We have found that the fluid's temperature goes up while the concentration goes down when there is a decrease in the thermal stratification and a rise in the mass stratification.</p>","PeriodicalId":44939,"journal":{"name":"Heat Transfer","volume":"53 7","pages":"3605-3624"},"PeriodicalIF":2.8000,"publicationDate":"2024-06-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Theoretical investigation of thermal and mass stratification effects on unsteady flow across a vertical oscillating plate with periodic temperature variation and variable mass diffusion\",\"authors\":\"Rupam Shankar Nath, Himangshu Kumar, Rudra Kanta Deka\",\"doi\":\"10.1002/htj.23105\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>This research paper examines the combined effects of thermal and mass stratification on unsteady flow past a vertical oscillating plate with periodic temperature variation and variable mass diffusion. The Laplace transform technique is introduced to deal with the linear coupled parabolic equations satisfying initial as well as boundary conditions and obtained solutions in closed form for concentration, temperature, and velocity. For example, to find the Laplace transform of an exponentially ordered piece wise continuous function <span></span><math>\\n <semantics>\\n <mrow>\\n <mrow>\\n <mi>n</mi>\\n \\n <mrow>\\n <mo>(</mo>\\n \\n <mi>t</mi>\\n \\n <mo>)</mo>\\n </mrow>\\n </mrow>\\n </mrow>\\n <annotation> $n(t)$</annotation>\\n </semantics></math>, one can uses the formula <span></span><math>\\n <semantics>\\n <mrow>\\n <mrow>\\n <mi>L</mi>\\n \\n <mrow>\\n <mo>{</mo>\\n \\n <mrow>\\n <mi>n</mi>\\n \\n <mrow>\\n <mo>(</mo>\\n \\n <mi>t</mi>\\n \\n <mo>)</mo>\\n </mrow>\\n </mrow>\\n \\n <mo>}</mo>\\n </mrow>\\n \\n <mo>=</mo>\\n \\n <msubsup>\\n <mo>∫</mo>\\n \\n <mn>0</mn>\\n \\n <mi>∞</mi>\\n </msubsup>\\n \\n <msup>\\n <mi>e</mi>\\n \\n <mrow>\\n <mo>−</mo>\\n \\n <mi>s</mi>\\n \\n <mi>t</mi>\\n </mrow>\\n </msup>\\n \\n <mi>n</mi>\\n \\n <mrow>\\n <mo>(</mo>\\n \\n <mi>t</mi>\\n \\n <mo>)</mo>\\n </mrow>\\n \\n <mi>d</mi>\\n \\n <mi>t</mi>\\n \\n <mo>=</mo>\\n \\n <mover>\\n <mi>n</mi>\\n \\n <mo>¯</mo>\\n </mover>\\n \\n <mrow>\\n <mo>(</mo>\\n \\n <mi>s</mi>\\n \\n <mo>)</mo>\\n </mrow>\\n </mrow>\\n </mrow>\\n <annotation> $L\\\\{n(t)\\\\}={\\\\int }_{0}^{\\\\infty }{e}^{-st}n(t)dt=\\\\bar{n}(s)$</annotation>\\n </semantics></math>, <i>t</i> being the time and <i>s</i> is a parameter. In this study, we explore the effects of different factors such as plate amplitude, plate frequency, thermal Grashof number, and the mass Grashof number on the concentration, velocity, and temperature profiles and shows them graphically. We see a decline in the fluid's velocity for thermal and mass stratification. Most interestingly, in presence of higher temperature gradient, as the frequency of the oscillations increases close to the plate surface, the fluid velocity declines. The reason behind this is that the flow system has a plate with very high fluctuations. We have found that the fluid's temperature goes up while the concentration goes down when there is a decrease in the thermal stratification and a rise in the mass stratification.</p>\",\"PeriodicalId\":44939,\"journal\":{\"name\":\"Heat Transfer\",\"volume\":\"53 7\",\"pages\":\"3605-3624\"},\"PeriodicalIF\":2.8000,\"publicationDate\":\"2024-06-12\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Heat Transfer\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1002/htj.23105\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"THERMODYNAMICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Heat Transfer","FirstCategoryId":"1085","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1002/htj.23105","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"THERMODYNAMICS","Score":null,"Total":0}
引用次数: 0
摘要
本研究论文探讨了热分层和质量分层对经过具有周期性温度变化和可变质量扩散的垂直振荡板的非稳态流动的综合影响。本文引入了拉普拉斯变换技术来处理满足初始条件和边界条件的线性耦合抛物线方程,并获得了浓度、温度和速度的闭式解。例如,要找到指数有序片断连续函数 , 的拉普拉斯变换,可以使用公式 , t 是时间,s 是参数。在本研究中,我们探讨了板幅、板频、热格拉肖夫数和质量格拉肖夫数等不同因素对浓度、速度和温度曲线的影响,并以图表形式显示出来。我们可以看到,在热分层和质量分层的情况下,流体的速度有所下降。最有趣的是,在温度梯度较高的情况下,随着靠近板面的振荡频率增加,流体速度下降。这背后的原因是流动系统的板面波动非常大。我们发现,当热力分层减少、质量分层增加时,流体的温度会升高,而浓度会降低。
Theoretical investigation of thermal and mass stratification effects on unsteady flow across a vertical oscillating plate with periodic temperature variation and variable mass diffusion
This research paper examines the combined effects of thermal and mass stratification on unsteady flow past a vertical oscillating plate with periodic temperature variation and variable mass diffusion. The Laplace transform technique is introduced to deal with the linear coupled parabolic equations satisfying initial as well as boundary conditions and obtained solutions in closed form for concentration, temperature, and velocity. For example, to find the Laplace transform of an exponentially ordered piece wise continuous function , one can uses the formula , t being the time and s is a parameter. In this study, we explore the effects of different factors such as plate amplitude, plate frequency, thermal Grashof number, and the mass Grashof number on the concentration, velocity, and temperature profiles and shows them graphically. We see a decline in the fluid's velocity for thermal and mass stratification. Most interestingly, in presence of higher temperature gradient, as the frequency of the oscillations increases close to the plate surface, the fluid velocity declines. The reason behind this is that the flow system has a plate with very high fluctuations. We have found that the fluid's temperature goes up while the concentration goes down when there is a decrease in the thermal stratification and a rise in the mass stratification.