四川大学学报(自然科学版)
四川大學學報(自然科學版)
사천대학학보(자연과학판)
JOURNAL OF SICHUAN UNIVERSITY(NATURAL SCIENCE EDITION)
2014年
2期
340-344
,共5页
自然对流%多孔介质%数值模拟%底部加热
自然對流%多孔介質%數值模擬%底部加熱
자연대류%다공개질%수치모의%저부가열
Natural heat transfer%Porous medium%Numerical simulation%Bottom heating
为了研究底部加热多孔介质方腔内的自然对流传热,采用整体求解法对方腔内的温度场和流场进行了数值模拟计算,着重分析了瑞利数Ra对多孔介质方腔内自然对流换热特性的影响。计算结果表明:随着Ra数的逐渐增加,对流换热开始占主要作用,等温线变得扭曲;流线由逆时针单胞对流逐渐变化为正反两个双胞对流,流动出现分叉现象,温度场和流线相互对应。平均Nusselt也随之增大,换热效果得到增强。
為瞭研究底部加熱多孔介質方腔內的自然對流傳熱,採用整體求解法對方腔內的溫度場和流場進行瞭數值模擬計算,著重分析瞭瑞利數Ra對多孔介質方腔內自然對流換熱特性的影響。計算結果錶明:隨著Ra數的逐漸增加,對流換熱開始佔主要作用,等溫線變得扭麯;流線由逆時針單胞對流逐漸變化為正反兩箇雙胞對流,流動齣現分扠現象,溫度場和流線相互對應。平均Nusselt也隨之增大,換熱效果得到增彊。
위료연구저부가열다공개질방강내적자연대류전열,채용정체구해법대방강내적온도장화류장진행료수치모의계산,착중분석료서리수Ra대다공개질방강내자연대류환열특성적영향。계산결과표명:수착Ra수적축점증가,대류환열개시점주요작용,등온선변득뉴곡;류선유역시침단포대류축점변화위정반량개쌍포대류,류동출현분차현상,온도장화류선상호대응。평균Nusselt야수지증대,환열효과득도증강。
In order to study natural convection heat transfer in square porous medium heated from below, numerical simulation calculation is carried out to analyze the temperature and velocity field of square cav-ity using whole-field solution.The effects of Ra number on the natural convection heat transfer charac-teristics in square enclosure filled with porous medium are analysed especially.The results of the study show that with the increase of Ra,heat convection begans to play the main role and the temperature con-tour becomes distorted.The streamline changes gradually from the counterclockwise single cellular con-vection to the positive and negative two twin convection.The flow bifurcation occurs,the temperature field and the streamline correspond to each other.The average Nusselt number increases and the effect of heat transfer gets enhanced.