期刊文献+
共找到5篇文章
< 1 >
每页显示 20 50 100
关于地热水水量计算的探讨 被引量:1
1
作者 金丽燕 鲁云龙 王益军 《地下水》 2010年第6期31-31,64,共2页
地热水是新型的清洁能源,现在很多城市建设中对地热水的开发已经很普遍。介绍了一些概念及对地热水的水资源论证工作的一些步骤和方法,希望能和大家探讨和交流。
关键词 热水 热水资源 地热田 热能储 盖层 热水通道 热源 地热地质条件 热水资源量的计算
下载PDF
浅析武夷山市“奥特莱斯”地热成因
2
作者 郑维添 《能源与环境》 2020年第3期46-46,共1页
在武夷山"奥特莱斯"小镇进行的物探及钻探工作的基础上,分析地热资源赋存条件及形成原因。
关键词 盖层 热水通道 热储 热源
下载PDF
Development of Single Phase Heat Transfer Correlations for Water & R134a in Rectangular Channel with Smooth Wavy Fin
3
作者 Amaranatha Raju. Muppala Ashok Babu T. P Ranganayakulu.Chennu 《Journal of Physical Science and Application》 2015年第3期199-208,共10页
Single phase heat transfer analysis of water and R134a refrigerant (liquid phase) has been carried out using CFD (Computational fluid dynamics) approach for rectangular channel with smooth wavy fin. Colburnj facto... Single phase heat transfer analysis of water and R134a refrigerant (liquid phase) has been carried out using CFD (Computational fluid dynamics) approach for rectangular channel with smooth wavy fin. Colburnj factor and Fanning friction factorf are predicted for wavy fin. The correlations are developed at Reynolds number range of 100-15,000. The effect of fin geometry (fin spacing, fin height, wave height and wave length) on the enhanced heat transfer and pressure drops are investigated. Results show that there is no significant variation off factor for water and liquid R134a at constant Reynolds number. However variations inj factor were observed at constant Reynolds number. Colburnj factor and Fanning friction factorfcorrelations are proposed in terms of Re and geometry parameters (h/s, a/s, L/a) for water and liquid refrigerant R134a in the present study. Two separate equations are proposed for the low and high Re regions i.e. between Re of 100-1,000 and Re of 1,000-15,000. 展开更多
关键词 Compact heat exchanger numerical analysis friction factor Colbum factor wavy fin lance offset fin heat transfer coefficient.
下载PDF
天水街子温泉控热推覆构造的发现及地热前景探讨 被引量:3
4
作者 罗文广 孙知新 +1 位作者 安永康 李百祥 《甘肃地质》 2006年第1期68-71,共4页
天水街子温泉通过可控源音频大地电磁测深,在温泉所在的温家峡及其附近深部发现的低阻电性层呈层状分布,其深度与以往钻孔中所见地下热水部位一致,推断此低阻层为热水通道。结合地表地质和地面磁测推测逆断层与上盘推覆体(牵引背斜)构... 天水街子温泉通过可控源音频大地电磁测深,在温泉所在的温家峡及其附近深部发现的低阻电性层呈层状分布,其深度与以往钻孔中所见地下热水部位一致,推断此低阻层为热水通道。结合地表地质和地面磁测推测逆断层与上盘推覆体(牵引背斜)构成推覆构造,逆冲断层为阻水构造,活动上盘岩块破碎和裂隙发育是地下热水良好通道,控制着中低温地热田分布。街子温家峡温泉和黄家峡有利热储地段,地下热水具有充沛的补给来源、较好储存和开采条件,具有进一步钻探开发扩大地热利用的远景。 展开更多
关键词 电磁测深 地面磁测 推覆构造 逆冲断层 热水通道
原文传递
Analysis of streamwise conduction in forced convection of microchannels using fin approach
5
作者 Suhandran MUNIANDY Yew Mun HUNG 《Journal of Zhejiang University-Science A(Applied Physics & Engineering)》 SCIE EI CAS CSCD 2011年第9期655-664,共10页
The effects induced by streamwise conduction on the thermal characteristics of forced convection for single-phase liquid flow in rectangular microchannel heat sinks under imposed constant wall temperature have been st... The effects induced by streamwise conduction on the thermal characteristics of forced convection for single-phase liquid flow in rectangular microchannel heat sinks under imposed constant wall temperature have been studied. By employing the fin approach in the first law of analysis, models with and without streamwise conduction term in the energy equation were developed for hydrodynamically and thermally fully-developed flow under local thermal non-equilibrium for the solid and fluid phases. These two models were solved to obtain closed form analytical solutions for the fluid and solid temperature distributions and the analysis emphasized details of the variations induced by the streamwise conduction on the fluid temperature distributions. The effects of the Peclet number, aspect ratio, and thermal conductivity ratio on the thermal characteristics of forced convection in microchannel heat sinks were analyzed and discussed. This study reveals the conditions under which the effect of streamwise conduction is significant and should not be neglected in the forced convective heat transfer analysis of microchannel heat sinks. 展开更多
关键词 Streamwise conduction Fin approach Microchannel heat sink
原文传递
上一页 1 下一页 到第
使用帮助 返回顶部