A novel design of Return Flow Solar Air Heater(RFSAH)with different arrangements of baffles especially V-Type Artificial roughness is simulated and numerically analyzed with energy balance equations.To enhance the eff...A novel design of Return Flow Solar Air Heater(RFSAH)with different arrangements of baffles especially V-Type Artificial roughness is simulated and numerically analyzed with energy balance equations.To enhance the effectiveness of baffles,numerous studies have been conducted.The performance of the RFSAH is studied in terms of thermal efficiency,thermo-hydraulic efficiency,and optimization of baffle parameters.Maximum Thermal efficiency and thermo-hydraulic efficiency are found in RFSAH with baffle on both sides of the absorber plate and mass flow rate above 0.2kg/s.Sensitivity analysis of the influencing parameters is carried out and reported the best performance of the system on selective geometrical parameters(ψ=0.7,β=20%,e/H=1,p/e=0.8,α=60°).The results obtained from the present model are validated with the published experimental results and have been found in quite reasonable agreement with an average error of 16.45%.Thermal and Thermohydraulic efficiency of RFSAH with a baffle on both sides of the absorber plate is maximum among baffles below,above,and on both sides of the absorber plate.It is observed that the thermal efficiency of RFSAH is greater than SF-SAH.The proposed optimum baffles roughness is suggested to increase the air upholding time period for more efficient output.展开更多
本文利用常规气象观测资料、美国国家环境预报中心再分析资料(NCEP)、天津铁塔、风廓线雷达及微波辐射计探测资料,对2014年2月6—7日渤海西岸天津滨海国际机场一次回流降雪过程的结构特征和发生机理进行了分析,重点讨论了此次回流降雪...本文利用常规气象观测资料、美国国家环境预报中心再分析资料(NCEP)、天津铁塔、风廓线雷达及微波辐射计探测资料,对2014年2月6—7日渤海西岸天津滨海国际机场一次回流降雪过程的结构特征和发生机理进行了分析,重点讨论了此次回流降雪过程中两个降雪阶段边界层东风的性质和作用及上升运动的形成机制。结果表明:天津地区此次回流降雪过程可分为两个阶段,第一阶段降雪为2014年2月6日15:06—19:00,第二阶段降雪为7日凌晨00:25—15:46。2月6日降雪是发生在回流形势建立初期的弱降雪过程,低层的弱东风将海面上充沛的水汽输送至天津地区,同时配合偏东气流中的中尺度扰动,在2.0 km以下形成浅薄的辐合上升运动。2月7日降雪是中层的西来槽和低层冷空气共同作用的结果,以偏东路径南下的冷空气本来是较干的,由于经过渤海湾,使贴近海面(约600 m以下)的大气湿度明显增加,因此影响天津地区的偏东风为湿冷的,并在边界层内形成了一个明显的冷垫,当500 h Pa高空槽移至天津地区时与边界层偏东风形成的冷垫相遇,暖湿空气沿冷垫爬升促进了上升运动的发展,同时槽前的西南气流也起到输送水汽的作用。展开更多
文摘A novel design of Return Flow Solar Air Heater(RFSAH)with different arrangements of baffles especially V-Type Artificial roughness is simulated and numerically analyzed with energy balance equations.To enhance the effectiveness of baffles,numerous studies have been conducted.The performance of the RFSAH is studied in terms of thermal efficiency,thermo-hydraulic efficiency,and optimization of baffle parameters.Maximum Thermal efficiency and thermo-hydraulic efficiency are found in RFSAH with baffle on both sides of the absorber plate and mass flow rate above 0.2kg/s.Sensitivity analysis of the influencing parameters is carried out and reported the best performance of the system on selective geometrical parameters(ψ=0.7,β=20%,e/H=1,p/e=0.8,α=60°).The results obtained from the present model are validated with the published experimental results and have been found in quite reasonable agreement with an average error of 16.45%.Thermal and Thermohydraulic efficiency of RFSAH with a baffle on both sides of the absorber plate is maximum among baffles below,above,and on both sides of the absorber plate.It is observed that the thermal efficiency of RFSAH is greater than SF-SAH.The proposed optimum baffles roughness is suggested to increase the air upholding time period for more efficient output.
文摘本文利用常规气象观测资料、美国国家环境预报中心再分析资料(NCEP)、天津铁塔、风廓线雷达及微波辐射计探测资料,对2014年2月6—7日渤海西岸天津滨海国际机场一次回流降雪过程的结构特征和发生机理进行了分析,重点讨论了此次回流降雪过程中两个降雪阶段边界层东风的性质和作用及上升运动的形成机制。结果表明:天津地区此次回流降雪过程可分为两个阶段,第一阶段降雪为2014年2月6日15:06—19:00,第二阶段降雪为7日凌晨00:25—15:46。2月6日降雪是发生在回流形势建立初期的弱降雪过程,低层的弱东风将海面上充沛的水汽输送至天津地区,同时配合偏东气流中的中尺度扰动,在2.0 km以下形成浅薄的辐合上升运动。2月7日降雪是中层的西来槽和低层冷空气共同作用的结果,以偏东路径南下的冷空气本来是较干的,由于经过渤海湾,使贴近海面(约600 m以下)的大气湿度明显增加,因此影响天津地区的偏东风为湿冷的,并在边界层内形成了一个明显的冷垫,当500 h Pa高空槽移至天津地区时与边界层偏东风形成的冷垫相遇,暖湿空气沿冷垫爬升促进了上升运动的发展,同时槽前的西南气流也起到输送水汽的作用。
