Thermal Energy Storage Systems and Applications. Ibrahim Dincer
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Название: Thermal Energy Storage Systems and Applications

Автор: Ibrahim Dincer

Издательство: John Wiley & Sons Limited

Жанр: Физика

Серия:

isbn: 9781119713142

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СКАЧАТЬ greater distance normal to the plate takes place between the fluid in the free stream and the plate surface. The rate of change of velocity determines the velocity gradient at the surface as well as the shear stresses. The shear stress for the laminar boundary layer becomes

      (1.79)equation

      which varies with distance along the plate by the change in velocity. Further along the plate, the shear force is gradually increased, as the laminar boundary layer thickens, because of the increasing plate surface area affected, and the fluid becomes retarded, so that a turbulent boundary layer occurs as instabilities set in. Thus, the shear stress for the turbulent flow can be approximated as

      (1.80)equation

      Experimental studies indicate that there are two boundary layer flow regimes; a laminar flow regime and a turbulent flow regime, which can be characterized by the Reynolds number, as pointed out earlier. The transition from a laminar to a turbulent boundary layer is dependent mainly upon the following:

       Re = usxc/v;

       the roughness of the plate; and

       the turbulence level in the free stream.

      There are various boundary‐layer parameters to be considered, such as boundary‐layer thickness, the local wall shear stress (or local friction or drag coefficient), and the average wall shear stress (or average friction or drag coefficient). The boundary‐layer thickness may be expressed in several ways. The simplest approach is that the velocity u within the boundary layer approaches the free‐stream velocity us. From experimental measurements, it was observed that the boundary‐layer thickness δ can be defined as the distance from the boundary to the point at which u = 0.99us.

      Source: Olson and Wright [8].

η 0.0 0.6 1.2 1.8 2.4 3.0 3.6 4.2 4.8 5.4 6.0
δ 0.000 0.200 0.394 0.575 0.729 0.846 0.924 0.967 0.988 0.996 0.999

      Source: Olson and Wright [8].

Velocity profile δ/x C f δ * /x
u/us = y/δ images images images
u/us = 2(y/δ) − (y/δ)2 images images images
u/us = 1.5(y/δ) − 0.5(y/δ)3 images images images
u/us = sin πy/2δ images images images
Blasius exact solution images images СКАЧАТЬ