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KURENAI : Kyoto University Research Information Repository

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d<br />

In<br />

cal<br />

S. are<br />

and<br />

The similarity groups appeared in the above equations are defined below.<br />

Richardson No. ; R -.<br />

gsAT0Qo<br />

2<br />

uo<br />

Friction No.<br />

Modified<br />

Time<br />

Biot No.<br />

Stanton<br />

Ratio No.<br />

' F.(fk<br />

+ Ki=<br />

4hto<br />

No.; St. =<br />

PCud pi<br />

* as<br />

Ti =<br />

62<br />

_ha B.=<br />

Heat Source No. Rsi=pC<br />

addition to<br />

similarity<br />

Axial<br />

Flow<br />

It<br />

Scale<br />

Area<br />

is noted<br />

defined-by<br />

di = 4aiRi<br />

si = asi/E.<br />

the above<br />

groups are<br />

o<br />

Uo<br />

(IT s<br />

qs to<br />

ps<br />

defined physical<br />

' Li ti/to<br />

Scale; Ai = ai/ao<br />

obtained. These<br />

Buoyancy<br />

Inertia Force<br />

Friction<br />

Inertia<br />

Force<br />

Wall Convection<br />

Axial Convection<br />

Transport Time<br />

Conduction Time<br />

Wall Convection<br />

Conduction<br />

u0ATo<br />

similarity<br />

are;<br />

(Lh = th/2,o)<br />

Heat Source<br />

Axial Energy Change<br />

. (12)<br />

groups, several geometri-<br />

(13)<br />

here that the hydraulic diameter d. and the conduction depth<br />

335<br />

(14)<br />

(15)

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