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KURENAI : Kyoto University Research Information Repository

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Mixture<br />

ap mum •<br />

at<br />

Mixture<br />

apmHm<br />

at<br />

Solid<br />

PSCps<br />

Momentum<br />

a<br />

az<br />

Equation<br />

3p<br />

(Pmum)-azmPm g -<br />

2D+K<br />

Enthalpy<br />

a<br />

az<br />

s(z-z i)] pm<br />

Energy<br />

4hm<br />

(pmumHm)d<br />

Energy Equation (ith<br />

aT<br />

umlum~.<br />

aapgp V2<br />

az (1-a)p mgj<br />

Equation (ith Section)<br />

a aPgP<br />

(Ts-Tsat)az p moHf9Vgj<br />

Section)<br />

ats + ksv2Ts - qs=0 (66)<br />

Solid-Fluid Boundary Condition (ith Section)<br />

-<br />

aT<br />

k<br />

s= aym h (Ts-Tsat) (67)<br />

Here Vgjis the drift velocity given byVgj= (1-a)(u q-uf). The mixture f<br />

riction factor and heat transfer coefficient are denoted by f m and hm, re-<br />

spectively. The constitutive relations for the drift velocity, V gj, and the<br />

vapor source term r g should be specified in the above formulation. Under the<br />

thermal equilibrium condition, it can be shown [3] that<br />

rg =<br />

4hm(Ts-Tsat)<br />

dAH fg<br />

For water at relatively high<br />

the assumption of the thermal<br />

constitutive equation [7] for<br />

V.<br />

pressure and under natural circulation conditions,<br />

equilibrium is reasonable. The representative<br />

the drift velocity is given by<br />

= 0.2 (1 -)F- 1.42<br />

g-7;;) J + (c)op1/4<br />

,<br />

347<br />

(64)<br />

(65)<br />

(68)<br />

(69)

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