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Code Manual for CONTAIN 2.0 - Federation of American Scientists

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The coolant pool layer is unique in that it is the only lower cell layer, outside <strong>of</strong> the models in<br />

CORCON, in which phase changes are allowed. As discussed in Chapter 10, surface evaporation ~<br />

and surface condensation <strong>of</strong> coolant vapor can occur much in the same manner as <strong>for</strong> heat transfer<br />

structures. As discussed in Section 11.2.1, pool evaporation and condensation can also occur with<br />

respect to gases vented into the pool under the pool surface. Boiling <strong>of</strong> the coolant can occur if the<br />

BOIL keyword is specified in the lower cell input block. If boiling is not activated, the pool is<br />

treated like other nodes in the conduction model, and the pool could reach unreasonable<br />

temperatures. There<strong>for</strong>e, boiling should always be activated. The BOIL keyword is also required <strong>for</strong><br />

proper equilibration <strong>of</strong> the coolant vapor between the pool and any gases vented under the pool<br />

surface. In the absence <strong>of</strong> the BOIL keyword, any coolant vapor in the vented gases is entirely<br />

condensed out in the pool.<br />

If boiling is activated, any net energy flux to the coolant pool that would raise the pool above<br />

saturation is assumed to contribute instead to the pool boiling rate. When such a saturated condition<br />

is detected, the conduction model solution is carried out with the pool temperature fixed at the<br />

saturation temperature, <strong>for</strong> the purpose <strong>of</strong> calculating the conduction flux to the pool and the boiling<br />

rate.<br />

Pool boiling is calculated fully implicitly with respect to pressure, if the implicit flow solver is<br />

invoked. Heat and mass sources to the pool are accumulated every cell timestep. They are then used<br />

to calculate a continuous boiling rate during the system timestep in which the sources are<br />

accumulated. Because <strong>of</strong> the fully implicit treatment, the pressurization due to the coolant mass and<br />

energy entering the atmosphere as a result <strong>of</strong> boiling is consistent with both the pool saturation<br />

temperature and the mass and energy flows to and from other cells. If the explicit flow solution is =<br />

invoked, pool boiling is evaluated explicitly outside <strong>of</strong> the flow and atmosphere thermodynamics<br />

solution. The expressions <strong>for</strong> the pool boiling rate <strong>for</strong> both flow methods are given in Section 4.4.6.<br />

5.5 Interlayer Heat Transfer<br />

The heat transfer coefficients used in the lower cell conduction model between layers are discussed<br />

in this section. The following, with one exception, applies to the heat transfer between the<br />

uppermost lower cell layer, which could be the pool, and any additional layers below. The heat<br />

transfer across the interfaces between the atmosphere and uppermost lower cell layer and between<br />

the coolant pool layer and submerged heat transfer structures is discussed in Section 10.1.2. The one<br />

exception mentioned above is an option, discussed in Section 5.5.2, <strong>for</strong> the user to specify the total<br />

convective heat transfer coefficient <strong>for</strong> the atmosphere-pool interface.<br />

This section consists <strong>of</strong> three parts: the fust describes the overall interlayer heat transfer coefllcient;<br />

the second discusses user-specified overall coet%cients; and the third discusses the heat conduction<br />

model.<br />

5.5.1 Interlayer Heat Transfer Coefficients<br />

The present section discusses the overall interlayer heat transfer coefficients that are defined <strong>for</strong> use<br />

in the heat conduction model, which is used when CORCON is not active. These heat transfer<br />

correlations are applied to the interface between layers; the heat transfer between nodes <strong>of</strong> a layer<br />

O 516 6/30/97

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