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Code Manual for CONTAIN 2.0 - Federation of American Scientists

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Ti, total gas mass W, and free volume Vi, respectively, in each cell i. On the first timestep, if the<br />

relative rates <strong>of</strong> change satisfj<br />

lVi-l dVi/dt I s ~<br />

the cell i is replaced in subsequent flow timesteps within the same system timestep by fixed-flowrate<br />

boundary conditions, with the flow rates and composition taken to be those calculated in the fnst<br />

flow timestep. In addition, the atmospheric conditions in the cell related to the noncondensable<br />

gases and the condensable material will be held constant <strong>for</strong> those timesteps. Note that while the<br />

atmosphere thermodynamic and flow conditions will be held constant, aerosol and fission product<br />

inventories will not be held constant but will be calculated as evolving according to the assumed<br />

flow rates and thermodynamic conditions.<br />

4.4.9.2 Gu idelines <strong>for</strong> Applvimz the FIX-FLO W ODtion. In applying the FIX-FLOW option, the<br />

user should be aware <strong>of</strong> the fact that even <strong>for</strong> relatively small tolerances, mass and energy<br />

conservation problems may result and the calculated cell conditions <strong>for</strong> the cell atmospheres replaced<br />

by fixed-flow boundary conditions may deviate significantly from the correct ones. These effects<br />

in general scale with the user-specified rate tolerance ~. The degree to which these effects occur<br />

depends on the detailed nature <strong>of</strong> the processes occurring within a cell. The purpose <strong>of</strong> this section<br />

is to supply guidelines to the user as to when FIX-FLOW should be invoked.<br />

Mass and energy will in general not be conserved in a cell replaced by fixed-flow boundary<br />

conditions, since these quantities should in general be changing, albeit slowly. Under the quasisteady<br />

conditions likely to be present when the fixed-flow boundary conditions are invoked, one can<br />

estimate errors by assuming linear rates <strong>of</strong> change <strong>of</strong> mass and energy over the system timestep.<br />

Estimates <strong>for</strong> the relative error per system timestep on the atmosphere temperature and total<br />

atmospheric mass in this case can be expressed, respectively, as:<br />

(4-29)<br />

where At, is the system timestep and s is the ratio A? /At, <strong>of</strong> the fwst flow timestep to the system<br />

timestep. The degree to which such errors accumulate and can be tolerated depends on the situation.<br />

In some cases, such as an adiabatic closed cell with a very low source rate extending over a long<br />

period <strong>of</strong> time, the cumulative errors may not be acceptable even <strong>for</strong> q = 10-6. However, as<br />

discussed below, <strong>for</strong> a cell that rapidly relaxes to a quasi-steady state and is comected to a very large<br />

reservoir (i.e., the environment), the cumulative errors may be negligible.<br />

Rev. O 4-42 6/30/97

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