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Code Manual for CONTAIN 2.0 - Federation of American Scientists

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The user-specified trapping rate is normally a constant; however, time-varying rates can be specified<br />

through the use <strong>of</strong> user tables. To speci~ a constant trapping rate in a cell the value desired is given ~<br />

in the DCH-CELL block as explained in Section 14.3.1.11. User trapping values specified in the<br />

global DHEAT block are used as default constant trapping rates <strong>for</strong> all cells. To specify a timevarying<br />

trapping rate, the VAR-PARM keyword is used in the DCH-CELL input block. The name<br />

<strong>of</strong> the VAR-Y variable in the VAR-PARM block must be TRAPRATE to specifi the trapping rate<br />

as the dependent variable in the table.<br />

6.3.4 GIW Trapping Model<br />

In this model, the trapping rate is taken to be controlled by the gravitational fall rate <strong>of</strong> a sphere in<br />

the cell atmosphere:<br />

(6-88)<br />

where the terminal fall veloclty <strong>for</strong> debris parhcles<br />

. .<br />

m field n and cell 1 IS vx~,i,~. In the interest <strong>of</strong><br />

notational convenience, this velocity is simply referred to as vti~hereafter, but the reader should<br />

remember that Vgt <strong>for</strong> each field and in each cell is unique. The characteristic gravitational fall<br />

height <strong>for</strong> debris particles in cell i is L@t,i. Again, the i subscript will be dropped <strong>for</strong> notational<br />

convenience, but the reader should remember that Lqt <strong>for</strong> each cell can be unique.<br />

The terminal fall velocity, vg~,is computed using the following drag correlation <strong>for</strong> spheres:<br />

V.=[-cl+q=pk.-l<br />

(6-89)<br />

where g is the acceleration <strong>of</strong> gravity, p~ is the gas viscosity, p~is the gas density, d is the particle<br />

diameter, and p~is the debris material density.<br />

Note that Vx,is dependent upon both cell i and field n, through the gas density, gas viscosity, debris<br />

density, and particle diameter. The above correlation assumes that the particles are spheres, the<br />

atmosphere is stagnant, and that the particles do not physically interact with each other as they fall.<br />

The characteristic gravitational fall height, L@,by default, is calculated to be the cube root <strong>of</strong> the<br />

initial cell gas volume. A DCH-specific Lti~value can also be specified independent <strong>of</strong> the cell<br />

volume. This is done using the LENGFT keyword in the DCH-CELL input block.<br />

Rev O 638 6/30/97

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