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User's guide of Proceessing Modflow 5.0

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134 Processing <strong>Modflow</strong><br />

described below. Using these two options, you have the choice <strong>of</strong> specifying the initial<br />

concentration for the sorbed or immobile phase for each species. To do this, simple check Use<br />

the initial concentration for the sorbed or immobile phase <strong>of</strong> all species and specify the<br />

concentration value to Initial concentration for the sorbed phase or Initial concentration for<br />

the immobile phase in the Chemical Reaction (MT3DMS) dialog box.<br />

D b @ M ¯C<br />

Mt<br />

C & ¯ C<br />

K d<br />

' $ C & ¯C<br />

K d<br />

-1<br />

where $ [T ] is the first-order mass transfer rate between the dissolved and sorbed phases,<br />

-3<br />

D [ML ] is the bulk density <strong>of</strong> the porous medium, ¯C is the sorbed concentration and K<br />

' Db $ @ M ¯ C<br />

Mt<br />

¯C M ¯ If sufficient time is available for the system to reach equilibrium (for example, the flow<br />

velocity <strong>of</strong> groundwater is very slow), then there is no further change in and C/Mt'0 ,<br />

3.6.4 MT3DMS<br />

Fig. 3.50 The Chemical Reaction (MT3DMS) dialog box<br />

< First-order kinetic sorption: When the local equilibrium assumption is not valid, it is<br />

assumed in MT3DMS that sorption can be represented by a first-order reversible kinetic<br />

sorption described by<br />

(3.48)<br />

b d<br />

3 -1<br />

[L M ] is the distribution coefficient as defined previously in eq. 3.41.<br />

Eq. 3.48 can be rearranged in<br />

(3.49)<br />

so that eq. 3.49 is reduced to linear sorption (eq. 3.41). If the first-order mass transfer rate

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