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7.7 Conclusion<br />

. . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . .<br />

network model and optimize the solution <strong>of</strong> non-equilibrium model to these<br />

BTCs. Our results (Figure 7.9) show that the chemical non-equilibrium model<br />

accurately fits the BTCs obtained from the pore network model, resulting in a<br />

better fit compared to that obtained via the ADE model. Figure (7.9) shows<br />

an example <strong>of</strong> fitting the analytical solution <strong>of</strong> the nonequilibrium model to the<br />

BTC obtained from the pore network. In this case, we estimated the dispersion<br />

coefficient independently using the BTC <strong>of</strong> a conservative (non adsorptive)<br />

solute. This value for the dispersion coefficient was then used for adsorptive<br />

solute (under the same saturation) and only the adsorptive parameters were<br />

estimated.<br />

Co oncentration [‐]<br />

1<br />

0.1<br />

0.01<br />

Network model<br />

0.001<br />

Nonequilibrium model<br />

0.0 50.0 100.0<br />

Time [min]<br />

150.0<br />

Figure 7.9: The resulting BTC from the network together with the fitted<br />

BTC using the Nonequilibrium model. The BTC belong to a pore network with<br />

a pore scale adsorption distribution coefficient <strong>of</strong> 1.0 and saturation <strong>of</strong> 0.53.<br />

Compared with the ADE model, the non-equilibrium model provides a more<br />

appropriate model for the tailing behavior <strong>of</strong> the BTCs under different saturations.<br />

7.7 Conclusion<br />

Multi-phase and (partially-) saturated reactive/adsorptive transport in porous<br />

media is characterized by means <strong>of</strong> several macroscopic transport properties<br />

including: relative permeability; capillary pressure; unsaturated dispersivity;<br />

and upscaled reactive/adsorptive transport parameters. These properties have<br />

been found to depend on macro-scale parameters such as average saturation<br />

but also on pore-scale properties. Indeed, the state <strong>of</strong> fluid distribution within<br />

175

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