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Original PCE mass in the source zone.
The gasoline mobility increased and it was redistributed in the source zone.
The developed models can accommodate any temporal variations of groundwater flux in the source zone.
It was estimated that at least 800 kg of TCE was present in the source zone.
Gasoline NAPL saturations in the soil increased two fold in the source zone.
Biotic dechlorination in the source zone area, however, caused cDCE to be the dominant dissolved-phase plume.
Partitioning tracer techniques are used to determine the pre and post treatment saturations in the source zone.
The prediction of the concentration in the plume requires a knowledge of the dissolution of NAPLs in the source zone.
An inverse modeling algorithm (PEST) was used to back-calculate the saturation distribution of DNAPL in the source zone.
These simulations use a friction angle of 10° in the source zone and 26° along the runout path (Table 1).
These factors result in errors in both locating and estimating volume of NAPL in the source zone.
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