Stallman[1956] proposed that numerical methods could be used to compute the transmissibility distribution in a heterogeneous but isotropic aquifer from potential data. This idea was further explored bySammel[1964] in work in which he attempted to apply Stallman's methods to electric analog models. Sammel tried to compute independently the known resistances of the model from observations of the potential distribution. His results were disappointing at best; he was not successful in reconstructing the resistance distribution.
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