Analysis of buildup data from the Initial Flow Test indicates that the MG-T/DOE Amoco Fee No. 1 Well penetrates a zone of relatively high permeability (approx. 150 md); this high permeability zone, however, extends to a radius of only about 200 ft from the wellbore. The far field permeability (i.e., for r > 200 ft) appears to be rather low (approx. 11 md). No reservoir boundaries can be identified from the Initial Flow Test. Tthe reservoir simulator MUSHRM together with the formation parameters inferred from the buildup data were employed to history match the observed drawdown/buildup pressures and flow data. ...
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Analysis of buildup data from the Initial Flow Test indicates that the MG-T/DOE Amoco Fee No. 1 Well penetrates a zone of relatively high permeability (approx. 150 md); this high permeability zone, however, extends to a radius of only about 200 ft from the wellbore. The far field permeability (i.e., for r > 200 ft) appears to be rather low (approx. 11 md). No reservoir boundaries can be identified from the Initial Flow Test. Tthe reservoir simulator MUSHRM together with the formation parameters inferred from the buildup data were employed to history match the observed drawdown/buildup pressures and flow data. The calculated buildup pressures closely agree with the measured values; the rather poor agreement between the measured and calculated drawdown pressures is ascribed to the uncertainties in the flow rate data.
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Garg, S.K.Analysis of initial flow data from MG-T/DOE Amoco Fee No. 1 Well,
report,
August 1, 1981;
United States.
(digital.library.unt.edu/ark:/67531/metadc1094713/:
accessed April 22, 2018),
University of North Texas Libraries, Digital Library, digital.library.unt.edu;
crediting UNT Libraries Government Documents Department.