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AbstractOccurrence of bilinear flow regime in various geological situations has been discussed rather extensively in the literature. In particular, it was theoretically demonstrated that the bilinear flow regime can arise in the case of horizontal wells draining fractured reservoirs due to transient dual porosity behavior originating during the intermediate linear flow period. The bilinear flow regime can be identified by analysis of the well transient pressure response as the pressure derivative exhibits the characteristic quarter slope on the loglog diagnostic plot. However, the duration of the transient dual porosity behavior depends on the system geometry, namely location and length of the horizontal well and thickness of the producing layer, and on the permeability contrast which reportedly exists between the more conductive fractures and the feeding matrix. Three interesting case histories are presented in this paper where the pressure derivative response for horizontal wells drilled in different fractured reservoirs indicated the occurrence of the transient dual porosity behavior before that the linear flow, which is typical of horizontal wells in homogeneous reservoirs, was achieved. In agreement with the geological surveys it was interpreted that the bilinear flow was caused by two intersecting fracture systems showing a strong permeability contrast whereas the feeding action of the matrix, if any, could only be detected at a later time. In two cases clear evidence of pseudo steady state dual porosity behavior, indicated by the distinctive inflection in the derivative pressure response, was also observed, thus confirming the proposed well test interpretation. Several parametric analyses are also presented to define the geometrical and petrophysical conditions under which evidence of the bilinear flow regime can be expected.