Abstract
New methods for analyzing drawdown and buildup pressure data obtained at a well located in an infinite, pressure data obtained at a well located in an infinite, naturally fractured reservoir were presented recently. In this work, the analysis of both drawdown and buildup data in a bounded, naturally fractured reservoir is considered. For the bounded case, we show that five possible flow regimes may be exhibited by drawdown data. We delineate the conditions under which each of these five flow regimes exists and the information that can be obtained from each possible combination of flow regimes. Conditions under which semilog methods can be used to analyze buildup data are discussed for the bounded fractured reservoir case. New Matthews-Brons-Hazebroek (MBH) functions for computing the average reservoir pressure from buildup data are presented. pressure from buildup data are presented.
Introduction
This work considers the analysis of pressure data obtained at a well located at the center of a cylindrical, bounded, naturally fractured reservoir of uniform thickness. As is typical, a naturally fractured reservoir indicates a reservoir system in which the conductive properties of the rock are mainly due to the fracture system, and the rock matrix provides most of the storage capacity of the system. Several models of naturally fractured reservoirs have been presented m the literature. Warren and Root and Odeh presented m the literature. Warren and Root and Odeh assume "pseudosteady-state flow" in the matrix, whereas Kazemi, deSwaan, Najurieta, and Kucuk and Sawyers assume unsteady-state flow. The model used in this study is identical to the one considered in Refs. 4, 5, 7, and 8; however, these works considered only infinite-acting reservoirs. To our knowledge, the behavior of wells in bounded, naturally fractured reservoirs with unsteady-state flow in the matrix system has not been examined until now. This work considers the analysis of constant-rate production and buildup pressure data in a bounded, naturally production and buildup pressure data in a bounded, naturally fractured reservoir. For a bounded reservoir, we show that there are five distinct, useful flow regimes that may be exhibited by drawdown data. Flow Regimes 1, 2, and 11 are identical to the flow regimes identified in Refs. 7 and 8. During each of these three flow regimes, a semilog plot of the dimensionless wellbore pressure drop vs. plot of the dimensionless wellbore pressure drop vs. dimensionless time exhibits a straight line. The information that can be obtained from the various possible combinations of Flow Regimes 1 through 3 is discussed in Refs. 7 and 8. Flow Regime 5 corresponds to pseudo-steady-state flow. Flow Regime 4 denotes a flow pseudo-steady-state flow. Flow Regime 4 denotes a flow period during which a Cartesian graph of the dimensionless period during which a Cartesian graph of the dimensionless wellbore pressure drop vs. the square root of dimensionless time will be a straight line. In this work, we first establish the conditions under which each of the flow regimes exists. In particular, we show that Flow Regime 3 does not exist unless either the drainage radius or the dimensionless fracture transfer coefficient is large. Second, we show that useful information can be obtained from drawdown pressure data that reflect Flow Regime 4. Third, we delineate conditions that ensure that the methods of Refs. 7, and 8 can be used to analyze buildup data. Finally, we present new MBH functions for computing the average reservoir pressure in a naturally fractured reservoir.
Mathematical Model
We consider laminar flow of a slightly compressible, single-phase fluid of constant viscosity in an isotropic, cylindrical, naturally fractured reservoir of uniform thickness. Gravitational forces are negligible. The top, bottom, and outer reservoir boundaries are closed. A well located at the center of the cylinder is produced at a constant rate and then shut in to obtain buildup data. Initially, the pressure is uniform throughout the reservoir. We assume that all production is by way of the fracture system and that we have one-dimensional (ID), unsteady-state flow in the matrix. The matrix structure consists of "rectangular slabs"; that is, the matrix is divided by a set of parallel horizontal fractures. A schematic of the reservoir geometry is shown in Fig. 1. We consider an infinitesimally thin skin and neglect wellbore storage effects. The properties of both the matrix and fracture systems are assumed to be constant. Thus, our current model is identical to the one considered in Ref. 7 except that here the reservoir is assumed to be bounded. Because of symmetry, the mathematical problem can be formulated by considering only the repetitive element of Fig. 1.
SPEJ
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