Abstract:Most of porous naturally fractured reservoirs present a two-timescale flow-system, due to a two-scale heterogeneity which cannot be modelled explicitly, nor homogenised in reservoir simulation models. When the only flowing domain is the fracture network, and when the accumulation lies in porous and low permeable matrix blocks, the rate of exchanges between the two domains drives the recovery of such reservoirs. So called dual-porosity simulation models must incorporate an adequate transfer function between fra… Show more
“…The exchange of oil, gas, and water between the two domains is modeled by transfer func-tions (describing the physics of fluid exchange between fracture and matrix) and a shape factor (describing the geometry of the rock matrix). Much research has been dedicated to the appropriate use of transfer functions (Abushaikha and Gosselin 2008;Lu et al 2008;Al-Kobaisi et al 2009;Babadagli et al 2009;Balogun et al 2009;Ramirez et al 2009) and shape factors (Lim and Aziz 1995;Hassanzadeh and Pooladi-Darvish 2006;Rangel-German and Kovscek 2006;Gong et al 2008), whereas scaling groups have been developed to quantify the rate of oil recovery from matrix blocks and its dependence on rock and fluid properties (Ma et al 1997;Tavassoli et al 2005;Mason et al 2010;Schmid and Geiger 2012).…”
A major part of the world's remaining oil reserves is in fractured carbonate reservoirs, which are dual-porosity (fracture-matrix) or multiporosity (fracture/vug/matrix) in nature. Fractured reservoirs suffer from poor recovery, high water cut, and generally low performance. They are modeled commonly by use of a dual-porosity approach, which assumes that the high-permeability fractures are mobile and low-permeability matrix is immobile. A single transfer function models the rate at which hydrocarbons migrate from the matrix into the fractures. As shown in many numerical, laboratory, and field experiments, a wide range of transfer rates occurs between the immobile matrix and mobile fractures. These arise, for example, from the different sizes of matrix blocks (yielding a distribution of shape factors), different porosity types, or the inhomogeneous distribution of saturations in the matrix blocks. Thus, accurate models are needed that capture all the transfer rates between immobile matrix and mobile fracture domains, particularly to predict late-time recovery more reliably when the water cut is already high. In this work, we propose a novel multi-rate mass-transfer (MRMT) model for two-phase flow, which accounts for viscous-dominated flow in the fracture domain and capillary flow in the matrix domain. It extends the classical (i.e., singlerate) dual-porosity model to allow us to simulate the wide range of transfer rates occurring in naturally fractured multiporosity rocks. We demonstrate, by use of numerical simulations of waterflooding in naturally fractured rock masses at the gridblock scale, that our MRMT model matches the observed recovery curves more accurately compared with the classical dual-porosity model. We further discuss how our multi-rate dual-porosity model can be parameterized in a predictive manner and how the model could be used to complement traditional commercial reservoir-simulation workflows.
“…The exchange of oil, gas, and water between the two domains is modeled by transfer func-tions (describing the physics of fluid exchange between fracture and matrix) and a shape factor (describing the geometry of the rock matrix). Much research has been dedicated to the appropriate use of transfer functions (Abushaikha and Gosselin 2008;Lu et al 2008;Al-Kobaisi et al 2009;Babadagli et al 2009;Balogun et al 2009;Ramirez et al 2009) and shape factors (Lim and Aziz 1995;Hassanzadeh and Pooladi-Darvish 2006;Rangel-German and Kovscek 2006;Gong et al 2008), whereas scaling groups have been developed to quantify the rate of oil recovery from matrix blocks and its dependence on rock and fluid properties (Ma et al 1997;Tavassoli et al 2005;Mason et al 2010;Schmid and Geiger 2012).…”
A major part of the world's remaining oil reserves is in fractured carbonate reservoirs, which are dual-porosity (fracture-matrix) or multiporosity (fracture/vug/matrix) in nature. Fractured reservoirs suffer from poor recovery, high water cut, and generally low performance. They are modeled commonly by use of a dual-porosity approach, which assumes that the high-permeability fractures are mobile and low-permeability matrix is immobile. A single transfer function models the rate at which hydrocarbons migrate from the matrix into the fractures. As shown in many numerical, laboratory, and field experiments, a wide range of transfer rates occurs between the immobile matrix and mobile fractures. These arise, for example, from the different sizes of matrix blocks (yielding a distribution of shape factors), different porosity types, or the inhomogeneous distribution of saturations in the matrix blocks. Thus, accurate models are needed that capture all the transfer rates between immobile matrix and mobile fracture domains, particularly to predict late-time recovery more reliably when the water cut is already high. In this work, we propose a novel multi-rate mass-transfer (MRMT) model for two-phase flow, which accounts for viscous-dominated flow in the fracture domain and capillary flow in the matrix domain. It extends the classical (i.e., singlerate) dual-porosity model to allow us to simulate the wide range of transfer rates occurring in naturally fractured multiporosity rocks. We demonstrate, by use of numerical simulations of waterflooding in naturally fractured rock masses at the gridblock scale, that our MRMT model matches the observed recovery curves more accurately compared with the classical dual-porosity model. We further discuss how our multi-rate dual-porosity model can be parameterized in a predictive manner and how the model could be used to complement traditional commercial reservoir-simulation workflows.
“…Their dimensions and aperture size (width) affect the kinetics and the final recovery of hydrocarbon reservoirs [38]. In this test, we saw how the fracture width was numerically extended (artificial smearing) by the NCVFE method prompting a delay of flow in the fracture region.…”
We present a new control volume finite element method that improves the modelling of multi-phase fluid flow in highly heterogeneous and fractured reservoirs, called the Interface Control Volume Finite Element (ICVFE) method. The method drastically decreases the smearing effects in other CVFE methods, while being mass conservative and numerically consistent. The pressure is computed at the interfaces of elements, and the control volumes are constructed around them, instead of at the elements' vertices. This assures that a control volume straddles, at most, two elements, which decreases the fluid smearing between neighbouring elements when large variations in their material properties are present. Lowest order Raviart-Thomas vectorial basis functions are used for the pressure calculation and first-order Courant basis functions are used to compute fluxes. The method is a combination of Mixed Hybrid Finite Element (MHFE) and CVFE methods. Its accuracy and convergence are tested using three dimensional tetrahedron elements to represent heterogeneous reservoirs. Our new approach is shown to be more accurate than current CVFE methods.
“…Several transfer functions exist and are routinely applied in reservoir simulators (Kazemi et al 1976;Gilman & Kazemi 1983;Quandalle & Sabathier 1989). A major problem is that these transfer functions do not capture the actual physics seen in experiments or high-resolution simulations of fracture-matrix transfer (Abushaikha & Gosselin 2008;Lu et al 2008;Geiger et al 2013;Ahmed Elfeel et al 2013a, b). Not surprisingly, this fundamental shortcoming poses major difficulties in the history matching of fractured carbonate reservoirs.…”
The introduction reviews topics relevant to the fundamental controls on fluid flow in carbonate reservoirs and to the prediction of reservoir performance. The review provides research and industry contexts for papers in this volume only. A discussion of global context and frameworks emphasizes the value yet to be captured from compare and contrast studies. Multidisciplinary efforts highlight the importance of greater integration of sedimentology, diagenesis and structural geology. Developments in analytical and experimental methods, stimulated by advances in the materials sciences, support new insights into fundamental (pore-scale) processes in carbonate rocks. Subsurface imaging methods relevant to the delineation of heterogeneities in carbonates highlight techniques that serve to decrease the gap between seismically resolvable features and well-scale measurements. Methods to fuse geological information across scales are advancing through multiscale integration and proxies. A surge in computational power over the last two decades has been accompanied by developments in computational methods and algorithms. Developments related to visualization and data interaction support stronger geoscience-engineering collaborations. High-resolution and real-time monitoring of the subsurface are driving novel sensing capabilities and growing interest in data mining and analytics. Together, these offer an exciting opportunity to learn more about the fundamental fluid-flow processes in carbonate reservoirs at the interwell scale.
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