Numerical Simulation of Coning Behavior of a Single Well in a Naturally Fractured Reservoir

1983 ◽  
Vol 23 (06) ◽  
pp. 879-884 ◽  
Author(s):  
Huan-Zhang Chen

Chen, Huan-Zhang; Scientific Research Inst. of Petroleum Exploration and Development Abstract The history matching and predicting of an actual well in a reservoir with double porosity is performed with a new coning simulation model that gives satisfactory results. A discussion of the parameters used for matching provides some insight into the structure and parameters of provides some insight into the structure and parameters of the reservoir. Other points discussed includebottomwater rising characteristics,a comparison between the dual porosity and the single porosity (assuming that the mass transfer between the fracture and matrix is equal to zero), andthe imbibition characteristics of matrix. Introduction The mathematical equations describing fluid flow in the dual-porosity medium were presented in the 1960's. Kazemi et al. obtained the numerical solution of this problem in 1976 but did not present the solution of problem in 1976 but did not present the solution of coning, and the flow terms of matrix in the equations were neglected. Since 1977, Wu Wan-yi of Beijing U. has done extensive research on this aspect. His work-the axially symmetric water coning problem-is based on a dual-porosity-medium model and equations presented by Barenblatt and Jeltov. All the terms that should appear in the equations are included-i.e., the fluid flow between the matrix blocks has not been neglected. The harmonic average value of mobility of fissure and matrix is used as the imbibition coefficient. All nonlinear coefficients are linearized, and the semi-implicit scheme is used in the difference equations. These equations are solved by the direct solution method. We performed a further study based on these works, using an improved program to give a good history matching with an actual program to give a good history matching with an actual well behavior. Our results are discussed in detail in this paper. This method may be used to solve the problems of paper. This method may be used to solve the problems of multidimensional, two-phase fluid flow. Model Structure The structure of the model is shown in Fig. 1. It is a cylinder, which represents a part of the reservoir controlled by the well. Its axis coincides with the axis of the well, and the radius of the cylinder represents the drainage radius of the well. The top and flank of this cylinder are impervious. The bottomwater is supplied from the lower surface of the cylinder, and the pressure on this surface is maintained at a constant value. The upper part of the cylinder is oil zone, the middle is transition zone, and the lower is water zone. The well may be perforated in both oil zone and water zone or in only one of the two zones. In any given depth, there may be a horizontal thin impervious break with a changeable radius. Fluid-Flow Equations Assume that the fluids are immiscible, and that both the medium and fluids are slightly compressible. In addition to the continuous flow in fracture and matrix, there is the mass transfer between the fracture and matrix. Under these assumptions, the flow of fluids satisfies the following equations. ..........................................(1) SPEJ p. 879

2015 ◽  
Vol 18 (02) ◽  
pp. 187-204 ◽  
Author(s):  
Fikri Kuchuk ◽  
Denis Biryukov

Summary Fractures are common features in many well-known reservoirs. Naturally fractured reservoirs include fractured igneous, metamorphic, and sedimentary rocks (matrix). Faults in many naturally fractured carbonate reservoirs often have high-permeability zones, and are connected to numerous fractures that have varying conductivities. Furthermore, in many naturally fractured reservoirs, faults and fractures can be discrete (rather than connected-network dual-porosity systems). In this paper, we investigate the pressure-transient behavior of continuously and discretely naturally fractured reservoirs with semianalytical solutions. These fractured reservoirs can contain periodically or arbitrarily distributed finite- and/or infinite-conductivity fractures with different lengths and orientations. Unlike the single-derivative shape of the Warren and Root (1963) model, fractured reservoirs exhibit diverse pressure behaviors as well as more than 10 flow regimes. There are seven important factors that dominate the pressure-transient test as well as flow-regime behaviors of fractured reservoirs: (1) fractures intersect the wellbore parallel to its axis, with a dipping angle of 90° (vertical fractures), including hydraulic fractures; (2) fractures intersect the wellbore with dipping angles from 0° to less than 90°; (3) fractures are in the vicinity of the wellbore; (4) fractures have extremely high or low fracture and fault conductivities; (5) fractures have various sizes and distributions; (6) fractures have high and low matrix block permeabilities; and (7) fractures are damaged (skin zone) as a result of drilling and completion operations and fluids. All flow regimes associated with these factors are shown for a number of continuously and discretely fractured reservoirs with different well and fracture configurations. For a few cases, these flow regimes were compared with those from the field data. We performed history matching of the pressure-transient data generated from our discretely and continuously fractured reservoir models with the Warren and Root (1963) dual-porosity-type models, and it is shown that they yield incorrect reservoir parameters.


Author(s):  
T. Salahuddin ◽  
Mair Khan ◽  
Fahad S. Al-Mubaddel ◽  
Mohammad Mahtab Alam ◽  
Irfan Ahmad

2021 ◽  
Vol 12 (1) ◽  
Author(s):  
Yanlu Xing ◽  
Joël Brugger ◽  
Barbara Etschmann ◽  
Andrew G. Tomkins ◽  
Andrew J. Frierdich ◽  
...  

AbstractReaction-induced porosity is a key factor enabling protracted fluid-rock interactions in the Earth’s crust, promoting large-scale mineralogical changes during diagenesis, metamorphism, and ore formation. Here, we show experimentally that the presence of trace amounts of dissolved cerium increases the porosity of hematite (Fe2O3) formed via fluid-induced, redox-independent replacement of magnetite (Fe3O4), thereby increasing the efficiency of coupled magnetite replacement, fluid flow, and element mass transfer. Cerium acts as a catalyst affecting the nucleation and growth of hematite by modifying the Fe2+(aq)/Fe3+(aq) ratio at the reaction interface. Our results demonstrate that trace elements can enhance fluid-mediated mineral replacement reactions, ultimately controlling the kinetics, texture, and composition of fluid-mineral systems. Applied to some of the world’s most valuable orebodies, these results provide new insights into how early formation of extensive magnetite alteration may have preconditioned these ore systems for later enhanced metal accumulation, contributing to their sizes and metal endowment.


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