Abstract
On the basis of a well-based model (Model I) developed in a previous work (Liu and Valkó in SPE J 2019. https://doi.org/10.2118/197049-PA), in which a fractional production decline model is developed based on anomalous diffusion to structurally account for the heterogeneity related to the complex fracture network, we incorporate two more components, i.e., the tempered anomalous diffusion and a source term, in the present work to develop a generalized model, namely Model II. Because of the two new components, Model II is capable of physically considering both the scale lower bound of heterogeneity and the influx from the matrix into the conductive fracture system. It consequently enables the new model to describe the complete sequence of regimes for the production of the slightly compressible single-phase fluid from the fractured unconventional reservoirs. Then, in the case studies, the synthetic data used in the previous work are better fitted to the new type curves in all observed periods, which demonstrates the advantage of Model II over Model I regarding the late-time flow regimes. In addition, the good fit of other sets of synthetic data to the Model II type curves exhibits the claimed capabilities of the new model and indicates the production of this type could be well characterized by seven parameters, i.e., \(\alpha\), \(c\), \({\lambda }_{\mathrm{D}}\), \(\omega\), \(\sigma\), \(\tau\), and \(\mathrm{EUR}\). Finally, the characteristics of Model II are further investigated by analyzing the effects of several parameters on the production performance, based on which some insights about the practice of developing unconventional reservoirs using massive hydraulic fracturing are provided.
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Abbreviations
- A cw :
-
Cross-section area perpendicular to the fracture flow in the models, \(\left[L\right]\)
- B :
-
Formation volume factor, dimensionless
- c :
-
Convergence term, dimensionless
- c t :
-
Total compressibility, \(\left[{M}^{-1}{L}^{1}{T}^{2}\right]\)
- EUR:
-
Estimated ultimate recovery, \(\left[{L}^{3}\right]\)
- h :
-
Formation thickness of the reference model, \(\left[L\right]\)
- h f :
-
Thickness of the problem domain, \(\left[L\right]\)
- I :
-
Source term due to the influx from the matrix, \(\left[{T}^{-1}\right]\)
- i u :
-
Flux normalized by the drawdown pressure, \(\left[{M}^{-1}{L}^{2}T\right]\)
- k :
-
Regular permeability, \(\left[{L}^{2}\right]\)
- k * :
-
Anomalous permeability of the fracture continuum, \(\left[{L}^{2}{T}^{1-\alpha }\right]\)
- k f :
-
Average permeability of the fracture network in convergence region, or permeability of the fracture continuum when \(\alpha =1.0\), \(\left[{L}^{2}\right]\)
- L :
-
Matrix length in the reference model, \(\left[L\right]\)
- L m :
-
Average effective size of the intact matrix surrounded by conductive fractures, \(\left[L\right]\)
- N p :
-
Number of effective perforations
- P :
-
Pressure, \(\left[M{L}^{-1}{T}^{-2}\right]\)
- ΔP c :
-
Extra pressure drop across the convergence region, \(\left[M{L}^{-1}{T}^{-2}\right]\)
- q :
-
Production rate, \(\left[{L}^{3}{T}^{-1}\right]\)
- q D * :
-
Dimensionless production rate in the reference model
- Q :
-
Cumulative production, \(\left[{L}^{3}\right]\)
- r c :
-
Radius of the hemisphere approximating the convergence region, \(\left[L\right]\)
- r p :
-
Radius of a typical perforation, \(\left[L\right]\)
- s :
-
Laplace variable associated with dimensionless time, dimensionless
- s′:
-
Laplace variable associated with dimensional time, \(\left[{T}^{-1}\right]\)
- s * :
-
Laplace variable associated with dimensionless time in the reference model, dimensionless
- s Ac :
-
Convergence skin factor in the reference model, dimensionless
- t :
-
Time, \(\left[T\right]\)
- t D * :
-
Dimensionless time in the reference model, \(\left[{L}^{3}{T}^{-1}\right]\)
- \(\overset{\lower0.5em\hbox{$\smash{\scriptscriptstyle\rightharpoonup}$}}{\upsilon }\) :
-
Volume flux, \(\left[L{T}^{-1}\right]\)
- x c :
-
Length of the convergence region/spacing between two consecutive perforation pair, \(\left[L\right]\)
- x e :
-
Model dimension along the horizontal well of the reference model, \(\left[L\right]\)
- y :
-
Coordinate in the fracture continuum, \(\left[L\right]\)
- y c :
-
Width of the convergence region, \(\left[L\right]\)
- y e :
-
Width of the area covering conductive fracture networks, \(\left[L\right]\)
- α :
-
Anomalous diffusivity exponent, dimensionless
- η :
-
Regular diffusivity coefficient, \(\left[{L}^{2}{T}^{-1}\right]\)
- η * :
-
Anomalous diffusivity coefficient, \(\left[{L}^{2}{T}^{-\alpha }\right]\)
- λ :
-
Tempering factor, \(\left[{T}^{-1}\right]\)
- λ Ac :
-
Interporosity flow coefficient, dimensionless
- μ :
-
Viscosity of the fluid, \(\left[M{L}^{-1}{T}^{-1}\right]\)
- ξ :
-
Coordinate in the matrix continuum, \(\left[L\right]\)
- σ :
-
Characteristic time ratio, dimensionless
- τ :
-
Time scale, \(\left[T\right]\)
- \(\phi\) :
-
Porosity, dimensionless
- ω :
-
Storativity ratio, dimensionless
- D :
-
Dimensionless
- f :
-
Fracture continuum
- i :
-
Initial condition
- m :
-
Matrix continuum
- sc :
-
Surface condition
- w :
-
Bottom-hole condition
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Acknowledgements
The authors gratefully acknowledge the assistance from Dr. Hongjie Xiong at University Lands for providing the reservoir simulation grids explicitly modeling conductive fracture networks. The datasets generated during and/or analyzed during the current study are available from the corresponding author on reasonable request.
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Appendices
Appendix 1: Derivation of the Hemispherical Steady State Flow
The extra pressure drop in the convergence region is modeled by the stabilized hemispherical Darcy’s flow of radius \({r}_{{\rm c}}\). The hemisphere is chopped by two parallel cross sections with radius of \({r}_{{\rm c}}\) and \({r}_{{\rm p}}\)(Fig. 3c). The coordinates shown in Fig. 3d are utilized to solve the problem.
In the coordinates, we assume constant pressure condition \(P={P}_{{\rm e}}\) at \(X=0\) and \(P={P}_{{\rm f}}\) at \(X=\sqrt{{r}_{{\rm c}}^{2}-{r}_{{\rm p}}^{2}}\). Given the condition of stabilized flow, the flow rate across an arbitrary intermediate cross section of \(X=x\) also keeps a constant of \({q}_{{\rm p}}\), as shown in Eq. (34):
After separating the variables in Eq. (34), Eq. (35) is obtained
Integrating both sides of Eq. (35) over the whole range, we can get Eq. (36):
Finally, the relationship between the extra pressure drop and the flow rate can be obtained as Eq. (37):
Appendix 2: Solution of the Boundary Value Problem in Laplace Space for the System of Model II
In this appendix, the solution of the system of Model II is obtained by solving the boundary value problem of Eq. (20).
Regarding the equations of the matrix continuum, the general solution of Eq. (20d) is
where \({C}_{1}\) and \({C}_{2}\) are the constants of integration with arbitrary values.
Taking the derivative of Eq. (38) with respect to \({\xi }_{{\rm D}}\), we can get
Substituting Eqs. (38) and (39) into the boundary conditions of the matrix continuum, i.e., Eqs. (20e) and (20f), the equations with respect to \({C}_{1}\) and \({C}_{2}\) are obtained, as shown in Eq. (40):
\({C}_{1}\)and \({C}_{2}\) are obtained as Eq. (41) from Eq. (40):
Substituting Eq. (41) into Eq. (39), we can get
Thus, the gradient at the interface is obtained by evaluating Eq. (42) at \({\xi }_{{\rm D}}=0\):
Then, substituting the expression in Eq. (43) into Eq. (20a) and rearranging the terms yield
Let \(f\left(\alpha ,{\lambda }_{{\rm D}},s\right)=\sqrt{{\left(s+{\lambda }_{{\rm D}}\right)}^{\alpha }-{{\lambda }_{{\rm D}}}^{\alpha }}\) and \(g\left(\omega , \sigma ,s\right)=\sqrt{\omega +\left(1-\omega \right)\mathrm{ tanh}\left(\sqrt{s/\sigma }\right)/\sqrt{s/\sigma }}\). Therefore, Eq. (44) can be written as Eq. (45):
With the same form as Eqs. (20d), (45) has the general solution as shown in Eq. (46):
where \({C}_{3}\) and \({C}_{4}\) are the another set of constants of integration with arbitrary.
Taking the derivative of Eq. (46) with respect to \({y}_{{\rm D}}\), we can get
Substituting Eqs. (46) and (47) into the boundary conditions of the fracture continuum, i.e., Eqs. (20b) and (20c), a system of equations with respect to \({C}_{3}\) and \({C}_{4}\) is obtained, as shown in Eq. (48):
By solving Eq. (48), \({C}_{3}\) and \({C}_{4}\) are expressed as Eq. (49)
Substituting Eq. (49) into Eq. (46), we can get
After doing some further simplifications to Eq. (50), finally we can obtain \(\widetilde{{P}_{{\rm fD}}}\) [Eq. (51)]:
Appendix 3: Derivation of the Relationship Between Rate and Pressure
In this appendix, the relationship between the production rate and the pressure in the setting of the tempered fractional diffusivity equation is derived to fill the gap between Eqs. (21) and (23) as well as (24).
Within the dimensional domain, the production rate is expressed as Eq. (52):
The factor 2 stands for the wellbore receiving production from both perforations for a typical perforation pair.
Performing Laplace transform on both sides of Eq. (52), we can get
according to the definition of the tempered fractional flux law in Eq. (10). \(s^{\prime}\) is the Laplace variable with respect to the dimensional time. Given the fact that Laplace transform is only performed with respect to the temporal coordinate, we have \(\widetilde{\frac{\partial {P}_{{\rm f}}}{\partial y}}=\frac{\partial \widetilde{{P}_{{\rm f}}}}{\partial y}\). Therefore,
Due to the zero Neumann boundary condition on the other boundary of the problem domain [Eq. (13c)], Eq. (54) could be rewritten as Eq. (55):
Applying the fundamental theorem of calculus to Eq. (55), we can get
After substituting the dimensionless groups into Eq. (56), the corresponding dimensionless form is obtained;
where \(s\) is the Laplace variable associated with the dimensionless time.
Then, substituting Eq. (44) into Eq. (57), we can get
which is the relationship we need for obtaining Eq. (24) from Eq. (21).
Additionally, with the relationship between production rate and cumulative production, we have
Hence, in Laplace space Eq. (59) would be written as Eq. (60):
Then, in dimensionless form, we have
after substituting Eq. (58) for \(\widetilde{{q}_{{\rm D}}}\). Equation (61) is the expression we need for obtaining Eq. (23) from Eq. (21).
Appendix 4: Equivalence Between the Proposed and the Reference Models
According to Eq. (32), the proposed and the reference models have different time scales, which would lead to some factors between their respective Laplace variables as well as the functions in Laplace space. At first, these factors will be derived. For simplicity, we denote the group \({y}_{{\rm e}}^{2}/{A}_{{\rm cw}}\) in Eq. (32) as \(C\).
Regarding a function \(F\) with respect to \({t}_{{\rm D}}\), its Laplace transform could be performed by
If we denote the Laplace variable with respect to \({t}_{{\rm D}}^{*}\) as \({s}^{*}\), then from Eq. (62) we get
Next substituting \(\left(\alpha , {\lambda }_{{\rm D}}, c\right)=\left(1.0, 0.0, 0.0\right)\) into Eq. (24), we could get
In the current scenario, Eq. (18 g) has the form of Eq. (66):
The definition of the interporosity flow coefficient \({\lambda }_{{\rm Ac}}\) in the reference model (Bello and Wattenbarger 2010) is
Combining Eq. (66) and (67), the relationship between the classic interporosity flow coefficient and the proposed characteristic time ratio is
By Eq. (68) and (63), we know that
After substituting Eq. (69), the argument of function \(\mathrm{coth}\) in Eq. (65) becomes
According to Eq. (2) in Bello and Wattenbarger (2010), Eq. (70) is directly related to the function \(f\) of the reference model as in Eq. (71):
Thus, Eq. (65) becomes
Then, we could observe that the right-hand side of Eq. (72) includes the rate solution of the reference model [Eq. (2A) in Bello and Wattenbarger (2010)]. Hence, we obtain
According to Eq. (64), we could use a single Laplace variable on both sides in Eq. (73):
Finally, we get
or in physical space,
Consequently, we get back to the dimensionless-rate relationship [Eq. (31)] by the derivation involving the rate solutions of both models, which proves the equivalence between Eq. (24) with \(\left(\alpha , {\lambda }_{{\rm D}}, c\right)=\left(1.0, 0.0, 0.0\right)\) and Eq. (2A) in Bello and Wattenbarger (2010).
Bello (2009) extends the above reference rate solution to account for convergence skin. After a bit reorganization, Eq. (6.18) in Bello (2009) could be written as
Based on the previous equivalence, it is straightforward to obtain that Eq. (77) is equivalent to Eq. (24) with \(\left(\alpha , {\lambda }_{{\rm D}}\right)=\left(1.0, 0.0\right)\) if we take \({s}_{{\rm Ac}}=c\). That is, even though the formulas of convergence skin factor are different due to the different assumptions of the fracture continuum shape, this factor has exactly the same effect in both the proposed and reference models.
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Liu, S., Valkó, P.P. A Fractional Decline Model Accounting for Complete Sequence of Regimes for Production from Fractured Unconventional Reservoirs. Transp Porous Med 136, 369–410 (2021). https://doi.org/10.1007/s11242-020-01516-8
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DOI: https://doi.org/10.1007/s11242-020-01516-8