The present application is a U.S. National Stage patent application of International Patent Application No. PCT/US2012/040023, filed on May 30, 2012, the benefit of which is claimed and the disclosure of which is incorporated herein by reference in its entirety.
The present invention relates to oil and gas production using computerized simulation of oil or gas reservoirs and of production facilities.
Design of production facilities involves choice of wellbore locations and injected chemicals, well shapes and dimensions, pipe and pump networks, drilling schedules, production schedules, etc. The optimal choices of these and other parameters depend on physical properties of reservoir 110 such as pressures, saturations, porosities, and possibly others. Such choices are facilitated by computer simulation that simulates production for existing or hypothetical production facilities and production schedules. A suitable computer system 204 (
A discrete model of reservoir 110 and the production facilities is created by computer 204 in memory 220 for use by simulation program 240 as illustrated in
A coordinate system (XYZ) is chosen to represent various locations. A time axis 304 with time points t1, t2, t3 . . . is defined in computer 204.
A set of equations is chosen to model the oil or gas field, including hydraulics equations between nodes in the wells, wellbores, and the surface network; Darcy and non-Darcy flow between cells 320; perforation equations between cells 320 and nodes 325; fluid component mass balance equations for nodes and cells; constraint equations, and possibly others. See U.S. Pat. No. 7,668,707 issued Feb. 23, 2010 to Watts, III et al., incorporated herein by reference. The equations may include differential equations, and the differential equations are discretized using known techniques. The equations can be symbolically written as:
F(Vari,j,k,l)=0 (1)
where Vari,j,k,l represents pressures, flow rates, or other variables at the nodes and connections at different times. The subscript “i” represents the time point ti on axis 304, and the subscripts j, k, l represent X, Y, and Z values respectively. The values Vari,j,k,l are treated as independent variables.
Since some physical parameters can be expressed through others, there is some latitude as to which parameters are chosen as the independent variables (primary variables) in equations (1). Further, the equations (1) depend on the discretization method, and in particular on whether any particular Var value is measured at a cell 320 or a node 324 or 325, or a segment 330 or 331. Such choices will affect how efficiently the computer can solve the equations. The term “efficiently” relates to minimal use of the computer resources, and particularly the processor and memory. It is desirable to reduce the execution time and memory amount needed to solve the equations while providing a solution that serves as a good approximation to the real world.
There can be millions of different locations and time points, so the equation (1) may represent millions or billions of scalar equations. In a typical procedure, the equations (1) are solved for each of consecutive times ti, i.e. for time t1, then for time t2, and so on. The solution for time t1 depends on the test measurements stored as shown at 230 in
Equations (1) are typically non-linear, and for each time ti these equations can be solved approximately using the Newton-Raphson method illustrated in
F(x)=0
Suppose xn is a current iterative solution in the Newton-Raphson method. Then the next iteration xn+1 is obtained as follows. The Jacobian matrix JF(xn) is calculated; this is the matrix of partial derivatives of F(x) evaluated at the current iteration xn. Then the following linear equation is solved for xn+1:
JF(xn)(xn+1−xn)=−F(xn)
This equation can be alternatively written as:
JF(xn)(xn+1)=JF(xn)(xn)−F(xn) (2)
or
F′L(xn+1)=b (3)
where F′L=JF, and b is the constant equal to the right-hand side of equation (3).
This process is illustrated in
The initial iterated values Var.NT is chosen at step 410, and this can be any desired values, e.g. the values Vari−1,j,k,l found in the previous iteration i−1 if i>1, or to some values obtained from the initial measurements 230 if i=1.
At step 414, the matrix JF(Var.NT) and the value
b=JF(Var.NT)Var.NT−F(Var.NT)
are determined for the equations (2)-(3). At step 418, these equations are solved, i.e. the following equation is solved:
F′L(Varj,k,l)=b (4)
Let us denote the solution as Var*j,k,l. If this is the last iteration, then the solution Var*j,k,l is taken as the solution of (1), i.e. the method of
Equations (4) may include billions of equations with billions of individual variables shown collectively as Varj,k,l. Therefore, computer system 240 solves equations (4) approximately. An exemplary approximate method is a Schwarz method illustrated in
f(x)=b (4′)
The function f represents many scalar linear functions, and the variable x represents just as many scalar components. The Schwarz method will be illustrated on the example in which each of x and f has 1000 scalar components, denoted as x1, x2, . . . , x1000 for x, and denoted as f1, f2, . . . , f1000 for f.
At step 610, the values x1, . . . , x1000 are divided into two overlapping groups of values (more than two groups can also be used). In the example discussed below, the two groups are:
G1: x1, . . . , x600
G2: x400, . . . x1000
Also, the scalar functions f1, . . . , f1000 are divided into two overlapping groups, with the same number of functions in each group as there are values in G1, G2. For example, the two groups of functions can be:
G1′: f1, . . . , f600
G2′: f400, . . . , f1000
We will use the notation G1′(x) to denote the values f1(x) through f600(x); the notation G2′(x) will denote the values f400(x) through f1000(x).
The Schwarz method is an iterative method, and the iterative solution will be denoted as x.sc. The value x.sc output by the Schwarz method is the solution x.
At step 620, the initial iterative value x.sc is determined using any suitable technique. For example, x.sc can be set to the value of Var.NT at step 418 of the current Newton-Raphson iteration of
At steps 630-640, the next iterated value is determined for x.sc as follows.
At step 630, the x values from G1\G2, i.e. the values x601 through x1000, are set to the corresponding values of the current iterative value x.sc, and the following equation is solved for x1 through x600:
G1′(x)=b1 (5)
where b1 is the “b” portion corresponding to G1′. In other words, the following equation is solved:
G1′(x1, . . . , x600, x.sc601, . . . , x.sc1000)=b1 (5′)
The solution will be denoted x1*, . . . , x600*.
The values x1* through x399* will be used as the corresponding values of the next iterative value of x.sc as explained below.
At step 640, the following equation is solved for x400* through x1000*:
G2′(x)=b2 (6)
where b2 is the b portion corresponding to G2. In this equation, the values x1, . . . , x399 are constant. In the additive Schwarz method, these values are set to the corresponding values of the current iterative value x.sc. In the multiplicative Schwarz method, these values are set to the corresponding values x1*, . . . , x399* found at step 630. The solution of (6) will be denoted x600*, . . . , x1000*. The values x1* through x1000* will be collectively denoted as x*.
If this is the last iteration, then x*can be taken as the solution of (4′), i.e. as the value Var*j,k,l at step 418. See step 650. If other iterations are desired (step 660), then the solution x* is used as the next iterated value of x.sc, and steps 630-640 are repeated. Any number of iterations can be used to obtain better and better approximations of the solution of (4′).
In some variations of the Schwarz method, iterations other than the first iteration are solved for the residual b−f(x) rather than x. The residual is updated at each iteration. In particular, the overlap values x400*, . . . , x600* found at step 630 are used to update the residual for step 640.
In a variation, the components x400*, . . . , x600* of x* are obtained for step 650 by combining the corresponding values obtained at steps 630 and 640, i.e. by combining the corresponding components of solutions of equations (5) and (6) so as to minimize the residual's norm ∥b−f(x*)∥. A known method for combining these components is GMRES (Generalized Minimum Residual method).
Clearly, the computational complexity of solving the equations (1) depends on the choice of variables Var and the groups G1, G2, G1′, G2′. Generally, the reservoirs are quite different from wells with respect to the physics models, so the reservoirs and the wells are usually in different groups. More particularly, each group G1, G2 can be defined through cells 320 or nodes 324 or 325: each group consists of variables pertaining to a group of cells 320 or nodes 324 or 325 or the related segments 330 or 331, and each function group G1′, G2′ consists of the equations for the corresponding cells and nodes. Thus, the reservoir cells can be placed in group G1 (i.e. in the node group defining G1), the wells in group G2, and the perforation cells 320 (the cells with perforations) and wellbore nodes 325 can be the overlap between G1 and G2. This scheme is used in NEXUS® Reservoir Simulation Software system available from Halliburton of Houston, Tex. In NEXUS®, the variables Var are pressures and component compositions at nodes 324 and 325, and pressures and component masses in the cells 320.
Background information can also be found in the following publications incorporated herein by reference (no representation is being made as to whether or not these publications are prior art relative to the present disclosure):
This section summarizes some features of the invention. Other features may be described in the subsequent sections. The invention is defined by the appended claims, which are incorporated into this section by reference.
The inventors have observed that it may be desirable to include the wells 120W in the overlap to obtain a better coupling between the reservoir and the surface network. In some embodiments however, the “perforation” cells 320 (i.e. the cells with perforations 134) are removed from the overlap. Smaller overlap reduces the computational complexity. Other embodiments include the perforation cells in the overlap.
According to another aspect of the invention, the equations for the well and wellbore nodes are processed to eliminate some non-pressure variables. Therefore, when these variables are treated explicitly, the error caused by the explicit treatment is reduced, so the pressure solution is more accurate. In many cases, the accuracy of the pressure solution across the reservoir and surface network determines the performance of the global linear solver for equations (4), i.e. determines the ability to get an accurate solution for all the variables at a minimum computational cost.
The invention is not limited to the features and advantages described above except as defined by the appended claims.
The embodiments described in this section illustrate but do not limit the invention. The invention is defined by the appended claims.
Some embodiments of the present invention will now be described on the example of the multiplicative Schwarz method as in
In oil and gas simulation, one type of such methods is IMPES (implicit pressure explicit saturation): to solve the equations (1) for each time ti given the solution at time ti−1 (where t0 means the initial values), the non-pressure variables are set to their ti−1 values, and the equations are solved to find the ti values of the pressures; then the pressures are set to their ti values, and the equations are solved to find the ti values of the non-pressure variables. Some of these and other methods are described in the following publications incorporated herein by reference:
Other such techniques include CPR (Constrained Pressure Residual).
Some embodiments are compatible with AIM (Adaptive Implicit Method), and others described in the documents cited immediately above. Some embodiments are also compatible with FIM (Fully Implicit Method), i.e. when all the variables are treated implicitly (none are replaced by constants) except for the Schwarz method at the stage of
Now some multiplicative Schwarz embodiments will be described with just two groups of variables, G1 and G2, for the models illustrated in
The global linear system (4) is, in matrix form:
Here the subscripts r, w, f denote the reservoir, well, and surface network 130 respectively. For subscript r, the reservoir includes the cells with perforations 134. The vector [br, bw, bf] on the right hand side (RHS) is the same as b in equation (4). The vector [xr, xw, xf] is the same as Varj,k,l.
In the matrix on the left, the rows with Arr correspond to the reservoir portion of equations (4), including the perforation cells 320. The rows with Awr correspond to the well equations, which include equations for flow from each perforated grid block 320 to the corresponding wellbore node 325. The rows with Afw correspond to the facilities equations. The columns with Arr correspond to the reservoir variables (including the perforation grid blocks 320). The columns with Arw correspond to the well variables. The columns with Awf correspond to the facilities variables. The blank entries in the matrix are zeroes.
The G1 group consists of variables xr, xw, and the G1′ equations can be written as:
These equations are obtained by setting xf to constant values as described above. The bw values in (8) are not necessarily the same as in (7).
The G2 group consists of variables xw, xf, and the G2′ equations can be written as:
The b values in (9) are not necessarily the same as in (7).
System (9) might not exist if the surface network 130 is absent or is not being simulated. If the surface network exists in the simulation system, the system (9) can be solved using known techniques, e.g. a sparse direct solver or ILU (Incomplete Lower/Upper) type iterative solver. We focus on the solution of system (8), which is more complicated in some embodiments.
For FIM, we need to construct the CPR pressure equation on the reservoir. For FIM and IMPES, an approximated pressure matrix for wellbore nodes needs to be constructed since an implicit well modeling is used in both formulations.
The model 690 includes a multisegment well which splits into two segments at node 324.1. In each segment, the respective bottom-hole node 324BH is connected to the respective wellbore node 325 connected to perforation cells 320. Above the common node 324.1, there are two other nodes 324.2 and 324.3. Node 324.3 is connected to surface network 130. The models of
Model 694 (gridded well model, i.e. with multiple nodes 325) contains three perforation nodes 325, marked as nodes 1, 2, 3 from the bottom. Node 3 is connected to bottom-hole node 4 (marked as 324BH). Each of nodes 1, 2, 3 is connected to a respective perforation cells 320. Node 324BH is connected to surface network 130.
The global matrix for implicit formulation (FIM) for model 694 is shown in
The pressure drop across the connection between an upstream node and the next downstream node (e.g. from node 1 to node 2 in model 680) can be determined by a hydraulics equation as follows:
R=Pup−Pdw−f(q1, q2, . . . qnc, Pup, Pdw) (e4)
Here the subscripts up and dw represent the upstream and downstream nodes (e.g. 1 and 2 in model 680) at a flow connection 330 or 331;
We define the composition of component k as
where qT is the total mass flow rate through the connection (i.e. the sum of qk). (The x notation for the compositions should not be confused with the x symbol in equations (7), (8) and (9)).
Thus,
Combining the equations (e6) and (e7) yields
Differentiating equation (e6) gives
dqk=qTdxk+xkdqT (e9)
Plugging equations (e8) and (e9) into equation (e4) yields
So the Jacobian derivatives (partial derivatives) with respect to the primary unknowns are
Of note, the letter R herein corresponds to F in equations (1). The same symbol R is used for different scalar equations (1).
are zero. This is true if f is treated explicitly (i.e. replaced with a value from the previous iteration), but can be true in case of implicitly treated f. Some derivatives (e13), (e14) are shown as h and ε symbols.
A pressure constraint may be applied to the bottom-hole node:
R=P−Pspec=0 (e15)
where Pspec is a predefined constant. Alternatively, a phase flow rate constraint can be activate at a connection, i.e.:
Here np is the number of phases (in many applications, there are three phases: gas, oil, and water). For each phase n, Qn is the corresponding volume flow rate; an is the corresponding predefined constant. Qspec is the maximum allowed volume flow rate that can flow in the connection.
Alternatively, the following constraint can be specified:
Plugging equations (e8) and (e9) into equation (e17) yields
Usually the rate constraint is specified at surface condition, so the pressure derivative term can be dropped, but it is shown herein for a more general case. The Jacobian derivatives with respect to the primary unknowns are obtained as follows:
The above equations are obtained by considering the flow through a connection 330.
For each node 324 and 325, mass balance equations are used. In particular (see for example nodes 2 and 3 of model 694), for each wellbore node, the total mass flow rate of each component into the node is equal to the sum of the mass flow rates of the same component from each incoming connection and each perforation. Each of these nodes may or may not have perforations, and let perf denote the number of perforations at an exemplary node “r”. The node r may have multiple incoming connections. Let “inc” denote the number of incoming connections 330; “out” denote the number of outgoing connections. The fluid flows into the node through perforations and connections, so the total mass flow rate into the node is:
where qTjr is the total mass flow rate from connection j into node r, and qpkr is the mass flow rate of component k from perforation p into the node.
Let xijr denote the composition of component i in the incoming flow into a node r through connection j; and let xir be the composition of component i in the total incoming flow into node r. For a component i, the component's mass flow rate out of the node is:
The incoming mass flow rate for component i is:
The mass balance equation for component i is then
and the corresponding Jacobian derivatives are
The equations (1) will include the mass balance equations for the components i=1, . . . , nc−1.
The example of
The other node is a bottom-hole node 2, corresponding to the last three rows. The corresponding variables are qT2 (total mass flow rate out of node 2), x21 (composition of component 1 at node 2), x22 (composition component 2 at node 2).
The mass balance equation may be simpler if there is only one incoming connection and one outgoing connection and the node has no perforations; the equation becomes:
R=xup−xdw=0 (e26)
where xup is the composition of component i at the upstream node of the incoming connection into node r, and xdw is the composition of component i at the node r. See the rows marked with (e26) near the bottom of
The total mass balance equation equates the incoming and outgoing mass flow rates at each node r as follows:
where qTlr is the total mass flow rate from the node r into outgoing connection l. The derivatives are
The mass transfer between a cell 320 with a perforation 134 and a wellbore node 325 is governed by the perforation equation as follows (here we assume that the perforations are producing, not injecting; the index r identifies the reservoir's cell 320 adjacent to the perforation):
Here qk is the mass flow rate from perforation p (cell 320) into node 325; C is a user defined constant; λnr is the mobility of phase n in perforation cell 320 identified by index r; ρnr is the density of phase n in the same cell; zknr is the mass fraction of component k in phase n in the cell; Pr is the pressure in the same cell; Pw is the pressure at node 325; Dr and Dw are the depths of cell 320 and node 325 respectively; and γr is the hydrostatic pressure gradient, so that the product γr(Dw−Dr) represents the difference in pressure due to the fluid head.
For the first three rows of
The primary variables are:
1. In the network domain (i.e. in wells, and thus in the overlap between G1 and G2, and possibly in the surface network and thus in group G2):
2. In the reservoir domain (i.e. in the reservoir cells 320, thus in group G1):
3. At the interface between these two domains (at perforation nodes 325, thus in group G1):
In equation (8):
In the following example illustrating a solution of equations (8) for the well model 680, we will show how to eliminate qT and qpk, and how to reduce the resulting linear system, in which the primary variables are xi, P in the network domain and mi, P in the reservoir domain, to a pressure only system. This example includes a single phase with three components. The Newton-Raphson Jacobian matrix at the network side is shown in
of equation (8). In equation (e4), the function f is treated explicitly (its value is the value obtained in the previous iteration, or is an initial value if this is the first iteration) so its derivatives are zero. The flow rates qpk at perforation connections and total flow rates qTk at all other network connections are eliminated as shown in
In
The c values in the first three columns in the (e31) rows in
The values T1, T2, T3 are:
where k=1, 2, 3. See equation (e31); the r index is omitted for simplicity.
The variable qT1 is the mass flow rate on the connection between nodes 1 and 2 (i.e. nodes 320 and 324BH) in model 680. The variable qT2 is the mass flow rate from node 2. The variables xij are compositions at different nodes; the first index, i, is the component number, and the second index is the node number. Thus, x12 is the composition of component 1 at node 2. The component number nc=3, and the primary variables include the compositions for the first two components only.
In the row for equation (e4), the values ε, h11, h21 depend on the function f in the equation. Suitable equations are well known. Of note, f can be treated implicitly or explicitly.
As noted above, np=1. The variables P1 and P2 are pressures at nodes 1 and 2 respectively.
In the row (e17), the constraint equation can be for node 2. In this case, xk indicates xk2, and qk are given by equation (e6), i.e. qk=xk2qT2. The volume flow rates Qn are on the connection from node 2 to the surface network. As noted above,
Of note, the columns x12, x22 (node 2 compositions) have zero entries in the mass balance rows (e21), (e21), (e27) for node 1. However, the columns x11, x21 (node 1 compositions) have some non-zero entries in the mass balance rows (three last rows (e26), (e26), (e27)) for node 2. It is desirable to eliminate these non-zero entries to construct a pressure matrix from the mass balance equations.
In
−ΣpperfΣkncqpk
Now the columns for node 1 compositions x11, x21 have zero entries for node 2 (in the last three rows). The columns for node 2 compositions x12, x22 retain zero entries for node 1 (in the first three rows).
At the reference node 2 (324BH), the composition terms only remain at the diagonal block as shown below:
We can eliminate the nonzero composition terms in the last row by left-multiplying the last three rows by the matrix
This means that the component mass balance equations (26) for node 2 are added to the total mass balance equation (27) for node 2 with respective factors ω1 and ω2 to eliminate the node-2 component terms xi2 and ω2 in the total mass balance equation. The node-1 component terms remain zero.
The resulting matrix is shown in
With regard to the embodiment of
Next we explain the physical meaning behind this pressure matrix. For an oil rate constraint in a black-oil system
a1=1, a2=0, a3=0
The denominator in equations (e36) and (e37) can be rewritten as
and the multipliers in equations (e36) and (e37) can be simplified as
Plugging equations (e39) and (e40) into the last row in
See equation (e31); the r index is omitted for simplicity.
It is evident that the pressure coefficient (P1 coefficient) is the sum of mobility of each component weighted by its contribution in the total oil phase flow rate, which is consistent with a simple well model. The only difference is that the pressure matrix is scaled by the constant −qT/Q1.
The coupling matrix between the reservoir and the well (the left three columns in the bottom row of
As can be seen in this example in
in equation (8)) after elimination of the total flow rates qTk and the perforation connection flow rates qpTi (i.e. at the stage of
The columns P1, P2, P3 in the left half denote pressures in the corresponding perforation cells 320. The same symbols in the right half refer to pressures at the respective nodes 325.
=(x1j−1)T1j+x1jT2j+x1jT3j
=x2jT2j+(x2j−1)T2j+x2jT3j
{tilde over (T)}j=−T1j−T2j−T3j
where j is the perforation index, and T is calculated using equation (e42).
In
columns, the terms
remain which are similar to each other. In these terms, the values h, ε are the hydraulics derivatives with respect to the composition and total flow rate, and are calculated using equations (e13) and (e14), respectively. Δx is the difference in component mass composition between a node and its upstream node. As in the lumped well model, if the pressure gradient is treated explicitly, i.e. the function f in equation (e4) is evaluated using results from the previous iteration, all those derivatives are zeroes, so all the composition columns in
In the previous two examples, if the function f in hydraulics equation (e4) is treated explicitly or the pressure gradient is taken constant, we should have
where ref denotes the reference node. We can apply the same approach to the coupling terms from the reservoir to the well side, and move those terms
to the column corresponding to the reference node, as shown in
for producing perforations. At the wellbore side, the mass coupling terms
can be eliminated using the reduced mass balance equations at the reservoir side, and new coupling terms between network and reservoir are introduced, as shown in
More particularly,
The coefficient matrix, which is derived from mass balance equations (MBEs), at the reservoir side can be reduced to a pressure only matrix, shown in
Prr=RArrP (e46)
where the prolongation matrix P and the restriction matrix R are defined as follows:
The restriction matrix R is a diagonal matrix as follows
where L is the lower matrix of an LDU factorization of the diagonal sub matrix Arr, i.e.
We finally get a global pressure linear system including reservoir and wells, as shown in
Due to the Jacobian processing described above, the approximation errors in generating the approximate solutions by Newton-Raphson or other methods are hopefully reduced, which may lead to a better pressure solution and hence a better overall solution of equation (7).
In the previous two examples, we assume there is a rate constraint at the well connection. When it is a pressure constraint, as shown in equation (e15), or there is no constraints at all (a constraint might be at the top of the surface network), the method to construct the pressure matrix is similar and simpler. The multipliers defined in equations (e33) and (e34) are all zeroes.
The Jacobian conditioning described above can be used in many simulation schemes. One example is illustrated in
The mass balance equations include, for each node in the set, equations for individual components and/or equations for total mass balance. Perforation equations may also be present.
The equations (1) are then solved for each time period ti by the Newton-Raphson method as follows. At step 410 (same as in
JF(Var.NT)Varj,k,l=b (e50A)
At step 1820, the Jacobian is processed to eliminate some non-pressure coefficients by combining the mass balance equations in each set of nodes, and possibly combining different columns, as illustrated above in connection with
JM(VarM.NT)VarMj,k,l=bM (e50B)
At step 418 (as in
At step 1824, the original variables' values Var*j,k,l are obtained from VarM*j,k,l. The values Var*j,k,l are thus a solution of equation (e50A), and this solution is used as the next iterative value for Var.NT, and control returns to step 414, or alternatively the Newton-Raphson method is stopped (steps 422, 426 are as in
Many variations are possible. For example, the modified Jacobian computation steps 414, 1820 can be performed in generalized form, without plugging in the value Var.NT, as in fact is illustrated in
At step 1920, the total mass flow variables qT are eliminated (as in
At step 1930, within each set of nodes, the mass balance equations for the non-reference nodes are added to the corresponding mass balance equations for the reference node. In particular, the mass balance equations for each component k are added to the reference node's mass balance equation for the same component k; the total mass balance equations (for the total flow through each non-reference node) are added to the reference node's total mass balance equation. The equations may have to be multiplied by some factors before the addition. The factors depend on the equations (1) and the choice of primary variables. The addition is performed so as to eliminate the off-diagonal mass flow variables (e.g. compositions) in the reference node's mass balance equations.
At step 1940, the reference node's MB (mass balance) equations are combined to eliminate the diagonal compositions in the reference node's MB equations. This operation can be expressed as left-multiplying the reference node's MB equations by the matrix L−1 where L is the lower matrix in the LU (lower-upper) factorization of the square matrix corresponding to the diagonal pressure and composition portion of the reference node's MB equations. An example of the L−1 matrix is described above in connection with equations (e33), (e34), i.e. the matrix:
At step 1950, the pressure columns may be combined as explained above in connection with equations (e44), (e45).
In some embodiments, some of these operations are omitted. For example, step 1950 and/or 1940 can be omitted.
As noted above, there are many ways to solve the modified Jacobian equation at step 418 in
Pre-Iteration
1) Initialize xr=0
2) Solve equation (9), i.e.
to determine xw and xf.
3) Update residual in equation (8):
Schwarz Iteration, by k, until Convergence
1) Solve equation (8) using a CPR method (Constrained Pressure Residual) using the pressure matrix (e46) as explained below.
2) Update residual in equation (9):
3) Solve equation (9), i.e.
4) Update residual in equation (8)
5) Compute the solution change δxr=δxr+Pδur where P is as in (e47). Compute the residual change δbr=brk+1−brk. Feed δxr, δxw, δxf, δbr to GMRES to update the solutions xr, xw, xf.
Step 1) above, Solving Equation (8) by CPR Method:
1) Update the residual in equation (e50):
where
2) Solve equation (e50):
3) Map the pressure solution to the full solution:
where η a prolongation matrix defined below.
4) Update residual of equation (8):
5) Solve equation (8):
The prolongation and restriction matrices are as follows:
where Rr is the restriction matrix on the reservoir domain, and is defined in Equation (e48). Rw is the restriction matrix at the well side, and is defined as:
and wi=[ω1 ω2 1 . . . ω1 ω2 1] where ω1 and ω2 are determined using equations (e33) and (e34). Here nw is the number of wells. Re is an operation matrix accounting for the elimination of mass coupling terms as shown in
η is the prolongation matrix:
Pr is the prolongation matrix on the reservoir domain as defined in (e47). Pw is the prolongation matrix on the well side:
where Ei for the well i is defined as:
Here the 0's correspond to the columns with composition unknowns, and the 1's correspond to the columns with pressure unknowns.
The invention is not limited to the embodiments described above. The invention includes modified Newton-Raphson and Schwarz methods. For example, in some Newton-Raphson modifications, the same Jacobian is used for a number of iterations. The invention is not limited to particular variables, and while the examples above used the compositions of nc-1 components and the mass total flow rates other variables can be used instead, e.g. mass flow rates for all the components can be used. Further, while the embodiments described above do not use volume flow rate equations (e.g. volume balance equations) on the network side, other embodiments use such equations on the network side and use volume flow rates and volume compositions (volume fractions of individual components) instead of (or together with) mass flow rates or mass compositions. Volume flow rate terms are eliminated from volume balance equations using techniques described above for mass balance equations.
Some embodiments provide a computer implemented method for determining a plurality of values (e.g. pressures, compositions, flow rates, etc.) in a facility comprising an oil and/or gas reservoir and a plurality of wellbores each of which has been made or is to be made, each wellbore providing one or more passages for fluid flow into or out of the reservoir. The method comprises:
obtaining, by a computer system, a data model (e.g. 680, 690, 694) which represents the reservoir and each wellbore, the model comprising one or more nodes at said facility, the nodes comprising one or more sets of nodes, each set comprising a single node or a plurality of interconnected nodes, at least one node in each set being in a wellbore. In some embodiments, a set contains just one node, and diagonal composition terms are eliminated as in step 1940; step 1920 may be omitted. Different sets may or may not have nodes in respective different wellbores or wellbore segments.
The method further comprises obtaining, by the computer system, a system of linear algebraic equations interrelating said values, said values being represented as variables in the equations, wherein said values include a pressure for each node in each set and include flow rate values (e.g. mass flow rates or mass compositions or volume flow rates or compositions) defined by flow rates into or out of the nodes in each set, and for each node the equations include a set of one or more equations with values at the node, wherein for at least one node of each set of nodes, the set of one or more equations comprises at least one equation with a pressure at the node and one or more flow rate values at the node;
performing, by the computer system, a linear transformation of the system of equations, the linear transformation comprising a linear transformation of the equations of each set of equations to eliminate at least one flow rate value from at least one equation in each set of equations, the linear transformation providing a transformed system of equations; and
solving, by the computer system, the transformed system of equations for said values.
Some embodiments provide a computer implemented method for determining a plurality of values in a facility comprising an oil and/or gas reservoir and a plurality of wellbores each of which has been made or is to be made, each wellbore providing one or more passages for fluid flow into or out of the reservoir, the method comprising:
obtaining, by a computer system, a data model which represents the reservoir and each wellbore, the model comprising one or more nodes at said facility, the nodes comprising a set of one or more well nodes each of which is a node in at least one wellbore with no perforations along the wellbore between the node and a ground surface;
obtaining, by the computer system, a system of linear algebraic equations (e.g. Jacobian based) interrelating said values, said values being represented as variables in the equations, wherein for each well node, said values include at least one value at the well node;
solving, by the computer system, the system of the equations for said values, wherein solving the system comprises:
solving, by the computer system, equations obtained from a first subsystem of the system of said equations (for example, the first subsystem may be equations (8)), to obtain values including at least one value at each well node of said set and at least one value in the reservoir, or for differences between such values and their approximations (e.g. the differences may be δxr, δxw, δxf as indicated above);
solving, by the computer system, equations obtained from a second subsystem of the system of said equations (e.g. the second subsystem may be equations (9)), to obtain values including at least one value at each well node of said set and at least one value in the reservoir, or for differences between such values and their approximations;
wherein the first subsystem overlaps with the second subsystem, and at least one value of a well node of said set, or the corresponding difference between the value and its approximation, is solved for in both solving the first subsystem and solving the second subsystem;
wherein the method further comprises constructing, by the computer system, a solution of the system of the equations from solutions of the first and second subsystems.
The invention includes computer programs operable to cause a computer system (such the system of
Some information related to the above disclosure can be obtained from the following documents incorporated herein by reference (no representation is being made as to whether or not the documents are prior art with respect to the present application):
Filing Document | Filing Date | Country | Kind | 371c Date |
---|---|---|---|---|
PCT/US2012/040023 | 5/30/2012 | WO | 00 | 10/20/2014 |
Publishing Document | Publishing Date | Country | Kind |
---|---|---|---|
WO2013/180709 | 12/5/2013 | WO | A |
Number | Name | Date | Kind |
---|---|---|---|
6230101 | Wallis | May 2001 | B1 |
6418381 | Fuller | Jul 2002 | B1 |
6662146 | Watts | Dec 2003 | B1 |
20060036418 | Pita et al. | Feb 2006 | A1 |
20060080071 | Bera | Apr 2006 | A1 |
20060111882 | Subbarao | May 2006 | A1 |
20060235667 | Fung | Oct 2006 | A1 |
20070192071 | Huang et al. | Aug 2007 | A1 |
20070255779 | Watts, III | Nov 2007 | A1 |
20070260333 | Peureux | Nov 2007 | A1 |
20080319726 | Berge | Dec 2008 | A1 |
20100036537 | Bieker | Feb 2010 | A1 |
20100082509 | Mishev | Apr 2010 | A1 |
20100082724 | Diyankov | Apr 2010 | A1 |
20100179436 | Sarfaty | Jul 2010 | A1 |
20100252271 | Kelley | Oct 2010 | A1 |
20110040536 | Levitan | Feb 2011 | A1 |
20110088898 | Horton et al. | Apr 2011 | A1 |
Number | Date | Country |
---|---|---|
WO 2001062603 | Aug 2001 | WO |
WO 2005122001 | Dec 2005 | WO |
Entry |
---|
Jiang_2007 (Techniques for Modeling Complex Reservoirs and Advanced Wells, Dissertation, Dec. 2007). |
Flux_Defined downloaded from https://en.wikipedia.org/wiki/Flux. |
Jiang_2007 (Techniques for Modeling Complex Reservoir and Advanced Wells, Dissertation, Dec. 2007). |
Devold_2009 (Oil and Gas production handbook: An introduction to oil and gas production, ABB, 2009). |
Devold_2009 (Oil and Gas Production Handbook : An Introduction to oil and gas production, ABB, 2009 ISBN 978-82-997886-1-8). |
Jiang_2007 (Techniques for Modeling Complex Reservoirs and Advanced Wells, Dec. 2007 Stanford University). |
Evidence that drilling, completing, and producing from an oil well is well-understood routine and conventional is provided by a Brief History of Oil and Gas Well Drilling dated Feb. 2012 downloaded from http://www.visions.az/en/news/366/4ca556e3/. |
International Search Report and the Written Opinion of the International Searching Authority, or the Declaration, dated Aug. 10, 2012, PCT/US2012/040023, 10 pages, International Searching Authority, U.S. |
Russian Office Action, RU 2014147377, dated Feb. 25, 2016, 6 pages. |
Canadian Office Action issued for Application No. 2,873,406, dated Oct. 4, 2016, 4 pages. |
Wu, Yu-Shu, “A Virtual Node Method for Handling Well Bore Boundary Conditions in Modeling Multiphase Flow in Porous and Fractured Media,” Water Resources Research, vol. 36, No. 3, Mar. 2000, pp. 807-814. |
Canadian Office Action issued for Application No. 2,873,406, dated Jul. 11, 2017, 6 pages. |
Mason et al., “Spontaneous Counter-Current Imbibition Outwards from a Hemi-Spherical Depression,” Journal of Petroleum Science and Engineering, vol. No. 90-91, Jul. 2012, pp. 131-138. |
Matthai et al., “Finite Element—Node-Centered Finite-Volume Two-Phase-Flow Experiments With Fractured Rock Represented by Unstructured Hybrid-Element Meshes,” SPE Reservoir Evaluation & Engineering, Society of Petroleum Engineers, vol. No. 10, Issue No. 6, Dec. 1, 2007, pp. 740-756. |
Number | Date | Country | |
---|---|---|---|
20150073763 A1 | Mar 2015 | US |