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Mathematical and Computer Modelling of Dynamical Systems
Methods, Tools and Applications in Engineering and Related Sciences
Volume 22, 2016 - Issue 4: Model Order Reduction
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Articles

A POD–EIM reduced two-scale model for precipitation in porous media

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Pages 323-344 | Received 09 Oct 2015, Accepted 02 Jun 2016, Published online: 27 Jun 2016

Figures & data

Figure 1. The considered initial configuration ℐ of the three substances in the microscopic pore-space μ, where Y=GΓGP. The grain μ is located in the centre of Y and the pore-space μ is occupied by the two immiscible and incompressible fluids P1 (water) and P2 (oil) as well as the precipitate P2. The spherical perforated precipitate P3 is attached to the boundary Гμ of the grain μ, the spherical fluid P2 domain is located in the corners of the microscopic domain Y and the fluid P1 occupies the remainder.

Figure 1. The considered initial configuration ℐ of the three substances in the microscopic pore-space μ, where Y=G∪ΓG∪P. The grain μ is located in the centre of Y and the pore-space μ is occupied by the two immiscible and incompressible fluids P1 (water) and P2 (oil) as well as the precipitate P2. The spherical perforated precipitate P3 is attached to the boundary Гμ of the grain μ, the spherical fluid P2 domain is located in the corners of the microscopic domain Y and the fluid P1 occupies the remainder.

Table 1. The varying parameters of the three settings S1, S2 and S3, which are explained in Section 4.1 and . The function u_(t) = a:b increases linearly from a to b with the time-steps in the course of a simulation. For = 1,2 an initial precipitate’s radius r0(i) results in a precipitate’s initial portion of ϕ3¯P(i) on the overall pore-space’s volume, analogously the water’s initial portion is ϕ1¯P(i), and the oil’s initial portion is ϕ2¯P(i)=0.07 due to a radius r˜0(i)=30h.

Figure 2. The initial phase configurations in the microscopic pore-space Ph in the two subdomains Ωhg(1) and Ωhg(2) of the macroscopic domain Ωhg. The black points in the very centre of Ph in (b) and (c) represent the small spherical grains Gh. Each grain is surrounded by a precipitate P3 (yellow). For i=1,2, r0,i defines the initial radius of the precipitates in the subdomain Ωhg(i). Each precipitate is surrounded by water (blue) and a spherical oil phase P2 (green) is located in the corners of Ph. The coloured subdomains Pi are characterized by ϕi12 for iI. Full colour available online.

Figure 2. The initial phase configurations in the microscopic pore-space Phℓ in the two subdomains Ωhg(1) and Ωhg(2) of the macroscopic domain Ωhg. The black points in the very centre of Phℓ in (b) and (c) represent the small spherical grains Ghℓ. Each grain is surrounded by a precipitate P3 (yellow). For i=1,2, r0,i defines the initial radius of the precipitates in the subdomain Ωhg(i). Each precipitate is surrounded by water (blue) and a spherical oil phase P2 (green) is located in the corners of Phℓ. The coloured subdomains Pi are characterized by ϕi≥12 for i∈I. Full colour available online.

Figure 3. The nodes in the subset Ωhg of the macroscopic grid Ωhg: nodes of ΩhgΩhg(1) are indicated in red, and in blue those of ΩhgΩhg(2). Full colour available online.

Figure 3. The nodes in the subset Ωhg⋆ of the macroscopic grid Ωhg: nodes of Ωhg⋆∩Ωhg(1) are indicated in red, and in blue those of Ωhg⋆∩Ωhg(2). Full colour available online.

Figure 4. High-dimensional solution of setting S1 at the end of the time-interval for T=5.

Figure 4. High-dimensional solution of setting S1 at the end of the time-interval for T=5.

Figure 5. High-dimensional solution of the setting S1: the evolution of the precipitates’ volume portion on the pore-space in the macroscopic nodes (00)T (red dashed), (126)T (blue dotted), (3618)T (black) and (4924)T (cyan). In Ωhg(1) the node (00)T (and respectively, (4924)T) is host of the precipitate with the minimum (maximum) volume portion throughout the time-interval. The same relation holds in Ωhg(2) for (126)T (minimum) and (3618)T (maximum). Full colour available online.

Figure 5. High-dimensional solution of the setting S1: the evolution of the precipitates’ volume portion on the pore-space in the macroscopic nodes (00)T (red dashed), (126)T (blue dotted), (3618)T (black) and (4924)T (cyan). In Ωhg(1) the node (00)T (and respectively, (4924)T) is host of the precipitate with the minimum (maximum) volume portion throughout the time-interval. The same relation holds in Ωhg(2) for (126)T (minimum) and (3618)T (maximum). Full colour available online.

Table 2. Results for setting S1: the column entitled by ‘speed-up’ presents the rough speed-up of the approximations’ computation time in comparison to the high-dimensional solution of S1 in 57 h (as for the high-dimensional solution 27 processors of type Intel(R) Xeon(R) CPU [email protected] GHz were used), and the columns entitled by ΔuQ, ΔKcorQ, ΔΦQ and Δ(ϕ1δw1)Q present the approximations’ accuracy. The line entitled by w1=0 presents the results of a high-dimensional approximation with prescribed w1=0 resulting in Kcor=0 and ϕ1δw1=0.

Table 3. Results for setting S1: the columns entitled by Nw, |YM| and |YM| present the average sizes of the 100 basis sets of a reduced model, and the column entitled by ‘reduction time’ presents the time that one processor of type Intel(R) Xeon(R) CPU [email protected] GHz needs to construct the reduced models from the pre-computed snapshots of the high-dimensional solution of S1. In particular, this time is not the full offline time, as it does not include the 57-h for the snapshots computation.

Figure 6. Results for the setting S1 and the low-dimensional solution R10 with ϵPOD=1e10: (a) presents the evolution of the precipitates’ volumes ϕ3¯P and (b) the utilized basis sets in the course of the simulation in the macroscopic nodes (00)T (red dashed), (126)T (blue dotted), (3618)T (black) and (4924)T (cyan). Full colour available online.

Figure 6. Results for the setting S1 and the low-dimensional solution R10 with ϵPOD=1e−10: (a) presents the evolution of the precipitates’ volumes ϕ3¯P and (b) the utilized basis sets in the course of the simulation in the macroscopic nodes (00)T (red dashed), (126)T (blue dotted), (3618)T (black) and (4924)T (cyan). Full colour available online.

Figure 7. Results for the setting S1 and the low-dimensional solution R10: (a) depicts the minimum (black) and maximum (cyan) of the volume interval for the precipitates for the 100 basis sets that are used in the online phase to determine the proper basis set in order to approximate the reduced solution of w1, where the minimum is for basis set 0 and the maximum is for basis set 99; (b) shows the number of POD modes (cyan) and the number of magic points (black) of the basis sets and (c) depicts exemplary for the basis set 73 for the increasing number of modes the decay of log10 of the eigenvalues of the correlation operator in the construction of the POD basis (cyan) and for the increasing number of magic points the error decay of the EI (black). Full colour available online.

Figure 7. Results for the setting S1 and the low-dimensional solution R10: (a) depicts the minimum (black) and maximum (cyan) of the volume interval for the precipitates for the 100 basis sets that are used in the online phase to determine the proper basis set in order to approximate the reduced solution of w1, where the minimum is −∞ for basis set 0 and the maximum is ∞ for basis set 99; (b) shows the number of POD modes (cyan) and the number of magic points (black) of the basis sets and (c) depicts exemplary for the basis set 73 for the increasing number of modes the decay of log10 of the eigenvalues of the correlation operator in the construction of the POD basis (cyan) and for the increasing number of magic points the error decay of the EI (black). Full colour available online.

Figure 8. Results for setting S1 and the low-dimensional solution R10, which consists of 100 basis sets: (a), (b) and (c) illustrates the distribution of the magic points in the basis sets 0, 73 and 99, where the inner circle marks the smallest and the outer one the largest subdomain supporting the precipitate in the snapshots, and the four quarters of a circle indicate the almost unchanged oil phase; (d), (e) and (f) depict the dominant POD mode for w1 for the corresponding basis sets.

Figure 8. Results for setting S1 and the low-dimensional solution R10, which consists of 100 basis sets: (a), (b) and (c) illustrates the distribution of the magic points in the basis sets 0, 73 and 99, where the inner circle marks the smallest and the outer one the largest subdomain supporting the precipitate in the snapshots, and the four quarters of a circle indicate the almost unchanged oil phase; (d), (e) and (f) depict the dominant POD mode for w1 for the corresponding basis sets.

Figure 9. High-dimensional solutions of the settings S2 and S3 in the end of the time-interval at T=2.5.

Figure 9. High-dimensional solutions of the settings S2 and S3 in the end of the time-interval at T=2.5.

Table 4. Setting S2: the approximations’ accuracy.

Table 5. Setting S3: the approximations’ accuracy.

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