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Correction

Correction: Tolmachev et al. Algorithmic Aspects of Simulation of Magnetic Field Generation by Thermal Convection in a Plane Layer of Fluid. Mathematics 2023, 11, 808

by
Daniil Tolmachev
1,
Roman Chertovskih
2,* and
Vladislav Zheligovsky
1
1
Institute of Earthquake Prediction Theory and Mathematical Geophysics, Russian Academy of Sciences, 84/32 Profsoyuznaya St., 117997 Moscow, Russia
2
Faculty of Engineering, University of Porto, Rua Dr. Roberto Frias, s/n, 4200-465 Porto, Portugal
*
Author to whom correspondence should be addressed.
Mathematics 2023, 11(10), 2395; https://doi.org/10.3390/math11102395
Submission received: 24 April 2023 / Accepted: 26 April 2023 / Published: 22 May 2023
(This article belongs to the Special Issue Numerical Analysis and Scientific Computing II)
There was an error in the original publication [1], and we make a number of corrections.
(1)
The wrong formula (20e) on p. 16 is as follows:
Γ k ' = 8 k ( k + 1 ) ( k + 2 ) π / Γ 2 .
The correct formula is
Γ k ' = 4 k ( k + 1 ) ( k + 2 ) / Γ 2 .
(2)
Section 4. The wrong equations on p. 21 are as follows:
T b | x 3 = ± 1 = 0 ,
P b | x 3 = 1 = h | x 3 = 1
2 P b x 3 2 | x 3 = 1 = P b | x 3 = 1 = 0 ,
M b | x 3 = ± 1 = 0 .
The corrected equations are:
T b | x 3 = 1 = T b x 3 | x 3 = 1 = 0 ,
P b | x 3 = 1 = h | x 3 = 1
2 P b x 3 2 | x 3 = 1 = P b | x 3 = 1 = 0 ,
M b | x 3 = 1 = M b x 3 | x 3 = 1 = 0 .
(3)
Section 4. The first paragraph on p. 22 is as follows:
and the mean-field component of the magnetic field from the equation derived by averaging over horizontal variables of the horizontal component of (1b). Since the boundary conditions for the toroidal and mean-field components of the magnetic field are the same as for the respective flow components, we use analogous expansions
T b ( x , t ) = | n 1 | N ,   | n 2 | N ,   0 n N 3 t n b ( t ) e i ( α 1 n 1 x 1 + α 2 n 2 x 2 ) T n ( x 3 ) ,
M b ( x 3 , t ) = 0 n N M n b ( t ) T n ( x 3 ) ,
where n = ( n 1 , n 2 , n ) , and equations for the coefficients in the expansions are obtainedsimilarly by orthogonal projection on the polynomials T m ( x 3 ) (10).
The second sentence here is deleted, i.e., the corrected paragraph is as follows:
and the mean-field component of the magnetic field from the equation is derived by averaging over horizontal variables of the horizontal component of (1b).
(4)
Section 4. The text in the middle of p. 22 is as follows:
T n ( x 3 ) = ( 4 ( n + 1 ) 4 2 ( n + 1 ) 2 + 1 + 2 Γ ( 2 ( n + 1 ) 2 + 1 ) ) Π n
( 4 n 4 2 n 2 + 1 + 2 Γ ( 2 n 2 + 1 ) ) Π n + 1
for n 1 . Thus, P n 1 ,   n 2 b ( x 3 , t ) can be expanded as
The revised text is:
T n ( x 3 ) = ( ( 4 ( n + 1 ) 4 2 ( n + 1 ) 2 + 1 + Γ ( 4 ( n + 1 ) 2 + 2 ) ) Π n ( 4 n 4 2 n 2 + 1 + Γ ( 4 n 2 + 2 ) ) Π n + 1 ) / ( 2 n + 1 ) = κ n + 1 T n 1 + ( κ n + λ n ) T n ( κ n + 1 λ n ) T n + 1 κ n T n + 2
for n 1 , where
κ n = n ( 4 n 4 2 n 2 + 1 + Γ ( 4 n 2 + 2 ) ) ,             λ n = 16 n ( n + 1 ) ( n ( n + 1 ) + 1 ) .
Thus, P n 1 ,   n 2 b ( x 3 , t )   can be expanded as
(5)
The following text is added at the end of Section 4:
The boundary conditions (27a) and (27d) for the toroidal potential and mean-field components of the magnetic field are satisfied by the polynomials
T n ( x 3 ) = μ n T n 1 4 n T n μ n 1 T n + 1 , where   μ n = 2 n ( n + 1 ) + 1 ,
and hence we use the expansions
T b ( x , t ) = | n 1 | N ,   | n 2 | N ,   1 n N 2 t n b ( t ) e i ( α 1 n 1 x 1 + α 2 n 2 x 2 ) T n ( x 3 ) ,
M b ( x 3 , t ) = 0 n N M n b ( t ) T n ( x 3 ) .
The coefficients in the expansion of a function in this basis can be determined by solving a linear system of equations with a pentadiagonal Gram matrix G, whose non-zero entries are as follows:
G k , k 2 = μ k 3 μ k ,       G k , k 1 = 4 ( k 1 ) μ k + 4 k μ k 2 ,       G k , k = μ k 2 ( 1 + δ 1 k ) + 16 k 2 + μ k 1 2 ,
G k , k + 1 = 4 k μ k + 1 + 4 ( k + 1 ) μ k 1 ,       G k , k + 2 = μ k 1 μ k + 2 .
Apparently, the system has no special properties enabling us to develop specialised methods for solving it numerically; it can be solved by the shuttle method (see Algorithm 1 in Section 3.2).
(6)
The erroneous second paragraph of Section 5 Conclusions is:
The Galerkin method is applied for computation of the toroidal and poloidal components of physical vector fields and their mean components. They are expanded in the basic functions that are products of linear combinations ( T n ( 10 ) , T n ( 18 ) and T n ( 30 ) ) of the Chebyshev polynomials in the vertical coordinate and Fourier harmonics in the horizontal coordinates. The basic functions involving the polynomials T n are used for the spatial discretisation of the unknown functions that take zero values on the horizontal boundaries   x 3 = ± 1 , namely, in the problem under discussion, the toroidal potentials of the flow and magnetic field, their mean fields, and the deviation of temperature from the steady-state linear profile. The basic functions involving T n are used for discretising the poloidal potential of the flow, which, for the no-slip boundary conditions, must vanish on the horizontal boundaries together with the first derivative in the vertical direction. Finally, the basic functions involving T n are used for discretising the poloidal potential of the magnetic field in the presence of the dielectric over the fluid layer and an electric conductor below it; while the no-slip boundary conditions for a solenoidal field are often considered in different problems, the latter boundary conditions are rather special.
It is substituted by the following correct paragraph:
The Galerkin method is applied for computing the toroidal and poloidal components of physical vector fields and their mean components. We exploit the bases of functions that are products of linear combinations ( T n ( 10 ) , T n ( 18 ) , T n ( 30 ) , and T n ( 32 ) ) of Chebyshev polynomials in the vertical coordinate and Fourier harmonics in the horizontal coordinates. The basic functions involving the polynomials T n are used for the spatial discretisation of the unknown functions that take zero values on the horizontal boundaries x 3 = ± 1 , namely, in the problem under discussion, the toroidal potential ofthe flow and its mean fields, and the deviation of temperature from the steady-state linear profile. The poloidal potential of the flow, which, for the no-slip boundary conditions, must vanish on the horizontal boundaries together with the first derivative in the vertical direction, is expanded in a series of functions involving the polynomial factors T n . The functions involving T n are used for discretising the poloidal potential of the magnetic field in the presence of the dielectric over the fluid layer and an electric conductor below it; while the no-slip boundary conditions for a solenoidal field are often considered in different problems, the latter boundary conditions are rather special. Finally, the toroidal potential of the magnetic field, which, for the boundary conditions considered here, is zero on the upper fluid boundary, and whose first derivative in x 3 vanishes on the lower boundary, is expanded in the series of the basic functions involving the polynomials T n .
(7)
The second sentence of the third paragraph of the Section 5 Conclusions is:
Specialised algorithms for determining the coefficients in expansion of an arbitrary function in a series of the basic functions are proposed and analysed.
It is now substituted with the following expanded sentence:
Specialised algorithms for determining the coefficients in the expansion of an arbitrary function in a series of the basic functions involving polynomials T n and T n are proposed and analysed.
The authors state that the scientific conclusions are unaffected. This correction was approved by the Academic Editor. The original publication has also been updated.

Reference

  1. Tolmachev, D.; Chertovskih, R.; Zheligovsky, V. Algorithmic Aspects of Simulation of Magnetic Field Generation by Thermal Convection in a Plane Layer of Fluid. Mathematics 2023, 11, 808. [Google Scholar] [CrossRef]
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MDPI and ACS Style

Tolmachev, D.; Chertovskih, R.; Zheligovsky, V. Correction: Tolmachev et al. Algorithmic Aspects of Simulation of Magnetic Field Generation by Thermal Convection in a Plane Layer of Fluid. Mathematics 2023, 11, 808. Mathematics 2023, 11, 2395. https://doi.org/10.3390/math11102395

AMA Style

Tolmachev D, Chertovskih R, Zheligovsky V. Correction: Tolmachev et al. Algorithmic Aspects of Simulation of Magnetic Field Generation by Thermal Convection in a Plane Layer of Fluid. Mathematics 2023, 11, 808. Mathematics. 2023; 11(10):2395. https://doi.org/10.3390/math11102395

Chicago/Turabian Style

Tolmachev, Daniil, Roman Chertovskih, and Vladislav Zheligovsky. 2023. "Correction: Tolmachev et al. Algorithmic Aspects of Simulation of Magnetic Field Generation by Thermal Convection in a Plane Layer of Fluid. Mathematics 2023, 11, 808" Mathematics 11, no. 10: 2395. https://doi.org/10.3390/math11102395

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