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Research article

Stability of the 3D MHD equations without vertical dissipation near an equilibrium

  • Received: 02 November 2022 Revised: 06 March 2023 Accepted: 12 March 2023 Published: 22 March 2023
  • MSC : 35A05, 35Q35, 76D03

  • Important progress has been made on the standard Laplacian case with mixed partial dissipation and diffusion. The stability problem of the 3D incompressible magnetohydrodynamic (MHD) equations without vertical dissipation but with the fractional velocity dissipation (Δ)αu and magnetic diffusion (Δ)βb is unfortunately not often well understood for many ranges of fractional powers. This paper discovers that there are new phenomena with the case α,β1. We establish that, if an initial datum (u0,b0) in the Sobolev space H3(R3) is close enough to the equilibrium state, and we replace the terms (Δ)αu and (Δ)βb by (Δh)αu and (Δh)βb, respectively, the resulting equations with α,β(12,1] then always lead to a steady solution, where Δh=2x1+2x2.

    Citation: Ruihong Ji, Liya Jiang, Wen Luo. Stability of the 3D MHD equations without vertical dissipation near an equilibrium[J]. AIMS Mathematics, 2023, 8(5): 12143-12167. doi: 10.3934/math.2023612

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  • Important progress has been made on the standard Laplacian case with mixed partial dissipation and diffusion. The stability problem of the 3D incompressible magnetohydrodynamic (MHD) equations without vertical dissipation but with the fractional velocity dissipation (Δ)αu and magnetic diffusion (Δ)βb is unfortunately not often well understood for many ranges of fractional powers. This paper discovers that there are new phenomena with the case α,β1. We establish that, if an initial datum (u0,b0) in the Sobolev space H3(R3) is close enough to the equilibrium state, and we replace the terms (Δ)αu and (Δ)βb by (Δh)αu and (Δh)βb, respectively, the resulting equations with α,β(12,1] then always lead to a steady solution, where Δh=2x1+2x2.



    The MHD equations describe the evolution in time of velocity field u and magnetic field b of some electrically conducting fluids such as plasmas, liquid metals and salt water or electrolytes[1,2]. The set of equations that describe MHD is a combination of the Navier-Stokes equations of fluid dynamics and Maxwell's equations of electro-magnetism. The field of MHD was initiated by Hannes Alfvén[3], for which he received the Nobel Prize in physics in 1970.

    The MHD equations are also of great interest in mathematics. In recent years, the stability of the MHD equations has attracted considerable interest, and one focus has been on the MHD equations with partial or fractional dissipation and diffusion. Elegant works have been made (see, e.g., [4,5,6,7,8,9,10,11,12]). For the 3D incompressible generalized MHD equations with fractional dissipation and diffusion,

    {tu+uu=ν(Δ)αuP+BB,xR3,t>0,tB+uB=η(Δ)βB+Bu,xR3,t>0,u=0,B=0,xR3,t>0, (1.1)

    where α,β>0 are real parameters, u=u(x,t)R3 represents the velocity field, B=B(x,t)R3 represents the magnetic field, P=P(x,t)R represents the pressure, ν>0 denotes the kinematic viscosity, and η>0 denotes the magnetic diffusivity. For notational convenience, we write i for the partial derivatives xi(i = 1, 2, 3). The fractional Laplacian operator (Δ)α is defined via the Fourier transform,

    ^(Δ)αf(ξ)=|ξ|2αˆf(ξ)

    for

    ˆf(ξ)=1(2π)d/2Rdeixξf(x)dx.

    The MHD equations with fractional dissipation given by (1.1) have recently attracted considerable interest, due to their mathematical importance and physical applications. The justification for the study of this fractionally dissipated system can be made from several different perspectives. First, (1.1) represents a two-parameter family of systems and contains the MHD systems with standard Laplacian dissipation as special cases. (1.1) allows us to simultaneously examine a whole family of equations and potentially reveals how the properties of its solutions are related to the sizes of α and β. Second, the fractional diffusion operators can model the so-called anomalous diffusion, a much studied topic in physics, probability and finance (see, e.g., [13,14]). Third, fractional dissipation has been widely used in turbulence modeling to control the effective range of the non-local dissipation and to make numerical resolutions more efficient (see, e.g., [15]).

    A range of global well-posedness results on (1.1) have been obtained. When α=β=1, (1.1) reduces to the standard MHD equations, which is well-known possessing global L2 weak solutions; in two dimensions, it is also unique[7,16]. When combined with the already established global weak solutions[8], these bounds allow us to conclude that MHD equations possess a global classical solution if α and β satisfy

    α12+d4,β>0,α+β1+d2.

    Wu[9] was able to sharpen this result by replacing the fractional Laplacian operators by general Fourier multiplier operators. In particular, (1.1) with a (Δ)αlog(IΔ)u and (Δ)βlog(IΔ)b for α and β satisfying the bounds above is also globally well posed[6]. Yamazaki obtained the global regularity for the case when α=2 and β=0 and for a logarithmically reduced fractional dissipation [17]. Logarithmic refinement of these fractional powers is contained in [18]. Ye and Xu[19] considered the global existence of the 2D generalized incompressible MHD system with velocity dissipation exponent α>14 and magnetic diffusion exponent β=1. After that, Ye established the global regularity solutions to the 2D incompressible MHD equations with almost Laplacian magnetic diffusion in the whole space [20]. Recently, Dai and Ji[5] established the local existence and uniqueness in inhomogeneous Besov spaces when

    α>12,β0,α+β1.

    Since (1.1) was proposed in [8], there have been considerable activities, and the global well-posedness problem on (1.1) is now much better understood (see, e.g., [21,22,23,24,25,26]).

    The nonlinear stability for the ideal MHD equations was established in several beautiful papers [27,28,29,30]. Nevertheless, the stability of (1.1) remains unknown. The focus of this paper is the stability of perturbation near a background magnetic field which is

    u(0)(0,0,0),B(0)(0,1,0).

    The perturbation (u,b) with

    b:=BB(0)

    solves the MHD system

    {tu+uu=ν(Δ)αuP+bb+2b,xR3,t>0,tb+ub=η(Δ)βb+bu+2u,xR3,t>0,u=0,B=0,xR3,t>0,u(x,0)=u0(x),b(x,0)=b0(x). (1.2)

    We now address the problem as to whether the steady weak solution of the MHD equations (1.1) does in fact depend continuously on the perturbation of (u(0),B(0)) given in the problem. In this paper, we consider (1.1) with only horizontal fractional dissipation and lacking vertical dissipation

    {tu+uu=ν(Δh)αuP+bb+2b,xR3,t>0,tb+ub=η(Δh)βb+bu+2u,xR3,t>0,u=0,B=0,xR3,t>0,u(x,0)=u0(x),b(x,0)=b0(x), (1.3)

    with α,β(12,1]. The concept of horizontal dissipation comes from geophysical fluid dynamics (see [31]), and meteorologists model the turbulent diffusion with anisotropic viscosity νhΔhν323, where the horizontal kinetic viscosity coefficient νh and the vertical kinetic viscosity coefficient ν3 are empirical constants and satisfy 0<ν3νh. In this paper, we take the limit case νh=ν and ν3=0. To give a complete view of current studies on the stability problem concerning the MHD equations with partial dissipation, we mention some of the encouraging results in [4,10,16,22,32,33,34,35,36,37,38,39,40] and the references therein.

    A natural consideration is how the parameters α and β are determined, and this is what we choose to do in our tentative estimation work, based primarily on energy estimate method. When we bound the ˙H3-norm of (u,b), we plan to utilize a series of anisotropic inequalities derived from a Sobolev embedding inequality and Gagliardo-Nirenberg (G-N) interpolation inequality[41,42,43]. Based on the relationship between the parameters of these inequalities, we ended up choosing α,β(12,1] in (1.3) to study the stability of the MHD equations with fractional horizontal dissipation.

    To construct a steady solution of (1.3), we make use of a bootstrap argument by anisotropic estimates

    E(t)=sup0τt{u(τ)2H3+b(τ)2H3}+2νt0Λαhu(τ)2H3dτ+2ηt0Λβhb(τ)2H3dτ. (1.4)

    Here Λh=(Δh)12 denotes the Zygmund operator. Our precise result is stated in the following theorem.

    Theorem 1.1. Consider (1.3) with initial data (u0,b0)H3(R3) satisfying u0=b0=0 and α,β(12,1]. Then, there exists a constant δ=δ(ν,η)>0 such that, if

    (u0,b0)H3δ, (1.5)

    then (1.3) has a unique global classical solution satisfying

    sup0τt(u(τ)2H3+b(τ)2H3)+2νt0Λαhu(τ)2H3dτ+2ηt0Λβhb(τ)2H3dτCδ2,

    for any t>0, and C=C(ν,η) is a constant.

    A natural starting point is to bound u(t)H3+b(t)H3 via energy estimate. We are able to derive the following energy inequality:

    E(t)E(0)+CE(t)32. (1.6)

    Combined with the bootstrapping argument (see[44]), we can prove Theorem 1.1. However, the proof of Theorem 1.1 is not superficial. Due to the lack of the vertical dissipation and vertical magnetic diffusion, some nonlinear terms are not easy to control in terms of u(t)H3+b(t)H3 or the dissipation parts ΛαhuH3 and ΛβhbH3. One of the most difficult terms is

    R33uhh23b33bdx3uh112αL23Λαhuh12αL233b112βL233Λβhb12βL2h23b112βL2h23Λα3b12βL2.

    Clearly, it does not appear possible to bound the subterms

    3uh112αL233b112βL2 (1.7)

    directly in terms of Λαhu2H3Λβhb2H3, but in terms of u(t)2H3b(t)2H3. Therefore, we hope the sum of the corresponding exponents of the two subterms to be less than or equal to 1 for all given α and β, which is

    112α+112β1. (1.8)

    To establish the inequality of (1.6), we choose α,β(12,1]. In the case of

    112α+112β=1,

    the subterms of (1.7) can be estimated directly by

    u(t)H3+b(t)H3.

    The other case is

    112α+112β<1.

    Our strategy is to extract part from the rest subterms

    3Λαhuh12αL2h23b112βL2

    to fill the subterms of (1.7) by G-N interpolation inequality. One reason which cannot be ignored is that 3ΛαhuhL2 could be bounded by either uH3 or ΛαhuH3, and h23bL2 could be bounded by either bH3 or ΛαhbH3. In the last section of our paper, we have successfully used this method to solve all similar difficulties in proving stability and obtain inequality (1.6).

    Lemma 1.2. Assume that α,β,γ(12,1], f,g,h,Λαhf,Λβhg,Λγhh and 3h are all in L2(R3). Then,

    R3|fgh|dxf112αL2Λαhf12αL2g112βL2Λβhg12βL2h12L23h12L2,R3|fgh|dxf112αL2Λαhf12αL2g112βL2Λβhg12βL2h112γL2Λγ3h12γL2.

    Here, we write AB to mean that ACB for some constant C and Λ3=(33)12.

    These anisotropic inequalities are greatly powerful in the study of global regularity and stability problems on partial differential equations with only partial dissipation. Similar inequalities have previously been used in the investigation of partially dissipated MHD systems and related equations (see, e.g., [45,46])

    The rest of this paper is divided into two sections. Section 2 provides the proofs of Theorem 1.1 and Lemma 1.2. Section 3 derives the energy inequality (1.6).

    This section proves Theorem 1.1 and Lemma 1.2.

    Roughly speaking, the bootstrap argument starts with an ansatz that E(t) is bounded, say,

    E(t)M,

    and shows that E(t) actually admits a smaller bound, say,

    E(t)12M,

    when the initial condition is sufficiently small. A rigorous statement of the abstract bootstrap principle can be found in T. Tao's book[44].

    It follows that

    E(t)E(0)+CE(t)32, (2.1)

    for some pure constants C. To initiate the bootstrapping argument, we make the ansatz

    E(t)M:=14C2. (2.2)

    We then show that (2.1) allows us to conclude that E(t) actually admits an even smaller bound by taking the initial H3-norm E(0) sufficiently small. In fact, when (2.2) holds, (2.1) implies

    E(t)E(0)+12E(t)

    or

    E(t)2E(0). (2.3)

    Therefore, if we choose δ>0 sufficiently small such that

    δ214M, (2.4)

    then

    E(t)12M. (2.5)

    E(t) actually admits a smaller bound in (2.3) than the one in the ansatz (2.2). The bootstrapping argument then assesses that (2.2) holds for all times when E(0) obeys (2.4). This completes the proof.

    The proof makes use of the version of Minkowski's inequality

    fLqy(Rn)Lpx(Rm)fLpx(Rm)Lqy(Rn),

    for any 1qp, where f=f(x,y) with xRm, and yRn is a measurable function on Rm×Rn, and the following basic one-dimensional Sobolev embedding inequality [12], for fHs(R),

    fL(R)Cf112sL2(R)Λsf12sL2(R),

    where s>12. By the above inequality and Hölder's inequality,

    R3|fgh|dxfLx1L2x2L2x3gL2x1Lx2L2x3hL2x1L2x2Lx3Cf112s1L2x1Λs11f12s1L2x1L2x2x3g112s2L2x2Λs22g12s2L2x2L2x1x3×h112s3L2x3Λs33h12s3L2x3L2x1x2Cf112s1L2Λs11f12s1L2g112s2L2Λs22g12s2L2h112s3L2Λs33h12s3L2.

    Let s1=α,s2=β,s3=1, and we obtain

    R3|fgh|dxf112αL2Λα1f12αL2g112βL2Λβ2g12βL2h12L23h12L2f112αL2Λαhf12αL2g112βL2Λβhg12βL2h12L23h12L2.

    Let s1=α,s2=β,s3=γ, and we obtain

    R3|fgh|dxf112αL2Λα1f12αL2g112βL2Λβ2g12βL2h112γL2Λγ3h12γL2f112αL2Λαhf12αL2g112βL2Λβhg12βL2h112γL2Λγ3h12γL2.

    Here, fLx1L2x2L2x3 represents the L-norm in the x1-variable, followed by the L2-norm in x2 and the L2-norm in x3. This finishes the proof of Lemma 1.2.

    Due to the equivalence of (u,b)H3 with (u,b)L2+(u,b)˙H3, it suffices to bound the L2-norm and the ˙H3-norm of (u,b). By a simple energy estimate and u=b=0, we find that the L2-norm of (u,b) obeys

    u(t)2L2+b(t)2L2+2νt0Λαhu(τ)2L2dτ+2ηt0Λβhb(τ)2L2dτ=u(0)2L2+b(0)2L2. (3.1)

    The rest of the proof focuses on the ˙H3-norm. Applying 3i to (1.3) and then dotting by (3iu, 3ib), we obtain

    12ddt3i=1(3iu2L2+3ib2L2)+ν3iΛαhu2L2+η3iΛβhb2L2=I1+I2+I3+I4+I5, (3.2)

    where

    I1=3i=1R33i2b33u+3i2u33bdx,I2=3i=1R33i(uu)3iudx,I3=3i=1R3[3i(bb)b3ib]3iudx,I4=3i=1R33i(ub)3ibdx,I5=3i=1R3[3i(bu)b3iu]3ibdx.

    Note that, by integration by parts,

    I1=0,

    and

    3i=1R3b3ib3iudx+R3b3iu3ibdx=0.

    To bound I2, we decompose it into three pieces,

    I2=3i=1R33i(uu)3iudx=3i=1(R33iuu3iudx+3R32iuiu3iudx+3R3iu2iu3iudx)=I21+3I22+3I23, (3.3)

    where we have used the fact that R3u33u33udx=0. I21 is naturally split into three parts,

    I21=3i=1R33iuu3iudx=2i=1R33iuu3iudxR333uhhu33udxR333u33u33udx=I211+I212+I213.

    By Lemma 1.2 and G-N interpolation inequality,

    |I211|=|2i=1R33iuu3iudx|2i=13iu21αL23iΛαhu1αL2u12L23u12L22i=12iΛαhuγ(21α)L22iΛ1+αhu(1γ)(21α)L23iΛαhu1αL2u12L23u12L2uH3Λαhu2H3, (3.4)

    where we have applied inequality

    iuL2ΛαhuγL2Λ1+αhu1γL2(i=1,2).

    We now turn to I212, by Lemma 1.2,

    |I212|=|R333uhhu33udx|33uh112αL233Λαhuh12αL233u112αL233Λαhu12αL2hu12L2h3u12L233uh112αL233Λαhuh12αL233u112αL233Λαhu12αL2×hu12α12L2Λαhuγ(112α)L2Λ1+αhu(1γ)(112α)L2×h3u12α12L2Λαh3uγ(112α)L2Λ1+αh3u(1γ)(112α)L2uH3Λαhu2H3. (3.5)

    In fact, we take hu112αL2h3u112αL2 from hu12L2h3u12L2 and combine it with 33Λαhuh12αL233Λαhu12αL2 to reach our desired bound. In addition, by G-N interpolation inequality, we get

    huL2ΛαhuγL2Λ1+αhu1γL2.

    We next consider the term I213, and we have

    |I213|=|R333u33u33udx|=|2j=1R323juj3u33udx|2j=123juj112αL223Λα3juj12αL23u112αL23Λαhu12αL233u112αL233Λαhu12αL22j=123Λαhujγ(112α)L223Λ1+αhuj(1γ)(112α)L233Λαhuγ12αL223Λα+1hu(1γ)12αL2×3u112αL23Λαhu1α1L23Λαhu112αL233u112αL233Λαhu12αL2uH3Λαhu2H3, (3.6)

    where we used

    23Λα3jujL233ΛαhuγL223Λα+1hu1γL2,3Λαhu1α1L2u1α1H3

    and u=0. To deal with I22, this term is split into three parts,

    I22=3i=1R32iuiu3iudx=2i=1R32iuiu3iudxR323uhh3u33udxR323u323u33udx=I221+I222+I223.

    Similarly to (3.4),

    |I221|=|2i=1R32iuiu3iudx|2i=12iu112αL22iΛαhu12αL23iu112αL23iΛαhu12αL2iu12L2i3u12L22i=1iΛαhuγ(112α)L2iΛ1+αhu(1γ)(112α)L22iΛαhu12αL2×2iΛαhuγ(112α)L22iΛ1+αhu(1γ)(112α)L23iΛαhu12αL2iu12L2i3u12L2uH3Λαhu2H3. (3.7)

    Applying Lemma 1.2 and G-N interpolation inequality, we obtain

    |I222|=|R323uhh3u33udx|23uh112αL223Λαhuh12αL233u112αL233Λαhu12αL2h3u12L2h23u12L223uh112αL223Λαhuh12αL233u112αL233Λαhu12αL2×h3u12α12L2Λαh3uγ(112α)L2Λ1+αh3u(1γ)(112α)L2×h23u12α12L2Λαh23uγ(112α)L2Λ1+αh23u(1γ)(112α)L2uH3Λαhu2H3. (3.8)

    Note that we separate out a part of h3u12L2h23u12L2 and make it controlled by ΛhuH3. Similarly,

    |I223|=|R323u323u33udx|=|2j=1R33juj23u33udx|2j=123uh112αL223Λαhuh12αL233u112αL233Λαhu12αL23juj12L223juj12L22j=123uh112αL223Λαhuh12αL233u112αL233Λαhu12αL2×3juj12α12L23Λαhuγ(112α)L23Λ1+αhu(1γ)(112α)L2×23juj12α12L223Λαhuγ(112α)L223Λ1+αhu(1γ)(112α)L2uH3Λαhu2H3. (3.9)

    We deal with I23 in the same method, as I23 is naturally split into three parts,

    I23=3i=1R3iu2iu3iudx=2i=1R3iu2iu3iudxR33uhh23u33udxR33u333u33udx=I231+I232+I233.

    By Lemma 1.2 and G-N interpolation inequality, we have

    |I231|=|2i=1R3iu2iu3iudx|2i=12iu112αL22iΛαhu12αL23iu112αL23iΛαhu12αL2iu12L2i3u12L22i=1iΛαhuγ(112α)L2iΛ1+αhu(1γ)(112α)L22iΛαhu12αL2×2iΛαhuγ(112α)L22iΛ1+αhu(1γ)(112α)L23iΛαhu12αL2iu12L2i3u12L2uH3Λαhu2H3. (3.10)

    We estimate I232 similarly as I213, which yields

    |I232|=|R33uhh23u33udx|h23u112αL2h23Λα3u12αL23uh112αL23Λαhuh12αL233u112αL233Λαhu12αL2Λαh23uγ(112α)L2Λ1+αh23u(1γ)(112α)L233Λαhuγ12αL223Λα+1hu(1γ)12αL2×3uh112αL23Λαhuh1α1L23Λαhuh112αL233u112αL233Λαhu12αL2uH3Λαhu2H3. (3.11)

    We next consider the term I233, and utilizing the incompressible condition again, we have

    |I233|=|R33u333u33udx|=|2j=1R3juj33u33udx|2j=133u21αL233Λαhu1αL2juj12L23juj12L22j=133u21αL233Λαhu1αL2juj12α12L2Λαhujγ(112α)L2Λ1+αhuj(1γ)(112α)L2×3juj12α12L23Λαhujγ(112α)L23Λ1+αhuj(1γ)(112α)L2uH3Λαhu2H3. (3.12)

    Combined with (3.3)–(3.12), we obtain

    I2(τ)uH3Λαhu2H3.

    To bound I3, we can refer to the way which is used in I2 and then divide it into three terms,

    I3=3i=1R3[3i(bb)b3ib]3iudx,=3i=1(R33ibb3iudx+3R32ibib3iudx+3R3ib2ib3iudx)=I31+3I32+3I33. (3.13)

    I31 can be further decomposed into three parts,

    I31=3i=1R33ibb3iudx=2i=1R33ibb3iudx+R333bhhb33udx+R333b33b33udx=I311+I312+I313.

    By Lemma 1.2 and G-N interpolation inequality,

    |I311|=|2i=1R33ibb3iudx|2i=13ib112βL23iΛβhb12βL23iu112αL23iΛαhu12αL2b12L23b12L22i=12iΛβhbγ(112β)L22iΛ1+βhb(1γ)(112β)L22iΛαhuγ(112α)L22iΛ1+αhu(1γ)(112α)L2×3iΛβhb12βL23iΛαhu12αL2b12L23b12L2bH3ΛαhuH3ΛβhbH3, (3.14)

    where we have applied inequality

    ibL2ΛβhbγL2Λ1+βhb1γL2(i=1,2).

    By divergence-free condition b=0 and Lemma 1.2, we have

    |I312|=|R333bhhb33udx|33bh112βL233Λβhbh12βL233u112αL233Λαhu12αL2hb12L2h3b12L233bh112βL233Λβhbh12βL233u112αL233Λαhu12αL2×Λβhbγ(112β)L2Λ1+βhb(1γ)(112β)L2hb12β12L2×Λβh3bγ(112α)L2Λ1+βh3b(1γ)(112α)L2hb12α12L2u112αH3b12αH3Λαhu12αH3Λβhb212αH3. (3.15)

    Significantly, we have used G-N interpolation inequality

    hbL2ΛβhbγL2Λ1+βhb1γL2.

    We simplify I313 by the same way as I213, that is,

    |I313|=|R333b33b33udx|=|2j=1R323jbj3b33udx|2j=13b112βL23Λβhb12βL233u112αL233Λαhu12αL223jbj112βL223Λβ3jbj12βL22j=13b112βL23Λβhb12β(12α+12β1)L23Λβhb12β(212α12β)L2×33u112αL233Λαhu12αL223jbj(112β)(12α+12β1)L2×23Λβhbjγ(112β)(212α12β)L223Λ1+βhbj(1γ)(112β)(212α12β)L2×33Λβhbγ12βL223Λ1+βhb(1γ)12βL2u112αH3b12αH3Λαhu12αH3Λβhb212αH3, (3.16)

    where we have used

    23Λβ3jbjL233ΛβhbγL223Λβ+1hb1γL2

    and

    3Λβhb12βL223jbj(112β)L2bH3.

    To deal with I32, we also split it into three parts,

    I32=3i=1R32ibib3iudx=2i=1R32ibib3iudx+R323bhh3b33u+R323b323b33udx=I321+I322+I323.

    By Lemma 1.2 and G-N interpolation inequality,

    |I321|=|2i=1R32ibib3iudx|2i=12ib112βL22iΛβhb12βL23iu112αL23iΛαhu12αL2ib12L2i3b12L22i=1iΛβhbγ(112β)L2iΛ1+βhb(1γ)(112β)L22iΛβhb12βL2×2iΛαhuγ(112α)L22iΛ1+αhu(1γ)(112α)L23iΛαhu12αL2ib12L2i3b12L2bH3ΛαhuH3ΛβhbH3. (3.17)

    Naturally,

    |I322|=|R323bhh3b33udx|23bh112βL223Λβhbh12βL233u112αL233Λαhu12αL2h3b12L2h23b12L223bh112βL223Λβhbh12βL233u112αL233Λαhu12αL2×Λβh3bγ(112β)L2Λ1+βh3b(1γ)(112β)L2h3b12β12L2×Λβh23bγ(112α)L2Λ1+βh23b(1γ)(112α)L2h23b12α12L2u112αH3b12αH3Λαhu12αH3Λβhb212αH3 (3.18)

    and

    |I323|=|R323b323b33udx|=|2j=1R33jbj23b33udx|2j=123b112βL223Λβhb12βL233u112αL233Λαhu12αL23jbj12L223jbj12L22j=123b112βL223Λβhb12βL233u112αL233Λαhu12αL2×3Λβhbjγ(112β)L23Λ1+βhbj(1γ)(112β)L23jbj12β12L2×23Λβhbjγ(112α)L223Λ1+βhbj(1γ)(112α)L223jbj12α12L2u112αH3b12αH3Λαhu12αH3Λβhb212αH3. (3.19)

    In the same way, I33 is split into three parts,

    I33=3i=1R3ib2ib3iudx=2i=1R3ib2ib3iudx+R33bhh23b33udx+R33b333b33udx=I331+I332+I333.

    Lemma 1.2 and G-N interpolation inequality imply

    |I331|=|2i=1R3ib2ib3iudx|2i=12ib112βL22iΛβhb12βL23iu112αL23iΛαhu12αL2ib12L2i3b12L22i=1iΛβhbγ(112β)L2iΛ1+βhb(1γ)(112β)L22iΛβhb12βL2×2iΛαhuγ(112α)L22iΛ1+αhu(1γ)(112α)L23iΛαhu12αL2ib12L2i3b12L2bH3ΛαhuH3ΛβhbH3. (3.20)

    We estimate I332 similarly as I313, which yields

    |I332|=|R33bhh23b33udx|3bh112βL23Λβhbh12βL233u112αL233Λαhu12αL223hb112βL223hΛβ3b12βL23bh112βL23Λβhbh12β(12α+12β1)L23Λβhbh12β(212α12β)L2×33u112αL233Λαhu12αL223hb(112β)(12α+12β1)L2×23Λβhbγ(112β)(212α12β)L223Λ1+βhb(1γ)(112β)(212α12β)L2×33Λβhbγ12βL223Λ1+βhb(1γ)12βL2u112αH3b12αH3Λαhu12αH3Λβhb212αH3. (3.21)

    Now we turn to the next term I333, by b=0,

    |I333|=|R33b333b33udx|=|2j=1R3jbj33b33udx|2j=133b112βL233Λβhb12βL233u112αL233Λαhu12αL2jbj12L23jbj12L22j=133b112βL233Λβhb12βL233u112αL233Λαhu12αL2×Λβhbjγ(112β)L2Λ1+βhbj(1γ)(112β)L2jbj12β12L2×3Λβhbjγ(112α)L23Λ1+βhbj(1γ)(112α)L23jbj12α12L2u112αH3b12αH3Λαhu12αH3Λβhb212αH3. (3.22)

    Utilizing Young's inequality, combining with (3.13)–(3.22), we have

    I3(τ)bH3ΛαhuH3ΛβhbH3+u112αH3b12αH3Λαhu12αH3Λβhb212αH3(uH3+bH3)(Λαhu2H3+Λβhb2H3).

    Now, we try to bound I4, and we split it into three parts,

    I4=3i=1R33i(ub)3ibdx=3i=1(R33iub3ibdx+3R32iuib3ibdx+3R3iu2ib3ibdx)=I41+3I42+3I43. (3.23)

    Similarly as I31, I41 can be divided directly into three parts,

    I41=3i=1R33iub3ibdx=2i=1R33iub3ibdxR333uhhb33bdxR333u33b33bdx=I411+I412+I413,

    and each term can be bounded by Lemma 1.2 and G-N interpolation inequality. Same as (3.14)–(3.15), we have

    |I411|=|2i=1R33iub3ibdx|2i=13iu112αL23iΛαhu12αL23ib112βL23iΛβhb12βL2b12L23b12L2bH3ΛαhuH3ΛβhbH3 (3.24)

    and

    |I412|=|R333uhhb33bdx|33uh|112αL233Λαhuh12αL233b112βL233Λβhb12βL2hb12L2h3b12L2u112αH3b12αH3Λαhu12αH3Λβhb212αH3. (3.25)

    By u=0 and 3Λβhb1β1L2b1β1H3,

    |I413|=|R333u33b33bdx|=|2j=1R323juj3b33bdx|2j=123juj112αL223Λα3juj12αL23b112βL23Λβhb12βL233b112βL233Λβhb12βL22j=123Λαhujγ(112α)L223Λ1+αhuj(1γ)(112α)L233Λαhuγ12αL223Λα+1hu(1γ)12αL2×3b112βL23Λβhb1β1L23Λβhb112βL233b112βL233Λαhb12βL2bH3ΛαhuH3ΛβhbH3. (3.26)

    Similarity, I42 can also be divided directly into three terms,

    I42=3i=1R32iuib3ibdx=2i=1R32iuib3ibdxR323uhh3b33bdxR323u323b33bdx=I421+I422+I423.

    Then, Lemma 1.2 and (3.17)–(3.18) imply

    |I421|=|2i=1R32iuib3ibdx|2i=12iu112αL22iΛαhu12αL23ib112βL23iΛβhb12βL2ib12L2i3b12L2bH3ΛαhuH3ΛβhbH3 (3.27)

    and

    |I422|=|R323uhh3b33bdx|23uh112αL223Λαhuh12αL233b112βL233Λβhb12βL2h3b12L2h23b12L2u112αH3b12αH3Λαhu12αH3Λβhb212αH3. (3.28)

    I423 can also be bounded via u=0, Lemma 1.2 and G-N interpolation inequality,

    |I423|=|R323u323b33bdx|=|2j=1R33juj23b33bdx|2j=123b112βL223Λβhb12βL233b112βL233Λβhb12βL23juj12L223juj12L22j=123b112βL223Λβhb12βL233b112βL233Λβhb12βL2×3Λαhujγ(112β)L23Λ1+αhuj(1γ)(112β)L23juj12β12L2×23Λαhujγ(112β)L223Λ1+αhuj(1γ)(112β)L223juj12β12L2u1β1H3b21βH3Λαhu21βH3Λβhb1βH3. (3.29)

    To deal with I43, we rewrite it as

    I43=3i=1R3iu2ib3ibdx=2i=1R3iu2ib3ibdxR33uhh23b33bdxR33u333b33bdx=I431+I432+I433.

    Again, by Lemma 1.2 and G-N interpolation inequality,

    |I431|=|2i=1R3iu2ib3ibdx|2i=12ib112βL22iΛβhb12βL23ib112βL23iΛβhb12βL2iu12L2i3u12L22i=1iΛβhbγ(112β)L2iΛ1+βhb(1γ)(112β)L22iΛβhb12βL2×2iΛβhbγ(112β)L22iΛ1+βhb(1γ)(112β)L23iΛβhb12βL2iu12L2i3u12L2uH3Λβhb2H3. (3.30)

    The estimate for I432 is more complex, and utilizing Lemma 1.2 and G-N interpolation inequality, we have

    |I432|=|R33uhh23b33bdx|3uh112αL23Λαhuh12αL233b112βL233Λβhb12βL2h23b112βL2h23Λα3b12βL23uh112αL233b112βL233Λβhb12βL2h23Λα3b12βL2×3Λαhuhθ12αL23Λαhuh(1θ)12αL2h23bθ(112β)L2h23b(1θ)(112β)L23uh112αL233b112βL233Λβhb12βL233Λβhbγ12βL223Λ1+βhb(1γ)12βL2×3Λαhuhθ12αL23Λαhuh(1θ)12αL2×h23bθ(112β)L2Λβh23bγ(1θ)(112β)L2Λ1+βh23b(1γ)(1θ)(112β)L2u(112α)+θ12αH3b(112β)+θ(112β)H3Λαhu(1θ)12αH3Λβhb(1θ)(112β)+1βH3, (3.31)

    where θ=12α+12β112α12β+1,1θ=21β12α12β+1. It is worth noting that

    3Λαhuh12αL2h23b112βL2

    allows us to extract part of

    3Λαhuhθ12αL2h23bθ(112β)L2

    which can be bounded by uθ12αH3 and bθ(112β)H3, and this brings us the hope of controlling I432 suitably. We estimate I433 by the same way as I423, which is

    |I433|=|R33u333b33bdxdx|=|2j=1R3juj33b33bdx|2j=133b21βL233Λβhb1βL2juj12L23juj12L22j=133b21βL233Λβhb1βL2Λαhujγ(112β)L2Λ1+αhuj(1γ)(112β)L2juj12β12L2×3Λαhujγ(112β)L23Λ1+αhuj(1γ)(112β)L23juj12β12L2u1β1H3b21βH3Λαhu21βH3Λβhb1βH3. (3.32)

    Combining with (3.23)–(3.32), we obtain

    I4(τ)uH3Λβhb2H3+bH3ΛαhuH3ΛβhbH3+u112αH3b12αH3Λαhu12αH3Λβhb212αH3+u1β1H3b21βH3Λαhu21βH3Λβhb1βH3+u(112α)+θ12αH3b(112β)+θ(112β)H3Λαhu(1θ)12αH3Λβhb(1θ)(112β)+1βH3(uH3+bH3)(Λαhu2H3+Λβhb2H3).

    It remains to estimate I5, and since the estimation in I5 is similar to what is done in I2I4, we will omit the specific calculation process for I5.

    I5=3i=1R3[3i(bu)b3iu]3ibdx=3i=1(R33ibu3ibdx+3R32ibiu3ibdx+3R3ib2iu3ibdx)=I51+3I52+3I53. (3.33)

    We turn to estimate I51,

    I51=3i=1R33ibu3ibdx=2i=1R33ibu3ibdx+R333bhhu33bdx+R333b33u33bdx=I511+I512+I513.

    By Lemma 1.2 and G-N interpolation inequality,

    |I511|=|2i=1R33ibu3ibdx|uH3Λβhb2H3, (3.34)
    |I512|=|R333bhhu33bdx|u1β1H3b21βH3Λαhu21βH3Λβhb1βH3 (3.35)

    and

    |I513|=|R333b33u33bdx|=|2j=1R323jbj3u33bdx|u(112α)+θ12αH3b(112β)+θ(112β)H3Λαhu(1θ)12αH3Λβhb(1θ)(112β)+1βH3, (3.36)

    where θ=12α+12β112α12β+1,1θ=21β12α12β+1. Now, we focus on I52 and set

    I52=3i=1R32ibiu3ibdx=2i=1R32ibiu3ibdx+R323bhh3u33bdx+R323b323u33bdx=I521+I522+I523.

    By Lemma 1.2 and G-N interpolation inequality,

    |I521|=|2i=1R32ibiu3ibdx|uH3Λβhb2H3, (3.37)
    |I522|=|R323bhh3u33bdx|u1β1H3b21βH3Λαhu21βH3Λβhb1βH3 (3.38)

    and

    |I523|=|R323b323u33bdx|=|2j=1R33jbj23u33bdx|u112αH3b12αH3Λαhu12αH3Λβhb212αH3. (3.39)

    We try to bound I53,

    I53=3i=1R3ib2iu3ibdx=2i=1R3ib2iu3ibdx+R33bhh23u33bdx+R33b333u33bdx=I531+I532+I533.

    Again, by Lemma 1.2 and G-N interpolation inequality,

    |I531|=|2i=1R3ib2iu3ibdx|bH3ΛαhuH3ΛβhbH3, (3.40)
    |I532|=|R33bhh23u33bdx|bH3ΛαhuH3ΛβhbH3 (3.41)

    and

    |I533|=|R33b333u33bdx|=|2j=1R3jbj33u33bdx|u112αH3b12αH3Λαhu12αH3Λβhb212αH3. (3.42)

    Combined with (3.33)–(3.42), we obtain

    I5(τ)uH3Λβhb2H3+bH3ΛαhuH3ΛβhbH3+u1β1H3b21βH3Λαhu21βH3Λβhb1βH3+u112αH3b12αH3Λαhu12αH3Λβhb212αH3+u(112α)+θ12αH3b(112β)+θ(112β)H3Λαhu(1θ)12αH3Λβhb(1θ)(112β)+1βH3(uH3+bH3)(Λαhu2H3+Λβhb2H3).

    Adding (3.1), (3.2) and integrating in time,

    E(t)E(0)+t0I2(τ)+I3(τ)+I4(τ)+I5(τ)dτ,

    and inserting all the bounds obtained above for I2 through I5, we obtain (1.6). For example, the bounds for I2 yield

    t0|I2(τ)|dτt0uH3Λαhu2H3dτsupτ[0,t]u(τ)H3t0Λαhu2H3dτE(t)32.

    The time integrals of I3I5 are similarly bounded, which completes the proof of (1.6).

    Ji is supported by the National Natural Science Foundation of China (NNSFC) under grant number 12001065 and Creative Research Groups of the Natural Science Foundation of Sichuan under grant number 2023NSFSC1984. The authors are grateful to the referee for careful reading of the paper and valuable suggestions and comments.

    The authors declare no conflict of interest.



    [1] P. A. Davidson, An introduction to magnetohydrodynamics, Cambridge: Cambridge University Press, 2001. https://doi.org/10.1017/CBO9780511626333
    [2] D. Biskamp, Nonlinear magnetohydrodynamics, Cambridge, New York: Cambridge University Press, 1993. https://doi.org/10.1017/CBO9780511599965
    [3] H. Alfvén, Existence of electromagnetic-hydrodynamic vaves, Nature, 150 (1942), 405–406. https://doi.org/10.1038/150405d0 doi: 10.1038/150405d0
    [4] B. Dong, Y. Jia, J. Li, J. Wu, Global regularity for the 2D magnetohydrodynamics equations with horizontal dissipation and horizontal magnetic diffusion, J. Math. Fluid Mech., 20 (2018), 1541–1565. https://doi.org/10.1007/s00021-018-0376-3 doi: 10.1007/s00021-018-0376-3
    [5] Y. Dai, R. Ji, J. Wu, Unique weak solutions of the magnetohydrodynamic equations with fractional dissipation, Z. Angew. Math. Mech., 100 (2020), e201900290. https://doi.org/10.1002/zamm.201900290 doi: 10.1002/zamm.201900290
    [6] Y. Dai, Z. Tan, J. Wu, A class of global large solutions to the magnetohydrodynamic equations with fractional dissipation, Z. Angew. Math. Phys., 70 (2019), 153. https://doi.org/10.1007/s00033-019-1193-0 doi: 10.1007/s00033-019-1193-0
    [7] M. Sermange, R. Temam, Some mathematical questions related to the MHD equations, Commun. Pure Appl. Math., 36 (1983), 635–664. https://doi.org/10.1002/cpa.3160360506 doi: 10.1002/cpa.3160360506
    [8] J. Wu, Generalized MHD equations, J. Differ. Equations, 195 (2003), 284–312. https://doi.org/10.1016/j.jde.2003.07.007 doi: 10.1016/j.jde.2003.07.007
    [9] J. Wu, Global regularity for a class of generalized magnetohydrodynamic equations, J. Math. Fluid Mech., 13 (2011), 295–305. https://doi.org/10.1007/s00021-009-0017-y doi: 10.1007/s00021-009-0017-y
    [10] J. Wu, The 2D magnetohydrodynamic equations with partial or fractional dissipation, In: Lectures on the analysis of nonlinear partial differential equations: part 5, International Press of Boston, Inc., 2018,283–332.
    [11] K. Yamazaki, On the global well-posedness of N-dimensional generalized MHD system in anisotropic spaces, Adv. Differential Equations, 19 (2014), 201–224. https://doi.org/10.57262/ade/1391109084 doi: 10.57262/ade/1391109084
    [12] W. Yang, Q. Jiu, J. Wu, The 3D incompressible magnetohydrodynamic equations with fractional partial dissipation, J. Differ. Equations, 266 (2019), 630–652. https://doi.org/10.1016/j.jde.2018.07.046 doi: 10.1016/j.jde.2018.07.046
    [13] S. Abe, S. Thurner, Anomalous diffusion in view of Einsteins 1905 theory of Brownian motion, Physica A, 356 (2005), 403–407. https://doi.org/10.1016/j.physa.2005.03.035 doi: 10.1016/j.physa.2005.03.035
    [14] M. Jara, Nonequilibrium scaling limit for a tagged particle in the simple exclusion process with long jumps, Commun. Pure Appl. Math., 62 (2009), 198–214. https://doi.org/10.1002/cpa.20253 doi: 10.1002/cpa.20253
    [15] U. Frisch, S. Kurien, R. Pandit, W. Pauls, S. Ray, A. Wirth, et al., Hyperviscosity, Galerkin truncation, and bottlenecks in turbulence, Phys. Rev. Lett., 101 (2008), 144501. https://doi.org/10.1103/PhysRevLett.101.144501 doi: 10.1103/PhysRevLett.101.144501
    [16] K. Yamazaki, On the global regularity of two-dimensional generalized magnetohydrodynamics system, J. Math. Anal. Appl., 416 (2014), 99–111. https://doi.org/10.1016/j.jmaa.2014.02.027 doi: 10.1016/j.jmaa.2014.02.027
    [17] K. Yamazaki, Global regularity of logarithmically supercritical MHD system with zero diffusivity, Appl. Math. Lett., 29 (2014), 46–51. https://doi.org/10.1016/j.aml.2013.10.014 doi: 10.1016/j.aml.2013.10.014
    [18] K. Yamazaki, Global regularity of logarithmically supercritical MHD system with improved logarithmic powers, Dynam. Part. Differ. Eq., 15 (2018), 147–173. https://doi.org/10.4310/DPDE.2018.v15.n2.a4 doi: 10.4310/DPDE.2018.v15.n2.a4
    [19] Z. Ye, X. Xu, Global regularity of the two-dimensional incompressible generalized magnetohydrodynamics system, Nonlinear Anal., 100 (2014), 86–96. https://doi.org/10.1016/j.na.2014.01.012 doi: 10.1016/j.na.2014.01.012
    [20] Z. Ye, Remark on the global regularity of 2D MHD equations with almost Laplacian magnetic diffusion, J. Evol. Equ., 18 (2018), 821–844. https://doi.org/10.1007/s00028-017-0421-3 doi: 10.1007/s00028-017-0421-3
    [21] Q. Jiu, J. Zhao, A remark on global regularity of 2D generalized magnetohydrodynamic equations, J. Math. Anal. Appl., 412 (2014), 478–484. https://doi.org/10.1016/j.jmaa.2013.10.074 doi: 10.1016/j.jmaa.2013.10.074
    [22] Q. Jiu, J. Zhao, Global regularity of 2D generalized MHD equations with magnetic diffusion, Z. Angew. Math. Phys., 66 (2015), 677–687. https://doi.org/10.1007/s00033-014-0415-8 doi: 10.1007/s00033-014-0415-8
    [23] C. Tran, X. Yu, Z. Zhai, On global regularity of 2D generalized magnetohydrodynamic equations, J. Differ. Equations, 254 (2013), 4194–4216. https://doi.org/10.1016/j.jde.2013.02.016 doi: 10.1016/j.jde.2013.02.016
    [24] J. Wu, Regularity criteria for the generalized MHD equations, Commun. Part. Diff. Eq., 33 (2008), 285–306. https://doi.org/10.1080/03605300701382530 doi: 10.1080/03605300701382530
    [25] K. Yamazaki, Remarks on the global regularity of the two-dimensional magnetohydrodynamics system with zero dissipation, Nonlinear Anal., 94 (2014), 194–205. https://doi.org/10.1016/j.na.2013.08.020 doi: 10.1016/j.na.2013.08.020
    [26] B. Yuan, L. Bai, Remarks on global regularity of 2D generalized MHD equations, J. Math. Anal. Appl., 413 (2014), 633–640. https://doi.org/10.1016/j.jmaa.2013.12.024 doi: 10.1016/j.jmaa.2013.12.024
    [27] Y. Cai, Z. Lei, Global well-posedness of the incompressible magnetohydrodynamics, Arch. Rational Mech. Anal., 228 (2018), 969–993. https://doi.org/10.1007/s00205-017-1210-4 doi: 10.1007/s00205-017-1210-4
    [28] L. He, L. Xu, P. Yu, On global dynamics of three dimensional magnetohydrodynamics: nonlinear stability of Alfvén waves, Ann. PDE, 4 (2018), 5. https://doi.org/10.1007/s40818-017-0041-9 doi: 10.1007/s40818-017-0041-9
    [29] R. Pan, Y. Zhou, Y. Zhu, Global classical solutions of three dimensional viscous MHD system without magnetic diffusion on periodic boxes, Arch. Rational Mech. Anal., 227 (2018), 637–662. https://doi.org/10.1007/s00205-017-1170-8 doi: 10.1007/s00205-017-1170-8
    [30] D. Wei, Z. Zhang, Global well-posedness of the MHD equations in a homogeneous magnetic field, Anal. PDE, 10 (2017), 1361–1406. https://doi.org/10.2140/apde.2017.10.1361 doi: 10.2140/apde.2017.10.1361
    [31] J. Pedlosky, Geophysical fluid dynamics, New York: Springer, 1987. https://doi.org/10.1007/978-1-4612-4650-3
    [32] N. Boardman, H. Lin, J. Wu, Stabilization of a background magnetic field on a 2D magnetohydrodynamic flow, SIAM J. Math. Anal., 52 (2020), 5001–5035. https://doi.org/10.1137/20M1324776 doi: 10.1137/20M1324776
    [33] C. Cao, J. Wu, B. Yuan, The 2D incompressible magnetohydrodynamics equations with only magnetic diffusion, SIAM J. Math. Anal., 46 (2014), 588–602. https://doi.org/10.1137/130937718 doi: 10.1137/130937718
    [34] B. Dong, J. Li, J. Wu, Global regularity for the 2D MHD equations with partial hyperresistivity, Int. Math. Res. Notices, 14 (2019), 4261–4280. https://doi.org/10.1093/imrn/rnx240 doi: 10.1093/imrn/rnx240
    [35] R. Ji, H. Lin, J. Wu, L. Yan, Stability for a system of the 2D magnetohydrodynamic equations with partial dissipation, Appl. Math. Lett., 94 (2019), 244–249. https://doi.org/10.1016/j.aml.2019.03.013 doi: 10.1016/j.aml.2019.03.013
    [36] R. Ji, J. Wu, W. Yang, Stability and optimal decay for the 3D Navier-Stokes equations with horizontal dissipation, J. Differ. Equations, 290 (2021), 57–77. https://doi.org/10.1016/j.jde.2021.04.026 doi: 10.1016/j.jde.2021.04.026
    [37] Q. Jiu, D. Niu, J. Wu, X. Xu, H. Yu, The 2D magnetohydrodynamic equations with magnetic diffusion, Nonlinearity, 28 (2015), 3935–3955. https://doi.org/10.1088/0951-7715/28/11/3935 doi: 10.1088/0951-7715/28/11/3935
    [38] H. Lin, R. Ji, J. Wu, L. Yan, Stability of perturbations near a background magnetic field of the 2D incompressible MHD equations with mixed partial dissipation, J. Funct. Anal., 279 (2020), 108519. https://doi.org/10.1016/j.jfa.2020.108519 doi: 10.1016/j.jfa.2020.108519
    [39] J. Wu, Y. Zhu, Global solutions of 3D incompressible MHD system with mixed partial dissipation and magnetic diffusion near an equilibrium, Adv. Math., 377 (2021), 107466. https://doi.org/10.1016/j.aim.2020.107466 doi: 10.1016/j.aim.2020.107466
    [40] Y. Zhou, Y. Zhu, Global classical solutions of 2D MHD system with only magnetic diffusion on periodic domain, J. Math. Phys., 59 (2018), 081505. https://doi.org/10.1063/1.5018641 doi: 10.1063/1.5018641
    [41] P. Mironescu, H. Brezis, Gagliardo-Nirenberg inequalities and non-inequalities: the full story, Ann. Inst. H. Poincaré Anal. Non Linéaire, 35 (2018), 1355–1376. https://doi.org/10.1016/j.anihpc.2017.11.007 doi: 10.1016/j.anihpc.2017.11.007
    [42] E. Gagliardo, Ulteriori proprietà di alcune classi di funzioni in pià variabili, Ricerche Mat., 8 (1959), 24–51.
    [43] L. Nirenberg, On elliptic partial differential equations, Ann. Scuola Norm. Sup. Pisa, 13 (1959), 115–162.
    [44] T. Tao, Nonlinear dispersive equations: local and global analysis, Providence, RI: American Mathematical Society, 2006.
    [45] C. Cao, D. Regmi, J. Wu, The 2D MHD equations with horizontal dissipation and horizontal magnetic diffusion, J. Differ. Equations, 254 (2013), 2661–2681. https://doi.org/10.1016/j.jde.2013.01.002 doi: 10.1016/j.jde.2013.01.002
    [46] C. Cao, J. Wu, Global regularity for the 2D MHD equations with mixed partial dissipation and magnetic diffusion, Adv. Math., 226 (2011), 1803–1822. https://doi.org/10.1016/j.aim.2010.08.017 doi: 10.1016/j.aim.2010.08.017
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