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Research article

Stability of the 3D incompressible MHD equations with horizontal dissipation in periodic domain

  • Received: 28 May 2021 Accepted: 09 August 2021 Published: 13 August 2021
  • MSC : 35A05, 35Q35, 76D03

  • The stability problem on the magnetohydrodynamics (MHD) equations with partial or no dissipation is not well-understood. This paper focuses on the 3D incompressible MHD equations with mixed partial dissipation and magnetic diffusion. Our main result assesses the stability of perturbations near the steady solution given by a background magnetic field in periodic domain. The new stability result presented here is among few stability conclusions currently available for ideal or partially dissipated MHD equations.

    Citation: Ruihong Ji, Ling Tian. Stability of the 3D incompressible MHD equations with horizontal dissipation in periodic domain[J]. AIMS Mathematics, 2021, 6(11): 11837-11849. doi: 10.3934/math.2021687

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  • The stability problem on the magnetohydrodynamics (MHD) equations with partial or no dissipation is not well-understood. This paper focuses on the 3D incompressible MHD equations with mixed partial dissipation and magnetic diffusion. Our main result assesses the stability of perturbations near the steady solution given by a background magnetic field in periodic domain. The new stability result presented here is among few stability conclusions currently available for ideal or partially dissipated MHD equations.



    In recent few years, there have been substantial developments concerning the MHD equations, especially there is only partial or fractional dissipation. The MHD equations govern the motion of electrically conducting fluids such as plasmas, liquid metals, and electrolytes. The fundamental concept behind MHD is that magnetic fields can induce currents in a moving conductive fluid, which in turn polarizes the fluid and reciprocally changes the magnetic field itself. The set of equations that describe MHD are a combination of the Navier-Stokes equations of fluid dynamics and Maxwell's equations of electromagnetism. Since their initial derivation by the Nobel Laureate H. Alfvén [1] in 1924, the MHD equations have played vital roles in the study of many phenomena in geophysics, astrophysics, cosmology and engineering (see, e.g., [2,3]).

    This paper establishes the stability of perturbations near a background magnetic field of the 3D MHD equations with mixed partial dissipation and magnetic diffusion in periodic domain.

    {tu+uu=P+ν Δhu+BB,xΩ,t>0,tB+uB=ηΔhB+Bu,xΩ,t>0,u=B=0,xΩ,t>0, (1.1)

    where u denotes the velocity field of the fluid, P the total pressure, B the magnetic field, ν>0 and η>0 are the viscosity and the magnetic diffusivity. We define the 3D periodic space domain Ω=[0,L]2×R, the periodic solution means u(x+ei,t)=u(x,t)(i=1,2,3), for all x and t0, where ei are the standard basis vectors, e1=(1,0,0)t. We know that (1.1) admits the following steady state solution

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

    It is clear that a special solution of (1.1) is given by the zero velocity field and the background magnetic fields B(0)=(1,0,0). The perturbation (u,b) with b=BB(0) obeys,

    {tu+uu=P+ν Δhu+bb+1b,xΩ,t>0,tb+ub=ηΔhb+bu+1u,xΩ,t>0,u=b=0,xΩ,t>0, (1.2)

    where, for notational convenience, we write

    i=xi,h=(1,2),h=21+22.

    In addition, for convenience, we define the norm for the Lp(Ω) space, for p[1,], is denoted by fp. The inner product of f and g in the Lp(Ω) space is denoted by (f,g)=Ωfgdx1dx2dx3:=Ωfgdx. Respectively, the horizontal flow is defined in Ω with [0,L]2udx=0 and [0,L]2bdx=0.

    This paper aims at the stability problem on the perturbation of (1.1) near (u(0),B(0)). Equivalently, we establish a small data global well-posedness result for (1.2) supplemented with the initial condition

    u(x,0)=u0(x),b(x,0)=b0(x).

    Our main result can be stated as follows.

    Theorem 1.1. Consider (1.2) with initial data (u0,b0)H2(Ω) satisfies u0=b0=0,[0,L]2u0dx=0 and [0,L]2b0dx=0. Then there exists a constant δ=δ(ν,η)>0 such that, if

    (u0,b0)H2δ, (1.3)

    then (1.2) has a unique global solution

    (u,b)L(0,;H2(Ω)),hu,hbL2(0,;H2(Ω)), (1.4)

    satisfying

    supτ[0,t](u(τ)2H2+b(τ)2H2)+2νt0hu(τ)2H2dτ+2ηt0hb(τ)2H2dτCδ2, (1.5)

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

    The MHD equation, especially those with partial dissipation have recently attracted considerable interests. There are substantial developments on two fundamental problems, the global regularity and stability problems, which have been successfully established by many authors via different approaches [4,5,6,7]. In particular, it is also worth mentioning the beautiful work of [8], which made further progress by providing the stability of perturbations near a background magnetic field of the 3D incompressible MHD equation with mixed partial dissipation and deal with the H3-estimate. To give a more complete views of current studies on the stability, we also mention some of exciting results in [9,10,11,12]. In this paper, we mainly deal with the H2-estimate for the solution of (1.2). The stability of the incompressible MHD equation with mixed partial dissipation is not well-solved, except in the periodic case. Our study of the stability problem on (1.2) is inspired by the recent important result in [13], which is different with the whole region is that helps to solve the periodic problem.

    We employ the bootstrapping argument to prove the desired H2-stability. And we define the H2-energy E(t) by

    E(t)=supτ[0,t](u(τ)2H2+b(τ)2H2)+2νt0hu(τ)2H2dτ+2ηt0hb(τ)2H2dτ,

    and prove that, for a constant C>0 and any t0,

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

    Once (1.6) is established, an application of the bootstrapping argument would imply the desired global stability. The details are given in section 2. Due to the presence of the anisotropic dissipation, we make use of anisotropic estimates for triple products (see Lemma 2.1 in section 2).

    The proof of Theorem 1.1 is not trivial. A natural starting point is to bound uH3+bH3 via the energy estimates. However, due to the lack of the vertical dissipation, some of the nonlinear terms can not be controlled in terms of uH3+bH3 or the dissipation parts huH3 and hbH3. Thus, we show the stability of equations (1.1) by bootstrapping argument which will be shown in section 3, and we also show the uniqueness in that section.

    This section applies the bootstrapping argument to prove Theorem 1.1. In addition, we provide the anisotropic inequality to be used in the proof of (2.1) in the subsequent section.

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

    E(t)M,

    and show 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 bootstrapping principle can be found in T. Tao's book (see[14]). To apply the bootstrapping argument to (2.1), we assume that

    E(t)M=14C2, (2.1)

    When (2.1) holds, we have

    CE(t)1212.

    It then follows from (1.6) that

    E(t)E(0)+12E(t)  or  E(t)2E(0), (2.2)

    if we choose δ>0 sufficiently small such that

    δ2M4,

    then (1.3) and (2.2) imply that

    E(t)12M,

    the bootstrapping argument then leads to the desired global bound

    E(t)M,

    this completes the proof of Theorem 1.1.

    As usual, the Sobolev space H1(Ω)={fL2(Ω):fL2(Ω)}. In addition, we define the following Hilbert space,

    H1h(Ω)={fL2(Ω):hfL2(Ω)},

    that features the inner product (f,g)H1h(Ω)=(f,g)L2(Ω)+(hf,hg)L2(Ω).

    The rest of this section provides the anisotropic inequality. The MHD system examined in this paper involves the estimates of quite a few triple terms. Anisotropic inequality appears to be necessary to deal with such partially dissipated system.

    Lemma 2.1. Let fH1(Ω), gH1h(Ω), hL2(Ω). Then,

    Ω|fgh|dxC(f2+hf2)12(f2+3f2)12g122(g2+hg2)12h2.

    The proof of Lemma 2.1 can be found in [9].

    This section proves the major estimate in (1.6), namely

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

    where E(t) is defined in (1.5). The core of the proof is to bound the H2-norm of (u,b) suitably. For the sake of clarity, the proof is divided to two main parts, the first one is devoted to the H2-stability and the second one is to the uniqueness. The local existence can be obtained by a standard approach of Friedrichs' method of cutoff in Fourier space (see, e.g., [15]), we omit the details here.

    Due to the equivalence of (u,b)H2 with (u,b)L2+(u,b)˙H2, it suffices to bound the L2-norm and the ˙H2-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)22+b(t)22+2νt0hu(τ)22dτ+2ηt0hb(τ)22dτ=u(0)22+b(0)22. (3.1)

    The rest of the proof focuses on the ˙H2-norm, applying 2i(i=1,2,3) to (1.2) and then dotting by (2iu,2ib), we find

    12ddt3i=1(2iu22+2ib22)+ν2ihu22+η2ihb22=I1+I2+I3+I4+I5, (3.2)

    where

    I1=3i=1Ω2i1b2iu+2i1u2ibdx,I2=3i=1Ω2i(uu)2iudx,I3=3i=1Ω[2i(bb)b2ib]2iudx,I4=3i=1Ω2i(ub)2ibdx,I5=3i=1Ω[2i(bu)b2iu]2ibdx.

    Note that

    Ωb2ib2iudx+Ωb2iu2ibdx=0.

    Integrating by parts and u(x+ei,t)=u(x,t)(i=1,2,3), I1=0. To bound I2, we decompose it into two pieces

    I2=3i=1Ω2i(uu)2iudx=I21+I22.

    I21 involves the favorable partial derivatives in x1 and x2, respectively. Its handling is not difficult. In contrast, I22 has partial in terms of x3 and the control of I22 is delicate.

    By Lemma 2.1 with f=kiu, g=2kiu, h=2iu and Poincaré's inequality, we obtain

    I21=2i=12k=1Ck2Ωkiu2kiu2iudxC2i=12k=1(kiu2+kihu2)12(kiu2+3kiu2)12(2kiu2+2kihu2)122kiu1222iu2C(uH2+huH2)12(uH2+huH2)12(uH2+huH2)12u12H2uH2Chu32H2u12H2uH2Chu2H2uH2, (3.3)

    where we have used the Poincaré's inequality

    uH2ChuH2.

    We further decomposed I22 into two terms

    I22=Ω23(uu)23udx=Ω23(uhhu+u33u)23udx=I221+I222.

    By Lemma 2.1,

    I221=2k=1Ck2Ωk3uh2k3hu23udxC2k=1(2k3hu2+h2k3hu2)12(2k3hu2+32k3hu2)12k3uh122(k3uh2+hk3uh2)1223u2C(uH2+huH2)12(uH2+huH2)12u12H2(uH2+huH2)12uH2CuH2hu2H2. (3.4)

    Using Lemma 2.1 and u=0, we obtain

    I222=2k=1Ck2Ωk3u32k33u23udx=2k=1Ck2Ωk13huh2k33u23udxC2k=1(k13huh2+hk13huh2)12(k13huh2+3k13huh2)123k3u122(3k3u2+h3k3u2)1223u2C(uH2+huH2)12(uH2+huH2)12u12H2(uH2+huH2)12uH2CuH2hu2H2. (3.5)

    Combining (3.3)–(3.5), we find

    I2CuH2hu2H2.

    We now turn to the estimates of I3,

    I3=3i=12k=1Ck2Ωkib2kib2iudx=I31+I32.

    By Lemma 2.1,

    I31=2i=12k=1Ck2Ωkib2kib2iudxC2i=12k=1(kib2+hkib2)12(kib2+3kib2)122kib122(2kib2+h2kib2)122iu2C(bH2+hbH2)12(bH2+hbH2)12b12H2(bH2+hbH2)12uH2CuH2hb2H2. (3.6)

    Similar to I22, I32 is naturally split into two terms

    I32=2k=1Ck2Ωk3b2k3b23udx=I321+I322.

    By Lemma 2.1,

    I321=2Ω3b3b23udxC(3b2+h3b2)12(3b2+33b2)123b122(3b2+h3b2)1223u2C(bH2+hbH2)12(bH2+bH2)12b12H2(bH2+hbH2)12uH2CuH2hb2H2. (3.7)

    Also

    I322=Ω23bb23udxC(b2+hb2)12(b2+3b2)1223b122(23b2+h23b2)1223u2C(bH2+hbH2)12(bH2+bH2)12b12H2(bH2+hbH2)12uH2CuH2hb2H2. (3.8)

    Combining(3.6)–(3.8) yields

    I3CuH2hb2H2.

    For I4,

    I4=3i=12k=1Ck2Ωkiu2kib2ibdx=I41+I42.

    By Lemma 2.1,

    I41=2i=12k=1Ck2Ωkiu2kib2ibdxC2i=12k=1(kiu2+hkiu2)12(kiu2+3kiu2)122kib122(2kib2+h2kib2)122ib2C(uH2+huH2)12(uH2+huH2)12b12H2(bH2+hbH2)12bH2CbH2hbH2huH2. (3.9)

    We decompose I42 into two terms

    I42=2k=1Ck2Ωk3u2k3b23bdx=I421+I422.

    Using Lemma 2.1,

    I421=2Ω3u3b23bdxC(3u2+h3u2)12(3u2+33u2)123b122(3b2+h3b2)1223b2.C(uH2+huH2)12(uH2+uH2)12b12H2(bH2+hbH2)12bH2CbH2hbH2huH2. (3.10)

    Similarly

    I422=Ω23ub23bdxC(b2+hb2)12(b2+3b2)1223u122(23u2+h23u2)1223b2C(bH2+hbH2)12(bH2+bH2)12u12H2(uH2+huH2)12bH2CbH2hbH2huH2. (3.11)

    Combining all the estimates(3.9) through (3.11) yields

    I4CbH2hbH2huH2.

    It remains to estimate I5,

    I5=3i=12k=1Ck2Ωkib2kiu2ibdx=I51+I52.

    By Lemma 2.1,

    I51=2i=12k=1Ck2Ωkib2kiu2ibdxC2i=12k=1(kib2+hkib2)12(kib2+3kib2)122kiu122(2kiu2+h2kiu2)122ib2C(bH2+hbH2)12(bH2+hbH2)12u12H2(uH2+huH2)12bH2CbH2huH2hbH2. (3.12)

    The difficult term is I52, which is further decomposed into two terms

    I52=2k=1Ck2Ωk3b2k3u23bdx=I521+I522.

    By Lemma 2.1,

    I521=2Ω3b3u23bdxC(3b2+h3b2)12(3b2+33b2)123u122(3u2+h3u2)1223b2.C(bH2+hbH2)12(bH2+bH2)12u12H2(uH2+huH2)12bH2CbH2huH2hbH2. (3.13)

    Similarly, I522 can be estimated as follows

    I522=Ω23bu23bdxC(u2+hu2)12(u2+3u2)1223b122(23b2+h23b2)1223b2C(uH2+huH2)12(uH2+uH2)12b12H2(bH2+hbH2)12bH2CbH2huH2hbH2. (3.14)

    Combining (3.12)–(3.14), we have

    I5CbH2huH2hbH2.

    Therefore, if we set

    E(t)=supτ[0,t](u(τ)2H2+b(τ)2H2)+2νt0hu(τ)2H2dτ+2ηt0hb(τ)2H2dτ.

    By Hölder's inequality, the time integral of the bounds for I2,I3,I4 and I5 can be estimated as follows

    t0|I2|dτCt0u(τ)H2hu(τ)2H2dτCsupτ[0,t]u(τ)H2t0hu(τ)2H2dτCE(t)32,
    t0|I3|dτCt0u(τ)H2hb(τ)2H2dτCsupτ[0,t]u(τ)H2t0hb(τ)2H2dτCE(t)32,
    t0|I4|dτCt0b(τ)H2hu(τ)H2hb(τ)H2dτCE(t)12E(t)12E(t)12=CE(t)32,t0|I5|dτCt0b(τ)H2hu(τ)H2hb(τ)H2dτCE(t)12E(t)12E(t)12=CE(t)32.

    Integrating (3.2) in time and combining with (3.1), we find

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

    A bootstrapping argument implies that, there is δ>0, such that, if E(0)<δ2, then

    E(t)Cδ2

    for a pure constant C and for all t>0, which implies H2-stability.

    This subsection proves the uniqueness part of Theorem 1.1. We show that two solutions (u(1),P(1),b(1)) and (u(2),P(2),b(2)) of (1.2) in the regularity class (1.4) must coincide. Their difference (˜u,˜P,˜b) with

    ˜u=u(1)u(2),˜P=P(1)P(2),˜b=b(1)b(2)

    satisfies, according to (1.2)

    {t˜u+u(1)˜u+˜uu(2)=˜P+ν Δh˜u+b(1)˜b+˜bb(2)+1˜b,t˜b+u(1)˜b+˜ub(2)=η Δh˜b+b(1)˜u+˜bu(2)+1˜u,u=b=0. (3.15)

    Basic energy estimates show that

    12ddt(˜u22+˜b22)+νh˜u22+ηh˜b22=K1+K2+K3+K4,

    where

    K1=Ω˜uu(2)˜udx,K2=Ω˜bb(2)˜udx,K3=Ω˜ub(2)˜bdx,K4=Ω˜bu(2)˜bdx.

    By Lemma 2.1, K1, K2, K3, K4 can be bounded as follows

    K1C(u(2)2+hu(2)2)12(u(2)2+3u(2)2)12˜u122(˜u2+h˜u2)12˜u2Chu(2)122(u(2)2+3u(2)2)12˜u2h˜u2ν6h˜u22+C˜u22hu(2)2(u(2)2+3u(2)2). (3.16)
    K2C(b(2)2+hb(2)2)12(b(2)2+3b(2)2)12˜b12L2(˜b2+h˜b2)12˜u2Chb(2)122(b(2)2+3b(2)2)12˜b122h˜b122h˜u2ν6h˜u22+η6h˜b22+C˜b22hb(2)22(b(2)2+3b(2)2)2. (3.17)
    K3C(b(2)2+hb(2)2)12(b(2)2+3b(2)2)12˜u122(˜uL2+h˜u2)12˜bL2Chb(2)122(b(2)2+3b(2)2)12˜u122h˜u122h˜b2ν6h˜u22+η6h˜b22+C˜u22hb(2)22(b(2)2+3b(2)2)2. (3.18)
    K4C(u(2)2+hu(2)2)12(u(2)2+3u(2)2)12˜b122(˜b2+h˜b2)12˜b2Chu(2)122(u(2)2+3u(2)2)12˜b2h˜b2ν6h˜b22+C˜b22hu(2)2(u(2)2+3u(2)2). (3.19)

    Combining (3.16)–(3.19), we set Y(t)=(˜u(t)22+˜b(t)22),

    ddtY(t)+νh˜u22+ηh˜b22a(t)Y(t), (3.20)

    where

    a(t)=Chu(2)2(u(2)2+3u(2)2)+Chb(2)22(b(2)2+3b(2)2)2.

    Since (u(2),b(2)) is in the regularity class (1.4). For any T>0, we have

    T0a(t)dtCT0hu(2)2(u(2)2+3u(2)2)+hb(2)22(b(2)2+3b(2)2)2dtCT0hu(2)2H2+hb(2)2H2b(2)2H2dtCT0hu(2)2H2dt+Csupτ[0,t]b(2)2H2T0hb(2)2H2dtC(T)<+.

    Gronwall's inequality applied to (3.20) implies that, for any T>0,

    ˜u(t)22+˜b(t)22(˜u(0)22+˜b(0)22)eCT0a(t)dtC(˜u(0)22+˜b(0)22). (3.21)

    In particular, the initial values of the two solutions in the regularity class (1.4), then (3.21) implies Y(t)=˜u(t)22+˜b(t)220 for any T>0. This completes the proof of the uniqueness.

    In this paper, we gave the stability of the 3D incompressible MHD equations near a background magnetic field with horizontal dissipation in periodic domain by bootstrapping argument. The main part of bootstrapping argument relies on proof of inequality (2.1). We get through it by the anisotropic inequality, and Poincaré's inequality helps a lot in periodic domain.

    We would like to thank the referees for giving us many helpful suggestions in improving our paper. Ji is supported by the National Natural Science Foundation of China (NSFC) under grant number 12001065.

    The authors declare no conflict of interest.



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