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Global stability solution of the 2D incompressible anisotropic magneto-micropolar fluid equations

  • In this paper, we consider the two dimensional incompressible anisotropic magneto-micropolar fluid equations with partial mixed velocity dissipations, magnetic diffusion and horizontal vortex viscosity, and analyze the stability near a background magnetic field. At present, major works on the equations of magneto-micropolar fluid mainly focus on the global regularity of the solutions. While the stability of the solutions remains an open problem. This paper concentrates on establishing the stability for the linear and nonlinear system respectively. Two goals have been achieved. The first is to obtain the explicit decay rates for the solution of the linear system in Hs(R2) Sobolev space. The second assesses the nonlinear stability by establishing the a priori estimate and employing bootstrapping arguments. Our results reveal that any perturbations near a background magnetic field is globally stable in Sobolev space H2(R2).

    Citation: Ru Bai, Tiantian Chen, Sen Liu. Global stability solution of the 2D incompressible anisotropic magneto-micropolar fluid equations[J]. AIMS Mathematics, 2022, 7(12): 20627-20644. doi: 10.3934/math.20221131

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  • In this paper, we consider the two dimensional incompressible anisotropic magneto-micropolar fluid equations with partial mixed velocity dissipations, magnetic diffusion and horizontal vortex viscosity, and analyze the stability near a background magnetic field. At present, major works on the equations of magneto-micropolar fluid mainly focus on the global regularity of the solutions. While the stability of the solutions remains an open problem. This paper concentrates on establishing the stability for the linear and nonlinear system respectively. Two goals have been achieved. The first is to obtain the explicit decay rates for the solution of the linear system in Hs(R2) Sobolev space. The second assesses the nonlinear stability by establishing the a priori estimate and employing bootstrapping arguments. Our results reveal that any perturbations near a background magnetic field is globally stable in Sobolev space H2(R2).



    The incompressible magneto-micropolar fluid equations describes the motion of an incompressible conducting micropolar fluid in an arbitrary magnetic field. In this paper, we consider the 2D incompressible anisotropic magneto-micropolar fluid equations,

    {tu1+uu1+1P=(μ+χ)22u1+BB12χ2m,xR2,t>0tu2+uu2+2P=(μ+χ)21u2+BB2+2χ1m,tB+uB=ν21B+Bu,tm+um+4χm=κ21m+2χ×u,u=0,B=0, (1.1)

    where u=(u1,u2), b=(b1,b2), m=(2m,1m). Also m and P are the scalars. The nonnegative parameters μ>0, ν>0 and χ>0 denote the kinematic viscosity, magnetic diffusion coefficient and the dynamic micro-rotation viscosity. Besides, γ and κ are the angular viscosities. The operators 1, 2 represent the horizontal and vertical direction respectively.

    Our goal is to investigate the stability problem on the perturbation (u,b,m) near the steady solution (u0,B0,m0) with b=BB0. Here

    u0=(0,0),B0=(0,1),m0=0.

    Without loss of generality, set μ=χ=12 and ν=κ=1. It is easy to verify that (u,b,m) satisfies

    {tu1+uu1+1P=22u1+bb12m+2b1,tu2+uu2+2P=21u2+bb2+1m+2b2,tb+ub=21b+bu+2u,tm+um+2m=21m+×u,u=b=0. (1.2)

    The standard magneto-micropolar fluid equations with full velocity field dissipation, magnetic diffusion and angular viscosities can be written as

    {tu+(u)u+P=(μ+χ)Δu+(B)B+2χ×m,tB+(u)B=νΔB+(B)u,tm+(u)m+4χm=γΔm+2χ×m+κdivm,u=B=0. (1.3)

    Because of the mathematically significant, the magneto-micropolar fluid equations and closely related equations have attracted considerable attentions for mathematical scholars and many important results have been achieved. Major works mainly concentrated on the global well-posedness and global regularity of the solution. Let's recall some of these results.

    For the 2D incompressible magneto-micropolar equations, Yuan and Qiao [1] established the global smooth solution for the equations with zero angular viscosity and zero magnetic diffusion or with only angular viscosity and magnetic diffusion. In a two dimensional bounded domain with Navier type boundary condition for the velocity, Fan and Zhou [2] proved the existence and uniqueness of global strong solutions to the incompressible magneto-micropolar system. Ma in [3] obtained the global existence and regularity of classical solutions to the equations with mixed partial dissipation, magnetic diffusion and angular viscosity. In addition, some conditional regularity of strong solutions also be obtained. Guo and Shang in [4] showed the global regularity of solutions to the 2D incompressible magneto-micropolar equations with partial dissipation. For 212 dimensional system, the results of the global well-posedness for the incompressible magneto-micropolar fluid equations with mixed partial dissipation have been obtained (see e.g., [5,6]). Besides, for 3D case, the global existence results for the Cauchy problem in R3 are obtained by Tan and Wu in [7]. The global well-posedness and global regularity of the incompressible magneto-micropolar system have been studied in [8,9]. For more results, we refer to [7,10,11,12,13,14] and references therein.

    However, there are few results to our knowledge on the large-time behavior of the magneto-micropolar fluids. Shang and Gu [15] obtained the L2-decay estimates of solutions for the two-dimensional incompressible magneto-micropolar fluid equations, which is u(t)L2+w(t)L2C(1+t)43 and bL2C(1+t)12. Moreover, by proving the optimal decay for b(t)L, the authors optimized the decay rates to u(t)L2+w(t)L2Ct2 in [15]. In this paper, we will show decay rates for the linear system (1.2) in the next section.

    If the magnetic field B=0, the equations (1.3) become the micropolar fluid equations. For the 2D incompressible micropolar equations, Liu in [16] studied the global well-posedness to the Cauchy problem of 2D micropolar equations with large initial data and vacuum, and showed that the problem admits a unique global strong solution. Ye [17] studied the global regularity for the system of the 2D incompressible micropolar equations with vertical dissipation in the horizontal velocity equation, horizontal dissipation in the vertical velocity equation. Dong and Li [18] studied the global regularity in time and large time behavior of solutions to the 2D micropolar equations with only angular viscosity dissipation. The more results of the well-posedness, regularity and large time decay problems on the micropolar fluid equations can be shown in [19,20,21,22]. On the other hand, if χ=0 and m=0, the equations in (1.3) reduce to the magneto-hydrodynamic equations (MHD). The case of full dissipation and magnetic diffusion, the classical solution is global (see e.g., [23]). There are numerous works on the global regularity and the stability. One of the significant works on the global regularity for the 2D MHD equations with mixed partial dissipation and magnetic diffusion is completed by Wu and Cao in [24]. One can also refer to [25,26,27,28,29] and so on.

    Motivated by the results of the magneto-micropolar fluid equations and closely related equations, this paper investigates the stability of the solution of the system (1.2). We attempt to achieve two main goals. The first is to give the linear asymptotic stability, which is equivalent to assessing the small data global well-posedness. We need to consider the corresponding linear system of (1.2) to illustrate it,

    {tu1=22u12m+2b1,tu2=21u2+1m+2b2,tb=21b+2u,tm+2m=21m+×u,u=b=0. (1.4)

    With some assumptions on the initial data, we establish explicit decay rates of the solutions for the linear system (1.4). To give decay rates, we define the fractional operator Λαf via the Fourier transform,

    ^Λαf(ξ)=|ξ|αˆf(ξ).

    Our first result is as follows.

    Theorem 1.1. For any s0, let the initial data (u0,b0,m0)Hs(R2) with u0=b0=0. Suppose that (u,b,m) is the solution of the linear system (1.4).

    1. Assume that (u0,b0,m0)Hs(R2). Then the decay rates holds

    uHs(R2)+bHs(R2)+mHs(R2)C(1+t)12. (1.5)

    2. Suppose (Λσ1u0,Λσ1b0,Λσ1m0),(Λσ2u0,Λσ2b0,Λσ2m0)Hs(R2), where σ>0 is a real number. Then (u,b,m) satisfies

    u(t)Hs(R2)+b(t)Hs(R2)+m(t)Hs(R2)C(1+t)σ2. (1.6)

    The second goal is to prove the stability of the nonlinear system in (1.2).

    Theorem 1.2. Suppose that (u0,b0,m0)H2(R2) with u0=b0=0. Let (u,b,m) be the solution of the nonlinear system (1.2). Then there exists δ>0, such that if

    (u0,b0,m0)H2(R2)δ,

    then (1.2) possesses a unique global solution (u,b,m)C(0,;H2(R2)) satisfying

    (u1(t),u2(t),b(t),m(t))2H2(R2)+t0(2u12H2+1u22H2+1b2H2+1m2H2+2m2H2)dτCδ2, (1.7)

    for all t0, where C is a pure constant.

    By the technology of bootstrapping argument (see [30,p.21]) and the energy method, we are able to obtain the nonlinear stability. To prove Theorem 1.1, we first introduce the energy E(t) as follows

    E(t)=sup0τt(u(τ),b(τ),m(τ))2H2(R2)+2t0(2u1(τ)2H2(R2)+1u2(τ)2H2(R2)+1b(τ)2H2(R2)+1m(τ)2H2(R2)+2m(τ)d2H2(R2))dτ,

    for any t0. Our efforts concentrate on establishing the a priori estimate of E(t) in Section 3,

    E(t)E(0)+CE(t)32. (1.8)

    Then the bootstrapping argument implies the global bound and also the stability.

    This paper is organized as follows. In section 2, we give the proof of decay rates in Theorem 1.1. In section 3, by employing the energy method and using the bootstrapping argument, we establish the H2-estimate and then complete the proof of Theorem 1.2.

    In this section, we will show the decay rates in Hs for the solutions based on the linearized system (1.2). Under the different assumptions on the initial data, we establish the asymptotic stability for the linear system. Before stating our results in (1.5), we first give a tool which will be used in the proof of (1.5).

    Lemma 2.1. Let f=f(t) be a nonnegative continuous function satisfying, for two constants a0>0 and a1>0,

    f(t)a0f(s)and0f(τ)dτa1<forany0s<t. (2.1)

    Then, for any t>0, for a2=max{2a0f(0),2a1a0},

    f(t)a2(1+t)1. (2.2)

    The tool of Lemma 2.1 (see[25]) will be used to establish the decay rate (1.5). It indicates that generalized monotone nonnegative integrable functions have a precise decay rate.

    Proof of (1.5). We show the proof of s=0, then by the iterate, we can derive the case of s>0. First of all, we consider the first condition of monotonous. Taking the L2-inner product of (1.4) with (Δu,Δb,Δm), we have

    ddt(u(t)2L2+b(t)2L2+m(t)2L2+2(2u1(t)2L2+1u2(t)2L2)+1b(t)2L2+2m(t)2L2+1m(t)2L2=0. (2.3)

    where we used the fact that

    Δumdx+×uΔmdx=0.

    We denote the f(t) as

    f(t)=u(t)2L2+b(t)2L2+m(t)2L2. (2.4)

    Thus (2.3) implies that

    f(t)f(s), (2.5)

    for any s<t.

    As a result, we prove the first condition. Next we verify the second condition that is 0f(t)dtC. First, we have the H1-estimates,

    (u,b,m)2H1+2t0(2u12H1+1u22H1+1b2H1+2m2H1+1m2H1)dτ=u02H1+b02H1+m02H1. (2.6)

    By integration by parts and Hölder's inequality, we infer

    1u12L2=2u21u1dx=1u22u1dx12(1u22L2+2u12L2), (2.7)

    thus, it implies

    u2L22(1u22L2+2u12L2). (2.8)

    Combining (2.6), we can deduce

    0u(t)2L2dtC. (2.9)

    Besides, from (2.6), we can infer

    01b(t)2L2dtCand0m(t)2L2dtC. (2.10)

    Now it suffices to prove the integrability for 2b2L2 on the time. Dotting 2b to the velocity equation of (1.4), integrating over R2, then replacing tb by the other terms of the magnetic equation, we obtain

    2b2L2=tu2bdx22u12b1dx21u22b2dxm2bdx=ddtu2bdxu2tbdx22u12b1dx21u22b2dxm2bdx=ddtu2bdx+2u21bdx+2u2L222u12b1dx21u22b2dxm2bdx. (2.11)

    The four integral terms above can be estimated as

    2u21bdx22u12b1dx21u22b2dxm2bdx12(2u2L2+21b2L2+22u12L2+2b12L2+21u22L2+2b22L2+m2L2+2b2L2). (2.12)

    where we used the Hölder's inequality and Young's inequality. Inserting (2.12) into (2.11) and integrating it on [0,t], we have

    t02b(τ)2L2dτ(u(t)2L2+2b(t)2L2+u02L2+2b02L2)+t0(32u2L2+21b2L2+22u12L2+21u22L2+m2L2+2b2L2)dτ. (2.13)

    Then, adding λ× (2.13) into (2.6), where λ>0 is a small number, we have

    (u,b,m)2H1+2t0(2u12H1+1u22H1+b2H1+2m2H1+1m2H1)dτC(u02H1+b02H1+m02H1). (2.14)

    From (2.14), we infer

    t0b2L2dtC. (2.15)

    Collecting (2.9), (2.10) and (2.15), it suffices to verify f(t) satisfying the second condition which is nonnegative integrable. As a consequence, by Lemma 2.1 we conclude,

    f(t)C(1+t)1, (2.16)

    where C is a constant and (2.16) gives the desired result (2.2). Thus, we conclude the proof of (1.5).

    Proof of (1.6). Using the consideration of the itera again, we only prove the case of s=0 similarly to the (1.5). We have the H1-estimate as follows,

    12ddt(u1,u2,b,m)2H1+1u22H1+2u12H1+1b2H1+1m2H1+2m2H1=0.

    where

    F(t)=u1(t)2H1+u2(t)2H1+b(t)2H1+m(t)2H1,

    and

    G(t)=2(1u22H1+2u12H1+1b2H1+1m2H1+2m2H1).

    Applying Λσ1 and Λσ2 to the linear system (1.4) respectively, and dotting the correspending equations with (Λσ1u1,Λσ1u2,Λσ1b,Λσ1m) and (Λσ2u1,Λσ2u2,Λσ2b,Λσ2m), then integrating over R2, we have

    ddt(Λσ1u1,Λσ1u2,Λσ1b,Λσ1m)(t)2L2+2Λσ12u12L2+2Λσ11u22L2+2Λσ11b2L2+2Λσ11m2L2+4Λσ1m2L2=0. (2.17)

    and,

    ddt(Λσ2u1,Λσ2u2,Λσ2b,Λσ2m)(t)2L2+2Λσ22u12L2+2Λσ21u22L2+2Λσ21b2L2+2Λσ21m2L2+4Λσ2m2L2=0. (2.18)

    Combining (2.17) and (2.18), then integrating by parts, it infers that

    (Λσ1(u1,u2,b,m),Λσ2(u1,u2,b,m))2L2(Λσ1(u1,0,u2,0,b,m),Λσ2(u1,0,u2,0,b,m))2L2, (2.19)

    which indicates that

    H(t)H(0).

    Then the estimate of u1L2 follows from the Plancherel's identity and Hölder's inequality, which can be written as

    u1(t)2L2=|^u1(ξ,t)|2dξ=(|ξ2|2|^u1(ξ,t)|2)σσ+1(|ξ2|2σ|^u1(ξ,t)|2)1σ+1dξ2u1(t)2σσ+1L2Λσ2u1(t)2σ+1L2. (2.20)

    Similarly,

    u2(t)2L21u2(t)2σσ+1L2Λσ1u2(t)2σ+1L2, (2.21)
    b(t)2L21b2σσ+1L2Λσ1b(t)2σ+1L2, (2.22)

    and

    m(t)2L21m2σσ+1L2Λσ1m(t)2σ+1L2. (2.23)

    Collecting (2.20), (2.22), (2.23) and (2.19), we have

    F(t)CG(t)σ1+σH(t)11+σCG(t)σ1+σH(0)11+σ.

    Then we infer that

    G(t)CF(t)1+1σH(0)1σ. (2.24)

    Which immediately leads to

    F(t)(C1(σ,(u0,b0,m0)L2)+C2(σ,(Λσ1(u0,b0,m0),Λσ2(u0,b0,m0))L2)t)σ.

    Thus, we finish the proof of Theorem 1.1.

    This section proves the stability of the nonlinear system (1.2). By exploiting the methods of bootstrapping and energy method, we establish the H2-estimate. Before our proof, we give two useful tools. The first provides an anisotropic inequality for the integral of triple product and the proof can be found in [24]. The second shows a basic fact.

    Lemma 3.1. Suppose that f, g, 2g, h and 1h are all in L2(R2). Then, for some constant C>0,

    |fgh|dxCfL2g12L22g12L2h12L21h12L2. (3.1)

    Lemma 3.2. Due to u=0, we have the fact that

    2u2H13(2u12H1+1u22H1). (3.2)

    The key step in the proof is to deal with the nonlinear and coupled terms. Therefore, we will take full use of the Lemma 3.1. Combining Sobolev inequality, Hölder's inequality and Young's inequality, the closed priori estimate of the energy E(t) can be established.

    Proof. This section aims to obtain the H2-estimate. Since the equivalent norms,

    (u1,u2,b,m)2H2∼∥(u1,u2,b,m)2L2+2i=1(2iu1,2iu2,2ib,2im)2L2, (3.3)

    it suffices to make the estimate on (u1,u2,b,m)2L2 and (2iu1,2iu2,2ib,2im)2L2 respectively.

    First of all, by taking L2-inner product of (1.2) with (u,b,m) and using integration by parts, it easily infers

    12ddt(u1,u2,b,m)2L2+2u12L2+1u22L2+1b2L2+1m2L2+2m2L2=0. (3.4)

    Next, it suffices to estimate (u1,u2,b,m)2˙H2. Applying 21 and 22 to every equation in (1.2) respectively, then taking the L2-inner product with (2iu1,2iu2,2ib,2im), and integrating them on [0,t], we have

    12ddt2i=1(2iu12L2+2iu22L2+2ib2L2+2im2L2)+2i=1(2i2u12+2i1u22L2+2i1b2L2+22im2L2+2i1m2L2)=I1+I2+I7. (3.5)

    They can be written as follows respectively,

    I1=2i=12i(uu1)2iu1dx,I2=2i=1(2i(bb1)2iu1b2ib12iu1)dx,I3=2i=12i(uu2)2iu2dx,I4=2i=1(2i(bb2)2iu2b2ib22iu2)dx,I5=2i=1(2i(ub)2ibdx,I6=2i=1(2i(bu)2ibb2iu2ib)dx,I7=2i=12i(um)2imdx, (3.6)

    where we have used the facts that

    2i=1(2i2b2iu+2i2u2ib)dx=0, (3.7)
    2i=1(b2ib2iu+b2iu2ib)dx=0, (3.8)
    2i=12iu2iPdx, (3.9)

    and

    2i=1(2im2iu+2i×u2im)dx=0. (3.10)

    Then we estimate I1+I2+I7 one by one. In the following calculations, the Hölder's inequality, Young's inequality and Sobolev embedding inequality will be applied frequently. By using the Lemma (3.2), I1 and I3 can be estimated together,

    I1+I3=2i=12i(uu)2iudx=21(uu)21udx22(uu)22udx=2k=1Ck2k1u2k1u21udx2k=1Ck2k2u2k2u22udx=21u1u21udx21uu21udx22u2u22udx22uu22udx6uL22u2L4CuH2(1u22H2+2u12H2). (3.11)

    The term I2 can be transformed into four terms,

    I2=21(bb1)21u1dx+22(bb1)22u1dx=2k=1Ck2k1b2k1b121u1dx+2k=1Ck2k2b2k2b122u1dx=21b1b121u1dx+21bb121u1dx+22b2b122u1dx+22bb122u1dx=I21+I22+I23+I24. (3.12)

    For I21 and I22, we have

    I21+I22=21b1b121u1dx21bb112u2dx221u1L21bL41b1L4+b1L221bL412u2L2C(uH2+bH2)(1b2H2+1u22H2). (3.13)

    When we estimate I23 and I24, the incompressible condition b=0 will be used,

    I23+I24=22b112b122u1dx+22b222b122u1dx+22b11b122u1dx+22b22b122u1dx=22b112b122u1dx21b122b122u1dx+22b11b122u1dx12b12b122u1dxC(2b1L212b1L422u1L4+22b1L21b1L422u1L4)CbH2(1b2H2+2u12H2). (3.14)

    Collecting the bounds for I2, we have

    I2C(uH2+bH2)(1u22H2+2u12H2+1b2H2). (3.15)

    For I4, due to u=b=0, it can be estimated as follows,

    I4=2k=121(bb2)21u2dx+2k=122(bb2)22u2dx=2k=1Ck2k1b2k1b221u2dx+2k=1Ck2k2b2k2b222u2dx=21b1b221u2dx+21bb221u2dx+22b1b121u1dx22b11b221u2dx+22b21b121u1dxC21u2L4(1bL41b2L2+21bL4b2L2)+C1bL421u2L422b1L2+C21u1L4(1b1L42bL2+1b1L422b2L2)CbH2(1u22H2+2u12H2+1b2H2). (3.16)

    Now we think about I5, which can be rewritten as following four parts,

    I5=21(ub)21bdx22(ub)22bdx=2k=1Ck2k1u2k1b21bdx2k=1Ck2k2u2k2b22bdx=21u1b21bdx21ub21bdx22u2b22bdx22ub22bdx=I51+I52+I53+I54. (3.17)

    I51 and I52 can be estimated easily. By Sobolev embedding inequality, we have

    I51+I52=21u1b21bdx21u11b21bdx21u22b21bdxC(1uL21bL421bL4+1bL421bL421u1L2+21bL421u2L42bL2)CuH21b2H2. (3.18)

    To deal with I53 and I54, writing them into four terms,

    I53+I54=22u112b22bdx22u222b22bdx22u11b22bdx22u22b22bdx=J1+J2+J3+J4. (3.19)

    Using the Hölder's inequality and Young's inequality, J1 and J3 can be estimated as follows,

    J1+J3C(2u1L412bL422bL2+22u1L41bL422bL2)CbH2(2u12H2+1b2H2). (3.20)

    Integrating by parts and using Lemma 3.1, we obtain

    J2+J4=21u122b22bdx+21u12b22bdx=4u1122b22bdx2u112b22bdx+2u12b122bdxC(u112L22u112L222b12L2122b12L2122bL2+2u112L222u112L22b12L221b12L2122bL2+2u1L412bL422bL2)C(uH2+bH2)(2u12H2+1b2H2). (3.21)

    Inserting (3.20) and (3.21) into (3.19),

    I53+I54C(uH2+bH2)(2u12H2+1b2H2). (3.22)

    Collecting (3.18) and (3.22), we infer

    I5C(uH2+bH2)(2u12H2+1b2H2). (3.23)

    Similarly to I5, I6 can be written as

    I6=21(bu)21bdx+22(bu)22bdx=2k=1Ck2k1b2k1u21bdx+2k=1Ck2k2b2k2u22bdx=21b1u21bdx+21bu21bdx+22b2u22bdx+22bu22bdx=I61+I62+I63+I64. (3.24)

    For I61 and I62, by the Sobolev embedding inequality, we obtain

    I61+I62=21b1u21bdx+21bu21bdxC21bL4(1bL41uL2+uL221bL4)CuH21b2H2. (3.25)

    I63 and I64 can be divided into six terms,

    I63+I64=22b2u22bdx+22bu22bdx=22b112u22bdx+22b222u122b1dx+22b222u222b2dx+22b11u22bdx+22b22u122b1dx+22b22u222b2dx=K1+K2+K3+K4+K5+K6. (3.26)

    Estimating K2, K3, K5 and K6 together,

    K2+K3+K5+K6=21b122u122b1dx+21b122u221b1dx21b12u122b1dx+21b12u221b1dxC1bL4(22u1L422b1L2+21b1L422u2L2)+C12b1L4(2u1L422b1L2+12b1L4+2u2L2)C(uH2+bH2)(1b2H2+2u12H2). (3.27)

    Considering K1, integrating it by parts,

    K1=22b112u22bdx=22b112u122b1dx+22b112u222b2dx=212b12u122b1dx22b12u1122b1dx22b112u212b1dxC12b1L4(2u1L422b1L2+2b1L212u2L4)+C2b1L42u1L4122b1L2C(uH2+bH2)(1b2H2+1u22H2+2u12H2). (3.28)

    Similarly to K1, and using the Lemma 3.1 again,

    K4=22b11u122b1dx+22b11u222b2dx=2u1122b122b1dx22b11u221b1dxC(u112L22u112L222b112L2122b112L2122b1L2+1b1L41u2L422b1L2C(uH2+bH2)(2u12H2+1b2H2). (3.29)

    Hence,

    I63+I64C(uH2+bH2)(1u22H2+2u12H2+1b2H2). (3.30)

    Consequently, combining (3.25) and (3.30), we have

    I6C(uH2+bH2)(1u22H2+2u12H2+1b2H2). (3.31)

    Now we concerning the last term I7, which can be rewritten as follows,

    I7=21(um)21mdx22(um)22mdx=21(u11m+u22m)21mdx22(u11m+u22m)22mdx=I71+I72. (3.32)

    First, by combining the Hölder's inequality and Young's inequality, I71 becomes

    I71=2k=1Ck2k1u12k11m21mdx2k=1Ck2k1u22k12m21mdx=21u121m21mdx21u11m21mdx21u212m21mdx21u22m21mdxC21mL4(1u1L221mL4+21u1L21mL4+1u2L42mL2+21u2L42mL2)C1mH2(u1H21mH2+1u2H2mH2)C(uH2+mH2)(1m2H2+1u22H2). (3.33)

    We can infer I72,

    I72=2k=1Ck2k2u12k21m22mdx2k=1Ck2k2u22k22m22mdx=22u121m22mdx22u11m22mdx+31u122m22mdxC22mL2(2u1L421mL4+22u1L41mL4+2u1L421mL4)CmH2(2u12H2+1m2H2). (3.34)

    Therefore, I7 is estimated as

    I7C(uH2+mH2)(1u22H2+2u12H2+1m2H2). (3.35)

    Collecting all the estimate I1+I2+I7 and inserting them into (3.5), we deduce

    12ddt2i=1(2iu12L2+2iu22L2+2ib2L2+2im2L2)+2i=1(2i2u12+2i1u22L2+2i1b2L2+22im2L2+2i1m2L2)C((u,b,m)(t)H2)(1u22H2+2u12H2+1b2H2+1m2H2+2m2H2). (3.36)

    Then we finished the estimate of (2iu1,2iu2,2ib,2im)2L2. Combining (3.4) and (3.36), then integrating the resulted equation on [0,t], we conclude

    |(u,b,m)(t)2H2+2t0(2u12H2+1u22H2+1b2H2+1m2H2+2m2H2)dτ(u0,b0,m0)(t)2H2+Ct0(uH2+bH2+mH2) (3.37)
    ×(1u22H2+2u12H2+1b2H2+1m2H2)dτ, (3.38)

    which indicates the desired estimate

    E(t)E(0)+CE(t)32. (3.39)

    Thus this completes the proof of (1.8).

    Proof of Theorem 1.2. We have the energy inequality, namely

    E(t)E(0)+CE(t)32, (3.40)

    where C is a pure constant. Due to the assumption that (u0,b0,m0)H2(R2)δ is sufficiently small, such that

    E(0)δ2:=M2C. (3.41)

    To initiate the bootstrapping argument to the energy inequality, we make the ansatz

    E(t)14C2=M. (3.42)

    It then implies that

    CE(t)1212. (3.43)

    Substituting (3.43) into (3.40) and combining with (3.41), we obtain

    E(t)2E(0)Cδ2:=M2. (3.44)

    Then we have obtained that E(t) actually admits an smaller upper bound, which is

    E(t)2E(0)Cδ2M2. (3.45)

    By the bootstrapping argument, this completes the proof of Theorem 1.2.

    In this paper, the stability of the 2D incompressible anisotropic magneto-micropolar fluid equations near a background magnetic field with partial mixed velocity dissipations, magnetic diffusion and horizontal vortex viscosity is considered. We obtained the explicit decay rates for the solution of the linear system in Hs(R2) Sobolev space and the stability of nonlinear system. And the results reveal that the background magnetic field can stabilize the electrically conducting fluids.

    We would like to thank the reviewers for their careful reading of our paper and for their insightful comments and suggestions. Also we would like to express sincere gratitude to Professor Hongxia Lin.

    The authors declare that there are no conflicts of interest.



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