A new result for the global existence (and boundedness), regularity and stabilization of a three-dimensional Keller-Segel-Navier-Stokes system modeling coral fertilization
Abstract
This paper deals with the following quasilinear Keller-Segel-Navier-Stokes system modeling coral fertilization (*): \ arrayl nt+u·∇ n= n-∇·(nS(x,n,c)∇ c)-nm, x∈ , t>0, ct+u·∇ c= c-c+m, x∈ , t>0, mt+u·∇ m= m-nm, x∈ , t>0,\\ ut+(u · ∇)u+∇ P= u+(n+m)∇ φ, x∈ , t>0,\\ ∇· u=0, x∈ , t>0 array. under no-flux boundary conditions in a bounded domain ⊂ R3 with smooth boundary, where φ∈ W2,∞ (). Here the matrix-valued function S(x,n,c) denotes the rotational effect which satisfies |S(x,n,c)|≤ S0 (c)(1 + n)-α with α≥0 and some nonnegative nondecreasing function S0. Based on this inequality and some carefully analysis, if α>0, then for any ∈R, system (*) possesses a global weak solution for which there exists T > 0 such that (n,c,m , u) is smooth in ×( T ,∞). Furthermore, for any p>1, this solution is uniformly bounded in with respect to the norm in Lp()× L∞() × L∞()× L2 (; R3). Building on this boundedness property and some other analysis, it can finally even be proved that in the large time limit, any such solution approaches the spatially homogeneous equilibrium (n,m,m,0) in an appropriate sense, where n=1||\∫n0-∫m0\+ and m=1||\∫m0 -∫n0\+.
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