배한택 교수
Hantaek Bae
UNIST · 수학
연구실 소개
배한택 교수의 연구실은 유체역학과 비선형 편미분방정식의 정칙성, 존재성 및 안정성에 중점을 두고 있으며, 특히 비압축성 나비에-스토크스 방정식, 쿠아지오스피컬 방정식, 에일러-포아송 방정식 등에 대한 전역적 해의 존재와 정(regularity)을 다룹니다. 해의 해석적 성질과 고차 도함수의 감쇠 특성에 대한 기하급수적 정규성(Gevrey class regularity) 분석을 통해 시간에 따른 해의 정밀한 동역학을 규명하고 있으며, 특히 비국소적 분산 연산자와 함께 작용하는 비선형 방정식의 전역 유일성과 정규성에 대한 이론적 기초를 구축하고 있습니다. 이는 나노소재, 의약품 제형 설계, 대기과학 등 응용 분야와도 密접하게 연결되어 있습니다.
연구 현황
연구 성과 추이
표시된 성과는 수집된 데이터 기준으로 산출되며, 일부 차이가 있을 수 있습니다.
주요 논문
15In this paper, we prove the recent work of Lei-Lin in a slightly different setting, which enables us to prove analyticity of the solution.
In this paper, we study the incompressible Navier-Stokes equations on a moving domain in $\mathbb{R}^{3}$ of finite depth, bounded above by the free surface and bounded below by a solid flat bottom. We prove that there exists a unique, global-in-time solution to the problem provided that the initial velocity field and the initial profile of the boundary are sufficiently small in Sobolev spaces.
We study the global regularity of multi-dimensional repulsive Euler-Poisson equations in the radial setup. We show that the question of global regularity vs. finite breakdown of smooth solutions depends on whether the initial configuration crosses an initial critical threshold in configuration space. Specifically, there exists a global-in-time smooth solution if and only if the initial configuration of density 0 , radial velocity R 0 , and electrical charge e 0 satisfies R 0 F ( 0 ,e 0 ,R 0 ) fo
We prove global well-posedness for the dissipative quasi-geostrophic equation with initial data in critical Besov spaces <inline-formula content-type="math/mathml"> <mml:math xmlns:mml="http://www.w3.org/1998/Math/MathML" alttext="upper B Subscript p comma q Superscript 1 plus StartFraction 2 Over p EndFraction minus 2 alpha"> <mml:semantics> <mml:msubsup> <mml:mi>B</mml:mi> <mml:mrow class="MJX-TeXAtom-ORD"> <mml:mi>p</mml:mi> <mml:mo>,</mml:mo> <mml:mi>q</mml:mi> </mml:mrow> <mml:mrow class="M
In this paper, we establish Gevrey class regularity of solutions to a class of dissipative equations with an analytic nonlinearity in the whole space. This generalizes the results of Ferrari and Titi in the periodic space case with initial data in L 2 -based Sobolev spaces to the L p setting and in the whole space. Our generalization also includes considering rougher initial data, in negative Sobolev spaces in some cases including the Navier-Stokes and the subcritical quasi-geostrophic equations
Polymeric fluids arise in many practical applications in biotechnology, medicine, chemistry, industrial processes, and atmospheric sciences. In this paper, the Doi model for the suspensions of rod-like molecules in a compressible fluid is investigated. The model under consideration describes the interaction between the orientation of rod-like polymer molecules on the microscopic scale and the macroscopic properties of the fluid in which these molecules are contained. Prescribing arbitrarily the
The Doi model for the suspensions of rod-like molecules in a dilute regime describes the interaction between the orientation of rod-like polymer molecules on the microscopic scale and the macroscopic properties of the fluid in which these molecules are contained (cf. [M. Doi and S.F. Edwards, Oxford University Press, 1986]). The orientation distribution of the rods on the microscopic level is described by a Fokker-Planck-type equation on the sphere, while the fluid flow is given by the Navier-St
We consider 1D dissipative transport equations with nonlocal velocity field: θt + uθx + δuxθ + Λ γ θ = 0, u = N (θ), where N is a nonlocal operator given by a Fourier multiplier. Especially we consider two types of nonlocal operators: (1) N = H, the Hilbert transform, (2) N = (1 − ∂xx) −α. In this paper, we show several global existence of weak solutions depending on the range of γ and δ. When 0 < γ < 1, we take initial data having finite energy, while we take initial data in weighted function s
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