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JOURNALS // Ufimskii Matematicheskii Zhurnal // Archive

Ufimsk. Mat. Zh., 2011 Volume 3, Issue 2, Pages 81–86 (Mi ufa95)

Explicit solution of the Cauchy problem to the equation for groundwater motion with a free surface

Kh. G. Umarov

Chechen State University, Groznyi, Russia

Abstract: A linear partial differential equation modelling evolution of a free surface of the filtered fluid
$$ \lambda u_t-\Delta_2u_t=\alpha\Delta_2u-\beta\Delta^2_2u+f $$
is considered. Here $u(x,y,t)$ is the searched function characterizing the fluid pressure, $f=f(x,y,t)$ is the given function calculating an external influence on the filtration flow, $\Delta_2=\frac{\partial^2}{\partial x^2}+\frac{\partial^2}{\partial y^2}$ is the Laplace differential operator, $\lambda,\alpha,\beta$ are positive constants depending on characteristics of the watery soil. The explicit solution to the Cauchy problem for the above linear partial differential equation is obtained in the space $L_p(R^2)$, $1<p<+\infty$, by means of reducing the considered filtration problem to the abstract Cauchy problem in a Banach space. Solution of the corresponding homogeneous equation with respect to the temporary variable $t$ satisfies the semi-group property. The resulting estimation of the solution to the Cauchy problem in the space $L_p(R^2)$, $1<p<+\infty$, entails that the solution is continuously dependent on the initial data in any finite time interval.

Keywords: free surface of the filtered fluid, strongly continuous semi-groups of operators.

UDC: 517.95+517.986.7

Received: 11.01.2011


 English version:
Ufa Mathematical Journal, 2011, 3:2, 79–84 (PDF, 354 kB)

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© Steklov Math. Inst. of RAS, 2026