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Riemann method

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Riemann–Volterra method

A method for solving the Goursat problem and the Cauchy problem for linear hyperbolic partial differential equations of the second order in two independent variables (cf. Hyperbolic partial differential equation),

\equiv \ u _ {xy} + a( x, y) u _ {x} + b( x, y) u _ {y} + c( x, y) u = \ f( x, y).

In Riemann's method a fundamental role is played by the Riemann function R = R( x, y; \xi , \eta ) which, under suitable conditions on the coefficients a , b , c , and f , is defined as the solution of the particular Goursat problem

L ^ {*} R \equiv \ R _ {xy} - \frac \partial {\partial x } ( aR) - \frac \partial {\partial y } ( bR) + cR = 0

with the characteristic boundary conditions

R( \xi , y; \xi , \eta ) = \mathop{\rm exp} \int\limits _ \eta ^ { y } a( \xi , t) dt,

R( x, \eta ; \xi , \eta ) = \mathop{\rm exp} \int\limits _ \xi ^ { x } b( t, \eta ) dt .

With respect to the variables \xi , \eta , the function R is a solution of the homogeneous equation

R _ {\xi \eta } + a( \xi , \eta ) R _ \xi + b( \xi , \eta ) R _ \eta + c( \xi , \eta ) R = 0.

When a = b = 0 , c = \textrm{ const } , one has R = J _ {0} ( \sqrt {4c( x- \xi )( y - \eta ) } ) , where J _ {0} ( z) is the Bessel function of order zero.

The Riemann function may also be defined as the solution of the weighted integral Volterra equation:

\tag{2 } R( x, y; \xi , \eta ) - \int\limits _ \eta ^ { y } a( x, \tau ) R( x, \tau ; \xi , \eta ) d \tau +

- \int\limits _ \xi ^ { x } b( t, y) R( t, y; \xi , \eta ) dt +

+ \int\limits _ \xi ^ { x } dt \int\limits _ \eta ^ { y } c( t, \tau ) R( t, \tau ; \xi , \eta ) d \tau = 1.

The Riemann method for solving the Goursat problem is as follows: For any function u = u( x, y) that can be differentiated to the corresponding order, the following identity is valid:

\frac{\partial ^ {2} }{\partial x \partial y } [ uR( x, y; \xi , \eta )] - R( x, y; \xi ,\ \eta ) Lu =

= \ \frac \partial {\partial x } \left [ u \left ( \frac{\partial R }{\partial y } - aR \ \right ) \right ] + \frac \partial {\partial y } \left [ u \left ( \frac{\partial R }{\partial x } - bR \right ) \right ] .

Integrating over the rectangle \{ ( x _ {0} , y _ {0} ); ( x , y) \} and integrating by parts yields that any solution u of (1) is a solution of the weighted integral equation:

\tag{3 } u( x, y) = R( x, y _ {0} ; x, y) u( x, y _ {0} ) +

+ R( x _ {0} , y; x , y) u( x _ {0} , y) - R( x _ {0} , y _ {0} ; x, y) u ( x _ {0} , y _ {0} )+

+ \int\limits _ {x _ {0} } ^ { x } \left [ b( t, y _ {0} ) R( t, y _ {0} ; x, y) - \frac{\partial R( t, y _ {0} ; x, y) }{\partial t } \right ] u( t, y _ {0} ) dt +

+ \int\limits _ {y _ {0} } ^ { y } \left [ a( x _ {0} , \tau ) R( x _ {0} , \tau ; x, y) - \frac{\partial R( x _ {0} , \tau ; x, y) }{ \partial \tau } \right ] u( x _ {0} , \tau ) dt +

+ \int\limits _ {x _ {0} } ^ { x } dt \int\limits _ {y _ {0} } ^ { y } R( t, \tau ; x, y) f( x, \tau ) d \tau ,\ x > x _ {0} ,\ y > y _ {0} .

Equation (3) demonstrates directly the well-posedness of the Goursat problem

u( x, y _ {0} ) = \phi ( x),\ \ u( x _ {0} , y _ {0} ) = \psi ( y),\ \ \phi ( x _ {0} ) = \psi ( y _ {0} )

for equation (1).

Riemann's method solves the Cauchy problem for equation (1) with initial data on any smooth non-characteristic curve by finding a Riemann function. It thus affords the possibility of writing the solution of this problem in the form of quadratures.

Riemann's method has been generalized to a broad class of linear hyperbolic partial differential equations and systems.

In the case of a linear hyperbolic system of partial differential equations of the second order,

u _ {xx} - u _ {yy} + a( x, y) u _ {x} + b( x, y) u _ {y} + c( x, y) u = f( x, y),

where a , b and c are given square, real, symmetric matrices of order m , f = ( f _ {1} \dots f _ {m} ) is a given, and u = ( u _ {1} \dots u _ {m} ) is the unknown vector, the Riemann matrix is unambiguously defined as the solution of a system of weighted Volterra integral equations of the form (2) whose right-hand side is the identity matrix I of order m .

V. Volterra was the first to generalize Riemann's method to the wave equation

\tag{4 } u _ {xx} + u _ {yy} - u _ {tt} = f( x, y, t).

The function

R = \mathop{\rm log} \left [ \sqrt { \frac{( t- \tau ) ^ {2} }{r ^ {2} } - 1 } + \frac{\tau - t }{r} \right ] ,

where r ^ {2} = ( x - \xi ) ^ {2} + ( y - \eta ) ^ {2} , acts as the Riemann function, which permits that the solution of the Cauchy problem with initial data on the plane t = \textrm{ const } and of the Goursat problem with data on a characteristic cone for equation (4) may be written in the form of quadratures.

The method was proposed by B. Riemann (1860).

References

[1] A.V. Bitsadse, "Equations of mixed type" , Pergamon (1964) (Translated from Russian)
[2] R. Courant, D. Hilbert, "Methods of mathematical physics. Partial differential equations" , 2 , Interscience (1965) (Translated from German)
[3] V.I. Smirnov, "A course of higher mathematics" , 2 , Addison-Wesley (1964) (Translated from Russian)

Comments

References

[a1] P.R. Garabedian, "Partial differential equations" , Wiley (1963)
How to Cite This Entry:
Riemann method. Encyclopedia of Mathematics. URL: http://encyclopediaofmath.org/index.php?title=Riemann_method&oldid=48549
This article was adapted from an original article by A.M. Nakhushev (originator), which appeared in Encyclopedia of Mathematics - ISBN 1402006098. See original article