
144 Chapter 5 Solution methods for ill-posed problems
In the solution of difference problems for well-posed mathematical physics prob-
lems, the choice of B should be made considering primarily the demand for improved
rate of convergence in the iteration method. In the solution of ill-posed problems the it-
erative process should be terminated on the achievement of a discrepancy whose value
is defined by the input-data inaccuracy. We are interested not only in the rate at which
the iterative process converges in this domain of decreasing, but also in the class of
smoothness on which this iterative process converges and in the norm in which the
desired level of discrepancy can be achieved. The most important feature of the ap-
proximate solution of ill-posed problems by iteration methods consists in the fact that
an appropriate approximate solution can be isolated from the necessary smoothness
class through the choice of B.
5.5 Program implementation
and computational experiments
As a routine ill-posed problem, the first-kind integral equation is normally considered.
Following the common practice, we consider here the points that arise in the numerical
solution of an integral equation used to continue anomalous gravitation fields given on
the earth surface towards disturbing masses. The program implementation is based on
the use of iteration methods in solving problems with random input-data inaccuracies.
5.5.1 Continuation of a potential
In gravimetrical and magnetic prospecting, and in direct-current geoelectrical
prospecting, most important are problems in which it is required to continue a po-
tential fields from the earth surface deep into the earth. The solution of such problems
is used to identify, to this or that extent, the position of gravitational and electromag-
netic anomalies. Here, we restrict ourselves to the formulation of the gravitational-field
continuation problem.
We designate as U the gravitational potential of an anomaly located in depth of the
earth. Let x be a horizontal coordinate and the axis Z be directed upward so that at
the earth surface we have z = 0. We consider a problem in which it is required to
determine the gravity potential in the zone z < 0 down to anomalies whose depth
is H .
We consider a problem in which it is required to continue the gravitational potential
from two disturbing masses (D
1
and D
2
in Figure 5.1). This potential U (x, z) satisfies
the Laplace equation in the zone outside the anomalies, so that
∂
2
U
∂x
2
+
∂
2
U
∂z
2
= 0, z > −H. (5.50)
At the earth surface (according to field observations measured in which is the first