The paper discusses integral equations of the type k (ξ 1 ... ξ n ) = ∫ -∞ ∞ ... ∫ -∞ ∞ ψ ( x 1 ... x n ) L (ξ 1 -x 1 ... ξ n -x n ;α) d x 1 ... d x n , where L is L -integrable, and ψ and k are bounded. Since rapidly oscillating ψ have a small k , and since measurements of k are necessarily uncertain within non-zero limits of experimental error, very different ψ are consistent with any given set of measurements of k . Thus ψ is not determined by measurements of k . Instead of ψ, partial information about ψ that is not sensitive to rapid oscillations of ψ, can be obtained from k . In the present paper we consider smoothed versions of ψ, and their applications to gravity survey and the theory of surface waves. (1) For given L we construct normalized smoothing functions μ( x 1 ... x n ), so that ψ( x 1 ... x n ) = ∫ -∞ ∞ ... ∫ -∞ ∞ ψ( u 1 ... u n )μ (x 1 - u 1 ... x n - u n ) d u 1 .... d u n can be calculated from measurements of k( (ξ 1 ... ξ n ). The method is applied to gravity survey, where the distribution ψ of masses on a plane ∑' is to be calculated from the normal force k on another (parallel) plane∑. (2) By studying suitable smoothing functions we get a lower bound for the maximum modulus of the functions ψ which are consistent with given experimental values of k . The bound is large if k is known to vary rapidly. The bound is also large if α is large and if the Fourier transform of L tends to 0 when α→∞. The results are applied to gravity survey where now we consider the normal force on ∑ due to masses of bounded density distributed in the space below ∑', where ∑' is itself below ∑. If the normal force is not uniform the distance between ∑ and ∑' must not be too large, the estimate depending on the bound for the density. Also fairly general conditions are imposed on ψ so that ψ that is approximately determined by measurements of k , and an example from the theory of propagation in dispersive media is given where such conditions may be justified. The gist of the paper is contained in theorems A and B.
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