Expansion of Measurement Grid in Field Problems

Abstract

Integral equations are very often used to solve inverse magnetometry problems. The initial data for them are the results of magnetic field measurements on a closed circuit or a bounded grid. However, mathematical models use infinity integration. Thus, this creates a significant discrepancy between actual and calculated results. Particular attention should be paid to the fact that inverse problems of magnetometry are not stable solutions. A priori information is used to solve them. Thus, there is a need to expand the grid of measurements by creating mathematical modeling.