On identifying magnetized anomalies using geomagnetic monitoring
arXiv:1803.05613 · doi:10.1007/s00205-018-1276-7
Abstract
We propose and investigate the inverse problem of identifying magnetized anomalies beneath the Earth using the geomagnetic monitoring. Suppose a collection of magnetized anomalies presented in the shell of the Earth. The presence of the anomalies interrupts the magnetic field of the Earth, monitored above the Earth. Using the difference of the magnetic fields before and after the presence of the magnetized anomalies, we show that one can uniquely recover the locations as well as their material parameters of the anomalies. Our study provides a rigorous mathematical theory to the geomagnetic detection technology that has been used in practice.
arXiv comment28 pages, 1 figure
References in corpus (2)
Cited by in corpus (5)
- Determining a random Schrödinger operator: both potential and source are random
- On identifying magnetized anomalies using geomagnetic monitoring II. A Magnetohydrodynamic Model
- Simultaneous recoveries for semilinear parabolic systems
- Inverse problem for a random Schrödinger equation with unknown source and potential
- On recent progress of single-realization recoveries of random Schrödinger systems