1 / 1

Overview Objective: Estimation of geo-physical parameters from Ground

Courtesy: JPL, NASA. Weaker returns cannot be resolved. Weaker returns are resolved. Model Based Signal Processing for GPR Data Inversion. MUSIC Algorithm. Overview Objective: Estimation of geo-physical parameters from Ground

cybil
Télécharger la présentation

Overview Objective: Estimation of geo-physical parameters from Ground

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. Courtesy: JPL, NASA Weaker returns cannot be resolved Weaker returns are resolved Model Based Signal Processing for GPR Data Inversion MUSIC Algorithm Overview Objective: Estimation of geo-physical parameters from Ground Penetrating Radar (GPR) data – also called Electro- Magnetic (EM) Inversion Principle: Permittivity contrast in layered media causes reflection of incident Electromagnetic Wave • MUSIC : MUltipleSIgnalClassification • Super resolution frequency estimation technique • Exploits Orthogonality of signal and noise • Enhances valid returns and suppresses noise peaks • Requires reliable propagation model Simulations Geo-Physical Profile PermittivityProfile Radar System Reconstructed Vs actual Permittivity profile Range profiles obtained using FFT & MUSIC A typical dielectric profile Inversion Techniques Inversion on Actual Radar Data • Layer Stripping Technique • Apply Fourier/Inverse Fourier Transform on received signal • Set threshold and locate position and amplitudes of interfaces • Reflection amplitudes and time delays are related to permittivity • Recursively estimate permittivity profile • Wide Band FMCW Radar (2 – 8 GHz) used in Antarctica to estimate snow thickness • MUSIC algorithm was used for enhancement and permittivity estimation • Core data was modeled into permittivity profile using theoretical models • Problem of False alarms and missed peaks • Weaker returns are buried under side-lobes of stronger returns Model Based Inversion • Based on MMSE Minimization: Gauss Newton Method Based on Spectral Estimation: MUSIC Algorithm . Convergence issues – produces unstable/un-useful solutions . Problem with depth discretization . Requires good SNR Works best ! Reconstructed Vs actual permittivity profile Range profiles obtained using FFT & MUSIC GUI for the inversion algorithm 040105

More Related