TY - GEN
T1 - Optimization of data sampling and image reconstruction by GPR
AU - Sato, Motoyuki
AU - Takahashi, Kazunori
AU - Yi, Li
PY - 2014/12/1
Y1 - 2014/12/1
N2 - This paper focuses on 3-dimensional (3D) image reconstruction by ground penetrating radar (GPR) data. Conventionally, we acquired a GPR gridded dataset with a fine interval, which satisfies the Nyquist spatial sampling criterion for an antenna. However, it takes long time for data acquisition. In this study, we tried two different approaches to reconstruct the image with sparse data that violated the Nyquist spatial sampling criterion: A non-gridded 3D migration method and a new interpolation method based on Projection onto convex sets (POCS) and frequency-wave number (f-k) filtering. Both methods are demonstrated with sand pit experiment datasets and a field experiment data that is acquired by our 3DGPR system. The results shows that both the non-gridded 3D migration method and the interpolation method can reconstruct the main target (a metal pipe at 0.8 m depth) well with the average spatial interval that equals to half wave length. But the non-gridded migration results (especially in shallow depth) suffer from the migration artifacts. The migrated result after interpolation is also demonstrated, and the migration artifacts can be reduced. These results indicate that it is possible to reduce the data density.
AB - This paper focuses on 3-dimensional (3D) image reconstruction by ground penetrating radar (GPR) data. Conventionally, we acquired a GPR gridded dataset with a fine interval, which satisfies the Nyquist spatial sampling criterion for an antenna. However, it takes long time for data acquisition. In this study, we tried two different approaches to reconstruct the image with sparse data that violated the Nyquist spatial sampling criterion: A non-gridded 3D migration method and a new interpolation method based on Projection onto convex sets (POCS) and frequency-wave number (f-k) filtering. Both methods are demonstrated with sand pit experiment datasets and a field experiment data that is acquired by our 3DGPR system. The results shows that both the non-gridded 3D migration method and the interpolation method can reconstruct the main target (a metal pipe at 0.8 m depth) well with the average spatial interval that equals to half wave length. But the non-gridded migration results (especially in shallow depth) suffer from the migration artifacts. The migrated result after interpolation is also demonstrated, and the migration artifacts can be reduced. These results indicate that it is possible to reduce the data density.
KW - 3D Interpolation
KW - 3D Migration
KW - Ground penetrating radar (GPR)
KW - Non-gridded data
KW - Projection onto convex sets (POCS)
UR - http://www.scopus.com/inward/record.url?scp=84919683850&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=84919683850&partnerID=8YFLogxK
U2 - 10.1109/ICGPR.2014.6970498
DO - 10.1109/ICGPR.2014.6970498
M3 - Conference contribution
AN - SCOPUS:84919683850
T3 - Proceedings of the 15th International Conference on Ground Penetrating Radar, GPR 2014
SP - 615
EP - 618
BT - Proceedings of the 15th International Conference on Ground Penetrating Radar, GPR 2014
A2 - Pajewski, Lara
A2 - Craeye, Christophe
A2 - Giannopoulos, Antonis
A2 - Andre, Frederic
A2 - Lambot, Sebastien
A2 - Slob, Evert
PB - Institute of Electrical and Electronics Engineers Inc.
T2 - 15th International Conference on Ground Penetrating Radar, GPR 2014
Y2 - 30 June 2014 through 4 July 2014
ER -