A Comparison of Two Travel-time Tomography Schemes for Crosshole Radar Data: Eikonal-equation-based Inversion Versus Ray-based Inversion

被引:9
作者
Balkaya, Caglayan [1 ,2 ]
Akcig, Zafer [1 ]
Gokturkler, Gokhan [1 ]
机构
[1] Dokuz Eylul Univ, Fac Engn, Dept Geophys Engn, TR-35160 Buca Izmir, Turkey
[2] Dokuz Eylul Univ, Grad Sch Nat & Appl Sci, TR-35160 Buca Izmir, Turkey
关键词
GROUND-PENETRATING RADAR; FINITE-DIFFERENCE CALCULATION; LEAST-SQUARES INVERSION; BOREHOLE RADAR; WATER-CONTENT; DELINEATION; TUTORIAL; GPR;
D O I
10.2113/JEEG15.4.203
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Some test studies were performed for comparison of two travel-time inversion schemes for tomographic evaluation of crosshole ground-penetrating radar (GPR) data. The first scheme was a linearized inversion based on Tikhonov regularization (Method 1). In this scheme, ray tracing was not a part of the inversion algorithm and the Jacobian matrix was calculated by numerical differentiation. Travel-time calculations were performed by a finite-difference eikonal equation solver. Model velocity fields were updated by matrix inversion techniques using iterative conjugate gradient solvers. The inversion process was stabilized by a smoothnessconstrained regularization. The second scheme was based on a ray tracing algorithm (Method 2) and velocities were updated by a simultaneous iterative reconstruction technique (SIRT) using both straight- and curved-ray approximations. The test studies included synthetic travel-time data sets generated from the models with various velocity distributions. Broyden's update was implemented within Method 1 to expedite the calculation of the Jacobian matrix, and this greatly improved the computational performance. In the tests, the effect of the regularization parameter on the models from Method 1 was examined. Also, how the straight-ray and curved-ray assumptions affected the solutions from Method 2 was illustrated. The effect of the initial velocity distribution on the resulting tomograms was exemplified by the solutions from both Method 1 and Method 2. The velocity tomograms from Method 1 were characterized by smaller travel-time residuals, Euclidean distances and lower errors in the velocity of cells. Also, the convergence rates of the solutions from Method I were faster than those from Method 2. Method 1 better imaged the zones with the high velocity contrast than Method 2, and both methods produced similar velocity distributions within the zones with low velocity contrast. Overall, Method I yielded better solutions compared to Method 2, and the curved-ray inversion generated relatively better results than the straight-ray inversion.
引用
收藏
页码:203 / 218
页数:16
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