| Literature DB >> 23961391 |
Abstract
Particle swarm optimization is a heuristic global optimization method and also an optimization algorithm, which is based on swarm intelligence. It comes from the research on the bird and fish flock movement behavior. In this paper we introduce and use this method in gravity inverse problem. We discuss the solution for the inverse problem of determining the shape of a fault whose gravity anomaly is known. Application of the proposed algorithm to this problem has proven its capability to deal with difficult optimization problems. The technique proved to work efficiently when tested to a number of models.Entities:
Keywords: Fault; Gravity inversion; Particle swarm optimization (PSO)
Year: 2013 PMID: 23961391 PMCID: PMC3724977 DOI: 10.1186/2193-1801-2-315
Source DB: PubMed Journal: Springerplus ISSN: 2193-1801
Figure 1Fault model illustrating various parameters used in work, and shape of expected gravity anomaly.
Figure 2Theoretical gravity anomaly produced by fault with known parameters and corresponding anomaly (solid triangles) of solution given by gravity inversion program.
Gravity anomaly for inversion
| x-coordinate (m) | Gravity anomaly (mgal) |
|---|---|
| −15000 | −2.24 |
| −10000 | −3.47 |
| −5000 | −5.60 |
| 0 | 0 |
| 5000 | 2.02 |
| 10000 | 1.61 |
| 15000 | 1.27 |
| 20000 | 1.04 |
Parameters of obtained solution
| Observed gravity | Calculated gravity |
|---|---|
| −2.24 | −2.23 |
| −3.47 | −3.47 |
| −5.60 | −5.60 |
| 0 | 0 |
| 2.02 | 2.00 |
| 1.61 | 1.63 |
| 1.27 | 1.29 |
| 1.04 | 1.05 |
h2 = 2001.6431, h1 = 6000 m a = 1.05*π- π =189-180 = 90 , t = 501.44849.
Cost = 3.6519e-005.
Figure 3Cost function value-PSO iteration.
Figure 4Observed g-calculated g graph.
Figure 5Calculated g graph.