Inversion seismic refraction data using particle swarm optimization: a case study of Tabriz, Iran
Autor: | Ahmad Zarean, Rashed Poormirzaee, Rasoul Hamidzadeh Moghadam |
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Rok vydání: | 2014 |
Předmět: |
education.field_of_study
Engineering geology Computer Science::Neural and Evolutionary Computation Population MathematicsofComputing_NUMERICALANALYSIS Particle swarm optimization Inversion (meteorology) Inverse problem Swarm intelligence Physics::Geophysics General Earth and Planetary Sciences Seismic inversion Seismic refraction education Algorithm Seismology Geology General Environmental Science |
Zdroj: | Arabian Journal of Geosciences. 8:5981-5989 |
ISSN: | 1866-7538 1866-7511 |
DOI: | 10.1007/s12517-014-1662-x |
Popis: | Seismic refraction method is a powerful geophysical tool that is used in the fields of engineering geology, geotechnical engineering, and exploration geophysics. In order to achieve reliable results, processing of seismic refraction data in particular inversion stage should be done accurately. Recently, particle swarm optimization (PSO) algorithm, as a swarm intelligence technique, is used in many fields of studies. The PSO is a stochastic, population-based algorithm modeled on swarm intelligence. The use of PSO in geophysical inverse problems is a relatively recent development and offers many advantages in dealing with the nonlinearity inherent in such applications. The current study intends to move one step ahead in application of PSO in inversion and discuss applying PSO to invert seismic refraction data. A new framework for inversion seismic refraction data will also be proposed. For efficiency evaluation of developed method, different synthetic models were inverted and then a statistically analyzed PSO parameters function was presented. Finally, PSO inversion method was investigated in a case study at the part of Tabriz city in NW-Iran to delineate subsurface features. The findings show that the study area is composed of two main layers: first layer velocity is 550 m/s and its thickness is 5.5 m, and second layer velocity is 1350 m/s. The results emphasize the reliability of the PSO inversion method in seismic refraction data interpretation with an acceptable misfit and convergence speed. |
Databáze: | OpenAIRE |
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