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  • About
  • The Global ETD Search service is a free service for researchers to find electronic theses and dissertations. This service is provided by the Networked Digital Library of Theses and Dissertations.
    Our metadata is collected from universities around the world. If you manage a university/consortium/country archive and want to be added, details can be found on the NDLTD website.
1

Interpolation strategy based on Dynamic Time Warping

Operti, Felipe Gioachino January 2015 (has links)
OPERTI, Felipe Gioachino. Interpolation strategy based on Dynamic Time Warping. 2015. 53 f. Dissertação (Mestrado em Física) - Programa de Pós-Graduação em Física, Departamento de Física, Centro de Ciências, Universidade Federal do Ceará, Fortaleza, 2015. / Submitted by Edvander Pires (edvanderpires@gmail.com) on 2015-04-14T22:11:14Z No. of bitstreams: 1 2015_dis_fgoperti.pdf: 5361657 bytes, checksum: b47dae9c4d72accf5fe2c50b89abaae4 (MD5) / Approved for entry into archive by Edvander Pires(edvanderpires@gmail.com) on 2015-04-16T18:35:49Z (GMT) No. of bitstreams: 1 2015_dis_fgoperti.pdf: 5361657 bytes, checksum: b47dae9c4d72accf5fe2c50b89abaae4 (MD5) / Made available in DSpace on 2015-04-16T18:35:49Z (GMT). No. of bitstreams: 1 2015_dis_fgoperti.pdf: 5361657 bytes, checksum: b47dae9c4d72accf5fe2c50b89abaae4 (MD5) Previous issue date: 2015 / In oil industry, it is essential to have the knowledge of the stratified rocks’ lithology and, as consequence, where are placed the oil and the natural gases reserves, in order to efficiently drill the soil, without a major expense. In this context, the analysis of seismological data is highly relevant for the extraction of such hydrocarbons, producing predictions of profiles through reflection of mechanical waves in the soil. The image of the seismic mapping produced by wave refraction and reflection into the soil can be analysed to find geological formations of interest. In 1978, H. Sakoe et al. defined a model called Dynamic Time Warping (DTW)[23] for the local detection of similarity between two time series. We apply the Dynamic Time Warping Interpolation (DTWI) strategy to interpolate and simulate a seismic landscape formed by 129 depth-dependent sequences of length 201 using different values of known sequences m, where m = 2, 3, 5, 9, 17, 33, 65. For comparison, we done the same operation of interpolation using a Standard Linear Interpolation (SLI). Results show that the DTWI strategy works better than the SLI when m = 3, 5, 9, 17, or rather when distance between the known series has the same order size of the soil layers.

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