Using Four-Component Geophones: Effect on the Quality and Reliability of Multicomponent Seismic Recording and Analysis of Processing Methods |
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| Authors: | P?S?Plotnitskii Email author" target="_blank">S?V?YaskevichEmail author A?A?Duchkov |
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| Institution: | 1.Trofimuk Institute of Petroleum Geology and Geophysics, Siberian Branch,Russian Academy of Sciences,Novosibirsk,Russia;2.Novosibirsk State University,Novosibirsk,Russia |
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| Abstract: | For seismic observations in mines or wells, instead of three-component geophones, four-component ones with sensors located along the tetrahedral axes are sometimes used. When a geophone is placed in a hard-to-reach area for a long time, the requirements on its reliability increase, so it is necessary to monitor its operation. From this viewpoint, a four-component geophone has certain advantages over the conventional three-component geophone, the three ones being suppression of instrument noise for the recalculation of a four-component record into a three-component one, saving of the polarization analysis data in case one geophone component fails, and sensitivity control of individual geophone components. To suppress instrument noise in records from a four-component geophone, the following processing should be performed: first, calculation of the covariance matrix of recording components, second calculation of the eigenvalues and eigenvectors of the covariance matrix, and third, the parameter used to assess the ratio of instrument noise to the useful signal is calculated. After that, the operator projecting a four-component displacement vector onto a three-dimensional subspace is constructed. Application of this operator to data suppresses interference or noise (which do not correspond to motion in three-dimensional space). The output of the processing is data partially cleaned of instrument noise. In this paper, using model examples, we analyze the features of processing data from four-component geophones. The possibility of suppressing instrument noise and controlling the sensitivities of individual geophone components is demonstrated, and the effect on polarization analysis results is shown. |
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