Repository of the Academy's Library

Joint inversion of seismic and geoelectric data recorded in an underground coal mine

Dobróka, Mihály and Gyulai, Ákos and Ormos, Tamás and Csókás, J. and Dresen, L. (1991) Joint inversion of seismic and geoelectric data recorded in an underground coal mine. Geophysical Prospecting, 39 (5). pp. 643-665. ISSN 0016-8025 (print), 1365-2478 (online)

[img] PDF
1034391.pdf
Restricted to Registered users only

Download (1016Kb) | Request a copy

Abstract

Until the present time the 'rock-coal-rock' layer sequence and offsets in coal-seams in underground coal mines have been detected with the aid of seismic waves and geoelectric measurements. In order to determine the geometrical and petrophysical parameters of the coal-seam situation, the data recorded using seismic and geoelectric methods have been inverted independently. In consequence, the inversion of partially inaccurate data resulted in a certain degree of ambiguity. This paper presents the first results of a joint inversion scheme to process underground vertical seismic profiling data, geolectric resistivity and resistance data. The joint inversion algorithm makes use of the damped least-squares method and its weighted version to solve the linearized set of equations for the seismic and geolectric unknowns. In order to estimate the accuracy and reliability of the derived geometrical and petrophysical layer parameters, both a model covariance matrix and a correlation matrix are calculated. The weighted least-squares algorithm is based on the method of most frequent values (MFV). The weight factors depend on the difference between measured data and those calculated by an iteration process. The joint inversion algorithm is tested by means of synthetic data. Compared to the damped least-squares algorithm, the MFV inversion leads to smaller estimation errors as well as lower sensitivities due to the choice of the initial model. It is shown that, compared to an independent inversion, the correlation between the model parameters is definitely reduced, while the accuracy of the parameter estimation is appreciably increased by the joint inversion process. Thus the ambiguity is significantly reduced. Finally, the joint inversion algorithm the MFV method is applied to underground field data. The model parameters can be derived with a sufficient degree of accuracy, even in the case of noisy data.

Item Type: Article
Subjects: Q Science / természettudomány > QE Geology / földtudományok > QE01 Geophysics / geofizika
Depositing User: Erika Bilicsi
Date Deposited: 15 Nov 2012 11:28
Last Modified: 15 Nov 2012 11:28
URI: http://real.mtak.hu/id/eprint/3378

Actions (login required)

View Item View Item