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- W843374857 abstract "The results of geodetic measurements provide information regarding the course of deformation process occurring because of the mining activity. Every analysis of deformations and theoretical considerations base on the results of measurements. The most important indicator of deformation taken into account in the analysis of adverse influence of the deformation on the objects on the surface is horizontal strain. Analysis of the distribution of the deformations determined by geodesic methods on the measurement lines indicates large oscillation of the recorded values. It is connected with occurrence of many factors disturbing deformation process. An image of deformations shows all types of errors occurring in the problems connected with measurement results’ analysis [1]. Part of errors appearing during measurement can be eliminated during this measurement or during initial analysis of the results. However, there are many factors that cannot be unequivocally identified what causes lasting disturbance of the image of deformation process. In case of dynamic courses of the process observed with use of geodesic methods a problem of error identification appears. A basic problem is to assume a criterion which would allow unequivocally eliminating values detached from deformation image disturbed by accidental factors. Measuring and working on the results are connected with errors (accidental, systematic, instrument, personal, etc.). In case of observing deformation process an obtained image is affected not only by the factors connected with realization of measurements but also by a whole group of factors disturbing the process itself. That is why it seems justified to change the nomenclature from errors to disturbances." @default.
- W843374857 created "2016-06-24" @default.
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- W843374857 date "2009-01-01" @default.
- W843374857 modified "2023-09-27" @default.
- W843374857 title "Outlier Identification Method for Horizontal Strain on the Mining Areas" @default.
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- W843374857 hasPublicationYear "2009" @default.
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