2-18-11

TREND ANALYSIS OF THE ROCK MASS PROPERTIES ON THE BASIS OF FRACTAL REPRESENTATION OF SPATIAL RANGES

O. G. Latyshev, O. O. Kazak

 

DOI http://dx.doi.org/10.21440/2307-2091-2018-2-79-84

O. G. Latyshev, O. O. Kazak / News of the Ural State Mining University 2 (2018) 79-84



Evaluation of rock mass characteristics is the basis for designing the technology of mineral deposits development, which indicates the relevance of the work.
The purpose of the present work is to establish the laws of spatial distribution of rock mass properties. Their establishment requires the solution of the following problems: determination of the probability of a trend; identification and elimination of emissions (local component) and construction of a trend line.
The research methodology consists of using the tools of fractal geometry to determine the properties of a random spatial series. The use of the apparatus of classical trend analysis, based on purely statistical analysis, in relation to the specifics of research data does not provide an adequate solution to these problems. This paper discusses the results of implementing the fractal representation of the spatial series in case of the rock mass strength distribution in the Yubileynoye deposit (Bashkortostan). The quantitative estimation of the trend line as a fractal object is to determine its fractal dimension by the method of “fractal lengths”. Step-by-step implementation of this method allowed identifying areas of the rock mass with natural variability of properties by depth. The variation of the values of a number (the random component) obeys an equation of the fractal Brownian motion (FBM). Determination of the parameters of this equation makes it possible to predict the characteristics of the rock mass in those areas where engineering-geological testing was not carried out. For this purpose, a statistical model of variability of the characteristics of the array, based on the Monte Carlo method was developed. Implementation of the model allows us to add the spatial series (replicate sample), i.e., to predict the properties of the array between the points of sampling.
Summary. The proposed techniques and software that forms the methodology of fractal analysis of variability of a rock mass at depth and along strike of the deposit. The methodology provides additional information for engineering and geological studies of deposits, especially with a limited amount of sample data. It allows increasing the reliability of the forecast of mining conditions for the construction of mines and mining operations.

Keywords: rocks; rock mass strength; fractal trend analysis.

 

REFERENCES

1. Latyshev O. G., Kazak O. O. 2013, Matematicheskiye metody v gornom dele [Mathematical methods in mining]. Ekaterinburg, 146 p.
2. Contreras L. F., Edwin T., Brown M. 2018, Bayesian data analysis to quantify the uncertainty of intact rock strength. Journal of Rock Mechanics and Geotechnical Engineering, no. 10, pp. 11–31.
3. Hoek E., Brown E. T. 1997, Practical estimates of rock mass strength. International Journal of Rock Mechanics and Mining Sciences, no. 34(8), рр. 1165–1186.
4. Miranda T., Sousa L. R., Gomes A. T., Tinoco J., C. Ferreira C. 2018, Geomechanical characterization of volcanic rocks using empirical systems and data mining techniques. Journal of Rock Mechanics and Geotechnical Engineering, no. 10, pp. 138–150.
5. Khani A., Baghbanan A., Norouzi S., Hashemolhosseini H. 2013, Effects of fracture geometry and stress on the strength of a fractured rock mass. International Journal of Rock Mechanics & Mining Sciences, no. 60, рp. 345–352.
6. Latyshev O. G., Karasev K. A., Martyushov K. S. 2013, Fraktalnyy trend-analiz izmenchivosti vremennykh i prostranstvennykh ryadov svoystv gornykh porod i massivov [The fractal trend-variability analysis of the temporal and spatial series properties of rocks and arrays]. Izv. vuzov. Gornyi zhurnal [News of the Higher Institutions. Mining Journal], no. 2, pp. 73–79.
7. Martyushov K. S. 2013, Prognoz prochnosti porodnogo massiva [Prediction of strength of rock mass]. Izv. vuzov. Gornyi zhurnal [News of the Higher Institutions. Mining Journal], no. 1, pp. 44–47.
8. Kobzar’ A. I. 2006, Prikladnaya matematicheskaya statistika: dlya inzhenerov i nauchnykh rabotnikov [Applied mathematical statistics: for
engineers and scientists]. Moscow, 816 p.
9. Mandelbrot B. 2002, Fraktal’naya geometriya prirody: per. s nem. [Fractal geometry of nature: Translated from German]. Moscow, 656 p.
10. Feder E. 1991, Fraktaly: per. s angl. [Fractals: Translated from English]. Moscow, 262 p.
11. Krylov S. S., Bobkov N. Yu. 2004, Fraktaly v geofizike [Fractals in Geophysics]. Saint Petersburg, 138 p.
12. Kronover R. 2006, Fraktaly i khaos v dinamicheskikh sistemakh: per. s angl. [Fractals and chaos in dynamic systems: Translated from English]. Moscow, 488 p.
13. 2007, Teoreticheskiye osnovy prognoza i upravleniya svoystvami geologicheskoy sredy pri podzemnykh tekhnogennykh vozdeystviyakh.pod red. O. G. Latysheva [Theoretical bases of forecasting and management of properties of the geological environment upon underground anthropogenic influences. Edited by O. G. Latyshev]. Ekaterinburg, 216 p.
14. Walter Wittke. 2014, Rock Mechanics Based on an Anisotropic Jointed Rock Model (AJRM). Wilhelm Ernst & Sohn. 865 p.
15. Sadovsky, M. A., Golubeva T. V., Pisarenko V. F., Schnierman M. G. 1984, Kharakternyye razmery gornoy porody i iyerarkhicheskiye svoystva seysmichnosti [Characteristic dimensions of rock and hierarchical properties of seismicity]. Izv. AN SSSR. Fizika Zemli [News of the USSR. Academy of Sciences. Physics of the Earth], no. 2, pp. 3–15.
16. Sadovsky M. A. 2004, Izbrannyye trudy: geofizika i fizika vzryva [Selected works: Geophysics and physics of explosion]. Moscow, 440 p.
17. Potapov A. A. 2005, Fraktaly v radiofizike i radiolokatsii: topologiya vyborki [Fractals in Radiophysics and radiolocation: topology of sample. Moscow, 848 p.
18. Sobol’ I. M. 1978, Metod Monte-Karlo [The Monte-Carlo method]. Moscow, 64 p.

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