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1

Davy, Ph. Modélisation thermo-mécanique de la collision continentale. Rennes, France: Centre armoricain d'étude structurale des socles, LP CNRS no 4661, Université de Rennes I, 1986.

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2

Luehring, Ronald W. Methods for determining in situ deformation of rock masses. Denver, Colo: Geotechnical Branch, Division of Research and Laboratory Services, Engineering and Research Center, U.S. Dept. of the Interior, Bureau of Reclamation, 1988.

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3

Modelling the effects of blasting on rock breakage. Rotterdam: A.A. Balkema, 1995.

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4

Lieblich, D. A. Integrated use of surface-geophysical methods to indicate subsurface fractures at Milford, New Hampshire. Hartford, Conn: U.S. Dept. of the Interior, U.S. Geological Survey, 1992.

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5

Lieblich, D. A. Integrated use of surface-geophysical methods to indicate subsurface fractures at Tibbetts Road, Barrington, New Hampshire. Hartford, Conn: U.S. Dept. of the Interior, U.S. Geological Survey, 1992.

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6

L, Hill John. Cut ter roof failure: An overview of the causes and methods for control. Avondale, Md: U.S. Dept. of the Interior, Bureau of Mines, 1986.

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7

Beus, Michael J. Application of field measurements and computer modeling to evaluate deep mine shaft stability in northern Idaho. [Washington, D.C.?]: U.S. Dept. of the Interior, Bureau of Mines, 1996.

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8

Massoud, Hamid. Modélisation de la petite fracturation par les techniques de la géostatistique. Orléans, France: BRGM, 1988.

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9

Shikhin, I͡U S. Geologicheskoe kartirovanie i ot͡senka rudonosnosti razryvnykh narusheniĭ. Moskva: "Nedra", 1991.

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10

Matematicheskie metody modelirovanii͡a︡ treshchinnykh struktur rudnykh mestorozhdeniĭ. Moskva: "Nauka", 1991.

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11

Yeh, T. C. Simulation of liquid and vapor movement in unsaturated fractured rock at the Apache Leap Tuff Site: Models and strategies. Washington, DC: Division of Engineering, Office of Nuclear Regulatory Research, U.S. Nuclear Regulatory Commission, 1988.

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12

Jakubowski, Jacek. Stochastyczna symulacja stateczności wyrobisk w nieciągłym masywie skalnym. Kraków: Wydawnictwa AGH, 2010.

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13

Christianson, Mark. Sensitivity of the stability of a waste emplacement drift to variation in assumed rock joint parameters in welded tuff. Washington, DC: Division of High-Level Waste Management, Office of Nuclear Material Safety and Safeguards, U.S. Nuclear Regulatory Commission, 1989.

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14

S, Suri Jasjit, and Farag Aly A, eds. Deformable models. New York: Springer, 2007.

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15

Zheng, Lu, Takeshi Sasaki, Guangqi Chen, and Yuzo Ohnishi. Frontiers of Discontinuous Numerical Methods and Practical Simulations in Engineering and Disaster Prevention. Taylor & Francis Group, 2013.

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16

Zheng, Lu, Takeshi Sasaki, Guangqi Chen, and Yuzo Ohnishi. Frontiers of Discontinuous Numerical Methods and Practical Simulations in Engineering and Disaster Prevention. Taylor & Francis Group, 2013.

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17

Zheng, Lu, Takeshi Sasaki, Guangqi Chen, and Yuzo Ohnishi. Frontiers of Discontinuous Numerical Methods and Practical Simulations in Engineering and Disaster Prevention. Taylor & Francis Group, 2013.

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18

Chen, Guangqi. Frontiers of Discontinuous Numerical Methods and Practical Simulations in Engineering and Disaster Prevention. Taylor & Francis Group, 2013.

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19

Zheng, Lu, Takeshi Sasaki, Guangqi Chen, and Yuzo Ohnishi. Frontiers of Discontinuous Numerical Methods and Practical Simulations in Engineering and Disaster Prevention. Taylor & Francis Group, 2013.

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20

Frontiers of Discontinuous Numerical Methods and Practical Simulations in Engineering and Disaster Prevention. Taylor & Francis Group, 2013.

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21

Zheng, Lu, Takeshi Sasaki, Guangqi Chen, and Yuzo Ohnishi. Frontiers of Discontinuous Numerical Methods and Practical Simulations in Engineering and Disaster Prevention. Taylor & Francis Group, 2013.

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22

Borovikov, V. A., and I. F. Vanyagin. Modelling the Effects of Blasting on Rock Breakage. Taylor & Francis Group, 2020.

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23

Borovikov, V. A., and I. F. Vanyagin. Modelling the Effects of Blasting on Rock Breakage. Taylor & Francis Group, 2020.

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24

Borovikov, V. A., and I. F. Vanyagin. Modelling the Effects of Blasting on Rock Breakage. Taylor & Francis Group, 2020.

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25

Borovikov, V. A., and I. F. Vanyagin. Modelling the Effects of Blasting on Rock Breakage. Taylor & Francis Group, 2020.

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26

visualized experiments and simulation on pore scale fluids flow and deformation mechanism of rock. ausasia science and technology press pty ltd, 2021. http://dx.doi.org/10.26804/2021070101.

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27

Witherspoon, Paul A., Boris Faybishenko, and Sally M. Benson. Dynamics of Fluids in Fractured Rock. Wiley & Sons, Limited, John, 2013.

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28

(Editor), Boris Faybishenko, Paul Adams Witherspoon (Editor), and Sally Benson (Editor), eds. Dynamics of Fluids in Fractured Rock (Geophysical Monograph). Amer Geophysical Union, 2000.

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29

J, Beus Michael, ed. Real-time monitoring of field measurements for mine design: Greens Creek Mine, Admiralty Island, Alaska. [Washington, D.C.?]: U.S. Dept. of the Interior, Bureau of Mines, 1996.

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30

J, Beus Michael, ed. Real-time monitoring of field measurements for mine design: Greens Creek Mine, Admiralty Island, Alaska. [Washington, D.C.?]: U.S. Dept. of the Interior, Bureau of Mines, 1996.

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31

J, Beus Michael, ed. Real-time monitoring of field measurements for mine design: Greens Creek Mine, Admiralty Island, Alaska. [Washington, D.C.?]: U.S. Dept. of the Interior, Bureau of Mines, 1996.

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32

J, Beus Michael, ed. Real-time monitoring of field measurements for mine design: Greens Creek Mine, Admiralty Island, Alaska. [Washington, D.C.?]: U.S. Dept. of the Interior, Bureau of Mines, 1996.

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33

Real-time monitoring of field measurements for mine design: Greens Creek Mine, Admiralty Island, Alaska. [Washington, D.C.?]: U.S. Dept. of the Interior, Bureau of Mines, 1996.

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34

J, Beus Michael, ed. Real-time monitoring of field measurements for mine design: Greens Creek Mine, Admiralty Island, Alaska. [Washington, D.C.?]: U.S. Dept. of the Interior, Bureau of Mines, 1996.

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35

Miller, Karol, Adam Wittek, and Poul M. F. Nielsen. Computational Biomechanics for Medicine: Deformation and Flow. Springer, 2012.

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36

Miller, Karol, Adam Wittek, and Poul M. F. Nielsen. Computational Biomechanics for Medicine: Deformation and Flow. Springer, 2014.

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37

Sahimi, Muhammad. Flow and Transport in Porous Media and Fractured Rock: From Classical Methods to Modern Approaches With Application to Reservoir Simulation. Wiley-VCH, 2008.

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38

(Editor), Jasjit S. Suri, and Aly A. Farag (Editor), eds. Deformable Models: Biomedical and Clinical Applications (Topics in Biomedical Engineering. International Book Series) (Topics in Biomedical Engineering. International Book Series). Springer, 2007.

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39

(Editor), Jasjit S. Suri, and Aly Farag (Editor), eds. Deformable Models: Theory & Biomaterial Applications (Topics in Biomedical Engineering. International Book Series) (Topics in Biomedical Engineering. International Book Series). Springer, 2007.

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40

Centrifuge Modelling for Civil Engineers. CRC Press, 2012.

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41

Madabhushi, Gopal. Centrifuge Modelling for Civil Engineers. Taylor & Francis Group, 2017.

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42

Madabhushi, Gopal. Centrifuge Modelling for Civil Engineers. Taylor & Francis Group, 2017.

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43

Madabhushi, Gopal. Centrifuge Modelling for Civil Engineers. Taylor & Francis Group, 2017.

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44

Centrifuge Modelling for Civil Engineers. Taylor & Francis Group, 2013.

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45

Madabhushi, Gopal. Centrifuge Modelling for Civil Engineers. Taylor & Francis Group, 2017.

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46

Madabhushi, Gopal. Centrifuge Modelling for Civil Engineers. Taylor & Francis Group, 2017.

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47

Geophysics today: A survey of the field as the journal celebrates its 75th anniversary. Tulsa, OK: Society of Exploration Geophysicists, 2010.

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48

Zydroń, Tymoteusz. Wpływ systemów korzeniowych wybranych gatunków drzew na przyrost wytrzymałości gruntu na ścinanie. Publishing House of the University of Agriculture in Krakow, 2019. http://dx.doi.org/10.15576/978-83-66602-46-5.

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The aim of the paper was to determine the influence of root systems of chosen tree species found in the Polish Flysch Carpathians on the increase of soil shear strength (root cohesion) in terms of slope stability. The paper's goal was achieved through comprehensive tests on root systems of eight relatively common in the Polish Flysch Carpathians tree species. The tests that were carried out included field work, laboratory work and analytical calculations. As part of the field work, the root area ratio (A IA) of the roots was determined using the method of profiling the walls of the trench at a distance of about 1.0 m from the tree trunk. The width of the. trenches was about 1.0 m, and their depth depended on the ground conditions and ranged from 0.6 to 1.0 m below the ground level. After preparing the walls of the trench, the profile was divided into vertical layers with a height of 0.1 m, within which root diameters were measured. Roots with diameters from 1 to 10 mm were taken into consideration in root area ratio calculations in accordance with the generally accepted methodology for this type of tests. These measurements were made in Biegnik (silver fir), Ropica Polska (silver birch, black locust) and Szymbark (silver birch, European beech, European hornbeam, silver fir, sycamore maple, Scots pine, European spruce) located near Gorlice (The Low Beskids) in areas with unplanned forest management. In case of each tested tree species the samples of roots were taken, transported to the laboratory and then saturated with water for at least one day. Before testing the samples were obtained from the water and stretched in a. tensile testing machine in order to determine their tensile strength and flexibility. In general, over 2200 root samples were tested. The results of tests on root area ratio of root systems and their tensile strength were used to determine the value of increase in shear strength of the soils, called root cohesion. To this purpose a classic Wu-Waldron calculation model was used as well as two types of bundle models, the so called static model (Fiber Bundle Model — FIRM, FBM2, FBM3) and the deformation model (Root Bundle Model— RBM1, RBM2, mRBM1) that differ in terms of the assumptions concerning the way the tensile force is distributed to the roots as well as the range of parameters taken into account during calculations. The stability analysis of 8 landslides in forest areas of Cicikowicleie and Wignickie Foothills was a form of verification of relevance of the obtained calculation results. The results of tests on root area ratio in the profile showed that, as expected, the number of roots in the soil profile and their ApIA values are very variable. It was shown that the values of the root area ratio of the tested tree species with a diameter 1-10 ram are a maximum of 0.8% close to the surface of the ground and they decrease along with the depth reaching the values at least one order of magnitude lower than close to the surface at the depth 0.5-1.0 m below the ground level. Average values of the root area ratio within the soil profile were from 0.05 to 0.13% adequately for Scots pine and European beech. The measured values of the root area ratio are relatively low in relation to the values of this parameter given in literature, which is probably connected with great cohesiveness of the soils and the fact that there were a lot of rock fragments in the soil, where the tests were carried out. Calculation results of the Gale-Grigal function indicate that a distribution of roots in the soil profile is similar for the tested species, apart from the silver fir from Bie§nik and European hornbeam. Considering the number of roots, their distribution in the soil profile and the root area ratio it appears that — considering slope stability — the root systems of European beech and black locust are the most optimal, which coincides with tests results given in literature. The results of tensile strength tests showed that the roots of the tested tree species have different tensile strength. The roots of European beech and European hornbeam had high tensile strength, whereas the roots of conifers and silver birch in deciduous trees — low. The analysis of test results also showed that the roots of the studied tree species are characterized by high variability of mechanical properties. The values Of shear strength increase are mainly related to the number and size (diameter) of the roots in the soil profile as well as their tensile strength and pullout resistance, although they can also result from the used calculation method (calculation model). The tests showed that the distribution of roots in the soil and their tensile strength are characterized by large variability, which allows the conclusion that using typical geotechnical calculations, which take into consideration the role of root systems is exposed to a high risk of overestimating their influence on the soil reinforcement. hence, while determining or assuming the increase in shear strength of soil reinforced with roots (root cohesion) for design calculations, a conservative (careful) approach that includes the most unfavourable values of this parameter should be used. Tests showed that the values of shear strength increase of the soil reinforced with roots calculated using Wu-Waldron model in extreme cases are three times higher than the values calculated using bundle models. In general, the most conservative calculation results of the shear strength increase were obtained using deformation bundle models: RBM2 (RBMw) or mRBM1. RBM2 model considers the variability of strength characteristics of soils described by Weibull survival function and in most cases gives the lowest values of the shear strength increase, which usually constitute 50% of the values of shear strength increase determined using classic Wu-Waldron model. Whereas the second model (mRBM1.) considers averaged values of roots strength parameters as well as the possibility that two main mechanism of destruction of a root bundle - rupture and pulling out - can occur at the same. time. The values of shear strength increase calculated using this model were the lowest in case of beech and hornbeam roots, which had high tensile strength. It indicates that in the surface part of the profile (down to 0.2 m below the ground level), primarily in case of deciduous trees, the main mechanism of failure of the root bundle will be pulling out. However, this model requires the knowledge of a much greater number of geometrical parameters of roots and geotechnical parameters of soil, and additionally it is very sensitive to input data. Therefore, it seems practical to use the RBM2 model to assess the influence of roots on the soil shear strength increase, and in order to obtain safe results of calculations in the surface part of the profile, the Weibull shape coefficient equal to 1.0 can be assumed. On the other hand, the Wu-Waldron model can be used for the initial assessment of the shear strength increase of soil reinforced with roots in the situation, where the deformation properties of the root system and its interaction with the soil are not considered, although the values of the shear strength increase calculated using this model should be corrected and reduced by half. Test results indicate that in terms of slope stability the root systems of beech and hornbeam have the most favourable properties - their maximum effect of soil reinforcement in the profile to the depth of 0.5 m does not usually exceed 30 kPa, and to the depth of 1 m - 20 kPa. The root systems of conifers have the least impact on the slope reinforcement, usually increasing the soil shear strength by less than 5 kPa. These values coincide to a large extent with the range of shear strength increase obtained from the direct shear test as well as results of stability analysis given in literature and carried out as part of this work. The analysis of the literature indicates that the methods of measuring tree's root systems as well as their interpretation are very different, which often limits the possibilities of comparing test results. This indicates the need to systematize this type of tests and for this purpose a root distribution model (RDM) can be used, which can be integrated with any deformation bundle model (RBM). A combination of these two calculation models allows the range of soil reinforcement around trees to be determined and this information might be used in practice, while planning bioengineering procedures in areas exposed to surface mass movements. The functionality of this solution can be increased by considering the dynamics of plant develop¬ment in the calculations. This, however, requires conducting this type of research in order to obtain more data.
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49

Sobczyk, Eugeniusz Jacek. Uciążliwość eksploatacji złóż węgla kamiennego wynikająca z warunków geologicznych i górniczych. Instytut Gospodarki Surowcami Mineralnymi i Energią PAN, 2022. http://dx.doi.org/10.33223/onermin/0222.

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Hard coal mining is characterised by features that pose numerous challenges to its current operations and cause strategic and operational problems in planning its development. The most important of these include the high capital intensity of mining investment projects and the dynamically changing environment in which the sector operates, while the long-term role of the sector is dependent on factors originating at both national and international level. At the same time, the conditions for coal mining are deteriorating, the resources more readily available in active mines are being exhausted, mining depths are increasing, temperature levels in pits are rising, transport routes for staff and materials are getting longer, effective working time is decreasing, natural hazards are increasing, and seams with an increasing content of waste rock are being mined. The mining industry is currently in a very difficult situation, both in technical (mining) and economic terms. It cannot be ignored, however, that the difficult financial situation of Polish mining companies is largely exacerbated by their high operating costs. The cost of obtaining coal and its price are two key elements that determine the level of efficiency of Polish mines. This situation could be improved by streamlining the planning processes. This would involve striving for production planning that is as predictable as possible and, on the other hand, economically efficient. In this respect, it is helpful to plan the production from operating longwalls with full awareness of the complexity of geological and mining conditions and the resulting economic consequences. The constraints on increasing the efficiency of the mining process are due to the technical potential of the mining process, organisational factors and, above all, geological and mining conditions. The main objective of the monograph is to identify relations between geological and mining parameters and the level of longwall mining costs, and their daily output. In view of the above, it was assumed that it was possible to present the relationship between the costs of longwall mining and the daily coal output from a longwall as a function of onerous geological and mining factors. The monograph presents two models of onerous geological and mining conditions, including natural hazards, deposit (seam) parameters, mining (technical) parameters and environmental factors. The models were used to calculate two onerousness indicators, Wue and WUt, which synthetically define the level of impact of onerous geological and mining conditions on the mining process in relation to: —— operating costs at longwall faces – indicator WUe, —— daily longwall mining output – indicator WUt. In the next research step, the analysis of direct relationships of selected geological and mining factors with longwall costs and the mining output level was conducted. For this purpose, two statistical models were built for the following dependent variables: unit operating cost (Model 1) and daily longwall mining output (Model 2). The models served two additional sub-objectives: interpretation of the influence of independent variables on dependent variables and point forecasting. The models were also used for forecasting purposes. Statistical models were built on the basis of historical production results of selected seven Polish mines. On the basis of variability of geological and mining conditions at 120 longwalls, the influence of individual parameters on longwall mining between 2010 and 2019 was determined. The identified relationships made it possible to formulate numerical forecast of unit production cost and daily longwall mining output in relation to the level of expected onerousness. The projection period was assumed to be 2020–2030. On this basis, an opinion was formulated on the forecast of the expected unit production costs and the output of the 259 longwalls planned to be mined at these mines. A procedure scheme was developed using the following methods: 1) Analytic Hierarchy Process (AHP) – mathematical multi-criteria decision-making method, 2) comparative multivariate analysis, 3) regression analysis, 4) Monte Carlo simulation. The utilitarian purpose of the monograph is to provide the research community with the concept of building models that can be used to solve real decision-making problems during longwall planning in hard coal mines. The layout of the monograph, consisting of an introduction, eight main sections and a conclusion, follows the objectives set out above. Section One presents the methodology used to assess the impact of onerous geological and mining conditions on the mining process. Multi-Criteria Decision Analysis (MCDA) is reviewed and basic definitions used in the following part of the paper are introduced. The section includes a description of AHP which was used in the presented analysis. Individual factors resulting from natural hazards, from the geological structure of the deposit (seam), from limitations caused by technical requirements, from the impact of mining on the environment, which affect the mining process, are described exhaustively in Section Two. Sections Three and Four present the construction of two hierarchical models of geological and mining conditions onerousness: the first in the context of extraction costs and the second in relation to daily longwall mining. The procedure for valuing the importance of their components by a group of experts (pairwise comparison of criteria and sub-criteria on the basis of Saaty’s 9-point comparison scale) is presented. The AHP method is very sensitive to even small changes in the value of the comparison matrix. In order to determine the stability of the valuation of both onerousness models, a sensitivity analysis was carried out, which is described in detail in Section Five. Section Six is devoted to the issue of constructing aggregate indices, WUe and WUt, which synthetically measure the impact of onerous geological and mining conditions on the mining process in individual longwalls and allow for a linear ordering of longwalls according to increasing levels of onerousness. Section Seven opens the research part of the work, which analyses the results of the developed models and indicators in individual mines. A detailed analysis is presented of the assessment of the impact of onerous mining conditions on mining costs in selected seams of the analysed mines, and in the case of the impact of onerous mining on daily longwall mining output, the variability of this process in individual fields (lots) of the mines is characterised. Section Eight presents the regression equations for the dependence of the costs and level of extraction on the aggregated onerousness indicators, WUe and WUt. The regression models f(KJC_N) and f(W) developed in this way are used to forecast the unit mining costs and daily output of the designed longwalls in the context of diversified geological and mining conditions. The use of regression models is of great practical importance. It makes it possible to approximate unit costs and daily output for newly designed longwall workings. The use of this knowledge may significantly improve the quality of planning processes and the effectiveness of the mining process.
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