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Partial Report III / 2015 - Rating of the deformation stress monitoring state of the rock mass during mining coal seam 30 (634) within the trial operation of mining method corridor - a pillar in OPJ ČSM - NORTH
Waclawik, Petr ; Ptáček, Jiří ; Kukutsch, Radovan ; Kajzar, Vlastimil ; Koníček, Petr ; Souček, Kamil ; Staš, Lubomír
Monitoring of the deformation stress state of the rock mass is a prerequisite for the verification of unapproved new mining methods hall-pillar and its further application in the Czech part of the Upper Silesian coal basin. This mining method is designed on the basis of experiences and practices that are verified in different natural conditions and depths below the surface and is therefore essential for the verification of conditions for the Czech part of the Upper Silesian Basin based on geotechnical monitoring. The present report is prepared on the basis of a contract no. 942/50/10, where the Institute of Geonics, v.v agrees to make periodic evaluation of monitoring data napěťodeformačního state of the rock mass. In accordance with the aforementioned agreement, the message is processed in the six-month period and continues in the interim report II / 2015 (Waclawik et al. 2015) passed buyers in April this year. Interim results of the geotechnical monitoring, such as the experience gained during the first conquest dobývky V show specifics of natural conditions in trial operation unapproved new mining methods hall-pillar.
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Bukov PVP underground research laboratory - geotechnical conditions of construction
Souček, Kamil ; Vavro, Martin ; Staš, Lubomír ; Koníček, Petr ; Ptáček, Jiří ; Waclawik, Petr ; Vavro, Leona ; Lednická, Markéta ; Kaláb, Zdeněk ; Šňupárek, Richard ; Vondrovic, L.
Bukov PVP Underground Research Laboratory (Bukov URL) is designed to be a test site for the evaluation of properties and behavior of the rock mass which is of similar type as selected candidate sites in the Czech Republic. It is situated at a depth corresponding to the proposed storage depth of the final locality for the national deep repository of high-level radioactive waste. The Bukov URL, the construction of which has begun in 2013, is situated in the southern part of the Rožná uranium deposit, at the northeastern periphery of the Strážek Moldanubicum close to its contact with the Svratka Unit. The rock mass is composed of relatively monotonous rock sequences primarily of a volcanosedimentary origin. They are currently represented, due to the subsequent tectonometa-morphic development, by migmatized biotite paragneisses up to stromatitic and/or oftalmitic migmatites, amphibole-biotite to biotite-amphibole gneisses, and amphibolites. The workings of the Bukov URL are situated on the level 12 of the Bukov-1 shaft, at the depth of about 600 m below the earth’s surface. The Bukov URL is still under construction and the research works by the consortium of several organizations – ÚJV Řež, a.s., Czech Geological Survey, Institute of Geonics of the CAS, v.v.i., and Arcadis CZ, a.s. - are carried out simultaneously. The research activities focus on a complex geological and geotechnical characterization of the rock mass of interest, which is vital for the realization of further research in situ. This paper briefly describes the technical solution of the Bukov URL and the process of its construction.
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Vliv pojezdového ústrojí zemědělské techniky na utužení půdy
Koníček, Petr
The diploma thesis provides an overview of the soil, its composition and attributes. Then, it briefly describes causes of soil solidification and methods of soil cultivation, which eliminate the unwanted soil solidification. This thesis also gives an overview of agricultural tyres, their composition and compression systems. Furthermore, it describes undercarriages of combine harvesters and their advantages and disadvantages. In the practical part of this thesis, there were done laboratory and field measurements of soil solidification after being run over by combine harvesters with different contents of grains in the grain hoppers and using the combine harvester inclination. Subsequently, the measurements were compared and evaluated in terms of changes in the soil porosity.
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Stress state rock mass monitoring ahead of longwall No. 371 202 at 2ndA block, Mine Plant 2, OKD, a.s
Waclawik, Petr ; Ptáček, Jiří ; Koníček, Petr ; Vavro, Martin ; Staš, Lubomír ; Souček, Kamil ; Kukutsch, Radovan ; Kajzar, Vlastimil
Generally, the accurate knowledge of the stress strain state of the rock mass in the neighbourhood of the mining galleries and underground openings is absolutely critical for their precise support designing, not only in the vicinity of them, but also at a greater distance from them if the phenomenon affecting the rock mass stress fields occurs. Measurement (investigation) of the rock stress is usually carried out by interpretation of the rock mass deformation processes, which can be relatively precisely observed and measured. The roadways are loaded not only by rock pressures in the front of the coalfaces but also by destress blasting realised in the overburden rock seam in the scope of the rockburst prevention. In addition, the rock stress distribution is influenced by old mining activities too, for example by abandoned coal pillars in the seams in overburden, respectively by goaf in the excavated seam. All of these factors can significantly affect the stress-strain behaviour of the rock mass around the mining works.
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Stress state rock mass monitoring ahead of longwall No. 371 202 at 2ndA block, Mine Plant 2, OKD, a.s
Waclawik, Petr ; Ptáček, Jiří ; Koníček, Petr ; Vavro, Martin ; Staš, Lubomír ; Souček, Kamil ; Kukutsch, Radovan ; Kajzar, Vlastimil
Generally, the accurate knowledge of the stress strain state of the rock mass in the neighbourhood of the mining galleries and underground openings is absolutely critical for their precise support designing, not only in the vicinity of them, but also at a greater distance from them if the phenomenon affecting the rock mass stress fields occurs. Measurement (investigation) of the rock stress is usually carried out by interpretation of the rock mass deformation processes, which can be relatively precisely observed and measured. The roadways are loaded not only by rock pressures in the front of the coalfaces but also by destress blasting realised in the overburden rock seam in the scope of the rockburst prevention. In addition, the rock stress distribution is influenced by old mining activities too, for example by abandoned coal pillars in the seams in overburden, respectively by goaf in the excavated seam. All of these factors can significantly affect the stress-strain behaviour of the rock mass around the mining works.
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Dílčí zpráva II/2015 Hodnocení monitoringu napěťodeformačního stavu horninového masivu při dobývání sloje 30(634) v rámci zkušebního provozu dobývací metody chodba-pilíř v OPJ Dolu ČSM - Sever
Waclawik, Petr ; Ptáček, Jiří ; Kukutsch, Radovan ; Kajzar, Vlastimil ; Koníček, Petr ; Souček, Kamil ; Staš, Lubomír
Monitoring napěťodeformačního stavu horninového masivu je nezbytným předpokladem pro ověření nové neschválené dobývací metody chodba-pilíř a jejího dalšího použití v podmínkách české části hornoslezské uhelné pánve. Tato dobývací metoda je projektována pouze na základě zkušeností a postupů, které jsou ověřeny v odlišných přírodních podmínkách a hloubkách pod povrchem a proto je nezbytná její verifikace pro podmínky české části hornoslezské pánve na základě geotechnického monitoringu. Předkládaná zpráva je zpracována na základě smlouvy o dílo č. 942/50/10, kde se Ústav Geoniky AV ČR, v.v.i. zavazuje provádět pravidelné vyhodnocování dat monitoringu napěťodeformačního stavu horninového masivu. V souladu s výše uvedenou smlouvou, je zpráva zpracována v 6-ti měsíčním intervalu a navazuje tak na dílčí zprávu I/2015 (Waclawik et al. 2015) předanou odběrateli v dubnu tohoto roku. Průběžné výsledky geotechnického monitoringu, tak jak zkušenosti získané v době dobývání první dobývky V, ukazují na specifika přírodních podmínek v lokalitě zkušebního provozu nové neschválené dobývací metody chodba-pilíř.
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Methodical instruction for effectiveness evaluation of destress blasting GM/15/UCIN
Koníček, Petr ; Čížek, P. ; Ptáček, Jiří ; Stoniš, M. ; Przeczek, A.
Rock bursts are one of the most dangerous phenomena occurring in coal mining in the Czech part of the Upper Silesian Coal Basin. In these terms, destress blastings belong to the most important of prevention measures. Seismic effects (as an indicator of stress release) represent the ratio of seismic energy released in the rock mass when blasting to the considered energy of the particular detonated chargé. The methodology is a result of ananalysis of a large data set of destress blastings from rock mass and seismological monitoring data collected over the period 2000 - 2013. A new, respectively verified rating system for evaluation of the effectiveness of destress blastings using the registered seismic energy is the basement of the methodology. The methodology determines to experts of underground hardcoal mining for procedure of effectiveness evaluation of destress blasting operations carried out in the rockburst prevention.
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The introductory view on the pressure load in the underground storage in the exploration zone Milasín-Bukov
Koníček, Petr ; Ptáček, Jiří ; Souček, Kamil ; Staš, Lubomír ; Vavro, Martin ; Waclawik, Petr
The report was prepared as the preliminary opinion on the pressure load resistance of the rock mass inside the gas storage Milasín-Bukov. It comprised the data summary and analysis, which were gained by measuring in mine or by laboratory tests. Rock and rock-mass parameters were obtained by deformation and/or stress/strain monitoring in the roadways in the mine using the index RMR or Q characterized the rock quality. The mechanical and stress/strain conditions were tested in labor on selected rock samples. The rock mass resistance to gas pressure inside the gas storage was determined based on the methodology stress strain in-situ measurements in the before driven roadways in the similar rock-mass conditions. The results were compared with the results of mathematical model.
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