![](https://us.edu.pl/instytut/inoz/wp-content/uploads/sites/37/Pracownicy/emptyperson.png)
• mgr Radosława Tomaszewska
Position: starszy specjalista administracyjny
Unit: Zespół ds. Projektów Wydziału Nauk Przyrodniczych
Adress: 41-200 Sosnowiec, ul. Będzińska 60
Floor: XIII
Room: 1320
Phone: (32) 3689 448
E-mail: radoslawa.tomaszewska@us.edu.pl
Publications list: Publications by CINiBA
Publications list: Publications by OPUS
Scopus Author ID: 7003695172
Publications from the Scopus database
2022
Stan-Kłeczek, I.; Pierwoła, J.; Marciniak, A.; Sutkowska, K.; Tomaszewska, R.
Multimethod geophysical investigation in karst areas: case studies from Silesia, Poland Journal Article
In: Bulletin of Engineering Geology and the Environment, vol. 81, no. 6, 2022, ISSN: 14359529, (3).
@article{2-s2.0-85129865803,
title = {Multimethod geophysical investigation in karst areas: case studies from Silesia, Poland},
author = { I. Stan-Kłeczek and J. Pierwoła and A. Marciniak and K. Sutkowska and R. Tomaszewska},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85129865803&doi=10.1007%2fs10064-022-02726-8&partnerID=40&md5=7ccb000bc718f1782efe4e0388cbbe58},
doi = {10.1007/s10064-022-02726-8},
issn = {14359529},
year = {2022},
date = {2022-01-01},
journal = {Bulletin of Engineering Geology and the Environment},
volume = {81},
number = {6},
publisher = {Springer Science and Business Media Deutschland GmbH},
abstract = {Carbonate rocks are particularly susceptible to karstification, resulting in the formation of structures, such as enlarged fissures, caverns, and sinkholes. These structures pose direct risk to construction and human safety, especially in urbanised areas. In this study, we demonstrate the application of multimethod geophysical reconnaissance, combining electrical resistivity tomography (ERT), induced polarisation (ERT-IP), seismic refraction tomography (SRT), and multichannel analysis of surface waves (MASW), to identify the subsurface karst structures at two sites in the Silesian District, Poland. This methodology allowed the identification of the geological structure to a depth of up to 40 m, which exceeds the requirements for geotechnical reconnaissance. At site 1, Niedzieliska, a 30-m-wide and 20-m-deep structure, filled with younger sediments, was interpreted as a karst sinkhole. At site 2, Tucznawa, a 180-m-wide fault zone overlain with suffusion-susceptible sediments was identified. The multimethod geophysical approach presented here can be applied to locate and interpret subsurface karst forms in similar karst terrains worldwide. © 2022, Springer-Verlag GmbH Germany, part of Springer Nature.},
note = {3},
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pubstate = {published},
tppubtype = {article}
}
2017
Mendecki, M. J.; Jochymczyk, K.; Zuberek, W. M.; Tomaszewska, R.
Determination of Elastic Parameters of Near-Surface Layers Over Subsidence Trough Development During Longwall Exploitation Journal Article
In: Archives of Mining Sciences, vol. 62, no. 4, pp. 705-716, 2017, ISSN: 08607001.
@article{2-s2.0-85040928763,
title = {Determination of Elastic Parameters of Near-Surface Layers Over Subsidence Trough Development During Longwall Exploitation},
author = { M.J. Mendecki and K. Jochymczyk and W.M. Zuberek and R. Tomaszewska},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-85040928763&doi=10.1515%2famsc-2017-0050&partnerID=40&md5=573005f337d213ff300a8280ee86d2d9},
doi = {10.1515/amsc-2017-0050},
issn = {08607001},
year = {2017},
date = {2017-01-01},
journal = {Archives of Mining Sciences},
volume = {62},
number = {4},
pages = {705-716},
publisher = {Walter de Gruyter GmbH},
abstract = {Seismic and geodetic studies were carried out before, during, and after underground exploitation of a coal bed in Katowice - Kleofas Coal Mine, located in the Upper Silesia Coal Basin, Poland. Development of a subsidence trough was completed approximately 3 months after passage of a longwall exploitation in the coal seam. This was the time required for the subsidence trough to appear on the surface, which was confirmed by levelling measurements. Sharp changes in the elastic parameters were observed on each profile during subsidence trough development. This observation can result from changing tension and compression forces caused by increase and/or decrease of the elastic parameters of the rock mass. After completion of subsidence trough development, the rock mass appeared to return to its isotropic state and the observed changes ceased. Some minor fluctuations were noted, but they probably resulted from changes in groundwater levels, which might have affected the measured parameters. © 2018 Archives of Mining Sciences.},
keywords = {},
pubstate = {published},
tppubtype = {article}
}
2006
Mirkowski, Z.; Tomaszewska, R.; Idziak, A. F.
vol. 29, no. 395, 2006, ISSN: 0138015X.
@proceedings{2-s2.0-34247642251,
title = {Calculation of block divisibility using structural and refraction seismic methods in Debnik and Imielin raw material deposits},
author = { Z. Mirkowski and R. Tomaszewska and A.F. Idziak},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-34247642251&partnerID=40&md5=5b7b3ac91a0a224a10df50c973a7952b},
issn = {0138015X},
year = {2006},
date = {2006-01-01},
journal = {Publications of the Institute of Geophysics, Polish Academy of Sciences, Series M: Miscellanea},
volume = {29},
number = {395},
pages = {223-229},
abstract = {The structural research was done in the Silesian-Kraków Upland in two open-cuts of building stone: Dȩbnik (limestone) and Imielin (dolomite). As a result of the investigations, the directions of fracture systems were delineated and block divisibility was calculated, as principal parameters in the documentation of building stone. Simultaneously, geophysical methods were applied using shallow seismic refraction. According to the azimuthal velocity of wave propagation, the orientation of fracture was estimated. In Dȩbnik a strong anisotropy of seismic waves occured and there was an excellent correlation between structural and seismic measurements, whereas in Imielin this correlation was rather weak, which was probably caused by using explosives for mining in the open-cut. The calculation of block divisibility using a seismic method was not possible in this case.},
keywords = {},
pubstate = {published},
tppubtype = {proceedings}
}
Badera, J.; Niemczuk, S.; Tomaszewska, R.
vol. 29, no. 395, 2006, ISSN: 0138015X, (1).
@proceedings{2-s2.0-34247606530,
title = {Application of the shallow refraction seismic method for analysis of block divisibility of Carpathian sandstones in the Górka-Mucharz deposit},
author = { J. Badera and S. Niemczuk and R. Tomaszewska},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-34247606530&partnerID=40&md5=8e2b0edd0dfdd99da82dbb52b85ca0c5},
issn = {0138015X},
year = {2006},
date = {2006-01-01},
journal = {Publications of the Institute of Geophysics, Polish Academy of Sciences, Series M: Miscellanea},
volume = {29},
number = {395},
pages = {231-237},
abstract = {The application of the shallow refraction seismic method for analysis of block divisibility of natural building stone is presented for an example of the Górka-Mucharz sandstone deposit (Polish Carpathians). Geological block divisibility is a relative participation of the block material in a deposit, profile etc. The applied method reflects the main fracture directions to the satisfactory degree but the estimation of fracture linear density has only an approximate character. The authors suggest the possibility to set the volume of average block as an additional (geophysical) index of the block divisibility.},
note = {1},
keywords = {},
pubstate = {published},
tppubtype = {proceedings}
}
2002
Król, M.; Tomaszewska, R.
Comparison of direct structural research and shallow seismic refraction method in systematic joints study Journal Article
In: Publications of the Institute of Geophysics, Polish Academy of Sciences, Series M: Miscellanea, vol. 24, no. 340, pp. 413-418, 2002, ISSN: 0138015X.
@article{2-s2.0-0036997658,
title = {Comparison of direct structural research and shallow seismic refraction method in systematic joints study},
author = { M. Król and R. Tomaszewska},
url = {https://www.scopus.com/inward/record.uri?eid=2-s2.0-0036997658&partnerID=40&md5=eb19b62bb4c6d0b453a9251057b6ff77},
issn = {0138015X},
year = {2002},
date = {2002-01-01},
journal = {Publications of the Institute of Geophysics, Polish Academy of Sciences, Series M: Miscellanea},
volume = {24},
number = {340},
pages = {413-418},
abstract = {The paper presents results of measurements of seismic wave velocity anisotropy. The results obtained were compared with direct structural measurements. The investigations were carried out in the Triassic carbonate deposits in the NE margin of the Upper Silesian Coal Basin (the USCB). Three areas have been chosen: Strzyzowice, Ujejsce, Strzemieszyce. The velocity of wave propagation was measured in profiles which were radially set, so it was possible to determine the orientation of fracture in the rock mass. The results were estimated on the basis of 2-rank and 4-rank tensors. In the case of strong anisotropy of seismic waves and small numbers of joint sets, there was a good correlation of seismic and structural measurements.},
keywords = {},
pubstate = {published},
tppubtype = {article}
}