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Author Profile dr hab. inż., prof. AGH

Tomecka-Suchoń, Sylwia

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ORCID: 0000-0002-7307-9448 
Web of Science: R-9128-2018 
ScopusID: 6602220011 
PBN - Polish Scientific Bibliography 
OPI - Polish Science Database 
Systemy AGH
Bibliografia: BaDAP AGH 
SkOs AGH 
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Now showing 1 - 4 of 4
  • thumbnail.journal.alt
    Item type:Article, Access status: Open Access ,
    Complex analysis of GPR signals for the delineation of subsurface subtle features
    (Wydawnictwa AGH, 2019) Akinsunmade, Akinniyi; Tomecka-Suchoń, Sylwia; Pysz, Paweł
    In this paper, complex signal analyses of ground penetrating radar (GPR) field data over an area of farmland in Krakow were interpreted alongside the basic filtered field data. The farmland was simulated with varying degrees of soil compaction induced by tractor movement. The focus of the study was the delineation of inherent characteristics of media through which the electromagnetic energy travelled. Fourteen GPR profiles were acquired from the area. The field data were subjected to pre- and post-processing prior to its the presentation and interpretation. Advance analysis operations on the field data which resorted in different attributes reveal more about the effects of the compaction on the soil than indicated by the basic filtered field data. Better resolution of subsurface layers boundary and lateral variation in the physical properties of the traversing media were well elucidated. The results have demonstrated that an advanced signal processing such as used in the study has ability to depict subtle characteristics of the propagating media.
  • thumbnail.journal.alt
    Item type:Article, Access status: Open Access ,
    Feasibility analysis of using GPR method for the examination of post-glacial deposits in mountainous geological environment
    (Wydawnictwa AGH, 2011) Tomecka-Suchoń, Sylwia; Gołębiowski, Tomisław
    The Ground Penetrating Radar (GPR) measurements presented in this paper had two main objectives. The first was to analize the possibility of using GPR method in examination of sediments in a mountainous geological environment and the second objective was to assess the special distribution of post-glacial sediments and their thickness at a selected site. The experimental measurements were carried out on in the alp of Ornak in the western part of Tatra Mountains This article provides a brief theoretical analysis of possible use of the georadar method in post-glacial sediment examination. The results of GPR surveys done in the reflection profiling mode enable the distinction of zones with different amount of till, clay, sand, gravel and rock debris in the post-glacial sediments.
  • thumbnail.journal.alt
    Item type:Article, Access status: Open Access ,
    Analiza możliwości wykorzystania georadarowych fal refrakcyjnych do lokalizacji zmian w budowie wałów przeciwpowodziowych
    (Wydawnictwa AGH, 2005) Marcak, Henryk; Gołębiowski, Tomisław; Tomecka-Suchoń, Sylwia
    The GPR refracted waves can be used for evaluation of parameters, which characterize two-layer ground, where upper layer has higher value of dielectric constant than lower one. Such situation can take a place in a river embankments, where over the zone of consolidation with low water content is placed a lose zone with large amount of rain-water. The results of GPR measurements carried out on the embankments in Kraków, give possibility for identification the consolidated and lose zones, between geotechnical bench-marks. The paper presents new technology of GPR profiling with various offset of antennas and it describes the technique of identification the different kinds of GPR waves, with special treatment of refracted waves.
  • thumbnail.journal.alt
    Item type:Article, Access status: Open Access ,
    Badania georadarowe dla oceny mineralizacji wody gruntowej
    (Wydawnictwa AGH, 2009) Marcak, Henryk; Tomecka-Suchoń, Sylwia
    Analysis of the physical properties of rock formation and electromagnetic waves propagation in rocks leads to conclusion, that three parameters estimated from GPR data, the reflection coefficient, wave attenuation and velocity can be used for assessment of the soil water mineralization. The field test measurements were carried out in the area, where the mineralization has been recognized with hydrogeological methods. The correlation has been found between sums of registered GPR signals from chosen depth interval and the mineralization of ground water.