Cichostępski, Kamil
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nauki o Ziemi i środowisku
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Item type:Article, Access status: Open Access , Application of inverse Q filtering for improvement of seismic resolution in the Zechstein formation (SW Poland)(Wydawnictwa AGH, 2013) Król, Monika; Cichostępski, Kamil; Dec, Jerzy; Pietsch, KajaSeismic wave attenuation has strong, negative effect on the seismic data resolution. The high influence of this phenomenon was observed during realization of seismic survey »Duża Wólka 3D« (Geofizyka Kraków S.A. 2010a). The resolution of recorded seismic data was very low due to high attenuation caused by the Lower Triassic Buntsandstein sandstones. In consequence, interpretation of the thin-layered Zechstein formation is ambiguous. The aim of this paper is to present the multi-stage algorithm for the purpose of minimizing the attenuation effect, hence increasing the resolution of the seismic data. In order to achieve this, the inverse <i>Q</i> filtering process was used. The <i>Q</i> factor (quality factor) was estimated from the vertical seismic profiling data (Geofizyka Kraków S.A. 2010c). To verify the effectiveness of inverse <i>Q</i> filtering, seismic modelling was performed. Results received from seismic modelling gave basis for application the inverse <i>Q</i> filtering on real data. For this operation the seismic time profile inline 112 was chosen from the seismic data set »Duża Wólka 3D«. Application of inverse <i>Q</i> filtering significantly increased the seismic resolution, which enabled the interpretation of the Zechstein formation with more accuracy.Item type:Article, Access status: Open Access , Integration of MASW and ERT methods for site characterisation: a case study from Czernichów (Southern Poland)(Wydawnictwa AGH, 2026) Cichostępski, Kamil; Bania, Grzegorz; Borecka, AleksandraThe paper presents an integrated use of multichannel analysis of surface waves (MASW) and electrical resistivity tomography (ERT) to characterise the physical properties of near-surface materials, identify subsurface structures, and estimate the depth to bedrock in a planned construction area near Czernichów, close to Krakow (southern Poland). The study shows that integrating MASW and ERT provides a cost-effective and complementary approach to subsurface characterisation, delivering more reliable and less ambiguous interpretations than when the methods are applied independently, thereby reducing the need for expensive and invasive in situ geotechnical investigations. Particular emphasis is also placed on the methodological aspects of both methods. The study site is located on an alluvial plain composed of alluvial soils, sands, sand–gravel mixtures, and silty clays overlying limestone bedrock. Geophysical data were collected along five profiles. The resulting shear wave velocity models and the inverse model resistivity sections show good agreement with borehole data. The study area is characterised by a wide range of physical parameters derived from both methods. The MASW survey enabled recognition of the subsurface down to the bedrock, revealing four seismic layers differing in S-wave velocity. Nevertheless, the MASW inversion did not provide reliable estimates of the limestone S-wave velocity, although it successfully delineated its depth and morphology. The ERT survey identified three geoelectrical layers and proved to be more effective in resolving shallow geological structure, particularly in identifying the boundaries between alluvial soils and sand–gravel mixtures, whereas the depth and morphology of the limestone bedrock were constrained primarily by MASW.
