Application of passive seismic to shallow geological structures in urban areas
Journal Title: Studia Quaternaria - Year 2014, Vol 31, Issue 2
Abstract
To study the shallow geological structure the Refraction Microtremor (ReMi) method was applied. This technique uses seismic noise analysis where a source of this small vibrations is the human activity e.g.: traffic, production, factories. The surveys were carried out in selected urban areas in the region of the Upper Silesian Industrial District : Sosnowiec - Pogoń , Chorzów - Chorzow Stary and Bytom - Karb. Each area is characterized by the presence of nearby roads with a very high traffic. The results of passive seismic (ReMi) were confronted with data obtained using Multichannel Analysis of Surface Waves (MASW) and resistivity imaging (RI). Seismic surveys were performed by apparatus PASI with 24 channels using geophones of 4.5Hz. The results showed that passive seismic can be satisfactorily used in such urban conditions. The shallow geological structure interpreted by seismic methods have been well-correlated with resistivity studies.
Authors and Affiliations
Maciej Mendecki, Michał Glazer, Mateusz Mycka
Keywords
Related Articles
- EP ID EP167282
- DOI 10.2478/squa-2014-0012
- Views 45
- Downloads 0
QUATERNARY VALLEY LEVELS AND RIVER TERRACES IN THE WESTERN PART OF THE HOLY CROSS MOUNTAINS
According to the current state of research five sand-gravel accumulation levels of Quaternary age are visible in the morphology of the western part of the Holy Cross Mountains, within the Wierna Rzeka, Hutka and Bobrza r...
COSMIC AIRBURST ON DEVELOPING ALLERØD SUBSTRATES (SOILS) IN THE WESTERN ALPS, MT. VISO AREA
Although much has been written about a cosmic impact event in the Western Alps of the Mt. Viso area, the event closely tied with the Younger Dryas Boundary (YDB) of 12.8 ka and onset of the Younger Dryas (YD), the affect...
Reading of ground-penetrating radar (GPR) images of prehistoric flint mine; case study from Krzemionki Opatowskie archaeological site in central Poland
Geophysical surveys conducted in order to map tunnels and vertical shafts at the Neolithic chert mining field Krzemionki used a ground-penetrating radar (GPR) to test hypotheses regarding orientation, depth and subsurfac...
Non-pollen palynomorphs from mid-Holocene peat of the raised bog Borsteler Moor (Lower Saxony, Germany)
In order to reconstruct regional vegetation changes and local conditions during the fen-bog transition in the Borsteler Moor (northwestern Germany), sediment core covering the period between 7.1 and 4.5 cal kyrs BP was p...
NON-POLLEN PALYNOMORPHS CHARACTERISTIC FOR THE DYSTROPHIC STAGE OF HUMIC LAKES IN THE WIGRY NATIONAL PARK, NE POLAND
The numerous dystrophic (humic) lakes are a very important feature of Wigry National Park, NE Poland. As the most recent palaeoecological data indicate, at the beginning of its development (in the Late Glacial and Early...