Mapping The Resonance Frequency of Sedimentary Layers in the Vicinity of a Permanent Seismic Station in Undermined Area

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F68145535%3A_____%2F14%3A00433752" target="_blank" >RIV/68145535:_____/14:00433752 - isvavai.cz</a>

Výsledek na webu

<a href="http://dx.doi.org/10.5593/sgem2014B11" target="_blank" >http://dx.doi.org/10.5593/sgem2014B11</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.5593/sgem2014B11" target="_blank" >10.5593/sgem2014B11</a>

Jazyk výsledku

angličtina

Název v původním jazyce

Mapping The Resonance Frequency of Sedimentary Layers in the Vicinity of a Permanent Seismic Station in Undermined Area

Popis výsledku v původním jazyce

Resonant frequency and its changes in the surroundings of the permanent seismic station in the village of Stonava have been studied in this paper. Three different sets of seismic events were elaborated: local mining induced seismic events, distant earthquakes and seismic noise. Two data sets recorded at the permanent seismic station STO2 were used for spectral ratio computation using the HVSR method. First data set contains 20 records of mining induced seismic events with maximum epicental distance of 4km. The second data set contains 7 records of intensive distant earthquakes. Third data set was used for spectral ratio computation using the HVNR method. This data set contains records of seismic noise, that was measured at 18 places on the profile ofthe length of 2 km.

Název v anglickém jazyce

Mapping The Resonance Frequency of Sedimentary Layers in the Vicinity of a Permanent Seismic Station in Undermined Area

Popis výsledku anglicky

Resonant frequency and its changes in the surroundings of the permanent seismic station in the village of Stonava have been studied in this paper. Three different sets of seismic events were elaborated: local mining induced seismic events, distant earthquakes and seismic noise. Two data sets recorded at the permanent seismic station STO2 were used for spectral ratio computation using the HVSR method. First data set contains 20 records of mining induced seismic events with maximum epicental distance of 4km. The second data set contains 7 records of intensive distant earthquakes. Third data set was used for spectral ratio computation using the HVNR method. This data set contains records of seismic noise, that was measured at 18 places on the profile ofthe length of 2 km.

Druh

D - Stať ve sborníku

CEP obor

JM - Inženýrské stavitelství

OECD FORD obor

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Projekt

<a href="/cs/project/GP13-07027P" target="_blank" >GP13-07027P: Studium seizmických charakteristik základových půd s využitím frekvenční analýzy vibračních projevů</a><br>

Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2014

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název statě ve sborníku

SGEM- 14th International Multidisciplinary Scientific Geoconference

ISBN

978-619-7105-07-0

ISSN

1314-2704

e-ISSN

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Počet stran výsledku

8

Strana od-do

513-520

Název nakladatele

SGEM

Místo vydání

Albena

Místo konání akce

Albena

Datum konání akce

17. 6. 2014

Typ akce podle státní příslušnosti

WRD - Celosvětová akce

Kód UT WoS článku

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