Geoelectrical imaging of slope deformations - towards repeated measurements, effective electrode array and limitations

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F12%3A10319237" target="_blank" >RIV/00216208:11310/12:10319237 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Geoelectrical imaging of slope deformations - towards repeated measurements, effective electrode array and limitations

Popis výsledku v původním jazyce

Use of geophysical methods within the research of the slope deformation became a standard during last decades. Electrical resistivity tomography (ERT), as one of the advanced geoelectrical methods, experiences boom in its utilization in numerous scientific fields, such as archaeology, geomorphology, engineering geology or hydrogeology. The presented contribution deals with utilization of ERT on the various types of mass movements. Recognition of the processes that affect slope stability, predispose or trigger slope movements, is fundamental for both understanding of the slope development and effective rehabilitation of failing slopes or sliding mass. Contribution points out (dis)advantages of the method, its limitations and related electrode array selection that can be crucial considering the required results. The choice of the appropriate electrode configuration always depends on the demanded resolution, depth range, and sensitivity to vertical/horizontal structures and, of course, on

Název v anglickém jazyce

Geoelectrical imaging of slope deformations - towards repeated measurements, effective electrode array and limitations

Popis výsledku anglicky

Use of geophysical methods within the research of the slope deformation became a standard during last decades. Electrical resistivity tomography (ERT), as one of the advanced geoelectrical methods, experiences boom in its utilization in numerous scientific fields, such as archaeology, geomorphology, engineering geology or hydrogeology. The presented contribution deals with utilization of ERT on the various types of mass movements. Recognition of the processes that affect slope stability, predispose or trigger slope movements, is fundamental for both understanding of the slope development and effective rehabilitation of failing slopes or sliding mass. Contribution points out (dis)advantages of the method, its limitations and related electrode array selection that can be crucial considering the required results. The choice of the appropriate electrode configuration always depends on the demanded resolution, depth range, and sensitivity to vertical/horizontal structures and, of course, on

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

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Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2012

Kód důvěrnosti údajů

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

Název periodika

Berichte der Geologischen Bundesanstalt

ISSN

1017-8880

e-ISSN

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Svazek periodika

2012

Číslo periodika v rámci svazku

93

Stát vydavatele periodika

AT - Rakouská republika

Počet stran výsledku

6

Strana od-do

198-203

Kód UT WoS článku

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EID výsledku v databázi Scopus

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