SPECIFICS IN THE FORMATION OF SUBSIDENCE TROUGHS IN THE KARVINA PART OF THE OSTRAVA-KARVINA COALFIELD WITH THE USE OF RADAR INTERFEROMETRY

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F61989100%3A27350%2F16%3A86097385" target="_blank" >RIV/61989100:27350/16:86097385 - isvavai.cz</a>

Nalezeny alternativní kódy

RIV/61989100:27740/16:86097385

Výsledek na webu

<a href="http://dx.doi.org/10.13168/AGG.2016.0008" target="_blank" >http://dx.doi.org/10.13168/AGG.2016.0008</a>

DOI - Digital Object Identifier

<a href="http://dx.doi.org/10.13168/AGG.2016.0008" target="_blank" >10.13168/AGG.2016.0008</a>

Jazyk výsledku

angličtina

Název v původním jazyce

SPECIFICS IN THE FORMATION OF SUBSIDENCE TROUGHS IN THE KARVINA PART OF THE OSTRAVA-KARVINA COALFIELD WITH THE USE OF RADAR INTERFEROMETRY

Popis výsledku v původním jazyce

Deep extraction of minerals is accompanied by deformations of the strata overlying extracted coal seams. Deformations of overlying layers run up to the surface where a subsidence trough gradually forms. The movement of individual surface points is curvilinear, spatial and, in relation to the time pattern, not uniform. In some cases, during the formation of a subsidence trough, temporary uplifts of the surface occur. This paper gives a particular area in which uplifts of the surface occurred when the rigid overlying strata was disturbed. The character of deformations of the overlying rocks is evaluated on the basis of a comparison of the results of the measurement of subsidence of the surface using geodetic methods with the development of mined-out areas and with their extracted thickness. For specifying the time of failure of the overlying strata, also information obtained from a system of continuous monitoring of seismic events is used. The spatial extent of the subsidence trough is identified by satellite radar interferometry (InSAR) techniques applied to TerraSAR-X images. The subsidence wave was possible to detect using a short temporal difference of 11 days between satellite radar images. This shows the potential of short-temporal high resolution InSAR for monitoring of progress of subsidence trough. A good knowledge of extents and shape of subsidence trough formation in time allows to verify values of parameters used for prediction purposes.

Název v anglickém jazyce

SPECIFICS IN THE FORMATION OF SUBSIDENCE TROUGHS IN THE KARVINA PART OF THE OSTRAVA-KARVINA COALFIELD WITH THE USE OF RADAR INTERFEROMETRY

Popis výsledku anglicky

Deep extraction of minerals is accompanied by deformations of the strata overlying extracted coal seams. Deformations of overlying layers run up to the surface where a subsidence trough gradually forms. The movement of individual surface points is curvilinear, spatial and, in relation to the time pattern, not uniform. In some cases, during the formation of a subsidence trough, temporary uplifts of the surface occur. This paper gives a particular area in which uplifts of the surface occurred when the rigid overlying strata was disturbed. The character of deformations of the overlying rocks is evaluated on the basis of a comparison of the results of the measurement of subsidence of the surface using geodetic methods with the development of mined-out areas and with their extracted thickness. For specifying the time of failure of the overlying strata, also information obtained from a system of continuous monitoring of seismic events is used. The spatial extent of the subsidence trough is identified by satellite radar interferometry (InSAR) techniques applied to TerraSAR-X images. The subsidence wave was possible to detect using a short temporal difference of 11 days between satellite radar images. This shows the potential of short-temporal high resolution InSAR for monitoring of progress of subsidence trough. A good knowledge of extents and shape of subsidence trough formation in time allows to verify values of parameters used for prediction purposes.

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10508 - Physical geography

Projekt

Výsledek vznikl pri realizaci vícero projektů. Více informací v záložce Projekty.

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2016

Kód důvěrnosti údajů

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

Název periodika

Acta Geodynamica et Geomaterialia

ISSN

1214-9705

e-ISSN

—

Svazek periodika

13

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

7

Strana od-do

263-269

Kód UT WoS článku

000384272300005

EID výsledku v databázi Scopus

2-s2.0-84988490226