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Statements

Subject Item
n2:RIV%2F61989100%3A27350%2F09%3A00022271%21RIV10-GA0-27350___
rdf:type
n10:Vysledek skos:Concept
dcterms:description
The locality of Doubrava Oplíží is one of the landslides within an extensive slope front situated between the municipalities of Doubrava and Dětmarovice in the Moravian-Silesian Region and at the same time, in the allotment of Karviná Mine, ČSA Plant. The slope deformation stability was assessed in terms of the impacts of underground making use of isocatabase maps, terrain deformation parameter values determining the group of building sites subject to ČSN 73 0039, movements measured by zone extensometry and rainfall totals. The assessment of rainfall totals as well as a generally significant factor influencing the mobility of landslides did not identify any reaction in the measured movements of the slope deformation. The maps of subsidence caused by underground revealed a concordant declination of the slope deformation with the subsidence basin slope inclination that shall further increase according to the prospective maps till 2010. Thus, it is the case of the least favourable impact of the subsidenc The locality of Doubrava Oplíží is one of the landslides within an extensive slope front situated between the municipalities of Doubrava and Dětmarovice in the Moravian-Silesian Region and at the same time, in the allotment of Karviná Mine, ČSA Plant. The slope deformation stability was assessed in terms of the impacts of underground making use of isocatabase maps, terrain deformation parameter values determining the group of building sites subject to ČSN 73 0039, movements measured by zone extensometry and rainfall totals. The assessment of rainfall totals as well as a generally significant factor influencing the mobility of landslides did not identify any reaction in the measured movements of the slope deformation. The maps of subsidence caused by underground revealed a concordant declination of the slope deformation with the subsidence basin slope inclination that shall further increase according to the prospective maps till 2010. Thus, it is the case of the least favourable impact of the subsidenc
dcterms:title
The Impacts of Underground Mining as a Possible Factor Affecting the Doubrava Oplíží Slope Movement Aktivity The Impacts of Underground Mining as a Possible Factor Affecting the Doubrava Oplíží Slope Movement Aktivity
skos:prefLabel
The Impacts of Underground Mining as a Possible Factor Affecting the Doubrava Oplíží Slope Movement Aktivity The Impacts of Underground Mining as a Possible Factor Affecting the Doubrava Oplíží Slope Movement Aktivity
skos:notation
RIV/61989100:27350/09:00022271!RIV10-GA0-27350___
n4:aktivita
n18:P
n4:aktivity
P(GA105/07/1308)
n4:cisloPeriodika
4
n4:dodaniDat
n11:2010
n4:domaciTvurceVysledku
n5:3411133
n4:druhVysledku
n16:J
n4:duvernostUdaju
n15:S
n4:entitaPredkladatele
n7:predkladatel
n4:idSjednocenehoVysledku
318659
n4:idVysledku
RIV/61989100:27350/09:00022271
n4:jazykVysledku
n6:eng
n4:klicovaSlova
engineering geology; slope deformations; mining; undermine
n4:klicoveSlovo
n14:undermine n14:mining n14:slope%20deformations n14:engineering%20geology
n4:kodStatuVydavatele
PL - Polská republika
n4:kontrolniKodProRIV
[B0BB76D21DB3]
n4:nazevZdroje
Studia Geotechnica et Mechanic
n4:obor
n9:DB
n4:pocetDomacichTvurcuVysledku
1
n4:pocetTvurcuVysledku
3
n4:projekt
n13:GA105%2F07%2F1308
n4:rokUplatneniVysledku
n11:2009
n4:svazekPeriodika
31
n4:tvurceVysledku
Marschalko, Marian Fuka, Matěj Třeslín, Lubomír
s:issn
0137-6365
s:numberOfPages
9
n17:organizacniJednotka
27350