Zobrazeno 1 - 10
of 18
pro vyhledávání: '"KŮRKOVÁ, IVA"'
Autor:
Kůrková, Iva
This thesis is divided into two parts. The first one is focused on tracer tests carried out in several karst conduits in the Moravian Karst. Several conduits were tracer repeatedly during different discharges. Flow velocity, flow cross section area,
Externí odkaz:
http://www.nusl.cz/ntk/nusl-312242
Autor:
Kůrková, Iva, Bruthans, Jiří, Balák, František, Slavík, Martin, Schweigstillová, Jana, Bruthansová, Jana, Mikuš, Petr, Vojtíšek, Jan, Grundloch, Jiří
Publikováno v:
In Journal of Hydrology July 2019 574:1062-1073
Autor:
Kůrková, Iva
The study focuses on water flow in sandstones and sandy limestones of the so-called facies transition in the western part of the Bohemian Cretaceous Basin. The area between Turnov, Milovice, Úštěk and Doksy is a part of most important aquifer in t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2186::52fde9882da539678942b75aa380b645
http://www.nusl.cz/ntk/nusl-524889
http://www.nusl.cz/ntk/nusl-524889
Akademický článek
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Autor:
Kůrková, Iva
This thesis is divided into two parts. The first one is focused on tracer tests carried out in several karst conduits in the Moravian Karst. Several conduits were tracer repeatedly during different discharges. Flow velocity, flow cross section area,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2186::375584003cb545de31c3d6c5c3794846
http://www.nusl.cz/ntk/nusl-312242
http://www.nusl.cz/ntk/nusl-312242
Publikováno v:
Geoscience Research Reports / Zprávy o Geologických Výzkumech v Roce; 2016, Vol. 49, p93-99, 7p
Autor:
Kůrková, Ivana
This diploma thesis deals with the possibilities of the teacher's influence on the pupils' self-conception. The first part contains the definition of basic terms, explanation of the process of forming of se1f-conception and sets as its goal to point
Externí odkaz:
http://www.nusl.cz/ntk/nusl-296351
Autor:
Bašus, Jan
EN There is an intense exchange of water between the quaternary fluvial sediments and river. Although the precise amount of seepage flow is needed for various hydrogeological models and calculations, the systematic measurements of the seepage flux in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2186::b4b9d241da933762e99278462f004679
http://www.nusl.cz/ntk/nusl-415873
http://www.nusl.cz/ntk/nusl-415873
Autor:
Mareš, Jakub
The karst aquifers are formed by highly permeable conduits that allow very fast and concentrated flow. They can transport contaminants and endanger drinking water sources. Due to the large abundance of karstified carbonate rocks, it is necessary to p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=od______2186::9645ab53e0a002d75a59f73e513acdb2
http://www.nusl.cz/ntk/nusl-369002
http://www.nusl.cz/ntk/nusl-369002
Autor:
Vojtíšek, Jan
The process of karstification doesn't occur only in easily soluble rock, such as limestone and evaporites, but also occurs in other rocks such as quartzites or siliciclastic rocks with carbonate cement. The "ghost rock" karstification is, unlike the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::3559c8ea3d01d5829e5d6e52f69cd446
http://www.nusl.cz/ntk/nusl-346606
http://www.nusl.cz/ntk/nusl-346606