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| rdf:type
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| Description
| - The geological structure of the catchment area of Jančovec tream is very various, east side is formed by the rocks at Brno Massif and the west side is formed by the devonian limestones of the Moravian Karst. There are situated deep boreholes HV 701, HV 401, HV 501, HV 801 and wells Prosba lesa, Liščí, Hubertova and Srnčí. Considerable quantity of contamination influenced groundwater and their quality. The very complicated geological and hydrogeological situation defends exactly designation of contaminator part. The extremely hight vulnerability of karst-fissure aquifer does not cause clear designation of contamiantors. The inclination of slope, scarp or valley is very important parameter in surroundings of shallow (entrance) holes in karst. Another very important parameter of groundwater vulnerability is tectonic system and his direction. The size of protective zone around springs, boreholes, entrance holes and others is very subjective and groundwater vulnerable, as a parameter of area, is neces
- The geological structure of the catchment area of Jančovec tream is very various, east side is formed by the rocks at Brno Massif and the west side is formed by the devonian limestones of the Moravian Karst. There are situated deep boreholes HV 701, HV 401, HV 501, HV 801 and wells Prosba lesa, Liščí, Hubertova and Srnčí. Considerable quantity of contamination influenced groundwater and their quality. The very complicated geological and hydrogeological situation defends exactly designation of contaminator part. The extremely hight vulnerability of karst-fissure aquifer does not cause clear designation of contamiantors. The inclination of slope, scarp or valley is very important parameter in surroundings of shallow (entrance) holes in karst. Another very important parameter of groundwater vulnerability is tectonic system and his direction. The size of protective zone around springs, boreholes, entrance holes and others is very subjective and groundwater vulnerable, as a parameter of area, is neces (en)
- Geologický povrch na území povodí potoka Jančovec je velmi rozmanitý, východní část pokrývají horniny Brněnského masívu a západní část je formována vápenci Moravského krasu. NA území se nacházejí 4 hluboké vrty HV 701, HV 401, HV 501, HV 801 a 4 studánky Prosba lesa, Liščí, Hubertova a Srnčí. Na území působí větší počet zdrojů znečištění. Přesnějšímu určení podílu jednotlivých znečišťovatelů na kontaminaci zdejších podzemních vod brání složité místní geologické a hydrogeologické poměry, zvláště pak na styku hornin brněnského masívu a vápenců Moravského krasu. Jednoznačnému určení původce znesnadňuje velmi vysoké riziko zranitelnosti puklinovo-krasového kolektoru. (cs)
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| Title
| - The methodology of assessment of groundwater vulnerability in the area of the Masaryk Forest Training Enterprise at Krtiny
- The methodology of assessment of groundwater vulnerability in the area of the Masaryk Forest Training Enterprise at Krtiny (en)
- Metodika hodnocení zranitelnosti podzemních vod na území ŠLP ML Křtiny (cs)
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| skos:prefLabel
| - The methodology of assessment of groundwater vulnerability in the area of the Masaryk Forest Training Enterprise at Krtiny
- The methodology of assessment of groundwater vulnerability in the area of the Masaryk Forest Training Enterprise at Krtiny (en)
- Metodika hodnocení zranitelnosti podzemních vod na území ŠLP ML Křtiny (cs)
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| skos:notation
| - RIV/62156489:43410/05:00084195!RIV06-GA0-43410___
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| http://linked.open.../vavai/riv/strany
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| http://linked.open...avai/riv/aktivita
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| http://linked.open...avai/riv/aktivity
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| http://linked.open...vai/riv/dodaniDat
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| http://linked.open...aciTvurceVysledku
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| http://linked.open.../riv/druhVysledku
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| http://linked.open...iv/duvernostUdaju
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| http://linked.open...titaPredkladatele
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| http://linked.open...dnocenehoVysledku
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| http://linked.open...ai/riv/idVysledku
| - RIV/62156489:43410/05:00084195
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| http://linked.open...riv/jazykVysledku
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| http://linked.open.../riv/klicovaSlova
| - Brno Massif, devonian limestone, Moravian Karst; groundwater vulnerability; well, spring, borehole (en)
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| http://linked.open.../riv/klicoveSlovo
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| http://linked.open...ontrolniKodProRIV
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| http://linked.open...i/riv/mistoVydani
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| http://linked.open...i/riv/nazevZdroje
| - MendelNet 2005 (sborník abstraktů z evropské vědecké konference doktorandů)
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| http://linked.open...in/vavai/riv/obor
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| http://linked.open...ichTvurcuVysledku
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| http://linked.open...cetTvurcuVysledku
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| http://linked.open...vavai/riv/projekt
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| http://linked.open...UplatneniVysledku
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| http://linked.open...iv/tvurceVysledku
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| number of pages
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| http://purl.org/ne...btex#hasPublisher
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| https://schema.org/isbn
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| http://localhost/t...ganizacniJednotka
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| is http://linked.open...avai/riv/vysledek
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