Poplave na Krasu v Sloveniji leta 2014

diplomska naloga

Maja Matič (Avtor), Mitja Brilly (Mentor), Dušan Žagar (Član komisije za zagovor)

Povzetek

Kras je pokrajina v Sloveniji z izjemnimi značilnostmi in posebnimi kraškimi pojavi, ki so znani po vsej Evropi. Še več, evropske države, ki so odkrile podobne pojave, so jih prav tako poimenovale kar kraški pojavi. Na krasu se, kot reden pojav, pojavljajo poplave. Vsakoletno poplavljanje kraških polj je vezano predvsem na padavine in povečan dotok vode, večja količina vode pa povzroči tudi zasičenje kraškega podzemlja z vodo, le ta pa nato privre na površje in poplavi polje. V teoretičnem delu diplomske naloge sem opisala nastanek krasa, kraške pojave ter značilnosti pretakanja vode pod površjem in tudi po njem. Osredotočila sem se na Planinsko polje, ki je bilo zaradi ekstremnih dogodkov februarja 2014 (močne padavine, žled, malo višje temperature, ki so povzročile dodaten dež namesto snega) poplavljeno. Poplavo v teh razsežnostih so strokovnjaki označili kot 100- letno. V drugem delu pa sem predstavila svoje delo, in sicer ogled poplavljenega Planinskega polja ter opravljene meritve, prav tako pa sem ves čas spremljala dogajanje in pripravila povzetek le tega ter podala svoje mnenje o nekaterih možnih rešitvah, ki bi v nadaljnje preprečile oziroma omejile tako velike poplave.

Ključne besede

gradbeništvo;diplomska naloga;UNI;B-VOI;Kras;Planinsko polje;poplave;

Podatki

Jezik:	Slovenski jezik
Leto izida:	2014
Tipologija:	2.11 - Diplomsko delo
Organizacija:	UL FGG - Fakulteta za gradbeništvo in geodezijo
Založnik:	M. Matič
UDK:	556.166(497.4Kras)(043.2)
COBISS:	6782305
Št. ogledov:	1800
Št. prenosov:	444
Ocena:	0 (0 glasov)
Metapodatki:

Ostali podatki

Sekundarni jezik:	Angleški jezik
Sekundarni naslov:	Floods in the Karst Region of Slovenia in 2014
Sekundarni povzetek:	The Slovenian Karst region has exceptional characteristics and special karst phenomena that are known throughout Europe. What is more, the similar occurrences discovered in other European countries have also been named karst phenomena. A regular occurrence in the Karst region is flooding. The annual flooding of karst fields is connected to precipitation and the increased water inflow; this greater amount of water then leads to the saturation of the karst underground with water, which then rises to the surface and floods the field. In the theoretical part of my thesis I have described the formation of the karst topography, the karst phenomena, and the characteristics of the streaming of groundwater, as well as the streaming of water on the surface. I have focused on the field Planinsko polje, which was flooded in February 2014 due to extreme weather events such as heavy rains, sleet, and slightly higher temperatures, which caused additional rain instead of snow. Experts claim that a flood this extensive was a 100-year-interval flood. In the second part of my thesis I have presented my work, which is the inspection of the flooded field Planinsko polje and the measurements taken. I have also followed further developments of the flooding and drawn up a summary of the events, as well as provided some possible solutions that would prevent or limit such extensive floods in the future.
Sekundarne ključne besede:	Karst;Planinsko polje;floods;
Vrsta datoteke:	application/pdf
Vrsta dela (COBISS):	Diplomsko delo/naloga
Komentar na gradivo:	Univ. v Ljubljani, Fak. za gradbeništvo in geodezijo
Strani:	VIII, 44 str.
ID:	8708416