1. (O)krog nasilja v družini in šoli : soočanje šole/vrtca z nasiljem nad otrokiDoroteja Lešnik, Ingrid Klemenčič, Mojca Pušnik, Katja Filipčič, Mitja Muršič, 2012 Keywords: otroci, učenci, medosebni odnosi, konflikti, reševanje konfliktov, agresivnost
DiRROS - Published: 19.10.2015; Views: 4611; Downloads: 910
 Fulltext (2,37 MB) |
2. Varnost cestnega prometaTatjana Polak, Dragan Petrovec, Nina Peršak, Mitja Muršič, Bogomil Brvar, Ljubo Bavcon, 2011 Keywords: cestni promet, varnost, kaznovalno pravo, kazni, prometne nesreče, prekrški
DiRROS - Published: 27.11.2015; Views: 5526; Downloads: 814
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3. Zapoved in zločin : stičišča prava, književnosti in teorijeMatej Accetto, Matjaž Ambrož, Matjaž Jager, Andrej Kristan, Mitja Muršič, Jurij Novak, Goran Č. Potočnik, Jernej Pribošič, John Stubbs, Aleš Završnik, 2012 Keywords: kriminologija, pravo, književnost
DiRROS - Published: 27.11.2015; Views: 4899; Downloads: 697
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4. Predlogi za izboljšanje razmer na področju upravljanja vodnih virovBrigita Jamnik, Mitja Janža, Joerg Prestor, Aleš Smrekar, Urša Vilhar, Branka Bračič-Železnik, Mateja Breg Valjavec, 2012 Keywords: hidrologija, upravljanje vodnih virov, razmere
DiRROS - Published: 12.07.2017; Views: 2231; Downloads: 585
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5. Characterizing the groundwater flow regime in a landslide recharge area using stable isotopes: a case study of the Urbas landslide area in NW SloveniaMitja Janža, Luka Serianz, Katja Koren, 2022 Abstract: Slope stability strongly depends on the prevailing hydrological and hydrogeological conditions. The amount and intensity of precipitation and changing groundwater levels are important landslide triggering factors. Environmental tracers, including the chemical and stable isotope compositions of precipitation and groundwater, were used to gain insight into the groundwater dynamics of the Urbas landslide. The landslide is situated in a mountainous area with steep slopes and high precipitation amount and poses a high risk for the safety of the Koroška Bela settlement that lies downstream. The stable isotope analyses of oxygen-18 (18O) and deuterium (2H) in the precipitation and groundwater were used to estimate the groundwater mean residence time and the average altitude of the landslide recharge area. This information will help to plan and prioritize remedial landslide measures aiming to reduce the recharge of the landslide body and, thus, lower the risk of transformation of the sliding material into debris flow. The results of the chemical analysis of samples taken from springs and a piezometer show a Ca–HCO3 water type. This indicates low water–rock interaction in a landslide area composed of Upper Carboniferous and Permian clastic rocks and points to upper laying carbonate rocks and scree deposits as the main recharge area. Water samples for stable isotope analyses of δ18O and δ2H were collected from a rain gauge, springs, and a piezometer over a two-year period (2018–2020). The estimated mean recharge altitude of the groundwater at sampling points was from approximately 1700 to 1800 m a.s.l. with a mean residence time of 2–5 months.
Keywords: landslide, groundwater, stable isotopes, oxygen-18, deuterium, hydrogeology, recharge dynamic
DiRROS - Published: 16.03.2022; Views: 189; Downloads: 87
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