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Subakvalne prsti Bohinjskega jezera
ID Stanovnik, Neža (Author), ID Repe, Blaž (Mentor) More about this mentor... This link opens in a new window

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Abstract
Bohinjsko jezero je največje stalno jezero v Sloveniji (Zorn, 2010),vendar so subakvalne prsti na tem območju še dokaj neraziskane. Namen dela je raziskati subakvalne prsti na jugozahodni obali, med izlivom Savice ter kampom Bohinj. To je bilo doseženo s terenskim delom oziroma vzorčenjem, kjer so bili zbrane tri lokacije, ki so bili po sušenju pripravljeni za laboratorijske analize. V laboratoriju je bila opisana mokra in suha barva vzorcev ter organska snov znotraj posameznih horizontov. Opravljene so bile tudi mehanska in pH analiza ter analiziran delež organske snovi za izbrane horizonte, ki je bil predvsem v primeru vzorca 1 nepričakovano visok. Rezultati so pokazali in izpostavili pomembne lastnosti vzorcev, s pomočjo katerih so bili ti uvrščeni na podlagi WRB klasifikacije. Rezultati dela so pokazali da se vzorci uvrščajo v tri različne skupine prsti. Prvi vzorec spada med arenosole, drugi med fluviosole ter zadnji med leptosole. Sestava in lastnosti prsti so v pomoč tudi pri opisovanju pedogenetskih dejavnikov ter procesov, ki vplivajo na izbrano območje.

Language:Slovenian
Keywords:Pedogeografija, Subakvalne prsti, Bohinjsko jezero, pedogenetska analiza, WRB klasifikacija
Work type:Bachelor thesis/paper
Organization:FF - Faculty of Arts
Year:2024
PID:20.500.12556/RUL-163604 This link opens in a new window
Publication date in RUL:09.10.2024
Views:60
Downloads:23
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Secondary language

Language:English
Title:Subaquatic soils of Bohinj lake
Abstract:
Lake Bohinj is the largest permanent lake in Slovenia (Zorn, 2010), but the subaquatic soils in this area are still relatively unexplored. The study aims to investigate the subaquatic soils on the south-western shore, between the mouth of the Savica River and the Bohinj campsite. This was achieved through field work and sampling, during which three samples were collected, dried and prepared for laboratory analysis. In the laboratory, the wet and dry colours of the samples and the organic matter within each horizon were described. Mechanical and pH analyses were also carried out and the organic matter content was analysed for selected horizons, which was unexpectedly high in the case of sample 1. The results revealed important characteristics of the samples that allowed them to be categorised according to the WRB classification. The results showed that the samples fall into three different soil groups: The first sample is classified as Arenosol, the second as Fluvisol and the last as Leptosol. The composition and properties of the soils also help to describe the pedogenetic factors and processes that influence the selected area.

Keywords:Soil geography, Subaquatic soils, Bohinj Lake, pedogenic analysis, WRB classification

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