Zobrazeno 1 - 10
of 15
pro vyhledávání: '"Luka SERIANZ"'
Publikováno v:
Geologija, Vol 66, Iss 2, Pp 285-299 (2023)
Waste disposal in landfills represents a severe threat to aquatic environments on the local, regional, and global levels. In Slovenia, there are 69 registered landfills where groundwater is regularly monitored. However, isotope techniques are not reg
Externí odkaz:
https://doaj.org/article/f48530841a84407db39930f32fc94a66
Publikováno v:
Geologija, Vol 64, Iss 2, Pp 205-220 (2021)
Triglavska Bistrica is a typical Alpine river in the north-western part of Slovenia. Its recharge area includes some of the highest peaks in the Julian Alps. The hydrogeological conditions and flow of the river depend largely on groundwater exchange
Externí odkaz:
https://doaj.org/article/0004d420002f4f13976f342d89e1d969
Publikováno v:
Geologija, Vol 63, Iss 2, Pp 281-294 (2020)
A comparative analysis of step-drawdown tests was performed in order to estimate the well performance in Slovenian thermal and mineral water wells. Tests were performed in 30 wells, each having its own maximum production rate determined in the conc
Externí odkaz:
https://doaj.org/article/a436ac3a677546d48c3dcfaca957b1be
Publikováno v:
Energies, Vol 15, Iss 14, p 5150 (2022)
Waste management in Europe has improved in recent years, reducing the amount of waste disposed at landfills. However, there are still many landfills in the countries. It is well known that landfills that do not have measures in place to control leach
Externí odkaz:
https://doaj.org/article/578917f853db45e1b64be761e35677ad
Publikováno v:
Geologija, Vol 61, Iss 2, Pp 191-203 (2018)
The area above the settlement of Koroška Bela is highly prone to slope mass movements and poses a high risk for the safety of the settlement. To get an insight into the hydrogeological conditions and processes which can affect mass movements in th
Externí odkaz:
https://doaj.org/article/03e5d6c089304dfc908cdd8b468128c7
Publikováno v:
Water, Vol 14, Iss 6, p 912 (2022)
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
Externí odkaz:
https://doaj.org/article/662ad04618284ad4986a8b800bc49964
Autor:
Luka Serianz
Publikováno v:
Geologija, Vol 59, Iss 2, Pp 193-204 (2016)
The Radovna River Valley is located in the northwest of Slovenia, in the Julian Alps, and bounded by two plateaus – Pokljuka in the south and Mežakla in the north. Typical geological and geomorphological shapes in the valley indicate several gla
Externí odkaz:
https://doaj.org/article/1136c3b47e9d40388959b8facb55e100
Publikováno v:
Water, Vol 12, Iss 5, p 1427 (2020)
The Alps represent an area where many deep groundwater circulations occur as thermal springs. In the Bled case study, the thermal water temperature, at it is discharged to the surface, is between 19–23 °C. In order to determine the extent (e.g., g
Externí odkaz:
https://doaj.org/article/825f6b51413e4235a6310f9d87899559
Publikováno v:
Renewable Energy. 182:751-763
Thermal water discharge within the gravity-driven groundwater flow system in the Alps and other similar areas around the world may be hidden in Quaternary deposits which, in these regions, often cover the regional aquifer. When thermal water drains i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::810bb448320fc1a9cf010ace5b8eb859
https://doi.org/10.1016/j.renene.2021.10.004
https://doi.org/10.1016/j.renene.2021.10.004
Publikováno v:
Geologija, Vol 63, Iss 2, Pp 281-294 (2020)
A comparative analysis of step-drawdown tests was performed in order to estimate the well performance in Slovenian thermal and mineral water wells. Tests were performed in 30 wells, each having its own maximum production rate determined in the conces
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::eec00867411762055250d5686e6e4528
https://doi.org/10.5474/geologija.2020.021
https://doi.org/10.5474/geologija.2020.021