Zobrazeno 1 - 10
of 19
pro vyhledávání: '"Maja Briški"'
Publikováno v:
Applied Water Science, Vol 14, Iss 10, Pp 1-24 (2024)
Abstract Many coastal and island communities depend on groundwater as the only source of freshwater, making it an invaluable resource. In the Mediterranean region, groundwater resources are highly vulnerable to natural and anthropogenic pressures, su
Externí odkaz:
https://doaj.org/article/32beb05a4e814991bff7de65d767c509
Publikováno v:
Hydrology, Vol 10, Iss 5, p 106 (2023)
Tracer testing is the only method in karst hydrogeology that can definitively determine whether a particular site belongs to a watershed of a particular karst spring. Therefore, it is an essential technique for delineating groundwater basins in karst
Externí odkaz:
https://doaj.org/article/99f7e407bbeb4091a82639467af9c8f1
Autor:
Željka Brkić, Maja Briški
Publikováno v:
Journal of Maps, Vol 14, Iss 2, Pp 173-177 (2018)
This paper presents a hydrogeological map of the western part of the Drava Basin in northern Croatia. An area of approximately 660 km2 is included in the hydrogeological map at a scale of 1:100,000. The map was made using ESRI ArcGIS 10 and ArcMap 10
Externí odkaz:
https://doaj.org/article/b4b25e99a9064d4589a89dd5faf0308a
Publikováno v:
Geosciences, Vol 10, Iss 4, p 137 (2020)
Crystalline rocks are generally characterized by negligible porosity and permeability in terms of groundwater exploitability. However, alteration processes can greatly increase their fracture permeability and induce formation of modest, but locally i
Externí odkaz:
https://doaj.org/article/f3e557ee32f84b42b732f35017084ac8
Autor:
Željko Duić, Maja Briški
Publikováno v:
Rudarsko-geološko-naftni Zbornik, Vol 22, Iss 1, Pp 1-9 (2010)
Shifts of structural units, which started in Pliocene are specifically expressed during the Quaternary. They last still today and affected the hydrogeological relations in the region of Baranja. Lithological development is dominated by one or maximum
Externí odkaz:
https://doaj.org/article/f40adc88bd984fc09652980b91166142
A hydrochemical and geothermometric study of thermal waters in Topusko (Croatia) was conducted in order to improve the existing conceptual model of the Topusko hydrothermal system. The town of Topusko is located 80 km south of Zagreb at the SW edge o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::384e4cfd228a6a41840fac31ceb10c4d
https://doi.org/10.5194/egusphere-egu23-14202
https://doi.org/10.5194/egusphere-egu23-14202
Publikováno v:
Sustainability; Volume 15; Issue 6; Pages: 5498
Topusko is the second warmest natural thermal water spring area in Croatia, located at the southwest edge of the Pannonian Basin System. Due to favourable geothermal properties, these waters have been used for heating and health and recreational tour
The assessment of groundwater resources quality and quantity in arid or semi-arid climates is crucial for achieving long-term sustainable management due to their limited volume and scarce replenishment. The relevance of this topic is enhanced by thei
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c310a8f71279485c1b7c9b8e5524564a
https://www.bib.irb.hr/1269202
https://www.bib.irb.hr/1269202
Autor:
Maja Briški, Bojan Verbič
Publikováno v:
International Journal of Parliamentary Studies. 1:199-206
Regarding the situation related to Covid-19, the National Assembly of the Republic of Slovenia in the spring of 2020 wanted to change the way of participation in the sessions of the National Assembly and its working bodies by means of information and
Autor:
Ozren Larva, Željka Brkić, Maja Briški, Ida Karlsson Seidenfaden, Julian Koch, Simon Stisen, Jens Christian Refsgaard
This paper presents the first study assessing the climate change impact on groundwater levels of the Zagreb alluvial aquifer in Croatia by coupling climate projections under RCP8.5 for the period 2040– 2070 with local scale groundwater flow modelli
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d3cf3ea5b15de50c1f97a11184b5e902
https://doi.org/10.1016/j.jhydrol.2022.128433
https://doi.org/10.1016/j.jhydrol.2022.128433