Ranko Biondić

Prof. Dr. Ranko Biondić

Faculty of Geotechnical Engineering, University of Zagreb
orcid

Research Focus & Metrics

Academic Career Length

29Years (1998-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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16 January 2022 in Water
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Journal Article
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Marko ŠrajbekMarko Šrajbek
Marko Šrajbek
LKLado Kranjčević
Lado Kranjčević
IKIvan Kovač
Ivan Kovač
Ranko BiondićRanko Biondić
Ranko Biondić
Nitrates are one of the most common groundwater contaminants and they come from different sources. The paper presents a study of groundwater quality at Varaždin wellfield in the north part of Croatia. The nitrate concentration at this location has been above the maximum allowed concentration for several decades, which has made the opening of new wellfields costly. Based on the previously developed groundwater flow model, a model that covers the narrow area of the wellfield is developed. The influential zone of the observed wellfield in working conditions is determined. Based on the developed model, the sources of nitrate pollution are located, which can be generally divided into non-point and point sources. Considering the time of groundwater retention in the horizontal flow, it is concluded that the water protection zones are marked following the applicable ordinance. Based on the developed groundwater flow model at the observed wellfield, a simulation of nitrate pollution propagation by advection and dispersion processes is performed. The simulation results point out the location of the poultry landfill as the largest source of nitrate pollution. However, poultry farms, which are located in the influence area of the wellfield, also contribute significantly to the nitrate concentration at the wellfield.

2 June 2010 in Geologia Croatica
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BBBožidar Biondić
Božidar Biondić
Ranko BiondićRanko Biondić
Ranko Biondić
HMHrvoje Meaški
Hrvoje Meaški
The conceptual hydrogeological model of the Plitvice Lakes

22 November 2019 in Hydrological Sciences Journal
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Journal Article
Closed access
Kreso PandzicKreso Pandzic
Kreso Pandzic
MKMira Kobold
Mira Kobold
Dijana OskorusDijana Oskorus
Dijana Oskorus
BBBožidar Biondić
Božidar Biondić
Ranko BiondićRanko Biondić
Ranko Biondić
OCOliver Curić
Oliver Curić
The study addresses homogeneity testing of annual discharge time series for eight hydrological stations and five annual climate time series for one weather station in the Kupa River Basin, between Slovenia and Croatia, and global annual average surface temperature time series for the period 1961–2010. The standard normal homogeneity test (SNHT) was used to detect both abrupt and gradual linear trend homogeneity breaks. The results reveal natural change points at the beginning of the 1980s. Absolute homogeneity testing of average annual weather station-level air pressure, annual precipitation, differences between precipitation totals and potential evapotranspiration and surface runoff from the independent observation time series confirmed an abrupt shift, also at the beginning of the 1980s. The trend of local air temperature for 1985–2000, which partly coincides with global surface temperature trend for 1974–2005, strengthened the river discharge regime shift since the beginning of the 1980s. These results could improve climate variation monitoring and estimation of the impact of climate variation on the environment in the area. Generally, an indication of climate regime change points and an assessment of their duration could provide significant benefits for the society.

29 June 1998 in Environmental Geology
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BBB. Biondić
B. Biondić
Ranko BiondićRanko Biondić
Ranko Biondić
FDF. Dukarić
F. Dukarić

25 February 2006 in Environmental Geology
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BBB. Biondić
B. Biondić
Ranko BiondićRanko Biondić
Ranko Biondić
SKS. Kapelj
S. Kapelj

17 March 2021 in Sustainability
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Ranko BiondićRanko Biondić
Ranko Biondić
HMHrvoje Measki
Hrvoje Measki
BBBožidar Biondić
Božidar Biondić
JLJelena Loborec
Jelena Loborec
Karst aquifers in the Dinaric karst are very rich with groundwater and are a very important resource for public water supply. The characteristics of the Dinaric karst are the lack, or very thin layer, of covering deposits, large amounts of precipitations, high groundwater velocities, very deep groundwater flow with a lot of faults and fault zones, pits to groundwater, concentrated sinking and large karst springs, making them extremely vulnerable to all anthropogenic influences, which are very quickly transmitted to the aquifer. Numerous multiparameter methods have been developed in the last 20 years to determine the level of vulnerability of aquifers. Each of them has its own specifics and is well adapted to the climate and region for which it was developed. The Karst Aquifer Vulnerability Assessment (KAVA) method was developed in accordance with all the characteristics of the deep karst aquifers of the Dinaric karst and tested on several basins in the area. It was developed as a part of the Global Environment Facility United Nations Environmental Programme – the Mediterranean Action Plan Strategic Partnership for the Mediterranean Sea Large Marine Ecosystem (GEF UNEP/MAP MedPartnership Project). This paper presents the KAVA method and its application to two characteristic karst basins of the Dinaric karst: the Novljanska Žrnovnica spring catchment area and the Bakar Bay catchment area.