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Influence of Carbonate-Flysch Contact and Groundwater Dynamics on the Occurrence of Geohazards in Istria, Croatia (CROSBI ID 294315)

Prilog u časopisu | izvorni znanstveni rad | međunarodna recenzija

Dugonjić Jovančević, Sanja ; Rubinić, Josip ; Ružić, Igor ; Radišić, Maja Influence of Carbonate-Flysch Contact and Groundwater Dynamics on the Occurrence of Geohazards in Istria, Croatia // Land (Basel), 10 (2021), 5; 441, 14. doi: 10.3390/land10050441

Podaci o odgovornosti

Dugonjić Jovančević, Sanja ; Rubinić, Josip ; Ružić, Igor ; Radišić, Maja

engleski

Influence of Carbonate-Flysch Contact and Groundwater Dynamics on the Occurrence of Geohazards in Istria, Croatia

This research focuses on the analysis of soil- water interaction at the carbonate-flysch contact on the Istrian peninsula in Croatia. As a result of the interaction of surface and groundwater and the position of flysch and carbonate rocks in the geotechnical profile, two problems occur in the study area: numerous instabilities and the occasionally high turbidity of drinking water. As an example, the St. Ivan spring was considered. The paper presents a complex mechanism of groundwater circulation in geological structures at carbonate-flysch contacts, differences in runoff through karst aquifers and flysch rocks during heavy rainfall under current and predicted (climate change) conditions, and the mentioned geohazards as a result of extreme precipitation. The analyses carried out showed the decisive influence of the existing geological structure on the dynamics of infiltration and precipitation runoff, as well as the risks of pronounced spring water turbidity and instability events. The main drivers of these geohazards are continuous long- term precipitation for landslides and intense daily precipitation for turbidity. Possible consequences of climate change are the increase in precipitation intensity, amount and higher variation, which subsequently brings risks such as the increase in maximum runoff, i.e., the expected more frequent occurrence of high turbidity and the more frequent occurrence of higher cumulative precipitation triggering instabilities in the area.

flysch ; karst ; groundwater dynamics ; turbidity ; landslides ; climate change ; Istria

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Podaci o izdanju

10 (5)

2021.

441

14

objavljeno

2073-445X

10.3390/land10050441

Trošak objave rada u otvorenom pristupu

Povezanost rada

Građevinarstvo

Poveznice
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