Naslov
Karst springs

Autori
Bonacci, Ognjen

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, pp prezentacija, ostalo

Skup
11. International Training Course on the belt and road initiative and karst landscape

Mjesto i datum
Guilin, Kina, 21.09.2019. - 29.09.2019

Vrsta sudjelovanja
Pozvano predavanje

Vrsta recenzije
Nije recenziran

Ključne riječi
karst hydrology, spring

Sažetak
Spring is a points of natural, concentrated discharge of groundwater at a rate high enough to maintain flow on the surface. Generally springs are formed where water table intersects with the earth’s surface, or groundwater rises to the surface through rock faults, fractures or depressions. Karst spring represents special kind of different water outflows from the underground to the surface which occurs in karst terrains. It is a natural exit for the groundwater to the surface of lithosphere through the hydrological active fissures of the karst mass. They appear most frequently in the places of contact between the carbonate masses and the impermeable layers (e.g. flysch).

Izvorni jezik
Engleski

Znanstvena područja
Geofizika, Građevinarstvo

POVEZANOST RADA