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dc.contributor.authorLenac, Danijela
dc.contributor.authorMance, Diana
dc.contributor.authorRadišić, Maja
dc.contributor.authorMance, Davor
dc.contributor.authorRubinić, Josip
dc.date.accessioned2023-05-01T13:46:30Z
dc.date.available2023-05-01T13:46:30Z
dc.date.issued2022
dc.identifierONIX_20230501_9791221500301_254
dc.identifier.urihttps://library.oapen.org/handle/20.500.12657/62838
dc.description.abstractComplexity of karst groundwater networks requires implementation of standard hydrogeological monitoring and unconventional methods of investigation. We present the results of isotope composition analysis for three karst springs and rain water collected in their hinterland. During two years, spring water samples were collected on a weekly and rain samples on a monthly basis. The main findings are: winter precipitation of Mediterranean origin dominates springs' recharge, a dual porosity model is a fit for the studied systems, and hinterlands of the springs have different retention capabilities.
dc.languageEnglish
dc.relation.ispartofseriesMonitoring of Mediterranean Coastal Areas: Problems and Measurement Techniques
dc.subject.classificationthema EDItEUR::R Earth Sciences, Geography, Environment, Planning::RN The environmenten_US
dc.subject.otherCoastal environmental physics
dc.subject.otherCoastal karstic aquifer
dc.subject.otherStable isotopes
dc.subject.otherStatistical modelling
dc.titleChapter The use of 2H and 18O isotopes in the study of coastal karstic aquifers
dc.typechapter
oapen.identifier.doi10.36253/979-12-215-0030-1.48
oapen.relation.isPublishedBybf65d21a-78e5-4ba2-983a-dbfa90962870
oapen.relation.isbn9791221500301
oapen.series.number1
oapen.pages10
oapen.place.publicationFlorence


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