| Naslov: | Groundwater Characterization by Means of Conservative (δ18O and δ2H) and Non-Conservative (87Sr/86Sr) Isotopic Values: The Classical Karst Region Aquifer Case (Italy–Slovenia) |
|---|
| Avtorji: | ID Calligaris, Chiara (Avtor)
ID Mezga, Kim (Avtor)
ID Slejko, Francesca Federica (Avtor)
ID Urbanc, Janko (Avtor)
ID Zini, Luca (Avtor) |
|---|
| Datoteke: |  PDF - Predstavitvena datoteka, prenos (4,83 MB)
MD5: FE10B67668698BB4CDFBC3AC29E280BC
 URL - Izvorni URL, za dostop obiščite http://dx.doi.org/10.3390/geosciences8090321
|
|---|
| Jezik: | Angleški jezik |
|---|
| Tipologija: | 1.01 - Izvirni znanstveni članek |
|---|
| Organizacija: |  ZAG - Zavod za gradbeništvo Slovenije
|
|---|
| Povzetek: | The study of the different hydrogeological compartments is a prerequisite for understanding and monitoring different fluxes, thereby evaluating the environmental changes in an ecosystem where anthropogenic disturbances are present in order to preserve the most vulnerable groundwaters from contamination and degradation. In many karst domains in the Mediterranean, areas groundwaters and surface waters are a single system, as a result of the features that facilitate the ingression of waters from surface to subsurface. This is also the case for the Classical Karst hydrostructure, which is a carbonate plateau that rises above the northern Adriatic Sea, shared between Italy and Slovenia. The main suppliers to the aquifer are the effective precipitations and the waters from three different rivers: Reka/Timavo, Soča/Isonzo and Vipava/Vipacco. Past and ongoing hydrogeological studies on the area have focused on the connections within the Classical Karst Region aquifer system through the analysis of water caves and springs hydrographs and chemographs. In this paper, the authors present new combined data from major ions, oxygen, hydrogen and strontium stable and radiogenic isotopes which have allowed a more complementary knowledge of the groundwater circulation, provenance and water-rock interactions. All the actions occurred in the framework of the European project HYDROKARST. |
|---|
| Ključne besede: | podzemna voda, kras, geokemija, izotopi, Hydrokarst projekt |
|---|
| Status publikacije: | Objavljeno |
|---|
| Verzija publikacije: | Objavljena publikacija |
|---|
| Datum objave: | 28.08.2018 |
|---|
| Založnik: | MDPI AG |
|---|
| Leto izida: | 2018 |
|---|
| Št. strani: | 25 str. |
|---|
| Številčenje: | vol. 8, iss. 9 |
|---|
| PID: | 20.500.12556/DiRROS-17508  |
|---|
| UDK: | 556.3 |
|---|
| ISSN pri članku: | 2076-3263 |
|---|
| DOI: | 10.3390/geosciences8090321 |
|---|
| COBISS.SI-ID: | 2833493 |
|---|
| Avtorske pravice: | © 2018 by the authors. Licensee MDPI, Basel, Switzerland. |
|---|
| Opomba: |
|
|---|
| Datum objave v DiRROS: | 12.12.2023 |
|---|
| Število ogledov: | 654 |
|---|
| Število prenosov: | 358 |
|---|
| Metapodatki: |    |
|---|
|
:
|
Kopiraj citat |
|---|
| | | | Objavi na: |  |
|---|
Postavite miškin kazalec na naslov za izpis povzetka. Klik na naslov izpiše
podrobnosti ali sproži prenos. |
