Monitoring the Flood Pulses in the Epiphreatic Zone of Karst Aquifers: The Case of Reka River System, Karst Plateau, SW Slovenia

Avtorji

  • Franci Gabrovšek Karst Research Institute, ZRC SAZU, Titov trg 2, SI-6230 Postojna
  • Borut Peric Park Škocjanske jame Public Agency , Škocjan 2, SI-6215 Divača

DOI:

https://doi.org/10.3986/ac.v35i1.241

Povzetek

The Reka river sinking into Škocjan caves (Škocjanske jame) is the main allogenic input into the aquifer of Classical Karst. So far the subsurface flow of the Reka river between Škocjan caves and the spring of Timava in Italy has been reached in five caves. Two were recently discovered in Slovenia. Continuous logging of water levels and temperatures in four of these caves was established in spring 2005. The paper presents and briefly discusses the first results obtained in three of them. The results are indicating a fast passage of a flood wave along a well developed conduit system.

Prenosi

Podatki o prenosih še niso na voljo.

Prenosi

Objavljeno

2006-06-01

Kako citirati

Gabrovšek, F., & Peric, B. (2006). Monitoring the Flood Pulses in the Epiphreatic Zone of Karst Aquifers: The Case of Reka River System, Karst Plateau, SW Slovenia. Acta Carsologica, 35(1). https://doi.org/10.3986/ac.v35i1.241

Številka

Letn. 35 Št. 1 (2006)

Rubrike

Original papers

Licenca

Avtorji jamčijo, da je delo njihova avtorska stvaritev, da v njem niso kršene avtorske pravice tretjih oseb ali kake druge pravice. V primeru zahtevkov tretjih oseb se avtorji zavezujejo, da bodo varovali interese založnika ter da bodo povrnili morebitno škodo.

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