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Title:Characteristics and reasons for the discharge interruption of the Iskrets karst spring (Western Balkans, Bulgaria)
Authors:ID Benderev, Aleksey (Author)
ID Damyanova, Evelina (Author)
ID Ivanov, Marin (Author)
ID Donkova, Yordanka (Author)
ID Gerginov, Peter (Author)
ID Karastanev, Doncho (Author)
ID Tchakalova, Boriana (Author)
Files:URL URL - Source URL, visit https://ojs.zrc-sazu.si/carsologica/article/view/13966
 
.pdf PDF - Presentation file, download (6,65 MB)
MD5: 6306E2690AFA303DC75ECB692316F825
 
Language:English
Typology:1.01 - Original Scientific Article
Organization:Logo ZRC SAZU - The Research Centre of the Slovenian Academy of Sciences and Arts
Abstract:The Iskrets spring is one of the most significant karst springs in Bulgaria. А specific feature of this spring are irregular and abrupt reductions of its discharge after some earthquakes as well as other reasons related to the recharge. This study aims to present a reasonable hypothesis for the reasons of the discharge interruptions. A main feature of the Iskrets karst system is the fact that it is dominated by unconfined water flow in the unsaturated zone with velocities varying in a wide range. This creates conditions for significant erosion, transport and redeposition of the fluvial cave sediments. As a result, in the zones where there is a sharp decrease in the water velocity, a considerable accumulation of sediments occurs which can even fill the entire section of the passage-way and leads to a temporary blocking of the spring discharge. It is supposed that an appropriate section where this happens is located near to the discharge point of the spring. Most likely the main reason for the cave deposit displacement is the soil liquefaction caused by the seismic impact. It has been found that the duration of the discharge interruption period is longer at low water flow rates.
Keywords:karst spring, regime, interruption of the flow, cave sediments
Publication status:Published
Publication version:Version of Record
Publication date:16.12.2025
Year of publishing:2025
Number of pages:str. 173-187
Numbering:letn. 54, št. 2-3
PID:20.500.12556/DiRROS-25117 New window
UDC:556.35:551.442:551.3.051(497.2
ISSN on article:0583-6050
DOI:10.3986/ac.v54i2.13966 New window
COBISS.SI-ID:263218691 New window
Publication date in DiRROS:10.01.2026
Views:45
Downloads:16
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Record is a part of a journal

Title:Acta carsologica = Krasoslovni zbornik
Shortened title:Acta carsol.
Publisher:Slovenska akademija znanosti in umetnosti
ISSN:0583-6050
COBISS.SI-ID:6427138 New window

Licences

License:CC BY 4.0, Creative Commons Attribution 4.0 International
Link:http://creativecommons.org/licenses/by/4.0/
Description:This is the standard Creative Commons license that gives others maximum freedom to do what they want with the work as long as they credit the author.

Secondary language

Language:Slovenian
Title:Značilnosti in vzroki za prekinitev pretoka kraškega izvira Iskrets (Zahodni Balkan, Bolgarija)
Abstract:Izvir Iskrets je eden najpomembnejših kraških izvirov v Bolgariji. Posebnost tega izvira so neenakomerna in nenadna zmanjšanja pretoka po nekaterih potresih, lahko pa tudi kot posledica razmer, povezanih z napajanjem. Namen te študije je postaviti razumno hipotezo o vzrokih za prekinitve pretoka. Glavna značilnost kraškega sistema Iskrets je, da v nenasičenem območju prevladuje tok vode s prosto gladino in velikim razponom hitrosti. To ustvarja pogoje za znatno erozijo, transport in ponovno odlaganje fluvialnih jamskih sedimentov. Posledično se na območjih, kjer pride do močnega zmanjšanja hitrosti vode, usedajo večje količine sedimenta, ki lahko zapolnijo celoten presek kraškega kanala in povzročijo začasno prekinitev pretoka izvira. Domnevamo, da se primeren odsek, kjer se to zgodi, nahaja v bližini izvira. Najverjetneje je glavni razlog za premik jamskih sedimentov utekočinjanje tal zaradi potresnega vpliva. Ugotovili smo, da je trajanje prekinitve pretoka daljše pri nizkih pretokih izvira.
Keywords:kraški izvir, režim, prekinitev toka, jamski sedimenti


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