Probable reasons for interruption of the flow of the Iskrets karst spring-Reference-Cited by-同舟云学术

Probable reasons for interruption of the flow of the Iskrets karst spring

Published:2022-12 Issue:3 Volume:83 Page:243-246
ISSN:0007-3938
Container-title:Review of the Bulgarian Geological Society
language:en
Short-container-title:Rev. Bulg. Geol. Soc.

Author:

Benderev Aleksey,Damyanova Evelina,Ivanov Marin,Donkova Yordanka,Gerginov Peter

Abstract

The object of research is the Iskrets spring, one of the large and important karst springs in Bulgaria. A characteristic feature of its regime is the temporary interruptions of its outflow. The purpose of the research is to establish the probable causes and mechanism for these interruptions. After analyzing the hydrogeological situation and data from the results of continuous measurements of changes in water quantities, it is assumed that the main cause of this phenomenon is the processes of erosion, transport and deposition of cave alluvial sediments.

Publisher

Bulgarian Geological Society

Reference7 articles.

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2. Benderev, A., A. Sultanov. 1991. Recent sedimentary processes in the Dushnika cave (Iskrets karst basin). – Ann. Uni. Mining and. Geol., 1– Geol., 101–109 (ìn Bulgarian).

3. Bögli, A. 1980. Karst Hydrology and Physical Speleology. Berlin, Heidelberg, New York, Springer Verlag, 284 p.; https://doi.org/10.1007/978-3-642-67669-7.

4. Dinev, P. 1959. Attempt for determining of the water catchment of the Iskrets springs. – In: Karst Underground Waters in Bulgaria. Sofia, Tehnika, 162–182 (in Bulgarian).

5. Ford, D., P. Williams. 2007. Karst Hydrogeology and Geomorphology. Chichester, John Wiley & Sons, Ltd, 561 р.; https://doi.org/10.1002/9781118684986.

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