中断伊斯克雷茨喀斯特泉流动的可能原因

IF 0.2 Q4 GEOSCIENCES, MULTIDISCIPLINARY

Spisanie Na B Lgarskoto Geologichesko Druzhestov-Review of the Bulgarian Geological Society Pub Date : 2022-12-01 DOI:10.52215/rev.bgs.2022.83.3.243

A. Benderev, E. Damyanova, M. Ivanov, Yordanka Donkova, P. Gerginov

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引用次数: 2

摘要

研究对象是伊斯克雷茨泉，它是保加利亚大型和重要的岩溶泉之一。其政权的一个特点是其外流的暂时中断。研究的目的是确定这些中断的可能原因和机制。在分析了水文地质情况和水量变化连续测量结果的数据后，认为这种现象的主要原因是洞穴冲积沉积物的侵蚀、运输和沉积过程。

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

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.

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Spisanie Na B Lgarskoto Geologichesko Druzhestov-Review of the Bulgarian Geological Society GEOSCIENCES, MULTIDISCIPLINARY-

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50.00%

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