Nové stopovací zkoušky v Moravském krasu I.: jeskynní systém Rudické propadání-Býčí skála

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Title in English New tracer tests in the Moravian karst I.: the Rudické propadání-Býčí skála cave system
Authors

KNÍŽEK Martin VOJTĚCHOVSKÁ Anna BRUTHANS Jiří VYSOKÁ Helena

Year of publication 2006
Type Article in Periodical
Magazine / Source Geologické výzkumy na Moravě a ve Slezsku v roce 2005
MU Faculty or unit

Faculty of Science

Citation
Field Geology and mineralogy
Keywords Moravian karst; Rudické propadání-Býčí skála cave system; tracer tests; karst hydrology
Description Five tracer tests were performed with uranine dye, chloride and iodide in the central part of the Moravian Karst (the Rudické propadání – Býčí skála cave system). Present results agree well with results of tracer test performed in 1953 by Dr. Burkhardt and they presented results well agree with previous works. Volume of whole conduit was 7000 m3. The Jedovnický brook resurgence consist of 4 spings situated in distance of several tens of meters. The study shows, that spings are fed by single conduit with no inflows after splitting the main conduit to individual springs (the same breakthrough curve detected on all springs). The only exception is spring No. III., which shows some delay in tracer arrival and peak concentration. This can be explained by large volume of conduit feeding this spring (some 140 m3) compare to other conduits.
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