Nové stopovací zkoušky v Moravském krasu I.: jeskynní systém Rudické propadání-Býčí skála
| Title in English | New tracer tests in the Moravian karst I.: the Rudické propadání-Býčí skála cave system |
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| Authors | |
| Year of publication | 2006 |
| Type | Article in Periodical |
| Magazine / Source | Geologické výzkumy na Moravě a ve Slezsku v roce 2005 |
| MU Faculty or unit | |
| 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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