Nové stopovací zkoušky v systému Rudické propadání - Býčí skála

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Title in English New tracer tests in the Rudické propadání-Býčí skála cave
Authors

VOJTĚCHOVSKÁ Anna KNÍŽEK Martin BRUTHANS Jiří VYSOKÁ Helena

Year of publication 2006
Type Article in Periodical
Magazine / Source Speleofórum 2006
MU Faculty or unit

Faculty of Science

Citation
Field Geology and mineralogy
Keywords Moravian karst; Rudické propadání-Býčí skála cave system; tracer test; karst hydrology
Description New tracer tests was performed with fluorescent, chloride and KI dye in the central part of the Moravian karst (cave system Rudické propadání – Býčí skála). The five tracer tests (see Fig. 1) was quantitative. The new results of carst aquifers well corne up to results of year 1953. The results are impressed with failed measuring of flow. Volume of aquifers cast of 7000 m3 (resungence siphons 2600 m3). Affluent is probably between Kaňony corridor and resungence 10-15 l/s into Jedovnický brook. This affluent is before seveřance of flow to four separate resungence. All resungence have almost identical excerpt of resungence III. This resungence have circa 1 hour delay, it matches biiger volume of aquifer (circa 140 m3). The best parameters shall we average afloat profile – recognize is possible freatic aquifers (Kaňony corridore – resungence 4 m2) from off aktive flow (inlet – Kaňony corridore 1,2 m2).
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