Tracing flow directions of the Pentung Allogenic River in Gunungsewu Karst Area, Gunungkidul, using artificial tracer test

Abstract Previous studies in the Gunungsewu Karst Area categorized the Pentung Allogenic River catchment that drains to the Sawah Ombo Pond as the upper part of the Bribin Karst Drainage Basin (KDB). However, more detailed results from natural isotope studies after 2010 have provided reasons to post...

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Bibliographic Details
Published inIOP conference series. Earth and environmental science Vol. 1098; no. 1; pp. 12048 - 12054
Main Authors Cahyadi, A, Adji, T N, Haryono, E, Widyastuti, M, Agniy, R F
Format Journal Article
LanguageEnglish
Published Bristol IOP Publishing 01.10.2022
Subjects
Drainage basins
Fluorescent dyes
Fluorescent indicators
Geology
Groundwater
Groundwater flow
Hydrogeology
Isotope studies
Karst
River catchments
Rivers
Underground caverns
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Summary:Abstract Previous studies in the Gunungsewu Karst Area categorized the Pentung Allogenic River catchment that drains to the Sawah Ombo Pond as the upper part of the Bribin Karst Drainage Basin (KDB). However, more detailed results from natural isotope studies after 2010 have provided reasons to postulate that the groundwater does not flow from the catchment to Bribin KDB. Therefore, the research aimed to trace the direction of Pentung’s groundwater flows in Gunungsewu’s karstic hydrogeological system. To achieve this, an artificial tracer test was used. There were two fluorescent dye injection namely uranine and tinopal. The results confirmed that the allogenic river’s catchment supplied groundwater to Beton KDB instead of Bribin KDB. While the artificial tracers were not detected in the water at Gilap Cave and Bribin Underground River, they appeared in Jomblangan Cave and Sriti Spring, parts of Beton KDB.
ISSN:1755-1307
1755-1315
DOI:10.1088/1755-1315/1098/1/012048