2017
DOI: 10.1007/s12665-017-7057-z
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Spatial and temporal hydrochemistry variations of karst water in Gunung Sewu, Java, Indonesia

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Cited by 29 publications
(13 citation statements)
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“…The classification of groundwater as unpolluted water indicates that the source of water flowing into Pindul Cave, especially the Kedung Buntung allogenic river, is included in a good quality water source. Groundwater sources classified as Unpolluted Groundwater and Calcium Enrichment are also found in other karst water sources in the Gunungsewu Karst Area in Gunungkidul Regency and the Jonggrangan Karst Area in Kulonprogo Regency, Special Region of Yogyakarta [26] [28]. The rectangular Piper diagram of Pindul Cave Underground River supports the results of hydrochemical characteristics of the previous discussion (Figure 5).…”
Section: Resultssupporting
confidence: 84%
“…The classification of groundwater as unpolluted water indicates that the source of water flowing into Pindul Cave, especially the Kedung Buntung allogenic river, is included in a good quality water source. Groundwater sources classified as Unpolluted Groundwater and Calcium Enrichment are also found in other karst water sources in the Gunungsewu Karst Area in Gunungkidul Regency and the Jonggrangan Karst Area in Kulonprogo Regency, Special Region of Yogyakarta [26] [28]. The rectangular Piper diagram of Pindul Cave Underground River supports the results of hydrochemical characteristics of the previous discussion (Figure 5).…”
Section: Resultssupporting
confidence: 84%
“…In addition to those mentioned above, another method of identifying karst aquifer characteristics is to analyse the karst spring's response to the recharge (precipitation or concentrated infiltration) that flows via the ponors into the aquifer system. This method is possible because the spring, as an outlet of the karst system, is a feature that encompasses the majority of karst aquifer characteristics and processes (Bonacci 1993;White 2003;Adji & Misqi 2009;Adji 2012;Adji et al 2017). The karst aquifer response is the spring's discharge, while the recharge is the precipitation or concentrated infiltration via the ponors.…”
Section: Introductionmentioning
confidence: 99%
“…The impact of physical conditions that are geologically located on the geological structure of Karst, resulted in the geomorphological condition of the research area in the form of hilly and undulating land. Karst areas are characterized by drought in the dry season [30]. This happens because the structure above the rock causes rainwater to not be accommodated on the surface for a long time.…”
Section: Topography and Geomorphologymentioning
confidence: 99%