2018
DOI: 10.1088/1755-1315/212/1/012007
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Conservation of groundwater in Nglanggeran Area, Gunung Kidul District, Yogyakarta

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Cited by 6 publications
(11 citation statements)
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“…The research method used is field observation, consisting of geological and hydrogeological observations. These observations include the location of spring emergence, lithology and morphology descriptions, and spring discharge measurements [12,13]. Secondary data collection is carried out first, which is the initial data, and becomes a reference in field observation and for mapping geological and hydrogeological conditions.…”
Section: Methodsmentioning
confidence: 99%
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“…The research method used is field observation, consisting of geological and hydrogeological observations. These observations include the location of spring emergence, lithology and morphology descriptions, and spring discharge measurements [12,13]. Secondary data collection is carried out first, which is the initial data, and becomes a reference in field observation and for mapping geological and hydrogeological conditions.…”
Section: Methodsmentioning
confidence: 99%
“…Basically, due to its compact rock, limestone is impermeable. However, the existence of fractures or dissolution holes within it allows limestone to act as a good aquifer [12]. In general, these springs occur from fractures or from dissolution holes of rocks and due to contact with rocks that have much lower permeability, such as claystone, and then these springs are suspected as contact springs.…”
Section: The Springs Occurrencementioning
confidence: 99%
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“…Kemudian untuk profil hidrogeologi yang didasarkan pada jenis litologi daerah bersumber dari analisis oleh Balai Wilayah Sungai (BWS) [10]. Ketersediaan air tanah sebagai cadangan air bersih dipengaruhi oleh kondisi geologi dan hidrogeologi wilayah setempat [11].…”
Section: Analisis Kondisi Daerahunclassified
“…Batuan Gunungapi Tengger (Qyt) terdiri dari tuf pasiran, tuf batuapung, tuf abu, aglomerat, sedangkan Tuf Malang (Qytm) terdiri dari tuf batuapung, tuf pasiran, tuf breksi, tuf halus, serta tuf lapili. Setting geologi Desa Jabung menyebabkan perbedaan potensi air tanah (Prastistho et al, 2018) di beberapa dusun, sehingga ada dusun-dusun yang memiliki potensi air tanah yang baik dan ada dusun-dusun yang mengalami kekeringan akibat potensi air tanah yang kurang baik.…”
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