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• W2279681832 abstract "Subsurface flow is one of the available water sources in the Karsts area such as in Gunung Kidul. The study of the pattern of the variations of stable isotopes content as a function of time and its interaction with other water sources such as rain waters, groundwater, river water will be a very good tool to assess the potential of the subsurface flow as a water source. For this purpose, the variations of stable isotopes content of subsurface flow around Gunung Kidul Karsts area and its interactions with other local water sources have been studied for the last two years. From the comparison of stable isotopes variations pattern of the subsurface flow with monthly rain water, the interaction of the subsurface flow with other water sources in the area has been quantified. Based on hydro-chemical data, it was found that the recharge area of subsurface flow were relatively further than other samples and it was also found that Seropan and Bribin subsurface flow systems originate from different geologic structures. Based on stable isotopes relative contents, it was found Ngobaran and Baron Caves have been mixed with domestic sewerage water or other surface water. Keywords : Karsts area, stable isotopes, subsurface flow ABSTRAK Interaksi Sungai Bawah Tanah Dengan Air Permukaan di Daerah Karst Gunung Kidul Menggunakan Variasi Data Hidrokimia dan Kandungan Isotop Stabil . Aliran sungai bawah tanah adalah salah satu sumber air yang tersedia di daerah Karst seperti halnya di daerah Gunung Kidul. Penelitian pola variasi kandungan isotop stabil sebagai fungsi waktu dan interaksinya dengan sumber air lainnya seperti air hujan, air tanah, dan sungai dapat digunakan sebagai alat untuk memperkirakan potensi aliran sungai bawah tanah dalam pengembangan selanjutnya. Untuk tujuan ini, pengamatan kandungan isotop stabil dan variasinya dan interaksinya dengan sumber air lainnya telah dilakukan pada dua tahun terakhir. Dari pola variasi kandungan isotop stabil aliran sungai bawah tanah dan perbandingan dengan pola variasi sumber air lainnya khususnya air hujan, besaran interaksi sungai bawah tanah dan sumber air lainnya telah dilakukan. Berdasarkan data kimia air, telah ditemukan bahwa daerah imbuh aliran bawah tanah adalah lebih jauh dari sumber air lainnya dan juga telah ditemukan bahwa air bawah tanah di Goa Seropan dan Bribin berasal dari struktur batuan yang berbeda. Berdasarkan data kelimpahan relatif isotope stabil, ditemukan bahwa aliran bawah tanah di Goa Ngobaran dan Baron telah mengalami percampuran dengan air buangan setempat atau air permukaan lainnya. Kata kunci : Daerah Karsts, isotop stabil, aliran sungai bawah tanah" @default.
• W2279681832 created "2016-06-24" @default.
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• W2279681832 date "2015-01-01" @default.
• W2279681832 modified "2023-09-23" @default.
• W2279681832 title "Subsurface Flow and Surface Water Interactions Quantification in Gunung Kidul Karst Area Using Hydro-Chemical and Stable Isotopes Data Variations" @default.
• W2279681832 hasPublicationYear "2015" @default.
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