KARAKTERISTIK FISIK MATAAIR PANAS DAERAH SAMBOJA, KUTAI KARTANEGARA

Jamaluddin Jamaluddin, Iwan Prabowo, Maria Maria

Abstract


Geothermal features can be observed in areas of active volcanism, or areas that have inactive volcanoes. In non-volcanic areas, the temperature of rocks within the Earth also increases with depth. This temperature increase is known as the Geothermal Gradient. If water percolates deeply enough into the crust, it comes into contact with hot rocks and can circulate to the surface to form hot springs. The collection of field hydrothermal data during field study with the help of portable instruments. The different physical parameters of the thermal springs such as temperature, pH, colour, and odour of thermal fluid are noted. The temperature of the thermal springs ranges from 43oC to 48oC. The pH value of the thermal waters shows a neutral (pH 6-6.6) and sulphur odour is discernible particularly. Based on geological, the system geothermal energy that develops is geopressured.

Keywords


Geochemistry; Hotspring; Samboja; Physical property

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References


Asdak, Chay, 2004.Hidrologi dan Pengelolaan Daerah Aliran Sungai. Yogyakarta: Gajah Mada University Press

Badan Geologi, 2008.Potensi Energi Panas Bumi Indonesia.

Edwards, L.M., 1982. Handbook of Geothermal Energy. Gulf Publishing Company, Houston, United State.

Giggenbach, W.F., 1996. Chemical Composition of Volcanic Gases. Institute of Geological and Nuclear Sciences, New Zealand.

Hidayat dan Umar, 1994. Peta Geologi Lembar Balikpapan, skala 1 : 250.000, Kalimantan.

Hochstein, Manfred P and Patrick R.L. Browne., 2000.Surface Manifestations of Systems with Volcanic Heat Sources in Encyclopedia of Volcanoes. Academic Press.

Monroe, J.S., 2006.The Changing Earth, Exploring Geology and Evolution, Michigan University.

Nicholson, Keith., 1993.Geothermal Fluids: Chemistry & Exploration Techniques. Berlin: Springer Verlag, Inc.

Saptadji, Nenny Miryani, 2000. Panduan Teknik Panas Bumi. Bandung: Jurusan Teknik Geologi ITB.

Satyana, A.H., Nugroho, D., Surantoko, I., 1999. Tectonic controls on the hydrocarbon habitats of the Barito,Kutei, and Tarakan Basins, Eastern Kalimantan, Indonesia : major dissimilarities in adjoining basins. Journal of Asian Earth Sciences., Vol. 17, hal 111-121.

Supriatna, S., Sukardi, E. Rustandi, 1995. Buku Lampiran Peta Geologi Lembar Samarinda, Kalimantan. Bandung: Pusat Penelitian dan Pengembangan Geologi.




DOI: https://doi.org/10.58267/petrogas.v3i2.70

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