Analisis Tipe Fluida Manifestasi Panas Bumi Daerah Mata Air Panas Sungai Kepangian Desa Sawangan Kabupaten Minahasa Utara
Article Sidebar
Main Article Content
Abstract
Geothermal is a source of heat energy contained in hot water, rocks, water vapor as well as gases and minerals and others that cannot be genetically separated from a geothermal system. Geothermal energy is a renewable natural resource with high potential. The source of this energy comes from heating magma against water rocks together with elements contained in the earth's crust. North Sulawesi has the potential to become a geothermal development area, both directly and indirectly. The existence of hot springs shows that the research location in Sawangan Village has geothermal potential. This research aims to determine the fluid type and molecular functional groups of hot springs in Sawangan Village, North Minahasa Regency, North Sulawesi Province. Using geochemical methods using Cl-SO2-HCO3 and FTIR diagrams, it is known that the type of hot spring fluid in Sawangan Village is Bicarbonate (HCO3) and the molecular functional group is C=O, where the parent chain C binds HCO3 (Bicarbonate) which corresponds to fluid type results.
Article Details
This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License.
References
Buchori, L. (2004). Buku Ajar “Perpindahan Panas Bagian I”. Semarang: Jurusan Teknik Kimia Fakultas Teknik Universitas Diponegoro.
Dipippo, R. (2012). Geothermal Power Plants: principles, Applicatons, Case, Studies and Enviromental Impact – 3rd ed. Amsterdan, Belanda; ELSEVIER
Emianto, Y.B., & Aribowo, Y. (2011). Studi geokimia fluida panas bumi daerah prospek panas bumi Nglimut, G. Ungaran Kecamatan Limbangan, Kabupaten Limbangan Jawa Tengah. 32(3), 230-233
Hisan, G. K., Bernaldo, P. A., Jasaputra, L. D., & Arhananta, (2020). Hidrokimia Air Tanah manifestasi Gedongsongo Panas Bumi Ungaran, Semarang, Jawa Tengah, Indonesia. 2(1), 489-493.
Kamil, L., Okto, A., & Muliddin, (2020). Karakteristik fluida terservoir mata air panas daerah Buranga Kecamatan Bonegunu Kabupaten Buon Utara Provinsi Sulawesi Tenggara. Jurnal Geologi Terapan, 2(2).
Masriat, R., Haryanti, A.,D., & Hutabarat, J. (2021). Karakteristik air panas dan estimasi temperatur reservoir daerah Cisolok – Cisukarame, Kabupateen Sukabumi, Provinsi Jawa Barat. 5(1), 40-48.
Nidya, F., Suharno., Zarkasyi, A., & Sugianto, A. Analisis karakteristik panas bumi daerah outflow Gunung Arjung- Welirang Berdasarkan geologi, geokimia, dan geofisika (3G). Jurusan geofisika Universitas Lampung dan 2Pusat Sumber Daya Geologi Bandung.
Ratag, A. S. 92020). Analisis Tipe Fluida Berdasarkan Diagram Cl-SO4-HCO3 Desa Pinaesaan Kabupaten Minahasa Selatan. 3(2), 1-7.
Toar, R. J., & Wenas, D.,R., & Mandang, T. (2021). Penentuan Tipe Fluida dan Gugus Fungsi Manifestasi Panas Bumi kawah Tua Gunung Api Soputan. 2(1), 49-54.
Saptadji, N. M. (2001). Teknik Panas Bumi. Bandung: Institut Teknologi Bandung.
Suparno, S. (2009). Energi Bumi “A present from the heart of the earth” – edisi I. Departemen Fisika – FMIPA Universitas Indonesia.
Wantalangi, W., Paliling, R., N., & Polii, J. (2020). Analisa tipe fluida manifestasi panas bumi di Desa Kaleosan Kabupaten Minahasa Utara. Charm Sains. 1(3), 139-142.