Distribution and Characterization of Thermal Springs in Northern Oman
This study was conducted in Northern Oman to assess the physical and chemical characteristics of 40 thermal springs distributed in Al Hajar Mountains in northern Oman. Physical measurements of water samples were carried out in two main seasons in Oman (winter and summer 2019). Studied springs were classified into three groups based on water temperature, four groups based on water pH values and two groups based on conductivity. Ten thermal alkaline springs that originated in Ophiolite (Samail Napp) were dominated by high pH (> 11), elevated concentration of Cl- and Na+ ions, relatively low temperature and discharge ratio. Other springs in the Hajar Super Group massif recorded high concentrations of Ca2+ and SO2-4 ions controlled by rock dominance, geochemistry processes, and mineralization. There was only one spring which has brackish water with very high conductivity (5500 µs/cm) and Total Dissolved Solids and it is not suitable for irrigation purposes because of the high abundance of Na+, Cl−, and Ca2+ ions.Procedia APA BibTeX Chicago EndNote Harvard JSON MLA RIS XML ISO 690 PDF Downloads 298
 Brugger, J., Long, N., McPhail, D. C., & Plimer, I. (2005). An active a magmatic hydrothermal system: The Paralana hot springs, Northern Flinders Ranges, South Australia. Chemical Geology, 222(1-2), 35-64.
 Roy, S., Kumar, B., Chowdhury, A., Singh, U. K., & Ray, S. (2018). Characterization of hydro-geochemical process and evaluation of water quality of seven geothermal springs, Bakreswar, India. Arabian Journal of Geosciences, 11(12), 314.
 McCleskey, R. B., Nordstrom, D. K., Susong, D. D., Ball, J. W., & Taylor, H. E. (2010). Source and fate of inorganic solutes in the Gibbon River, Yellowstone National Park, Wyoming, USA. II. Trace element chemistry. Journal of volcanology and geothermal research, 196(3-4), 139-155.
 Yamada, M., Shoji, J., Ohsawa, S., Mishima, T., Hata, M., Honda, H., & Taniguchi, M. (2017). Hot spring drainage impact on fish communities around temperate estuaries in southwestern Japan. Journal of Hydrology: Regional Studies, 11, 69-83.
 Chavagnac, V., Ceuleneer, G., Monnin, C., Lansac, B., Hoareau, G., & Boulart, C. (2013). Mineralogical assemblages forming at hyper alkaline warm springs hosted on ultramafic rocks: a case study of Oman and Ligurian Ophiolites. Geochemistry, Geophysics, Geosystems, 14(7), 2474-2495.
 Stanger, G. (1986). The hydrogeology of the Oman Mountains (Doctoral dissertation, The Open University).
 WHO, G. (2017). Guidelines for drinking-water quality. World Health Organization, 216, 303-4.
 Liao, Z. (2018). Thermal springs and geothermal energy in the Qinghai-Tibetan Plateau and the surroundings. Springer Singapore.
 Subtavewung, P. H., Raksaskulwong, M., & Tulyatid, J. (2005). The characteristic and classification of hot springs in Thailand. In Proceedings World Geothermal Congress. p. 7.
 Clements, W. H., Arnold, J. L., Koel, T. M., Daley, R., & Jean, C. (2011). Responses of benthic macroinvertebrate communities to natural geothermal discharges in Yellowstone National Park, USA. Aquatic ecology, 45(1), 137-149.
 Waring, G. A., & Blankenship, R. R. (1965). Thermal Springs of the United States and Other Countries: A Summary (Vol. 492): US Government Printing Office
 Schütz, F., Winterleitner, G., & Huenges, E. (2018). Geothermal exploration in a sedimentary basin: new continuous temperature data and physical rock properties from northern Oman. Geothermal Energy, 6(1), 5.
 Karimi, S., Samani, N., & Mohammadi, Z. (2019). Characterization of Semnan thermal springs using principal component analysis and geochemical inverse modeling. Arabian Journal of Geosciences, 12(24), 777.
 Sami, K. (1992). Recharge mechanisms and geochemical processes in a semi-arid sedimentary basin, Eastern Cape, South Africa. Journal of Hydrology, 139(1-4), 27-48.
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