Study of Thermal Water Resources in Sri Lanka Using Time Domain Electromagnetics (TDEM)

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Abstract:

Thermal springs can be utilized as an environmental friendly source of renewable energy, as well as for other purposes. Time domain electromagnetic (TDEM) method is used as an accessory tool in geothermal exploration to investigate the local heterogeneities in geology. The study consists of two of the thermal springs in Sri Lanka, Wahawa and Mahaoya, both in the same crustal unit. Major structural discontinuities of the area vary between two peculiar fracture sets striking ENE and NW. Close relationships between these individual springs have been witnessed by their approximate major cation chemistries, which provoke the idea of geochemical provinces. Survey reveals the pathways of the heated water to the surface, at Wahawa, although the path is not clear at Mahaoya. Near surface resistivity diagrams can be used only to interpret the immediate depths of the springs. The expected structural relationships may be identified with a grid of TDEM soundings encompassing both the spring systems.

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Advanced Materials Research (Volumes 955-959)

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3198-3201

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June 2014

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© 2014 Trans Tech Publications Ltd. All Rights Reserved

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[1] Dissanayake, C. and H. Jayasena, Origin of geothermal systems of Sri Lanka. Geothermics, (1988). 17(4): pp.657-669.

DOI: 10.1016/0375-6505(88)90050-8

Google Scholar

[2] Hobbs, B.A., G.M. Fonseka, A.G. Jones, S.N. de Silva, N.D. Subasinghe, G. Dawes, N. Johnson, T. Cooray, D. Wijesundara, N. Suriyaarachchi, T. Nimalsiri, K.M. PremathIlake, D. Kiyan, and D. Khoza, Geothermal Energy Potential in Sri Lanka: A Preliminary Magnetotelluric Survey of Thermal Springs. Jour. Geol. Soc. Sri Lanka, (2013).

DOI: 10.4028/www.scientific.net/amr.955-959.3198

Google Scholar

[3] Cooray, P.G., An introduction to the geology of Sri Lanka (Ceylon). (1984): National Museums of Sri Lanka Publication.

DOI: 10.1017/s0016756800018148

Google Scholar

[4] Cooray, P.G., The precambrian of Sri Lanka: a historical review. Precambrian Research, (1994). 66(1–4): pp.3-18.

DOI: 10.1016/0301-9268(94)90041-8

Google Scholar

[5] Senaratne, A. and D. Chandima. Exploration of a potential geothermal resource at Wahawa Padiyatalwa area Sri Lanka. in Thirty-Sixth Workshop on Geothermal Reservoir Engineering. (2011). Stanford University.

Google Scholar

[6] Chandrajith, R., J.A.C. Barth, N.D. Subasinghe, D. Merten, and C.B. Dissanayake, Geochemical and isotope characterization of geothermal spring waters in Sri Lanka: Evidence for steeper than expected geothermal gradients. Journal of Hydrology, (2013).

DOI: 10.1016/j.jhydrol.2012.11.004

Google Scholar

[7] Árnason, K., Central loop transient electromagnetic soundings over a horizontally layered earth. (1989): Orkustofnun.

Google Scholar

[8] McNeill, J., Principles and application of time domain electromagnetic techniques for resistivity sounding. (1994): Geonics.

Google Scholar