IJAER

International Journal of Agriculture and Environmental Research™

ISSN 2455-6939

Title:
ARSENIC IN GEOTHERMAL WATERS

Authors:
Abioye, O. FAYIGA and Uttam, K. SAHA

Abstract:
Geothermal waters are underground water with a temperature of at least 20 oC (Wiktorowicz, 2017). Geothermal energy is a form of renewable energy that makes use of heat emanating from geothermal waters to produce electricity and space heating of buildings such as greenhouses, spas and aquaculture (Baird and Cann, 2012). Deep groundwater with a temperature greater than 180 oC circulating within a geothermal zone and heated by contact with hot rocks is usually found in volcanic regions and island chains (Baird and Cann, 2012). Geothermal systems can either be volcanic or non-volcanic with volcanic based on the emplacement of magma (Meju, 2001). Volcanic geothermal systems include convective hydrothermal systems in hot dry rocks while non-volcanic geothermal systems involves hot fluids in sedimentary rocks flowing through fractures or faults (Meju, 2001). Volcanic rocks can be considered a heat source for geothermal waters (Yildirim and Ozgur, 2017).

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