E3S Web Conf.
Volume 98, 201916th International Symposium on Water-Rock Interaction (WRI-16) and 13th International Symposium on Applied Isotope Geochemistry (1st IAGC International Conference)
|Number of page(s)||5|
|Section||Water-Rock Interaction Controlling Water Quality and Human Health Issues|
|Published online||07 June 2019|
The Khaung Daing hot spring (Inle lake, Southern Shan State, Myanmar): development opportunities and challenges
Dep. of Earth and Environmental Sciences, University of Pavia, 27100 Pavia, Italy
2 Geologist, Erlangen, Germany
3 Dep. of Earth and Environmental Sciences, University of Milano-Bicocca, Milan, Italy
4 Dep. of Physics, University of Mandalay, Myanmar
* Corresponding author: firstname.lastname@example.org
Located on the north-western border of the Inle lake basin, the Khaung Daing hot spring outflows at ca. 70°C. Temperature at depth, calculated with chemical geothermometers is probably less than 150°C, therefore classifying it as a medium-low enthalpy geothermal resource. Geochemical and isotopic results also demonstrate that the hot spring is fed by local groundwater, equilibrated with the carbonate rocks but without isotopic exchange with the matrix. Trace elements, particularly As (119 µg/L), display high concentrations, raising some concern about potential environmental and health effects.
© The Authors, published by EDP Sciences, 2019
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