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Chemical geothermometers for geothermal exploration

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Titill: Chemical geothermometers for geothermal explorationChemical geothermometers for geothermal exploration
Höfundur: Karingithi, Cyrus W. 1963 ; KenGen ; Jarðhitaskóli Háskóla Sameinuðu þjóðanna ; United Nations University ; United Nations University, Geothermal Training Programme
URI: http://hdl.handle.net/10802/23829
Útgefandi: United Nations University
Útgáfa: 2018
Ritröð: United Nations University., UNU Geothermal Training Programme, Iceland. Short Course ; SC-27
Efnisorð: Jarðhiti; Jarðhitaleit; Jarðefnafræði; Hitamælingar
ISSN: 1670-794x
Tungumál: Enska
Tengd vefsíðuslóð: https://orkustofnun.is/gogn/unu-gtp-sc/UNU-GTP-SC-27-0503.pdf
Tegund: Bók
Gegnir ID: 991011813249706886
Athugasemdir: Presented at SDG Short Course III on Exploration and Development of Geothermal Resources, organized by UNU-GTP and KenGen, at Lake Bogoria and Lake Naivasha, Kenya, Nov. 7-27, 2018.
Útdráttur: Chemical and isotope geothermometers constitute an important geochemical tool for the exploration and development of geothermal resources. They are also important during exploitation in monitoring the response of geothermal reservoirs to production load. During the exploration phase, geothermometry is used to estimate subsurface temperatures, i.e., temperatures expected to be encountered by drilling, using the chemical and isotopic composition of the hot spring and fumarole discharges. During the later phases in geothermal development and monitoring, geothermometry has been successfully applied to interpret the composition of well discharges with respect to locating the levels of producing horizons in the wells. Geothermometry is also useful in elucidating chemical reactions occurring in the zone of depressurization around wells that result from boiling and or cooling by recharging cold water.


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