Geothermal Fluid Equilibrium Modeling: Comparison of Wellhead Fluid Samples to Deep Samples in the Reykjanes System, Iceland
Single phase geothermal fluids sampled in 2007 from 1500m depth in Well RN-12 of the Reykjanes geothermal system in Iceland show large differences in dissolved copper, zinc and iron concentrations when compared with fluid sampled from the wellhead. Equilibrium modeling of the samples taken at depth...
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| Language: | en_US |
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University of Oregon
2014
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| Online Access: | http://hdl.handle.net/1794/17933 |