2014
DOI: 10.1016/j.geothermics.2013.08.010
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Drilling of the well IDDP-1

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Cited by 32 publications
(10 citation statements)
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“…7b ) may also explain why the aureoles of shallow magma bodies serendipitously encountered by geothermal drilling 33 , 34 have very steep temperature gradients over short distances of a few tens of metres 35 , 36 . Drilling of these magmatic aureoles has been characterised by strong loss in drilling fluid circulation 37 ; the results here suggest that efficient cooling by injection of fluids at ~80 °C in a magmatic aureole at ca. 850 °C would have caused thermal jointing and a significant widening of fractures to allow drilling fluid circulation loss during drilling activity.…”
Section: Discussionmentioning
confidence: 62%
“…7b ) may also explain why the aureoles of shallow magma bodies serendipitously encountered by geothermal drilling 33 , 34 have very steep temperature gradients over short distances of a few tens of metres 35 , 36 . Drilling of these magmatic aureoles has been characterised by strong loss in drilling fluid circulation 37 ; the results here suggest that efficient cooling by injection of fluids at ~80 °C in a magmatic aureole at ca. 850 °C would have caused thermal jointing and a significant widening of fractures to allow drilling fluid circulation loss during drilling activity.…”
Section: Discussionmentioning
confidence: 62%
“…We know little of the internal and underground conditions at active volcanoes, other than the rough inferences that we make by observing and mapping extinct, ancient, eroded volcanoes or that we extract from geophysical, geochemical and petrologic information, which itself has large uncertainties. Our view of active underground magmatic systems, and their relationships with the surrounding rocks, is basically speculation, as we do not directly observe them (with the negligible exception of geothermal drilling at the Krafla caldera, in Iceland, that accidentally encountered magma, Pàlsson et al 2014; and of scientific drilling into the surficial Kilauea Iki lava lake, Heltz 1980Heltz , 1987. It may be discomforting, but it is not surprising that our attempts to predict the evolution of volcanic systems are destined to take the form of exceedingly uncertain approximations; and that our probabilistic forecasts are affected or dominated by substantial uncertainties.…”
Section: Rational Volcanic Hazard Forecastsmentioning
confidence: 79%
“…This generates additional net costs and in extreme cases compromises completion integrity, operational safety and the environment, thus increasing nonproductive time. Palsson et al 29 described a series of lost circulation events in the drilling of a geothermal well in the Krafla field in Iceland (designed to reach a depth of 4500 m). Over 60 L/s of mud losses occurred at a depth of 2043 m; this could not be stopped by the drilling team and the remedy was to replace the mud with water.…”
Section: Loss Circulationmentioning
confidence: 99%