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- W2038865080 abstract "A massive influx of gas was encountered in the Krafla geothermal system, Iceland, following the start of magmatic activity in the area in 1975. The gas was of magmatic origin, but its composition had been modified to predominantly carbon dioxide and a small amount of hydrogen sulphide. The gas concentrations of Krafla borehole fluids have been monitored since, and the pattern has been similar for wells in the affected Leirbotnar field, i.e. a maximum in 1977/1978, a secondary maximum in 1980 and a steady decline since. The more southerly Suđurhlíđar and Hvíthólar fields were not affected. Fumaroles were sampled extensively in 1978/1979 and 1984/1985. A similar decline was observed in the affected area, but a geographical trend that had been noticed for the borehole fluids was much clearer in this case. The decline is smallest in the northeastern part of the field, but more pronounced to the south and west. It is suggested that magmatic gas has not entered the geothermal system after 1980 and that the excess gas observed now comes from a supply located in the northeastern part of the field near the explosive crater, Víti." @default.
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- W2038865080 date "1989-09-01" @default.
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- W2038865080 title "Gas changes in the Krafla geothermal system, Iceland" @default.
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- W2038865080 doi "https://doi.org/10.1016/0009-2541(89)90089-2" @default.
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