作者: Halldór Ármannsson
DOI: 10.1016/J.APGEOCHEM.2018.07.013
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摘要: Abstract The origin of CO2 in fluids from Icelandic high-temperature geothermal systems is predominantly magmatic. Emissions producing areas have risen with increased production. Abnormal rises been recorded due to magmatic activity and the onset boiling increase Natural flow through soil but a small extent via steam vents heated pools. natural varies considerably between areas, apparently formation carbonate deposits (mainly calcite) relatively cool liquid dominated aquifers at shallow depths, where these are present. concentration higher temperatures decreases temperature for instance very low (