CO2 emissions and heat flow through soil, fumaroles, and steam heated mud pools at the Reykjanes geothermal area, SW Iceland

Carbon dioxide emissions and heat flow through soil, steam vents and fractures, and steam heated mud pools were
determined in the Reykjanes geothermal area, SW Iceland. Soil diffuse degassing of CO2 was quantified by soil flux measurements
on a 600 m by 375 m rectangular grid using a portable closed chamber soil flux meter and the resulting data were
analyzed by both a graphical statistical method and sequential Gaussian simulations. The soil temperature was measured
in each node of the grid and used to evaluate the heat flow. The heat flow data were also analyzed by sequential Gaussian
simulations. Heat flow from steam vents and fractures was determined by quantifying the amount of steam emitted from
the vents by direct measurements of steam flow rate. The heat loss from the steam heated mud pools was determined by
quantifying the rate of heat loss from the pools by evaporation, convection, and radiation. The steam flow rate into the
pools was calculated from the observed heat loss from the pools, assuming that steam flow was the only mechanism of heat
transport into the pool. The CO2 emissions from the steam vents and mud pools were determined by multiplying the steam
flow rate from the respective sources by the representative CO2 concentration of steam in the Reykjanes area. The observed
rates of CO2 emissions through soil, steam vents, and steam heated mud pools amounted to 13.5 ± 1.7, 0.23 ± 0.05, and
0.13 ± 0.03 tons per day, respectively. The heat flow through soil, steam vents, and mud pools was 16.9 ± 1.4, 2.2 ± 0.4,
and 1.2 ± 0.1 MW, respectively. Heat loss from the geothermal reservoir, inferred from the CO2 emissions through the soil
amounts to 130 ± 16 MW of thermal energy. The discrepancy between the observed heat loss and the heat loss inferred
from the CO2 emissions is attributed to steam condensation in the subsurface due to interactions with cold ground water.
These results demonstrate that soil diffuse degassing can be a more reliable proxy for heat loss from geothermal systems
than soil temperatures. The soil diffuse degassing at Reykjanes appears to be strongly controlled by the local tectonics. The
observed diffuse degassing defines 3–5 elongated N–S trending zones (000–020 ). The orientation of the diffuse degassing
structures at Reykjanes is consistent with reported trends of right lateral strike slip faults in the area. The natural CO2
emissions from Reykjanes under the current low-production conditions are about 16% of the expected emissions from
a 100 MWe power plant, which has recently been commissioned at Reykjanes.

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