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Hveravik, Iceland

Table 23.1. Chemical composition of water emanating from a hot sping at Gjogur, Hveravik, Iceland (Amorssonet al., 1983)... Table 23.1. Chemical composition of water emanating from a hot sping at Gjogur, Hveravik, Iceland (Amorssonet al., 1983)...
Fig. 23.6. Calculated saturation indices (log Q/K) of aluminum-bearing minerals plotted versus temperature for a hot spring water from Gjogur, Hveravik, Iceland. Lines for most of the minerals are not labeled, due to space limitations. Sampling temperature is 72 °C and predicted equilibrium temperature (arrow) is about 80 °C. Clinoptilolite (zeolite) minerals are the most supersaturated minerals below this temperature and saponite (smectite clay) minerals are the most supersaturated above it. Fig. 23.6. Calculated saturation indices (log Q/K) of aluminum-bearing minerals plotted versus temperature for a hot spring water from Gjogur, Hveravik, Iceland. Lines for most of the minerals are not labeled, due to space limitations. Sampling temperature is 72 °C and predicted equilibrium temperature (arrow) is about 80 °C. Clinoptilolite (zeolite) minerals are the most supersaturated minerals below this temperature and saponite (smectite clay) minerals are the most supersaturated above it.
See other pages where Hveravik, Iceland is mentioned: [Pg.347]    [Pg.347]    [Pg.347]    [Pg.349]    [Pg.252]    [Pg.252]    [Pg.347]    [Pg.347]    [Pg.347]    [Pg.349]    [Pg.252]    [Pg.252]   
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Hot spring at Hveravik, Iceland

Iceland

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