Jökull


Jökull - 01.12.1987, Page 36

Jökull - 01.12.1987, Page 36
heat source is compatible with the many isolated occur- rences of thermal manifestations and the short lifetime of some of them, like Hverinn Eini (no. 23 in Fig. 1). At the end of the last century this was an extremely strong fumarole (Thoroddsen, 1925). Today it is almost extinct. GAS COMPOSITIONS The concentrations of C02 in the fumarole steam is most often in the range 200-300 mmoles/kg and this gas constitutes 80-90% of the total gas (Tables 1 and 2). The remainder is mostly H2S and H2 except in samples which are significantly air contaminated and contain, there- fore, rather high N2. CH4 is very low in most samples, less than 0.1 mmoles per kg of steam. H2S and H2 show much larger variation than C02 in both the eastern (Sveifluháls area) and the western (Vesturháls area) parts of the Krísuvík field. However, their concentra- tions are an order of magnitude lower around Trölla- dyngja in the latter area. Drillhole data indicate that the reservoir water around Trölladyngja is more saline (>1000 ppm Cl') than that under Sveifluháls (500 ppm Cl') (Arnórsson etal. 1975a). Arnórsson and Gunnlaugs- son (1985) showed that water above 200°C and with less than about 500 ppm Cl' equilibrates with the buffer epidote + pyrite + pyrrhotite whereas saltier waters equilibrate with epidote + pyrite + magnetite or chlo- rite, the latter mineral buffer fixing H2S and H2 at lower concentrations at any particular temperature. It seems likely that H2S and H2 in the reservoir under Trölla- dyngja, and probably also by Köldunámur, equilibrate with the mineral buffer including magnetite/chlorite whereas equilibrium with the pyrrhotite containing buff- er is attained in the south, under Sveifluháls and Hve- rinn Eini (Fig. 1). However, it cannot be excluded that reactions with atmospheric oxygen contribute signifi- cantly to the low H2 and H2S concentrations in the fumarole steam at Trölladyngja and Köldunámur due to the high permeability of the surface formations. In the Sveifluháls area the H2 concentrations in the steam are low relative to H2S when compared with other studied geothermal fields in Iceland with low chloride reservoir waters (Arnórsson and Gunnlaugsson, 1985). In gas samples from hot pools of steam heated water in the Sveifluháls area C02/H2S ratios are on the whole A o o z t STEAM HEATED POOLS -► CO^/H^S B co2/h2 Fig. 2. Distribution of C02/H2S and C02/H2 ratios in fumarole steam and in gas from hot pools of steam heated water in the Sveifluháls area. — Dreifing C02/H2S og C02IH2 hlutfalla í gufuaugum og í gasi í hverum með gufuhituðu vatni á Sveifluhálssvœðinu. 34
Page 1
Page 2
Page 3
Page 4
Page 5
Page 6
Page 7
Page 8
Page 9
Page 10
Page 11
Page 12
Page 13
Page 14
Page 15
Page 16
Page 17
Page 18
Page 19
Page 20
Page 21
Page 22
Page 23
Page 24
Page 25
Page 26
Page 27
Page 28
Page 29
Page 30
Page 31
Page 32
Page 33
Page 34
Page 35
Page 36
Page 37
Page 38
Page 39
Page 40
Page 41
Page 42
Page 43
Page 44
Page 45
Page 46
Page 47
Page 48
Page 49
Page 50
Page 51
Page 52
Page 53
Page 54
Page 55
Page 56
Page 57
Page 58
Page 59
Page 60
Page 61
Page 62
Page 63
Page 64
Page 65
Page 66
Page 67
Page 68
Page 69
Page 70
Page 71
Page 72
Page 73
Page 74
Page 75
Page 76
Page 77
Page 78
Page 79
Page 80
Page 81
Page 82
Page 83
Page 84
Page 85
Page 86
Page 87
Page 88
Page 89
Page 90
Page 91
Page 92
Page 93
Page 94
Page 95
Page 96
Page 97
Page 98
Page 99
Page 100
Page 101
Page 102
Page 103
Page 104
Page 105
Page 106
Page 107
Page 108
Page 109
Page 110
Page 111
Page 112
Page 113
Page 114
Page 115
Page 116

x

Jökull

Direct Links

If you want to link to this newspaper/magazine, please use these links:

Link to this newspaper/magazine: Jökull
https://timarit.is/publication/1155

Link to this issue:

Link to this page:

Link to this article:

Please do not link directly to images or PDFs on Timarit.is as such URLs may change without warning. Please use the URLs provided above for linking to the website.