geothermal development and research in iceland - Orkustofnun
geothermal development and research in iceland - Orkustofnun
geothermal development and research in iceland - Orkustofnun
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Fig. 7.<br />
Generation of electricity<br />
us<strong>in</strong>g <strong>geothermal</strong> energy<br />
1970 - 2008<br />
4.2 Electric Power<br />
Generation<br />
Generat<strong>in</strong>g electricity with <strong>geothermal</strong> energy<br />
has <strong>in</strong>creased significantly <strong>in</strong> recent years.<br />
As a result of a rapid expansion <strong>in</strong> Icel<strong>and</strong>’s<br />
energy <strong>in</strong>tensive <strong>in</strong>dustry, the dem<strong>and</strong> for<br />
electricity has <strong>in</strong>creased considerably. Fig.<br />
7 shows the <strong>development</strong> from 1970-2005,<br />
<strong>and</strong> planned production up until 2008. The<br />
<strong>in</strong>stalled capacity of <strong>geothermal</strong> generat<strong>in</strong>g<br />
plants now totals some 200 MW e<br />
. The total<br />
production <strong>in</strong> 2005 was 1,658 Gwh, which<br />
was 19.1% of the country’s total electricity<br />
production. Enlargements of the exist<strong>in</strong>g<br />
power plants <strong>and</strong> two new plants will<br />
<strong>in</strong>crease the <strong>in</strong>stalled capacity by 210 MW e<br />
<strong>in</strong> 2006, br<strong>in</strong>g<strong>in</strong>g the total capacity up to<br />
410 MW e<br />
.<br />
Oddur Sigurdsson<br />
4.2.1 The Krafla Power Plant<br />
The Krafla power plant <strong>in</strong> north Icel<strong>and</strong> has been operat<strong>in</strong>g s<strong>in</strong>ce 1977. Two 30 MW e<br />
double flash condens<strong>in</strong>g turb<strong>in</strong>e units were purchased when the plant started, but<br />
due to unexpected difficulties w<strong>in</strong>n<strong>in</strong>g steam for the plant, Krafla was run with only<br />
one <strong>in</strong>stalled turb<strong>in</strong>e for the first 20 years. The shortfall of steam was due to volcanic<br />
activity that <strong>in</strong>jected volcanic gases <strong>in</strong>to<br />
the most productive part of the <strong>geothermal</strong><br />
reservoir. This contam<strong>in</strong>ation caused operational<br />
problems <strong>in</strong> some of the production<br />
wells, mostly <strong>in</strong> the form of rapid scal<strong>in</strong>g<br />
of the complex iron silicates. It also caused<br />
wells to corrode. Repeated drill<strong>in</strong>g <strong>in</strong> the area<br />
has shown that now, some 20 years after the<br />
eruptions, the concentration of magmatic<br />
gases <strong>in</strong> the steam has decreased drastically<br />
<strong>and</strong> now the reservoir can yield steam without<br />
problems with scal<strong>in</strong>g or corrosion. The<br />
plant operated successfully with one turb<strong>in</strong>e<br />
<strong>in</strong> spite of n<strong>in</strong>e volcanic eruptions, the last<br />
one <strong>in</strong> September 1984. Initially the power<br />
generation was 8 MW e<br />
, but reached 30 MW e<br />
<strong>in</strong> 1982. The capacity of the Krafla power<br />
plant was exp<strong>and</strong>ed <strong>in</strong> 1997 from 30 to 60<br />
MW e<br />
, <strong>and</strong> preparations are underway to <strong>in</strong>crease<br />
the plant’s output by an additional Krafla Power plant<br />
40<br />
20