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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

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