Cristin-resultat-ID: 183878
Sist endret: 21. oktober 2013, 12:14
Resultat
Vitenskapelig foredrag
2003

Technology and raw materials for solar cell quality quartz

Bidragsytere:
  • Knut Lyng Sandvik og
  • Erik Larsen

Presentasjon

Navn på arrangementet: XXII International Mineral Processing Congress 2003
Sted: Cape Town, Sør-Afrika
Dato fra: 3. oktober 2003

Arrangør:

Arrangørnavn: [Mangler data]

Om resultatet

Vitenskapelig foredrag
Publiseringsår: 2003

Importkilder

Bibsys-ID: r04008566

Beskrivelse Beskrivelse

Tittel

Technology and raw materials for solar cell quality quartz

Sammendrag

Crystalline silicon solar cells are the most important solar cells manufactured today. This will most probably remain the situation the next decade. The future silicon feedstock is most likely not reject from the production of electronic-grade silicon. There will probably be a more direct solar-grade silicon route, excluding the electronic-grade silicon "detour". Estimated global solar energy demand in 2001 required approximately 5,500 tons of silicon feedstock. This required 65,000 tons of quartz. If the trend continues, the solar energy demand in 2010 would require approximately 30,000 tons of silicon feedstock and 350,000 tons of quartz, although the need for quartz probably will be lower than this. Quartzite has been regarded as the most suitable primary raw material used in the silicon solar cell production chain. This may change as the raw material requirements for the production of metallurgical-grade silicon are most likely to change. In addition, quartz or other silica-containing minerals from other rocks may be of a higher purity or contain lesser amounts of the most harmful elements. This favours increased beneficiation of primary raw materials in the future solar silicon feedstock production chain.

Bidragsytere

Knut Lyng Sandvik

  • Tilknyttet:
    Forfatter
    ved Institutt for geovitenskap og petroleum ved Norges teknisk-naturvitenskapelige universitet

Erik Larsen

  • Tilknyttet:
    Forfatter
    ved Institutt for geovitenskap og petroleum ved Norges teknisk-naturvitenskapelige universitet
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