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Types of scaling occurring by geothermal utilization in Iceland

Journal Article · · Geothermics; (USA)
 [1]
  1. Orkustofnun, Grensasvegur 9, Reykjavik (IE)
The low-temperature geothermal fields in Iceland are mostly used for space heating. Scaling problems have only occurred in a few cases during exploitation. The most severe cases are due to precipitation of calcium carbonate in brackish water and occur both in downhole pumps and surface installations. In plants heating fresh water scaling by magnesium silicate has occurred. In the high-temperature geothermal fields calcium carbonate precipitation in wells is not uncommon but occurs at shallow levels and is amended by reaming the wells at regular intervals. Silica scaling in waste water is a general problem in most of the fields, but is mostly avoided inside the plants and in the distribution piping. Aluminium-silicates have been troublesome where the high-temperature waters have been used directly for heating as they are precipitated at temperatures well above saturation with opaline silica at which point the onset of scaling was expected. From the brine in the Reykjanes field there have been encountered downhole scales of iron-magnesium-silicates, and metalsulfide with high contents of precious metals is precipitated at the wellhead of one of the wells, Rn-9. Iron-silicates were precipitated from the magnetic influenced geothermal fluid in the Krafla field and metallic sulfides and oxides were also present in the scales blocking the wells at that time.
OSTI ID:
5322943
Journal Information:
Geothermics; (USA), Journal Name: Geothermics; (USA) Vol. 18:1; ISSN GTMCA; ISSN 0375-6505
Country of Publication:
United States
Language:
English