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Vapour/liquid fractionation of rare earths, Y3+, Na+, K+, NH4 +, Cl-, HCO3 -, SO4 2- and borate in fluids from the Piancastagnaio geothermal field, Italy

  • HelmholtzZentrum Dresden-Rossendorf
  • Ludwig-Maximilians-Universität München

Research output: Contribution to journalArticlepeer-review

18 Scopus citations

Abstract

Vapour/liquid fractionation of rare earth elements and yttrium (REY), Na+, K+, NH4 +, HCO3 -, SO4 2-, Cl- and borate in geothermal fluids from the Piancastagnaio geothermal field (Mt. Amiata geothermal area, Tuscany, central Italy) were evaluated based on the chemistry of collected liquids and condensed vapours. Apparent vapour-liquid partitioning factors (appDV/L) of REY vary from 0.3 to 0.01. These factors are much higher than those of Na (<0.001) and K (∼0.001). Volatile components are ion pairings such as NH4HCO3 o, NH4Clo, NaHCO3 o, CaSO4 o and REYO(HCO)3 o ⇔ REY(OH)CO3 o. In vapour, REY and NH4 + are negatively correlated. High and low appDV/L(REY) indicate variations of NH4 + concentrations in liquids. The results of this study are relevant to the understanding of element migration and deposition under hydrothermal boiling conditions.

Original languageEnglish
Pages (from-to)360-369
Number of pages10
JournalGeothermics
Volume38
Issue number4
DOIs
StatePublished - Dec 2009

Keywords

  • Element fractionation
  • Geothermal
  • Italy
  • Mt. Amiata
  • Rare earth elements
  • Scale formation
  • Vapour/liquid fractionation
  • Water/rock interaction

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