A natron source at Pikrolimni Lake in Greece? Geochemical evidence (Articolo in rivista)

Type
Label
  • A natron source at Pikrolimni Lake in Greece? Geochemical evidence (Articolo in rivista) (literal)
Anno
  • 2009-01-01T00:00:00+01:00 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
  • 10.1016/j.gexplo.2009.08.003 (literal)
Alternative label
  • E. Dotsika; D. Poutoukis; I. Tzavidopoulos; Y. Maniatis; D. Ignatiadou; B. Raco (2009)
    A natron source at Pikrolimni Lake in Greece? Geochemical evidence
    in Journal of geochemical exploration
    (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#autori
  • E. Dotsika; D. Poutoukis; I. Tzavidopoulos; Y. Maniatis; D. Ignatiadou; B. Raco (literal)
Pagina inizio
  • 133 (literal)
Pagina fine
  • 143 (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#url
  • http://www.journals.elsevier.com/journal-of-geochemical-exploration/ (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#numeroVolume
  • 103 (literal)
Rivista
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#pagineTotali
  • 11 (literal)
Note
  • ISI Web of Science (WOS) (literal)
Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#affiliazioni
  • Lab. of Archaeometry, NCSR \"Demokritos\", 153 10 Aghia Paraskevi, Attiki, Greece General Secretariat for Research and Technology, 10-14 Messogion, Athens, Greece Archaeological Museum of Thessaloniki, 6 M. Andronikou Street, Thessaloniki, Greece Institute of Geosciences and Earth Resources, Via G. Moruzzi 1, 56124 Pisa, Italy (literal)
Titolo
  • A natron source at Pikrolimni Lake in Greece? Geochemical evidence (literal)
Abstract
  • The geochemical conditions that are responsible for the formation of \"Chalastraion nitron\" in the basin of Lake Pikrolimni (Northern Greece) were investigated in this study. The goal of the study is to confirm Pliny's description: \"at Clitae in Macedonia it is found in abundance the best, called soda of Chalestra...\" The ionspecific interaction model based on Pitzer's equations showed that the lake brine samples are saturated versus carbonate-bicarbonate sodium and sodium-chloride-sulfate minerals. The results of individual XRay Diffraction (XRD) analyses on the evaporative deposits showed that the salts consist mostly of trona, burkeite, thenardite and halite confirming Pliny's description. (literal)
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