SwePub
Sök i LIBRIS databas

  Utökad sökning

id:"swepub:oai:DiVA.org:oru-58800"
 

Sökning: id:"swepub:oai:DiVA.org:oru-58800" > REE-Enriched Mn-Oxi...

REE-Enriched Mn-Oxide Precipitates in Water-Bearing Fractures in the Ytterby Mine, Sweden

Sjöberg, Susanne (författare)
Dept of Geological Sciences, Stockholm University, Stockholm, Sweden
Allard, Bert, 1945- (författare)
Örebro universitet,Institutionen för naturvetenskap och teknik,Man-Technology-Environment Research Centre
Rattray, Jayne E. (författare)
Dept of Geological Sciences, Stockholm University, Stockholm, Sweden
visa fler...
Sjöberg, Viktor, 1984- (författare)
Örebro universitet,Institutionen för naturvetenskap och teknik,Man-Technology-Environment Research Centre
Karlsson, Stefan, 1957- (författare)
Örebro universitet,Institutionen för naturvetenskap och teknik,Man-Technology-Environment Research Centre
visa färre...
 (creator_code:org_t)
Freiberg : TU Bergakademie Freiberg, Institute of Mining and Special Civil Engineering, 2016
2016
Engelska.
Ingår i: Mining Meets Water – Conflicts and Solutions. - Freiberg : TU Bergakademie Freiberg, Institute of Mining and Special Civil Engineering. - 9783860125335 ; , s. 346-352
  • Konferensbidrag (refereegranskat)
Abstract Ämnesord
Stäng  
  • The Ytterby mine, Sweden, is known for the discovery of eight elements, including yttrium and five of the rare earth elements (REE). The mine was in operation from 1750 to 1933 and was after closure used as a storage depot for fuel from the 1950s to 1995. A tunnel was opened in the 1950s through the bedrock into the mine to allow access to the storage depot. Recent water monitoring campaigns (20122015) in the mine revealed a black substance (denoted YBS) in some fractures opening into the tunnel. Analysis of the YBS (elemental analysis, phase analysis by XRD, SEM with energy dispersive X-ray spectrometry, IR-and EPR-spectroscopy, preferential leaching at pH 4) showed that the main mineral component of the YBS is the manganese oxide birnessite. Also minor quantities of other less well defined manganese oxides were found, as well as silicates (quartz grains, possibly feldspar grains) and calcite. Birnessite has typically the composition Mx(Mn3+, Mn(2)(4+))O(4)xAq, with M= Na, Ca and x= 0.5. The birnessite component in YBS had a Mn3+/Mn4+ ratio of 1.04/0.96 with M = 0.42 Ca + 0.03 (REE+Y), 0.03 Mg and 0.03 other metals. All of these metals were firmly associated with the structure, since no release was observed at pH 4, except for significant fractions of the total Na, Mg, Ca-contents. Thus, REE+Y correspond to 1% of the total YBS mass and up to 3% of the metal content in the birnessite phase. This corresponds to an REE enrichment factor of the order 106 (YBS-birnessite/ fracture water). Birnessite with a substantial fraction of REE in the lattice has not previously been reported. The formation of birnessite is a microbial process. Identification of the microorganisms present in the Ytterby system is in progress.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Miljövetenskap (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Environmental Sciences (hsv//eng)

Nyckelord

Mine water geochemistry
manganese oxide precipitation
birnessite
rare earth elements
Enviromental Science
Miljövetenskap

Publikations- och innehållstyp

ref (ämneskategori)
kon (ämneskategori)

Hitta via bibliotek

Till lärosätets databas

Sök utanför SwePub

Kungliga biblioteket hanterar dina personuppgifter i enlighet med EU:s dataskyddsförordning (2018), GDPR. Läs mer om hur det funkar här.
Så här hanterar KB dina uppgifter vid användning av denna tjänst.

 
pil uppåt Stäng

Kopiera och spara länken för att återkomma till aktuell vy