SwePub
Sök i LIBRIS databas

  Extended search

WFRF:(Tullborg Eva Lena)
 

Search: WFRF:(Tullborg Eva Lena) > Natural uranium in ...

Natural uranium in Forsmark, Sweden : The solid phase

Krall, Lindsay (author)
The Swedish Nuclear Fuel and Waste Management Company (SKB), Sweden
Sandström, Björn (author)
Tullborg, Eva-Lena (author)
show more...
Evins, Lena Z. (author)
show less...
 (creator_code:org_t)
Elsevier BV, 2015
2015
English.
In: Applied Geochemistry. - : Elsevier BV. - 0883-2927 .- 1872-9134. ; 59, s. 178-188
  • Journal article (peer-reviewed)
Abstract Subject headings
Close  
  • U-bearing solid phases from Forsmark, Sweden, a proposed host for radioactive waste repositories, havebeen identified and characterized. Elevated dissolved U was found in some groundwater samples duringthe site investigations, prompting a need to study the local U geochemistry. Previous hydrochemical andwhole-rock geochemical studies indicated that U was derived from local pegmatites, and mobilized andre-deposited during several geological events. In this study, down-hole gamma logs guided sampling oflocal pegmatites, cataclasites, and fracture fillings. Back-scattered electron-imaging, petrographic microscopy,and electron microprobe analyses were used to find and analyze U phases in thin sections. Theresults show that the principal U sources at Forsmark include pegmatitic uraninite (PbO up to22 wt%) and metamict uranothorite. These primary minerals show variable degrees of alteration suchas enrichment in Ca and Al and/or replacement by secondary Ca–U(VI)-silicates, haiweeite and uranophane.The haiweeite contains up to 5 wt% Al2O3, a chemical signature reflecting early (Proterozoic)events of hydrothermal fluid migration. Coffinitized, secondary uraninite is found in association withFeAl-silicates or Palaeozoic sulfide/sulfate minerals, indicating remobilization-precipitation and/or a secondary,sedimentary source of U. It is inferred that U was oxidized during geologically early periods.Later, U(IV) phases formed in fractures open to fluid circulation during the Palaeozoic. This study establishesthe phases available as local U sources and/or sinks, and which will be considered in future isotopicand hydrochemical studies aimed to constrain the mechanisms and timing of water–U phase interaction.

Subject headings

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

Keyword

Geology
geologi

Publication and Content Type

ref (subject category)
art (subject category)

Find in a library

To the university's database

Find more in SwePub

By the author/editor
Krall, Lindsay
Sandström, Björn
Tullborg, Eva-Le ...
Evins, Lena Z.
About the subject
NATURAL SCIENCES
NATURAL SCIENCES
and Earth and Relate ...
and Geology
Articles in the publication
Applied Geochemi ...
By the university
Stockholm University

Search outside 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 Close

Copy and save the link in order to return to this view