SwePub
Sök i LIBRIS databas

  Extended search

onr:"swepub:oai:DiVA.org:kth-293950"
 

Search: onr:"swepub:oai:DiVA.org:kth-293950" > How inorganic anion...

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist
  • El Jamal, GhadaKTH,Tillämpad fysikalisk kemi (author)

How inorganic anions in groundwater influence the mechanism of oxidativedissolution of nuclear fuels in geological repositories in case of barrier failure.

  • BookEnglish

Publisher, publication year, extent ...

  • printrdacarrier

Numbers

  • LIBRIS-ID:oai:DiVA.org:kth-293950
  • https://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-293950URI

Supplementary language notes

  • Language:English
  • Summary in:English

Part of subdatabase

Classification

  • Subject category:vet swepub-contenttype
  • Subject category:ovr swepub-publicationtype

Notes

  • QC 20210518
  • H2O2 has previously been shown to be the main oxidant responsible for driving the process of radiation-induced dissolution of spent nuclear fuel in geological repositories for spent nuclear fuel. As the groundwater composition will vary depending on geographical location as well as on the age of the repository (in relation to glacial cycles, etc.), it is important to elucidate the impact of different groundwater constituents. While several studies have addressed the impact of HCO3- and halide ions on the radiation chemistry of water in general and radiation-induced oxidative dissolution of spent nuclear fuel in particular, very few studies have addressed the impact of halide ions on the mechanism of the reaction between H2O2 and UO2. In this work, the impact of Cl-, Br- and ClO4- on the mechanism and kinetics of H2O2-induced oxidative dissolution of UO2-powder in aqueous suspensions with and without added HCO3- has been studied experimentally. The experiments show that for systems containing 10 mM HCO3- and an initial H2O2-concentration of 0.15 mM, the presence of 1 M Cl-, Br- or ClO4- does not influence the kinetics of the reaction. At higher initial H2O2-concentrations, the presence of 1 M Br- appears to increase the rate of H2O2 consumption as well as the rate of UO22+ release. In solutions without added HCO3-, the presence of 1 M Cl-, Br- or ClO4- has an impact on the overall kinetics of the process at all initial H2O2-concentrations. This is partly attributed to an ionic strength effect enhancing adsorption of UO22+ to UO2 and partly attributed to stabilization of soluble uranyl-peroxo complexes mainly by Cl- and Br-.

Subject headings and genre

Added entries (persons, corporate bodies, meetings, titles ...)

  • Li, JunyiKTH,Skolan för kemi, bioteknologi och hälsa (CBH)(Swepub:kth)PI000000 (author)
  • Jonsson, Mats,1967-KTH,Tillämpad fysikalisk kemi(Swepub:kth)u11mc94v (author)
  • KTHTillämpad fysikalisk kemi (creator_code:org_t)

Internet link

To the university's database

  • 1 of 1
  • Previous record
  • Next record
  •    To hitlist

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