Evolution of the porewater chemistry in compacted bentonite

Arto Muurinen, Jarmo Lehikoinen

Research output: Chapter in Book/Report/Conference proceedingConference article in proceedingsScientificpeer-review

8 Citations (Scopus)

Abstract

The evolution of porewater chemistry in bentonite was studied in solution-bentonite interaction experiments under anaerobic conditions at room temperature. The parameters varied were the bentonite density, bentonite-to-water ratio (b/w), ionic strength of the solution, and the composition of bentonite. At the end of the experiment, the equilibrating solution and the porewater squeezed out of the bentonite samples were analysed. This paper presents the preliminary experimental results of these ongoing studies.

The evolution of porewater chemistry was determined by the dissolving components initially present in the bentonite together with the ions coming with water from the surroundings. Ion-exchange processes occured between the exchangeable cations of montmorillonite and the cations in the water. The obtained concentrations in the external solution and porewater strongly depended on the b/w used. The concentrations in the squeezed porewaters were clearly lower than in the external waters and decreased with increasing density during squeezing.
Original languageEnglish
Title of host publicationScientific Basis for Nuclear Waste Management XXI
EditorsIan McKinley, Charles McCombie
Place of PublicationWarrendale
PublisherMaterials Research Society
Pages415-422
DOIs
Publication statusPublished - 1998
MoE publication typeA4 Article in a conference publication
EventMRS Symposium: Scientific Basis for Nuclear Waste Management XXI - Davos, Switzerland
Duration: 23 Sept 19973 Oct 1997

Publication series

SeriesMaterials Research Society Symposia Proceedings
Volume506
ISSN0272-9172

Conference

ConferenceMRS Symposium: Scientific Basis for Nuclear Waste Management XXI
Country/TerritorySwitzerland
CityDavos
Period23/09/973/10/97

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