Porosity and distribution of water in perlite from the island of Milos, Greece

dc.bibliographicCitation.firstPage598eng
dc.bibliographicCitation.journalTitleSpringerPluseng
dc.bibliographicCitation.volume3eng
dc.contributor.authorKaufhold, Stephan
dc.contributor.authorReese, Anke
dc.contributor.authorSchwiebacher, Werner
dc.contributor.authorDohrmann, Reiner
dc.contributor.authorGrathoff, Georg H.
dc.contributor.authorWarr, Laurence N.
dc.contributor.authorHalisch, Matthias
dc.contributor.authorMüller, Cornelia
dc.contributor.authorSchwarz-Schampera, Ulrich
dc.contributor.authorUfer, Kristian
dc.date.accessioned2022-03-24T13:18:24Z
dc.date.available2022-03-24T13:18:24Z
dc.date.issued2014
dc.description.abstractA perlite sample representative of an operating mine in Milos was investigated with respect to the type and spatial distribution of water. A set of different methods was used which finally provided a consistent view on the water at least in this perlite. Infrared spectroscopy showed the presence of different water species (molecular water and hydroxyl groups / strongly bound water). The presence of more than 0.5 mass% smectite, however, could be excluded considering the cation exchange capacity results. The dehydration measured by thermal analysis occurred over a wide range of temperatures hence confirming the infrared spectroscopical results. Both methods point to the existence of a continuous spectrum of water binding energies. The spatial distribution of water and/or pores was investigated using different methods (CT: computer tomography, FIB: scanning electron microscopy including focused ion beam technology, IRM: infrared microscopy). Computer tomography (CT) showed large macropores (20 – 100 μm) and additionally revealed a mottled microstructure of the silicate matrix with low density areas up to a few μm in diameter. Scanning electron microscopy (FIB) confirmed the presence of μm sized pores and IRM showed the filling of these pores with water. In summary, two types of pores were found. Airfilled 20 – 100 μm pores and μm-sized pores disseminated in the glass matrix containing at least some water. Porosity measurements indicate a total porosity of 26 Vol%, 11 Vol% corresponding to the μm-sized pores. It remains unsolved wether the water in the μm-sized pores entered after or throughout perlite formation. However, the pores are sealed and no indications of cracks were found which indicated a primary source of the water, i.e. water was probably entrapped by quenching of the lava. The water in these pores may be the main reason for the thermal expandability which results in the extraordinarily porous expanded perlite building materials.eng
dc.description.versionpublishedVersioneng
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/8363
dc.identifier.urihttps://doi.org/10.34657/7401
dc.language.isoengeng
dc.publisherBerlin : SpringerOpeneng
dc.relation.doihttps://doi.org/10.1186/2193-1801-3-598
dc.relation.essn2193-1801
dc.rights.licenseCC BY 4.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/eng
dc.subject.ddc600eng
dc.subject.otherCT-analysiseng
dc.subject.otherFIBeng
dc.subject.otherPerliteeng
dc.subject.otherPorosityeng
dc.subject.otherVolcanic glasseng
dc.subject.otherWater distributioneng
dc.titlePorosity and distribution of water in perlite from the island of Milos, Greeceeng
dc.typeArticleeng
dc.typeTexteng
tib.accessRightsopenAccesseng
wgl.contributorLIAGeng
wgl.subjectPhysikeng
wgl.typeZeitschriftenartikeleng
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