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                <full_title>Clay Minerals</full_title>
                <abbrev_title>Clay miner.</abbrev_title>
                <issn media_type="print">0009-8558</issn>
                <issn media_type="electronic">1471-8030</issn>
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                <publication_date media_type="print">
                  <month>12</month>
                  <year>2004</year>
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                <journal_volume>
                  <volume>39</volume>
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                <issue>4</issue>
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                <titles>
                  <title>Experimental study of swelling in unsaturated compacted clays</title>
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                  <person_name sequence="first" contributor_role="author">
                    <given_name>N.</given_name>
                    <surname>Saiyouri</surname>
                  </person_name>
                  <person_name sequence="additional" contributor_role="author">
                    <given_name>D.</given_name>
                    <surname>Tessier</surname>
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                  <person_name sequence="additional" contributor_role="author">
                    <given_name>P. Y.</given_name>
                    <surname>Hicher</surname>
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                  <jats:title>Abstract</jats:title>
                  <jats:p>This paper describes the swelling properties of two highly compacted clays, natural, untreated Wyoming montmorillonite (MX80) and Fourges smectite (FoCa7), saturated with Na and Ca, respectively.</jats:p>
                  <jats:p>The initially compacted samples were hydrated by subjecting them to different suction pressures in a range between 100 MPa and 1 kPa. For each equilibrium state, the volume change (swelling) and water content (hydration) were measured. The samples were then studied by X-ray diffraction using a transmission device to determine interlayer distance and particle size, in order to clarify both the swelling and hydration mechanisms. The distances between clay layers ranged between 10 and 21.6 Å , i.e. corresponding to between 0 and 4 water layers. Upon hydration, the particle size decreased from 350 and 100 clay layers per particle to 10 layers per particle when the suction pressure decreased from 100 MPa to 1 kPa for MX80 and FoCa7, respectively. The first swelling stage is described as being an insertion of water molecules between the layers. Then a division of the initial particles into particles of smaller size with increasingly large inter-particle distances was observed. Observations by transmission electronic microscopy confirmed these results.</jats:p>
                </jats:abstract>
                <publication_date media_type="online">
                  <month>07</month>
                  <day>09</day>
                  <year>2018</year>
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                <publication_date media_type="print">
                  <month>12</month>
                  <year>2004</year>
                </publication_date>
                <pages>
                  <first_page>469</first_page>
                  <last_page>479</last_page>
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                  <identifier id_type="pii">S0009855800001709</identifier>
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