Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite
Abstract Concrete and bentonite are being considered as engineered barriers for the deep geological disposal of high-level radioactive waste in argillaceous rocks. Three hydrothermal laboratory experiments of different scalable complexity were performed to improve our knowledge of the formation of c...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Fernández, Raúl [verfasserIn] |
|---|
| Format: |
Artikel |
|---|
| Erschienen: |
2016 |
|---|
| Anmerkung: |
© 2016 by Walter de Gruyter Berlin/Boston |
|---|
| Übergeordnetes Werk: |
Enthalten in: Clay minerals - Mineralogical Society, 1965, 51(2016), 2 vom: 01. Mai, Seite 223-235 |
|---|---|
| Übergeordnetes Werk: |
volume:51 ; year:2016 ; number:2 ; day:01 ; month:05 ; pages:223-235 |
| Links: |
|---|
| DOI / URN: |
10.1180/claymin.2016.051.2.09 |
|---|
| Katalog-ID: |
OLC2138541126 |
|---|
| LEADER | 01000naa a22002652 4500 | ||
|---|---|---|---|
| 001 | OLC2138541126 | ||
| 003 | DE-627 | ||
| 005 | 20230810091309.0 | ||
| 007 | tu | ||
| 008 | 230810s2016 xx ||||| 00| ||und c | ||
| 024 | 7 | |a 10.1180/claymin.2016.051.2.09 |2 doi | |
| 035 | |a (DE-627)OLC2138541126 | ||
| 035 | |a (DE-B1597)claymin.2016.051.2.09-p | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 082 | 0 | 4 | |a 000 |a 550 |q VZ |
| 084 | |a 13 |2 ssgn | ||
| 100 | 1 | |a Fernández, Raúl |e verfasserin |4 aut | |
| 245 | 1 | 0 | |a Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite |
| 264 | 1 | |c 2016 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 500 | |a © 2016 by Walter de Gruyter Berlin/Boston | ||
| 520 | |a Abstract Concrete and bentonite are being considered as engineered barriers for the deep geological disposal of high-level radioactive waste in argillaceous rocks. Three hydrothermal laboratory experiments of different scalable complexity were performed to improve our knowledge of the formation of calcium aluminate silicate hydrates (C-A-S-H) at the interface between the two materials: concretebentonite transport columns, lime mortar-bentonite transport columns and a portlandite- (bentonite and montmorillonite) batch experiment. Precipitation of C-A-S-H was observed in all experiments. Acicular and fibrous morphologies with certain laminar characteristics were observed which had smaller Ca/Si and larger Al/Si ratios with increasing temperature and lack of accessory minerals. The compositional fields of these C-A-S-H phases formed in the experiments are consistent with Al/(Si+Al) ratios of 0.2- 0.3 described in the literature. The most representative calcium silicate hydrate (C-S-H) phase from the montmorillonite-cement interface is Al-tobermorite. Structural analyses revealed a potential intercalation or association of montmorillonite and C-A-S-H phases at the pore scale. | ||
| 700 | 1 | |a Ruiz, Isabel |4 aut | |
| 700 | 1 | |a Cuevas, Jaime |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Clay minerals |d Mineralogical Society, 1965 |g 51(2016), 2 vom: 01. Mai, Seite 223-235 |w (DE-627)130703907 |w (DE-600)961059-5 |w (DE-576)016252330 |x 0009-8558 |7 nnns |
| 773 | 1 | 8 | |g volume:51 |g year:2016 |g number:2 |g day:01 |g month:05 |g pages:223-235 |
| 856 | 4 | 1 | |u https://doi.org/10.1180/claymin.2016.051.2.09 |z lizenzpflichtig |3 Volltext |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-TEC | ||
| 912 | |a SSG-OLC-CHE | ||
| 912 | |a SSG-OLC-GEO | ||
| 912 | |a SSG-OLC-PHA | ||
| 912 | |a SSG-OPC-GGO | ||
| 912 | |a GBV_ILN_70 | ||
| 912 | |a GBV_ILN_2026 | ||
| 912 | |a GBV_ILN_4219 | ||
| 951 | |a AR | ||
| 952 | |d 51 |j 2016 |e 2 |b 01 |c 05 |h 223-235 | ||
| author_variant |
r f rf i r ir j c jc |
|---|---|
| matchkey_str |
article:00098558:2016----::omtoocspaefoteneatobtenocee |
| hierarchy_sort_str |
2016 |
| publishDate |
2016 |
| allfields |
10.1180/claymin.2016.051.2.09 doi (DE-627)OLC2138541126 (DE-B1597)claymin.2016.051.2.09-p DE-627 ger DE-627 rakwb 000 550 VZ 13 ssgn Fernández, Raúl verfasserin aut Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © 2016 by Walter de Gruyter Berlin/Boston Abstract Concrete and bentonite are being considered as engineered barriers for the deep geological disposal of high-level radioactive waste in argillaceous rocks. Three hydrothermal laboratory experiments of different scalable complexity were performed to improve our knowledge of the formation of calcium aluminate silicate hydrates (C-A-S-H) at the interface between the two materials: concretebentonite transport columns, lime mortar-bentonite transport columns and a portlandite- (bentonite and montmorillonite) batch experiment. Precipitation of C-A-S-H was observed in all experiments. Acicular and fibrous morphologies with certain laminar characteristics were observed which had smaller Ca/Si and larger Al/Si ratios with increasing temperature and lack of accessory minerals. The compositional fields of these C-A-S-H phases formed in the experiments are consistent with Al/(Si+Al) ratios of 0.2- 0.3 described in the literature. The most representative calcium silicate hydrate (C-S-H) phase from the montmorillonite-cement interface is Al-tobermorite. Structural analyses revealed a potential intercalation or association of montmorillonite and C-A-S-H phases at the pore scale. Ruiz, Isabel aut Cuevas, Jaime aut Enthalten in Clay minerals Mineralogical Society, 1965 51(2016), 2 vom: 01. Mai, Seite 223-235 (DE-627)130703907 (DE-600)961059-5 (DE-576)016252330 0009-8558 nnns volume:51 year:2016 number:2 day:01 month:05 pages:223-235 https://doi.org/10.1180/claymin.2016.051.2.09 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_70 GBV_ILN_2026 GBV_ILN_4219 AR 51 2016 2 01 05 223-235 |
| spelling |
10.1180/claymin.2016.051.2.09 doi (DE-627)OLC2138541126 (DE-B1597)claymin.2016.051.2.09-p DE-627 ger DE-627 rakwb 000 550 VZ 13 ssgn Fernández, Raúl verfasserin aut Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © 2016 by Walter de Gruyter Berlin/Boston Abstract Concrete and bentonite are being considered as engineered barriers for the deep geological disposal of high-level radioactive waste in argillaceous rocks. Three hydrothermal laboratory experiments of different scalable complexity were performed to improve our knowledge of the formation of calcium aluminate silicate hydrates (C-A-S-H) at the interface between the two materials: concretebentonite transport columns, lime mortar-bentonite transport columns and a portlandite- (bentonite and montmorillonite) batch experiment. Precipitation of C-A-S-H was observed in all experiments. Acicular and fibrous morphologies with certain laminar characteristics were observed which had smaller Ca/Si and larger Al/Si ratios with increasing temperature and lack of accessory minerals. The compositional fields of these C-A-S-H phases formed in the experiments are consistent with Al/(Si+Al) ratios of 0.2- 0.3 described in the literature. The most representative calcium silicate hydrate (C-S-H) phase from the montmorillonite-cement interface is Al-tobermorite. Structural analyses revealed a potential intercalation or association of montmorillonite and C-A-S-H phases at the pore scale. Ruiz, Isabel aut Cuevas, Jaime aut Enthalten in Clay minerals Mineralogical Society, 1965 51(2016), 2 vom: 01. Mai, Seite 223-235 (DE-627)130703907 (DE-600)961059-5 (DE-576)016252330 0009-8558 nnns volume:51 year:2016 number:2 day:01 month:05 pages:223-235 https://doi.org/10.1180/claymin.2016.051.2.09 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_70 GBV_ILN_2026 GBV_ILN_4219 AR 51 2016 2 01 05 223-235 |
| allfields_unstemmed |
10.1180/claymin.2016.051.2.09 doi (DE-627)OLC2138541126 (DE-B1597)claymin.2016.051.2.09-p DE-627 ger DE-627 rakwb 000 550 VZ 13 ssgn Fernández, Raúl verfasserin aut Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © 2016 by Walter de Gruyter Berlin/Boston Abstract Concrete and bentonite are being considered as engineered barriers for the deep geological disposal of high-level radioactive waste in argillaceous rocks. Three hydrothermal laboratory experiments of different scalable complexity were performed to improve our knowledge of the formation of calcium aluminate silicate hydrates (C-A-S-H) at the interface between the two materials: concretebentonite transport columns, lime mortar-bentonite transport columns and a portlandite- (bentonite and montmorillonite) batch experiment. Precipitation of C-A-S-H was observed in all experiments. Acicular and fibrous morphologies with certain laminar characteristics were observed which had smaller Ca/Si and larger Al/Si ratios with increasing temperature and lack of accessory minerals. The compositional fields of these C-A-S-H phases formed in the experiments are consistent with Al/(Si+Al) ratios of 0.2- 0.3 described in the literature. The most representative calcium silicate hydrate (C-S-H) phase from the montmorillonite-cement interface is Al-tobermorite. Structural analyses revealed a potential intercalation or association of montmorillonite and C-A-S-H phases at the pore scale. Ruiz, Isabel aut Cuevas, Jaime aut Enthalten in Clay minerals Mineralogical Society, 1965 51(2016), 2 vom: 01. Mai, Seite 223-235 (DE-627)130703907 (DE-600)961059-5 (DE-576)016252330 0009-8558 nnns volume:51 year:2016 number:2 day:01 month:05 pages:223-235 https://doi.org/10.1180/claymin.2016.051.2.09 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_70 GBV_ILN_2026 GBV_ILN_4219 AR 51 2016 2 01 05 223-235 |
| allfieldsGer |
10.1180/claymin.2016.051.2.09 doi (DE-627)OLC2138541126 (DE-B1597)claymin.2016.051.2.09-p DE-627 ger DE-627 rakwb 000 550 VZ 13 ssgn Fernández, Raúl verfasserin aut Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © 2016 by Walter de Gruyter Berlin/Boston Abstract Concrete and bentonite are being considered as engineered barriers for the deep geological disposal of high-level radioactive waste in argillaceous rocks. Three hydrothermal laboratory experiments of different scalable complexity were performed to improve our knowledge of the formation of calcium aluminate silicate hydrates (C-A-S-H) at the interface between the two materials: concretebentonite transport columns, lime mortar-bentonite transport columns and a portlandite- (bentonite and montmorillonite) batch experiment. Precipitation of C-A-S-H was observed in all experiments. Acicular and fibrous morphologies with certain laminar characteristics were observed which had smaller Ca/Si and larger Al/Si ratios with increasing temperature and lack of accessory minerals. The compositional fields of these C-A-S-H phases formed in the experiments are consistent with Al/(Si+Al) ratios of 0.2- 0.3 described in the literature. The most representative calcium silicate hydrate (C-S-H) phase from the montmorillonite-cement interface is Al-tobermorite. Structural analyses revealed a potential intercalation or association of montmorillonite and C-A-S-H phases at the pore scale. Ruiz, Isabel aut Cuevas, Jaime aut Enthalten in Clay minerals Mineralogical Society, 1965 51(2016), 2 vom: 01. Mai, Seite 223-235 (DE-627)130703907 (DE-600)961059-5 (DE-576)016252330 0009-8558 nnns volume:51 year:2016 number:2 day:01 month:05 pages:223-235 https://doi.org/10.1180/claymin.2016.051.2.09 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_70 GBV_ILN_2026 GBV_ILN_4219 AR 51 2016 2 01 05 223-235 |
| allfieldsSound |
10.1180/claymin.2016.051.2.09 doi (DE-627)OLC2138541126 (DE-B1597)claymin.2016.051.2.09-p DE-627 ger DE-627 rakwb 000 550 VZ 13 ssgn Fernández, Raúl verfasserin aut Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite 2016 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © 2016 by Walter de Gruyter Berlin/Boston Abstract Concrete and bentonite are being considered as engineered barriers for the deep geological disposal of high-level radioactive waste in argillaceous rocks. Three hydrothermal laboratory experiments of different scalable complexity were performed to improve our knowledge of the formation of calcium aluminate silicate hydrates (C-A-S-H) at the interface between the two materials: concretebentonite transport columns, lime mortar-bentonite transport columns and a portlandite- (bentonite and montmorillonite) batch experiment. Precipitation of C-A-S-H was observed in all experiments. Acicular and fibrous morphologies with certain laminar characteristics were observed which had smaller Ca/Si and larger Al/Si ratios with increasing temperature and lack of accessory minerals. The compositional fields of these C-A-S-H phases formed in the experiments are consistent with Al/(Si+Al) ratios of 0.2- 0.3 described in the literature. The most representative calcium silicate hydrate (C-S-H) phase from the montmorillonite-cement interface is Al-tobermorite. Structural analyses revealed a potential intercalation or association of montmorillonite and C-A-S-H phases at the pore scale. Ruiz, Isabel aut Cuevas, Jaime aut Enthalten in Clay minerals Mineralogical Society, 1965 51(2016), 2 vom: 01. Mai, Seite 223-235 (DE-627)130703907 (DE-600)961059-5 (DE-576)016252330 0009-8558 nnns volume:51 year:2016 number:2 day:01 month:05 pages:223-235 https://doi.org/10.1180/claymin.2016.051.2.09 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_70 GBV_ILN_2026 GBV_ILN_4219 AR 51 2016 2 01 05 223-235 |
| source |
Enthalten in Clay minerals 51(2016), 2 vom: 01. Mai, Seite 223-235 volume:51 year:2016 number:2 day:01 month:05 pages:223-235 |
| sourceStr |
Enthalten in Clay minerals 51(2016), 2 vom: 01. Mai, Seite 223-235 volume:51 year:2016 number:2 day:01 month:05 pages:223-235 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| dewey-raw |
000 |
| isfreeaccess_bool |
false |
| container_title |
Clay minerals |
| authorswithroles_txt_mv |
Fernández, Raúl @@aut@@ Ruiz, Isabel @@aut@@ Cuevas, Jaime @@aut@@ |
| publishDateDaySort_date |
2016-05-01T00:00:00Z |
| hierarchy_top_id |
130703907 |
| dewey-sort |
0 |
| id |
OLC2138541126 |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">OLC2138541126</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230810091309.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">230810s2016 xx ||||| 00| ||und c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1180/claymin.2016.051.2.09</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2138541126</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-B1597)claymin.2016.051.2.09-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">000</subfield><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Fernández, Raúl</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2016</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© 2016 by Walter de Gruyter Berlin/Boston</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Concrete and bentonite are being considered as engineered barriers for the deep geological disposal of high-level radioactive waste in argillaceous rocks. Three hydrothermal laboratory experiments of different scalable complexity were performed to improve our knowledge of the formation of calcium aluminate silicate hydrates (C-A-S-H) at the interface between the two materials: concretebentonite transport columns, lime mortar-bentonite transport columns and a portlandite- (bentonite and montmorillonite) batch experiment. Precipitation of C-A-S-H was observed in all experiments. Acicular and fibrous morphologies with certain laminar characteristics were observed which had smaller Ca/Si and larger Al/Si ratios with increasing temperature and lack of accessory minerals. The compositional fields of these C-A-S-H phases formed in the experiments are consistent with Al/(Si+Al) ratios of 0.2- 0.3 described in the literature. The most representative calcium silicate hydrate (C-S-H) phase from the montmorillonite-cement interface is Al-tobermorite. Structural analyses revealed a potential intercalation or association of montmorillonite and C-A-S-H phases at the pore scale.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ruiz, Isabel</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Cuevas, Jaime</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Clay minerals</subfield><subfield code="d">Mineralogical Society, 1965</subfield><subfield code="g">51(2016), 2 vom: 01. Mai, Seite 223-235</subfield><subfield code="w">(DE-627)130703907</subfield><subfield code="w">(DE-600)961059-5</subfield><subfield code="w">(DE-576)016252330</subfield><subfield code="x">0009-8558</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:51</subfield><subfield code="g">year:2016</subfield><subfield code="g">number:2</subfield><subfield code="g">day:01</subfield><subfield code="g">month:05</subfield><subfield code="g">pages:223-235</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1180/claymin.2016.051.2.09</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-TEC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-CHE</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2026</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4219</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">51</subfield><subfield code="j">2016</subfield><subfield code="e">2</subfield><subfield code="b">01</subfield><subfield code="c">05</subfield><subfield code="h">223-235</subfield></datafield></record></collection>
|
| author |
Fernández, Raúl |
| spellingShingle |
Fernández, Raúl ddc 000 ssgn 13 Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite |
| authorStr |
Fernández, Raúl |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)130703907 |
| format |
Article |
| dewey-ones |
000 - Computer science, information & general works 550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut aut aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
0009-8558 |
| topic_title |
000 550 VZ 13 ssgn Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite |
| topic |
ddc 000 ssgn 13 |
| topic_unstemmed |
ddc 000 ssgn 13 |
| topic_browse |
ddc 000 ssgn 13 |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| hierarchy_parent_title |
Clay minerals |
| hierarchy_parent_id |
130703907 |
| dewey-tens |
000 - Computer science, knowledge & systems 550 - Earth sciences & geology |
| hierarchy_top_title |
Clay minerals |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)130703907 (DE-600)961059-5 (DE-576)016252330 |
| title |
Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite |
| ctrlnum |
(DE-627)OLC2138541126 (DE-B1597)claymin.2016.051.2.09-p |
| title_full |
Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite |
| author_sort |
Fernández, Raúl |
| journal |
Clay minerals |
| journalStr |
Clay minerals |
| isOA_bool |
false |
| dewey-hundreds |
000 - Computer science, information & general works 500 - Science |
| recordtype |
marc |
| publishDateSort |
2016 |
| contenttype_str_mv |
txt |
| container_start_page |
223 |
| author_browse |
Fernández, Raúl Ruiz, Isabel Cuevas, Jaime |
| container_volume |
51 |
| class |
000 550 VZ 13 ssgn |
| format_se |
Aufsätze |
| author-letter |
Fernández, Raúl |
| doi_str_mv |
10.1180/claymin.2016.051.2.09 |
| dewey-full |
000 550 |
| title_sort |
formation of c-a-s-h phases from the interaction between concrete or cement and bentonite |
| title_auth |
Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite |
| abstract |
Abstract Concrete and bentonite are being considered as engineered barriers for the deep geological disposal of high-level radioactive waste in argillaceous rocks. Three hydrothermal laboratory experiments of different scalable complexity were performed to improve our knowledge of the formation of calcium aluminate silicate hydrates (C-A-S-H) at the interface between the two materials: concretebentonite transport columns, lime mortar-bentonite transport columns and a portlandite- (bentonite and montmorillonite) batch experiment. Precipitation of C-A-S-H was observed in all experiments. Acicular and fibrous morphologies with certain laminar characteristics were observed which had smaller Ca/Si and larger Al/Si ratios with increasing temperature and lack of accessory minerals. The compositional fields of these C-A-S-H phases formed in the experiments are consistent with Al/(Si+Al) ratios of 0.2- 0.3 described in the literature. The most representative calcium silicate hydrate (C-S-H) phase from the montmorillonite-cement interface is Al-tobermorite. Structural analyses revealed a potential intercalation or association of montmorillonite and C-A-S-H phases at the pore scale. © 2016 by Walter de Gruyter Berlin/Boston |
| abstractGer |
Abstract Concrete and bentonite are being considered as engineered barriers for the deep geological disposal of high-level radioactive waste in argillaceous rocks. Three hydrothermal laboratory experiments of different scalable complexity were performed to improve our knowledge of the formation of calcium aluminate silicate hydrates (C-A-S-H) at the interface between the two materials: concretebentonite transport columns, lime mortar-bentonite transport columns and a portlandite- (bentonite and montmorillonite) batch experiment. Precipitation of C-A-S-H was observed in all experiments. Acicular and fibrous morphologies with certain laminar characteristics were observed which had smaller Ca/Si and larger Al/Si ratios with increasing temperature and lack of accessory minerals. The compositional fields of these C-A-S-H phases formed in the experiments are consistent with Al/(Si+Al) ratios of 0.2- 0.3 described in the literature. The most representative calcium silicate hydrate (C-S-H) phase from the montmorillonite-cement interface is Al-tobermorite. Structural analyses revealed a potential intercalation or association of montmorillonite and C-A-S-H phases at the pore scale. © 2016 by Walter de Gruyter Berlin/Boston |
| abstract_unstemmed |
Abstract Concrete and bentonite are being considered as engineered barriers for the deep geological disposal of high-level radioactive waste in argillaceous rocks. Three hydrothermal laboratory experiments of different scalable complexity were performed to improve our knowledge of the formation of calcium aluminate silicate hydrates (C-A-S-H) at the interface between the two materials: concretebentonite transport columns, lime mortar-bentonite transport columns and a portlandite- (bentonite and montmorillonite) batch experiment. Precipitation of C-A-S-H was observed in all experiments. Acicular and fibrous morphologies with certain laminar characteristics were observed which had smaller Ca/Si and larger Al/Si ratios with increasing temperature and lack of accessory minerals. The compositional fields of these C-A-S-H phases formed in the experiments are consistent with Al/(Si+Al) ratios of 0.2- 0.3 described in the literature. The most representative calcium silicate hydrate (C-S-H) phase from the montmorillonite-cement interface is Al-tobermorite. Structural analyses revealed a potential intercalation or association of montmorillonite and C-A-S-H phases at the pore scale. © 2016 by Walter de Gruyter Berlin/Boston |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-TEC SSG-OLC-CHE SSG-OLC-GEO SSG-OLC-PHA SSG-OPC-GGO GBV_ILN_70 GBV_ILN_2026 GBV_ILN_4219 |
| container_issue |
2 |
| title_short |
Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite |
| url |
https://doi.org/10.1180/claymin.2016.051.2.09 |
| remote_bool |
false |
| author2 |
Ruiz, Isabel Cuevas, Jaime |
| author2Str |
Ruiz, Isabel Cuevas, Jaime |
| ppnlink |
130703907 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1180/claymin.2016.051.2.09 |
| up_date |
2024-07-03T16:55:36.263Z |
| _version_ |
1803577706429808640 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000naa a22002652 4500</leader><controlfield tag="001">OLC2138541126</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230810091309.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">230810s2016 xx ||||| 00| ||und c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1180/claymin.2016.051.2.09</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2138541126</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-B1597)claymin.2016.051.2.09-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">000</subfield><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">13</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Fernández, Raúl</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Formation of C-A-S-H phases from the interaction between concrete or cement and bentonite</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2016</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© 2016 by Walter de Gruyter Berlin/Boston</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Concrete and bentonite are being considered as engineered barriers for the deep geological disposal of high-level radioactive waste in argillaceous rocks. Three hydrothermal laboratory experiments of different scalable complexity were performed to improve our knowledge of the formation of calcium aluminate silicate hydrates (C-A-S-H) at the interface between the two materials: concretebentonite transport columns, lime mortar-bentonite transport columns and a portlandite- (bentonite and montmorillonite) batch experiment. Precipitation of C-A-S-H was observed in all experiments. Acicular and fibrous morphologies with certain laminar characteristics were observed which had smaller Ca/Si and larger Al/Si ratios with increasing temperature and lack of accessory minerals. The compositional fields of these C-A-S-H phases formed in the experiments are consistent with Al/(Si+Al) ratios of 0.2- 0.3 described in the literature. The most representative calcium silicate hydrate (C-S-H) phase from the montmorillonite-cement interface is Al-tobermorite. Structural analyses revealed a potential intercalation or association of montmorillonite and C-A-S-H phases at the pore scale.</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Ruiz, Isabel</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Cuevas, Jaime</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Clay minerals</subfield><subfield code="d">Mineralogical Society, 1965</subfield><subfield code="g">51(2016), 2 vom: 01. Mai, Seite 223-235</subfield><subfield code="w">(DE-627)130703907</subfield><subfield code="w">(DE-600)961059-5</subfield><subfield code="w">(DE-576)016252330</subfield><subfield code="x">0009-8558</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:51</subfield><subfield code="g">year:2016</subfield><subfield code="g">number:2</subfield><subfield code="g">day:01</subfield><subfield code="g">month:05</subfield><subfield code="g">pages:223-235</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1180/claymin.2016.051.2.09</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-TEC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-CHE</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-GEO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHA</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_70</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_2026</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_4219</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">51</subfield><subfield code="j">2016</subfield><subfield code="e">2</subfield><subfield code="b">01</subfield><subfield code="c">05</subfield><subfield code="h">223-235</subfield></datafield></record></collection>
|
| score |
7.402815 |