Study of the Curing Behaviour of an Algerian Calcareous Crust
Abstract For some compaction water content, calcareous crust remains a solid, and may readily be collapsing when the saturation increased. After a period that depends on the evaporation of the water, the calcareous crust compacted begins to harden or gain strength. The strength gain is very rapid at...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Loualbia, Hamza [verfasserIn] Duc, Myriam [verfasserIn] Demdoum, Abdellah [verfasserIn] Feia, Sadok [verfasserIn] |
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| Format: |
E-Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2020 |
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| Schlagwörter: |
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| Übergeordnetes Werk: |
Enthalten in: Geotechnical and geological engineering - Dordrecht [u.a.] : Springer Science + Business Media B.V, 1983, 39(2020), 2 vom: 14. Sept., Seite 1173-1179 |
|---|---|
| Übergeordnetes Werk: |
volume:39 ; year:2020 ; number:2 ; day:14 ; month:09 ; pages:1173-1179 |
| Links: |
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| DOI / URN: |
10.1007/s10706-020-01552-7 |
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| Katalog-ID: |
SPR04340068X |
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| 520 | |a Abstract For some compaction water content, calcareous crust remains a solid, and may readily be collapsing when the saturation increased. After a period that depends on the evaporation of the water, the calcareous crust compacted begins to harden or gain strength. The strength gain is very rapid at quick drying, but it will be slow, for slow drying. Evaporation from the calcareous crust compacted should be related to the increase in strength. This experimental work carried out on samples dried under different conditions, attempts to explain the origin of the curing and the existence of a water content for which it is maximum. SEM observations and mercury intrusion porosimetry (MIP) test have shown that the assumption that suction contributes only to an increase in cohesion may not be always true. The dissolution of calcite during the imbibition may also influence the curing. | ||
| 650 | 4 | |a Calcareous crust |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Curing process |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Compaction |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Water content |7 (dpeaa)DE-He213 | |
| 650 | 4 | |a Strength |7 (dpeaa)DE-He213 | |
| 700 | 1 | |a Duc, Myriam |e verfasserin |4 aut | |
| 700 | 1 | |a Demdoum, Abdellah |e verfasserin |4 aut | |
| 700 | 1 | |a Feia, Sadok |e verfasserin |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Geotechnical and geological engineering |d Dordrecht [u.a.] : Springer Science + Business Media B.V, 1983 |g 39(2020), 2 vom: 14. Sept., Seite 1173-1179 |w (DE-627)312847475 |w (DE-600)2012363-2 |x 1573-1529 |7 nnns |
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10.1007/s10706-020-01552-7 doi (DE-627)SPR04340068X (DE-599)SPRs10706-020-01552-7-e (SPR)s10706-020-01552-7-e DE-627 ger DE-627 rakwb eng 690 ASE 57.00 bkl 38.58 bkl 56.20 bkl Loualbia, Hamza verfasserin aut Study of the Curing Behaviour of an Algerian Calcareous Crust 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract For some compaction water content, calcareous crust remains a solid, and may readily be collapsing when the saturation increased. After a period that depends on the evaporation of the water, the calcareous crust compacted begins to harden or gain strength. The strength gain is very rapid at quick drying, but it will be slow, for slow drying. Evaporation from the calcareous crust compacted should be related to the increase in strength. This experimental work carried out on samples dried under different conditions, attempts to explain the origin of the curing and the existence of a water content for which it is maximum. SEM observations and mercury intrusion porosimetry (MIP) test have shown that the assumption that suction contributes only to an increase in cohesion may not be always true. The dissolution of calcite during the imbibition may also influence the curing. Calcareous crust (dpeaa)DE-He213 Curing process (dpeaa)DE-He213 Compaction (dpeaa)DE-He213 Water content (dpeaa)DE-He213 Strength (dpeaa)DE-He213 Duc, Myriam verfasserin aut Demdoum, Abdellah verfasserin aut Feia, Sadok verfasserin aut Enthalten in Geotechnical and geological engineering Dordrecht [u.a.] : Springer Science + Business Media B.V, 1983 39(2020), 2 vom: 14. Sept., Seite 1173-1179 (DE-627)312847475 (DE-600)2012363-2 1573-1529 nnns volume:39 year:2020 number:2 day:14 month:09 pages:1173-1179 https://dx.doi.org/10.1007/s10706-020-01552-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 57.00 ASE 38.58 ASE 56.20 ASE AR 39 2020 2 14 09 1173-1179 |
| spelling |
10.1007/s10706-020-01552-7 doi (DE-627)SPR04340068X (DE-599)SPRs10706-020-01552-7-e (SPR)s10706-020-01552-7-e DE-627 ger DE-627 rakwb eng 690 ASE 57.00 bkl 38.58 bkl 56.20 bkl Loualbia, Hamza verfasserin aut Study of the Curing Behaviour of an Algerian Calcareous Crust 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract For some compaction water content, calcareous crust remains a solid, and may readily be collapsing when the saturation increased. After a period that depends on the evaporation of the water, the calcareous crust compacted begins to harden or gain strength. The strength gain is very rapid at quick drying, but it will be slow, for slow drying. Evaporation from the calcareous crust compacted should be related to the increase in strength. This experimental work carried out on samples dried under different conditions, attempts to explain the origin of the curing and the existence of a water content for which it is maximum. SEM observations and mercury intrusion porosimetry (MIP) test have shown that the assumption that suction contributes only to an increase in cohesion may not be always true. The dissolution of calcite during the imbibition may also influence the curing. Calcareous crust (dpeaa)DE-He213 Curing process (dpeaa)DE-He213 Compaction (dpeaa)DE-He213 Water content (dpeaa)DE-He213 Strength (dpeaa)DE-He213 Duc, Myriam verfasserin aut Demdoum, Abdellah verfasserin aut Feia, Sadok verfasserin aut Enthalten in Geotechnical and geological engineering Dordrecht [u.a.] : Springer Science + Business Media B.V, 1983 39(2020), 2 vom: 14. Sept., Seite 1173-1179 (DE-627)312847475 (DE-600)2012363-2 1573-1529 nnns volume:39 year:2020 number:2 day:14 month:09 pages:1173-1179 https://dx.doi.org/10.1007/s10706-020-01552-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 57.00 ASE 38.58 ASE 56.20 ASE AR 39 2020 2 14 09 1173-1179 |
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10.1007/s10706-020-01552-7 doi (DE-627)SPR04340068X (DE-599)SPRs10706-020-01552-7-e (SPR)s10706-020-01552-7-e DE-627 ger DE-627 rakwb eng 690 ASE 57.00 bkl 38.58 bkl 56.20 bkl Loualbia, Hamza verfasserin aut Study of the Curing Behaviour of an Algerian Calcareous Crust 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract For some compaction water content, calcareous crust remains a solid, and may readily be collapsing when the saturation increased. After a period that depends on the evaporation of the water, the calcareous crust compacted begins to harden or gain strength. The strength gain is very rapid at quick drying, but it will be slow, for slow drying. Evaporation from the calcareous crust compacted should be related to the increase in strength. This experimental work carried out on samples dried under different conditions, attempts to explain the origin of the curing and the existence of a water content for which it is maximum. SEM observations and mercury intrusion porosimetry (MIP) test have shown that the assumption that suction contributes only to an increase in cohesion may not be always true. The dissolution of calcite during the imbibition may also influence the curing. Calcareous crust (dpeaa)DE-He213 Curing process (dpeaa)DE-He213 Compaction (dpeaa)DE-He213 Water content (dpeaa)DE-He213 Strength (dpeaa)DE-He213 Duc, Myriam verfasserin aut Demdoum, Abdellah verfasserin aut Feia, Sadok verfasserin aut Enthalten in Geotechnical and geological engineering Dordrecht [u.a.] : Springer Science + Business Media B.V, 1983 39(2020), 2 vom: 14. Sept., Seite 1173-1179 (DE-627)312847475 (DE-600)2012363-2 1573-1529 nnns volume:39 year:2020 number:2 day:14 month:09 pages:1173-1179 https://dx.doi.org/10.1007/s10706-020-01552-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 57.00 ASE 38.58 ASE 56.20 ASE AR 39 2020 2 14 09 1173-1179 |
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10.1007/s10706-020-01552-7 doi (DE-627)SPR04340068X (DE-599)SPRs10706-020-01552-7-e (SPR)s10706-020-01552-7-e DE-627 ger DE-627 rakwb eng 690 ASE 57.00 bkl 38.58 bkl 56.20 bkl Loualbia, Hamza verfasserin aut Study of the Curing Behaviour of an Algerian Calcareous Crust 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract For some compaction water content, calcareous crust remains a solid, and may readily be collapsing when the saturation increased. After a period that depends on the evaporation of the water, the calcareous crust compacted begins to harden or gain strength. The strength gain is very rapid at quick drying, but it will be slow, for slow drying. Evaporation from the calcareous crust compacted should be related to the increase in strength. This experimental work carried out on samples dried under different conditions, attempts to explain the origin of the curing and the existence of a water content for which it is maximum. SEM observations and mercury intrusion porosimetry (MIP) test have shown that the assumption that suction contributes only to an increase in cohesion may not be always true. The dissolution of calcite during the imbibition may also influence the curing. Calcareous crust (dpeaa)DE-He213 Curing process (dpeaa)DE-He213 Compaction (dpeaa)DE-He213 Water content (dpeaa)DE-He213 Strength (dpeaa)DE-He213 Duc, Myriam verfasserin aut Demdoum, Abdellah verfasserin aut Feia, Sadok verfasserin aut Enthalten in Geotechnical and geological engineering Dordrecht [u.a.] : Springer Science + Business Media B.V, 1983 39(2020), 2 vom: 14. Sept., Seite 1173-1179 (DE-627)312847475 (DE-600)2012363-2 1573-1529 nnns volume:39 year:2020 number:2 day:14 month:09 pages:1173-1179 https://dx.doi.org/10.1007/s10706-020-01552-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 57.00 ASE 38.58 ASE 56.20 ASE AR 39 2020 2 14 09 1173-1179 |
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10.1007/s10706-020-01552-7 doi (DE-627)SPR04340068X (DE-599)SPRs10706-020-01552-7-e (SPR)s10706-020-01552-7-e DE-627 ger DE-627 rakwb eng 690 ASE 57.00 bkl 38.58 bkl 56.20 bkl Loualbia, Hamza verfasserin aut Study of the Curing Behaviour of an Algerian Calcareous Crust 2020 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Abstract For some compaction water content, calcareous crust remains a solid, and may readily be collapsing when the saturation increased. After a period that depends on the evaporation of the water, the calcareous crust compacted begins to harden or gain strength. The strength gain is very rapid at quick drying, but it will be slow, for slow drying. Evaporation from the calcareous crust compacted should be related to the increase in strength. This experimental work carried out on samples dried under different conditions, attempts to explain the origin of the curing and the existence of a water content for which it is maximum. SEM observations and mercury intrusion porosimetry (MIP) test have shown that the assumption that suction contributes only to an increase in cohesion may not be always true. The dissolution of calcite during the imbibition may also influence the curing. Calcareous crust (dpeaa)DE-He213 Curing process (dpeaa)DE-He213 Compaction (dpeaa)DE-He213 Water content (dpeaa)DE-He213 Strength (dpeaa)DE-He213 Duc, Myriam verfasserin aut Demdoum, Abdellah verfasserin aut Feia, Sadok verfasserin aut Enthalten in Geotechnical and geological engineering Dordrecht [u.a.] : Springer Science + Business Media B.V, 1983 39(2020), 2 vom: 14. Sept., Seite 1173-1179 (DE-627)312847475 (DE-600)2012363-2 1573-1529 nnns volume:39 year:2020 number:2 day:14 month:09 pages:1173-1179 https://dx.doi.org/10.1007/s10706-020-01552-7 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_SPRINGER SSG-OPC-GGO SSG-OPC-GEO SSG-OPC-ASE GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_32 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_74 GBV_ILN_90 GBV_ILN_95 GBV_ILN_100 GBV_ILN_105 GBV_ILN_110 GBV_ILN_120 GBV_ILN_138 GBV_ILN_150 GBV_ILN_151 GBV_ILN_152 GBV_ILN_161 GBV_ILN_170 GBV_ILN_171 GBV_ILN_187 GBV_ILN_213 GBV_ILN_224 GBV_ILN_230 GBV_ILN_250 GBV_ILN_281 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_636 GBV_ILN_702 GBV_ILN_2001 GBV_ILN_2003 GBV_ILN_2004 GBV_ILN_2005 GBV_ILN_2006 GBV_ILN_2007 GBV_ILN_2008 GBV_ILN_2009 GBV_ILN_2010 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2015 GBV_ILN_2020 GBV_ILN_2021 GBV_ILN_2025 GBV_ILN_2026 GBV_ILN_2027 GBV_ILN_2031 GBV_ILN_2034 GBV_ILN_2037 GBV_ILN_2038 GBV_ILN_2039 GBV_ILN_2044 GBV_ILN_2048 GBV_ILN_2049 GBV_ILN_2050 GBV_ILN_2055 GBV_ILN_2056 GBV_ILN_2057 GBV_ILN_2059 GBV_ILN_2061 GBV_ILN_2064 GBV_ILN_2065 GBV_ILN_2068 GBV_ILN_2088 GBV_ILN_2093 GBV_ILN_2106 GBV_ILN_2107 GBV_ILN_2108 GBV_ILN_2110 GBV_ILN_2111 GBV_ILN_2112 GBV_ILN_2113 GBV_ILN_2118 GBV_ILN_2122 GBV_ILN_2129 GBV_ILN_2143 GBV_ILN_2144 GBV_ILN_2147 GBV_ILN_2148 GBV_ILN_2152 GBV_ILN_2153 GBV_ILN_2188 GBV_ILN_2190 GBV_ILN_2232 GBV_ILN_2336 GBV_ILN_2446 GBV_ILN_2470 GBV_ILN_2472 GBV_ILN_2507 GBV_ILN_2522 GBV_ILN_2548 GBV_ILN_4035 GBV_ILN_4037 GBV_ILN_4046 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4242 GBV_ILN_4246 GBV_ILN_4249 GBV_ILN_4251 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4326 GBV_ILN_4328 GBV_ILN_4333 GBV_ILN_4334 GBV_ILN_4335 GBV_ILN_4336 GBV_ILN_4338 GBV_ILN_4393 GBV_ILN_4700 57.00 ASE 38.58 ASE 56.20 ASE AR 39 2020 2 14 09 1173-1179 |
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Enthalten in Geotechnical and geological engineering 39(2020), 2 vom: 14. Sept., Seite 1173-1179 volume:39 year:2020 number:2 day:14 month:09 pages:1173-1179 |
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Loualbia, Hamza @@aut@@ Duc, Myriam @@aut@@ Demdoum, Abdellah @@aut@@ Feia, Sadok @@aut@@ |
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After a period that depends on the evaporation of the water, the calcareous crust compacted begins to harden or gain strength. The strength gain is very rapid at quick drying, but it will be slow, for slow drying. Evaporation from the calcareous crust compacted should be related to the increase in strength. This experimental work carried out on samples dried under different conditions, attempts to explain the origin of the curing and the existence of a water content for which it is maximum. SEM observations and mercury intrusion porosimetry (MIP) test have shown that the assumption that suction contributes only to an increase in cohesion may not be always true. 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Loualbia, Hamza |
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Loualbia, Hamza ddc 690 bkl 57.00 bkl 38.58 bkl 56.20 misc Calcareous crust misc Curing process misc Compaction misc Water content misc Strength Study of the Curing Behaviour of an Algerian Calcareous Crust |
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690 ASE 57.00 bkl 38.58 bkl 56.20 bkl Study of the Curing Behaviour of an Algerian Calcareous Crust Calcareous crust (dpeaa)DE-He213 Curing process (dpeaa)DE-He213 Compaction (dpeaa)DE-He213 Water content (dpeaa)DE-He213 Strength (dpeaa)DE-He213 |
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ddc 690 bkl 57.00 bkl 38.58 bkl 56.20 misc Calcareous crust misc Curing process misc Compaction misc Water content misc Strength |
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study of the curing behaviour of an algerian calcareous crust |
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Study of the Curing Behaviour of an Algerian Calcareous Crust |
| abstract |
Abstract For some compaction water content, calcareous crust remains a solid, and may readily be collapsing when the saturation increased. After a period that depends on the evaporation of the water, the calcareous crust compacted begins to harden or gain strength. The strength gain is very rapid at quick drying, but it will be slow, for slow drying. Evaporation from the calcareous crust compacted should be related to the increase in strength. This experimental work carried out on samples dried under different conditions, attempts to explain the origin of the curing and the existence of a water content for which it is maximum. SEM observations and mercury intrusion porosimetry (MIP) test have shown that the assumption that suction contributes only to an increase in cohesion may not be always true. The dissolution of calcite during the imbibition may also influence the curing. |
| abstractGer |
Abstract For some compaction water content, calcareous crust remains a solid, and may readily be collapsing when the saturation increased. After a period that depends on the evaporation of the water, the calcareous crust compacted begins to harden or gain strength. The strength gain is very rapid at quick drying, but it will be slow, for slow drying. Evaporation from the calcareous crust compacted should be related to the increase in strength. This experimental work carried out on samples dried under different conditions, attempts to explain the origin of the curing and the existence of a water content for which it is maximum. SEM observations and mercury intrusion porosimetry (MIP) test have shown that the assumption that suction contributes only to an increase in cohesion may not be always true. The dissolution of calcite during the imbibition may also influence the curing. |
| abstract_unstemmed |
Abstract For some compaction water content, calcareous crust remains a solid, and may readily be collapsing when the saturation increased. After a period that depends on the evaporation of the water, the calcareous crust compacted begins to harden or gain strength. The strength gain is very rapid at quick drying, but it will be slow, for slow drying. Evaporation from the calcareous crust compacted should be related to the increase in strength. This experimental work carried out on samples dried under different conditions, attempts to explain the origin of the curing and the existence of a water content for which it is maximum. SEM observations and mercury intrusion porosimetry (MIP) test have shown that the assumption that suction contributes only to an increase in cohesion may not be always true. The dissolution of calcite during the imbibition may also influence the curing. |
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| container_issue |
2 |
| title_short |
Study of the Curing Behaviour of an Algerian Calcareous Crust |
| url |
https://dx.doi.org/10.1007/s10706-020-01552-7 |
| remote_bool |
true |
| author2 |
Duc, Myriam Demdoum, Abdellah Feia, Sadok |
| author2Str |
Duc, Myriam Demdoum, Abdellah Feia, Sadok |
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312847475 |
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false |
| doi_str |
10.1007/s10706-020-01552-7 |
| up_date |
2024-07-03T18:25:21.267Z |
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1803583353017860096 |
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| score |
7.4014015 |