Problems with collapsible soils: Particle types and inter-particle bonding
A collapsible soil is composed essentially of a packing of mineral particles and a set of interparticle bonds holding the system together. Failure requires the bond system to fail and the soil structure to collapse. A natural hazard is presented. The soil structure may collapse inwards (consolidate)...
| Main Authors: | , |
|---|---|
| Format: | Article |
| Language: | English |
| Published: |
De Gruyter
2019-11-01
|
| Series: | Open Geosciences |
| Subjects: | |
| Online Access: | https://doi.org/10.1515/geo-2019-0064 |
| _version_ | 1818718872266604544 |
|---|---|
| author | Smalley Ian Ng’ambi Samson |
| author_facet | Smalley Ian Ng’ambi Samson |
| author_sort | Smalley Ian |
| collection | DOAJ |
| description | A collapsible soil is composed essentially of a packing of mineral particles and a set of interparticle bonds holding the system together. Failure requires the bond system to fail and the soil structure to collapse. A natural hazard is presented. The soil structure may collapse inwards (consolidate), as in loess failure, or it may collapse outwards (disperse, disintegrate), as in the failure of quick-clays, some collapsing sands, some silty estuarine deposits, and in wind erosion of silty soils by saltating sand grains. Generalising about bonding systems allows two types of interparticle bond to be recognized: long range bonds and short range bonds. Long range bonds are found in clay mineral systems and allow the occurrence of plasticity. They are represented by c in the standard Coulomb equation. Short range bonds are found in inactive particle systems. These are soil systems where the constituent particles do not have a significant electrical charge. A slight deformation of a short-range bonded system causes much loss of strength. It is short range bonds which tend to dominate in collapsing soil systems, although in the complex case of loess the bond failure is initially mediated by long range bonds at the interparticle contact regions. A collapse failure involves a large scale remaking of the soil structure, and thus total failure of the bonding system. |
| first_indexed | 2024-12-17T19:57:57Z |
| format | Article |
| id | doaj.art-b4b7c267300f402c8b9fe124ff26ebd1 |
| institution | Directory Open Access Journal |
| issn | 2391-5447 |
| language | English |
| last_indexed | 2024-12-17T19:57:57Z |
| publishDate | 2019-11-01 |
| publisher | De Gruyter |
| record_format | Article |
| series | Open Geosciences |
| spelling | doaj.art-b4b7c267300f402c8b9fe124ff26ebd12022-12-21T21:34:33ZengDe GruyterOpen Geosciences2391-54472019-11-0111182983610.1515/geo-2019-0064geo-2019-0064Problems with collapsible soils: Particle types and inter-particle bondingSmalley Ian0Ng’ambi Samson1School of Geography, Geology & the Environment, University of Leicester, LeicesterLE1 7RH, United KingdomSchool of Environment Construction & Energy, Coventry University, CoventryCV1 5FB, United KingdomA collapsible soil is composed essentially of a packing of mineral particles and a set of interparticle bonds holding the system together. Failure requires the bond system to fail and the soil structure to collapse. A natural hazard is presented. The soil structure may collapse inwards (consolidate), as in loess failure, or it may collapse outwards (disperse, disintegrate), as in the failure of quick-clays, some collapsing sands, some silty estuarine deposits, and in wind erosion of silty soils by saltating sand grains. Generalising about bonding systems allows two types of interparticle bond to be recognized: long range bonds and short range bonds. Long range bonds are found in clay mineral systems and allow the occurrence of plasticity. They are represented by c in the standard Coulomb equation. Short range bonds are found in inactive particle systems. These are soil systems where the constituent particles do not have a significant electrical charge. A slight deformation of a short-range bonded system causes much loss of strength. It is short range bonds which tend to dominate in collapsing soil systems, although in the complex case of loess the bond failure is initially mediated by long range bonds at the interparticle contact regions. A collapse failure involves a large scale remaking of the soil structure, and thus total failure of the bonding system.https://doi.org/10.1515/geo-2019-0064collapsible soilssandsilt and clay-sizelong and short range bondssoil erosiontwo basic types of soil collapseloess |
| spellingShingle | Smalley Ian Ng’ambi Samson Problems with collapsible soils: Particle types and inter-particle bonding Open Geosciences collapsible soils sand silt and clay-size long and short range bonds soil erosion two basic types of soil collapse loess |
| title | Problems with collapsible soils: Particle types and inter-particle bonding |
| title_full | Problems with collapsible soils: Particle types and inter-particle bonding |
| title_fullStr | Problems with collapsible soils: Particle types and inter-particle bonding |
| title_full_unstemmed | Problems with collapsible soils: Particle types and inter-particle bonding |
| title_short | Problems with collapsible soils: Particle types and inter-particle bonding |
| title_sort | problems with collapsible soils particle types and inter particle bonding |
| topic | collapsible soils sand silt and clay-size long and short range bonds soil erosion two basic types of soil collapse loess |
| url | https://doi.org/10.1515/geo-2019-0064 |
| work_keys_str_mv | AT smalleyian problemswithcollapsiblesoilsparticletypesandinterparticlebonding AT ngambisamson problemswithcollapsiblesoilsparticletypesandinterparticlebonding |