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- Reynolds_dilatancy abstract "Reynolds' dilatancy is the observed tendency of a compacted granular material to dilate (expand in volume) as it is sheared. This occurs because the grains in a compacted state are interlocking and therefore do not have the freedom to move around one another. When stressed, a lever motion occurs between neighboring grains, which produces a bulk expansion of the material. On the other hand, when a granular material starts in a very loose state it may initially compact instead of dilating under shear. Reynolds' dilatancy is a common feature of the soils and sands studied by geotechnical engineers, and is a part of the broader topic of soil mechanics. It was first described scientifically by Osborne Reynolds (1842–1912) in 1885 and 1886.".
- Reynolds_dilatancy wikiPageID "7139092".
- Reynolds_dilatancy wikiPageLength "1509".
- Reynolds_dilatancy wikiPageOutDegree "13".
- Reynolds_dilatancy wikiPageRevisionID "260276504".
- Reynolds_dilatancy wikiPageWikiLink Category:Soil_mechanics.
- Reynolds_dilatancy wikiPageWikiLink Geotechnical_engineering.
- Reynolds_dilatancy wikiPageWikiLink Granular_material.
- Reynolds_dilatancy wikiPageWikiLink Lever.
- Reynolds_dilatancy wikiPageWikiLink Osborne_Reynolds.
- Reynolds_dilatancy wikiPageWikiLink Sand.
- Reynolds_dilatancy wikiPageWikiLink Soil.
- Reynolds_dilatancy wikiPageWikiLink Soil_compaction.
- Reynolds_dilatancy wikiPageWikiLink Soil_mechanics.
- Reynolds_dilatancy wikiPageWikiLink Triaxial_shear_test.
- Reynolds_dilatancy wikiPageWikiLink Triaxial_shear_tests.
- Reynolds_dilatancy wikiPageWikiLinkText "Reynolds' dilatancy".
- Reynolds_dilatancy wikiPageWikiLinkText "Reynolds' dilation".
- Reynolds_dilatancy wikiPageWikiLinkText "dilate".
- Reynolds_dilatancy hasPhotoCollection Reynolds_dilatancy.
- Reynolds_dilatancy wikiPageUsesTemplate Template:Geotechnical_engineering.
- Reynolds_dilatancy subject Category:Soil_mechanics.
- Reynolds_dilatancy hypernym Tendency.
- Reynolds_dilatancy type Organisation.
- Reynolds_dilatancy comment "Reynolds' dilatancy is the observed tendency of a compacted granular material to dilate (expand in volume) as it is sheared. This occurs because the grains in a compacted state are interlocking and therefore do not have the freedom to move around one another. When stressed, a lever motion occurs between neighboring grains, which produces a bulk expansion of the material.".
- Reynolds_dilatancy label "Reynolds' dilatancy".
- Reynolds_dilatancy sameAs m.0h68s9.
- Reynolds_dilatancy sameAs Q7319618.
- Reynolds_dilatancy sameAs Q7319618.
- Reynolds_dilatancy wasDerivedFrom Reynolds_dilatancyoldid=260276504.
- Reynolds_dilatancy isPrimaryTopicOf Reynolds_dilatancy.