FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2015778819> ?p ?o ?g. }

• W2015778819 endingPage "343" @default.
• W2015778819 startingPage "333" @default.
• W2015778819 abstract "In many clay soils, drying and wetting cause non-uniform changes in water content and in the volume of soil and peds. Theoretical relations between total volume of soil, soil thickness and water content are sought for non-uniformly swelling and shrinking soil. Such soil is assumed to be composed of small elemental volumes, each of which does swell or shrink uniformly. It is also assumed that the non-uniformity of swelling or shrinking in such soils arises solely from spatial variation brought about by variations in evapotranspiration and infiltration. A constant ratio between movement of the soil in the vertical and horizontal dimensions is assumed for all elements of soil. By averaging over the soil volume the equations describing the volume change of individual elemental volumes, the averaged equations for non-uniform volume changes may be obtained. They show that the average and the spatial distribution of the changes in soil thickness determine the average changes in water content of the soil. It is concluded that the equations for uniform and non-uniform volume changing soils, though formally different, should in practice produce nearly identical results for clay soils. Dans de nombreux sols argileux les phénomènes de dessiccation et d'humectation provoquent des variations de volume importantes et non-uniformes. Dans cet article sont recherchées des relations théoriques entre la teneur en eau, le volume spécifique et l'épaisseur du sol pour de tels sols. Dans ce but, tout sol hétérogène est supposé divisible en volumes de sol élémentaires dont chacun présente un comportement uniforme. L'hétérogénéité spatiale des variations de volume est supposée provenir d'hétérogénéités spatiales de l'infiltration et de l'évapotranspiration et non d'une variabilit6 des propriétés de gonflement-retrait. On considère que les volumes élémentaires présentent un rapport constant entre les mouvements verticaux et horizontaux du sol. Les équations décrivant les variations de volume á l'échelle du sol sont obtenues par prise de moyenne des équations á l'échelle des volumes élémentaires. ées équations montrent que la moyenne des variations de teneur en eau d'un sol non-unifforme est liée á la moyenne et la dispersion spatiale des variations d'épaisseur du sol. En pratique toutefois il apparaît que les équations de variation de volume en sols uniformes et non-uniformes, bien que différentes sur le plan formel, produisent des résultats numériques très voisins dans la gamme des variations de volume constatées pour les sols argileux." @default.
• W2015778819 created "2016-06-24" @default.
• W2015778819 creator A5001870755 @default.
• W2015778819 creator A5029460145 @default.
• W2015778819 date "1995-09-01" @default.
• W2015778819 modified "2023-09-27" @default.
• W2015778819 title "Non-uniform volume and water content changes in swelling clay soil: I. Theoretical analysis" @default.
• W2015778819 cites W1981110225 @default.
• W2015778819 cites W1981503440 @default.
• W2015778819 cites W1982718180 @default.
• W2015778819 cites W1982844254 @default.
• W2015778819 cites W1982884597 @default.
• W2015778819 cites W1991052736 @default.
• W2015778819 cites W1999239561 @default.
• W2015778819 cites W1999980481 @default.
• W2015778819 cites W2017173573 @default.
• W2015778819 cites W2021056056 @default.
• W2015778819 cites W2037858751 @default.
• W2015778819 cites W2053120545 @default.
• W2015778819 cites W2066663169 @default.
• W2015778819 cites W2071029027 @default.
• W2015778819 cites W2075832229 @default.
• W2015778819 cites W2083161028 @default.
• W2015778819 cites W2098547667 @default.
• W2015778819 cites W2125437547 @default.
• W2015778819 cites W4256668960 @default.
• W2015778819 doi "https://doi.org/10.1111/j.1365-2389.1995.tb01330.x" @default.
• W2015778819 hasPublicationYear "1995" @default.
• W2015778819 type Work @default.
• W2015778819 sameAs 2015778819 @default.
• W2015778819 citedByCount "15" @default.
• W2015778819 countsByYear W20157788192012 @default.
• W2015778819 countsByYear W20157788192013 @default.
• W2015778819 crossrefType "journal-article" @default.
• W2015778819 hasAuthorship W2015778819A5001870755 @default.
• W2015778819 hasAuthorship W2015778819A5029460145 @default.
• W2015778819 hasConcept C121332964 @default.
• W2015778819 hasConcept C127313418 @default.
• W2015778819 hasConcept C13058974 @default.
• W2015778819 hasConcept C134514944 @default.
• W2015778819 hasConcept C153400128 @default.
• W2015778819 hasConcept C159390177 @default.
• W2015778819 hasConcept C159750122 @default.
• W2015778819 hasConcept C159985019 @default.
• W2015778819 hasConcept C185592680 @default.
• W2015778819 hasConcept C187320778 @default.
• W2015778819 hasConcept C192562407 @default.
• W2015778819 hasConcept C199289684 @default.
• W2015778819 hasConcept C20556612 @default.
• W2015778819 hasConcept C24939127 @default.
• W2015778819 hasConcept C2778540859 @default.
• W2015778819 hasConcept C27934549 @default.
• W2015778819 hasConcept C3020601295 @default.
• W2015778819 hasConcept C97355855 @default.
• W2015778819 hasConceptScore W2015778819C121332964 @default.
• W2015778819 hasConceptScore W2015778819C127313418 @default.
• W2015778819 hasConceptScore W2015778819C13058974 @default.
• W2015778819 hasConceptScore W2015778819C134514944 @default.
• W2015778819 hasConceptScore W2015778819C153400128 @default.
• W2015778819 hasConceptScore W2015778819C159390177 @default.
• W2015778819 hasConceptScore W2015778819C159750122 @default.
• W2015778819 hasConceptScore W2015778819C159985019 @default.
• W2015778819 hasConceptScore W2015778819C185592680 @default.
• W2015778819 hasConceptScore W2015778819C187320778 @default.
• W2015778819 hasConceptScore W2015778819C192562407 @default.
• W2015778819 hasConceptScore W2015778819C199289684 @default.
• W2015778819 hasConceptScore W2015778819C20556612 @default.
• W2015778819 hasConceptScore W2015778819C24939127 @default.
• W2015778819 hasConceptScore W2015778819C2778540859 @default.
• W2015778819 hasConceptScore W2015778819C27934549 @default.
• W2015778819 hasConceptScore W2015778819C3020601295 @default.
• W2015778819 hasConceptScore W2015778819C97355855 @default.
• W2015778819 hasIssue "3" @default.
• W2015778819 hasLocation W20157788191 @default.
• W2015778819 hasOpenAccess W2015778819 @default.
• W2015778819 hasPrimaryLocation W20157788191 @default.
• W2015778819 hasRelatedWork W2000357888 @default.
• W2015778819 hasRelatedWork W2030202598 @default.
• W2015778819 hasRelatedWork W2067809007 @default.
• W2015778819 hasRelatedWork W2122210451 @default.
• W2015778819 hasRelatedWork W2331513655 @default.
• W2015778819 hasRelatedWork W2389617593 @default.
• W2015778819 hasRelatedWork W2915113413 @default.
• W2015778819 hasRelatedWork W3195362522 @default.
• W2015778819 hasRelatedWork W3199386688 @default.
• W2015778819 hasRelatedWork W4251317422 @default.
• W2015778819 hasVolume "46" @default.
• W2015778819 isParatext "false" @default.
• W2015778819 isRetracted "false" @default.
• W2015778819 magId "2015778819" @default.
• W2015778819 workType "article" @default.