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Sistema de porosidade do solo numa topossequĂȘncia Luviossolo-Solonetz no Sul de Portugal

dc.contributor.authorMonteiro, Fernando
dc.contributor.authorMadeira, Manuel
dc.contributor.authorSousa, E.
dc.contributor.authorMarcelino, V.
dc.date.accessioned2009-06-29T10:53:22Z
dc.date.available2009-06-29T10:53:22Z
dc.date.issued2007
dc.description.abstractSoils with stagnic properties occurring in Alentejo commonly have low porosity. The study of a typical soil toposequence, showed that soil pore features were significantly different amongst summit and foot/toe slope pedons. In the summit pedon the Ap1 horizon was more porous than the Ap2, both exhibiting similar void distribution patterns. Conversely, the Ap1 and Ap2 horizons of the footslope pedon had a similar pore space volume, but pores with diameter larger than 500 ÎŒm were less important in the later. Pore space volume of Bt horizons was low whatever the slope position of pedons. However, they differ significantly in terms of void type and orientation patterns. No preferred orientation patterns were found in soil voids that could be related with soil compaction, being their low porosity, namely their low “conductive” porosity, not attributable to soil compaction. Those features can instead be due to the sodicity and/or the low organic C of these soils.en
dc.identifier.citation"Revista de CiĂȘncias AgrĂĄrias". ISSN 0871-018X. 30:2 (2007) 15-26en
dc.identifier.urihttp://hdl.handle.net/10400.5/1050
dc.language.isoporen
dc.publisherSociedade de CiĂȘncias AgrĂĄrias de Portugalen
dc.subjectpore space characteristicsen
dc.subjectLuvisol-Solonetz toposequenceen
dc.subjectsistema de porosidade do soloen
dc.subjecttopossequĂȘncia Luvissolo-Solonetzen
dc.subjectPortugalen
dc.titleSistema de porosidade do solo numa topossequĂȘncia Luviossolo-Solonetz no Sul de Portugalen
dc.title.alternativePore space characteristics in a Luvisol-Solonetz toposequence in Southern Portugalen
dc.typejournal article
dspace.entity.typePublication
rcaap.rightsopenAccessen
rcaap.typearticleen

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