FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2019927283> ?p ?o ?g. }

• W2019927283 endingPage "748" @default.
• W2019927283 startingPage "741" @default.
• W2019927283 abstract "The mineralogy of the Latosols of the Brazilian Central Plateau remains under discussion in the absence of a clear relationship with their age according to their geomorphic location. The aim of this study was thus to clarify the origin of the kaolinite and gibbsite content variation by studying a regional toposequence and using data from the literature. Chemical composition and soil color were used to discuss mineralogy. The mineralogy of the clay fraction was also investigated using X-ray diagrams. Our results showed that the large variation of kaolinite and gibbsite content can be explained by taking into account both their local and regional location, the variation of the hematite and goethite content remaining limited. The model that is proposed to explain such variation combines a regional component, which is mainly associated to the age of the geomorphic surface and a local component which is mainly associated to the hydraulic conditions along the toposequence. La minéralogie des latosols du Plateau Central brésilien est discutée en l’absence de relation clairement établie avec leur âge qui est en fonction de leur position géomorphologique. L’objectif de cette étude est par conséquent de clarifier l’origine de la variation de teneur en kaolinite et gibbsite en étudiant une toposéquence régionale et les données de la littérature. La minéralogie a été discutée à partir de la composition chimique et de la couleur du sol. Elle a aussi été discutée à l’aide des données de la diffraction des rayons X. Les résultats montrent que la variation élevée de la proportion de kaolinite et de gibbsite des latosols peut être expliquée en prenant en compte à la fois leur localisation régionale et locale. Le modèle proposé combine en effet une composante régionale qui est principalement liée à l’âge de la surface géomorphologique et une composante locale qui est principalement liée aux conditions hydriques le long de la toposéquence." @default.
• W2019927283 created "2016-06-24" @default.
• W2019927283 creator A5025254803 @default.
• W2019927283 creator A5033664724 @default.
• W2019927283 creator A5056826299 @default.
• W2019927283 creator A5057260231 @default.
• W2019927283 creator A5060856470 @default.
• W2019927283 creator A5062635667 @default.
• W2019927283 creator A5083036615 @default.
• W2019927283 date "2008-11-01" @default.
• W2019927283 modified "2023-10-16" @default.
• W2019927283 title "Variation of the kaolinite and gibbsite content at regional and local scale in Latosols of the Brazilian Central Plateau" @default.
• W2019927283 cites W1972807188 @default.
• W2019927283 cites W1973779151 @default.
• W2019927283 cites W1990504172 @default.
• W2019927283 cites W2009403722 @default.
• W2019927283 cites W2025973691 @default.
• W2019927283 cites W2068243168 @default.
• W2019927283 cites W2070251122 @default.
• W2019927283 cites W2086430224 @default.
• W2019927283 cites W2092037936 @default.
• W2019927283 cites W2110451181 @default.
• W2019927283 cites W2121666778 @default.
• W2019927283 cites W2137046130 @default.
• W2019927283 cites W2145806409 @default.
• W2019927283 cites W2156313590 @default.
• W2019927283 cites W2750469720 @default.
• W2019927283 cites W2807912291 @default.
• W2019927283 doi "https://doi.org/10.1016/j.crte.2008.07.006" @default.
• W2019927283 hasPublicationYear "2008" @default.
• W2019927283 type Work @default.
• W2019927283 sameAs 2019927283 @default.
• W2019927283 citedByCount "32" @default.
• W2019927283 countsByYear W20199272832012 @default.
• W2019927283 countsByYear W20199272832013 @default.
• W2019927283 countsByYear W20199272832015 @default.
• W2019927283 countsByYear W20199272832016 @default.
• W2019927283 countsByYear W20199272832017 @default.
• W2019927283 countsByYear W20199272832018 @default.
• W2019927283 countsByYear W20199272832019 @default.
• W2019927283 countsByYear W20199272832020 @default.
• W2019927283 countsByYear W20199272832021 @default.
• W2019927283 countsByYear W20199272832022 @default.
• W2019927283 countsByYear W20199272832023 @default.
• W2019927283 crossrefType "journal-article" @default.
• W2019927283 hasAuthorship W2019927283A5025254803 @default.
• W2019927283 hasAuthorship W2019927283A5033664724 @default.
• W2019927283 hasAuthorship W2019927283A5056826299 @default.
• W2019927283 hasAuthorship W2019927283A5057260231 @default.
• W2019927283 hasAuthorship W2019927283A5060856470 @default.
• W2019927283 hasAuthorship W2019927283A5062635667 @default.
• W2019927283 hasAuthorship W2019927283A5083036615 @default.
• W2019927283 hasBestOaLocation W20199272832 @default.
• W2019927283 hasConcept C114793014 @default.
• W2019927283 hasConcept C127313418 @default.
• W2019927283 hasConcept C134306372 @default.
• W2019927283 hasConcept C150394285 @default.
• W2019927283 hasConcept C17409809 @default.
• W2019927283 hasConcept C178790620 @default.
• W2019927283 hasConcept C185592680 @default.
• W2019927283 hasConcept C199289684 @default.
• W2019927283 hasConcept C2777787761 @default.
• W2019927283 hasConcept C2777975867 @default.
• W2019927283 hasConcept C2779899878 @default.
• W2019927283 hasConcept C2780030769 @default.
• W2019927283 hasConcept C33923547 @default.
• W2019927283 hasConceptScore W2019927283C114793014 @default.
• W2019927283 hasConceptScore W2019927283C127313418 @default.
• W2019927283 hasConceptScore W2019927283C134306372 @default.
• W2019927283 hasConceptScore W2019927283C150394285 @default.
• W2019927283 hasConceptScore W2019927283C17409809 @default.
• W2019927283 hasConceptScore W2019927283C178790620 @default.
• W2019927283 hasConceptScore W2019927283C185592680 @default.
• W2019927283 hasConceptScore W2019927283C199289684 @default.
• W2019927283 hasConceptScore W2019927283C2777787761 @default.
• W2019927283 hasConceptScore W2019927283C2777975867 @default.
• W2019927283 hasConceptScore W2019927283C2779899878 @default.
• W2019927283 hasConceptScore W2019927283C2780030769 @default.
• W2019927283 hasConceptScore W2019927283C33923547 @default.
• W2019927283 hasIssue "11" @default.
• W2019927283 hasLocation W20199272831 @default.
• W2019927283 hasLocation W20199272832 @default.
• W2019927283 hasLocation W20199272833 @default.
• W2019927283 hasLocation W20199272834 @default.
• W2019927283 hasLocation W20199272835 @default.
• W2019927283 hasOpenAccess W2019927283 @default.
• W2019927283 hasPrimaryLocation W20199272831 @default.
• W2019927283 hasRelatedWork W1507814018 @default.
• W2019927283 hasRelatedWork W1968600917 @default.
• W2019927283 hasRelatedWork W2008228328 @default.
• W2019927283 hasRelatedWork W2032337630 @default.
• W2019927283 hasRelatedWork W2061394240 @default.
• W2019927283 hasRelatedWork W2070482744 @default.
• W2019927283 hasRelatedWork W2081480083 @default.
• W2019927283 hasRelatedWork W2171096168 @default.
• W2019927283 hasRelatedWork W2384820335 @default.
• W2019927283 hasRelatedWork W2391376214 @default.
• W2019927283 hasVolume "340" @default.

• next