FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2067160478> ?p ?o ?g. }

• W2067160478 endingPage "81" @default.
• W2067160478 startingPage "62" @default.
• W2067160478 abstract "This study examined pedogenesis, as well as the clay mineralogy of soil and rock samples obtained from a transect of gypsiferous and calcareous materials. The main objectives of this research were to study the relationship between clay minerals and physiographic units as well as the relative importance of key pedogenic processes in controlling clay mineralogy. Palygorskite, chlorite, illite, smectite, quartz and interstratified minerals were observed in both soil and rock samples, using XRD, TEM and EDX analyses. Illite, chlorite, and interstratified minerals are inherited largely from parent rocks. Most of the smectite is inherited from highly smectite marl formations, although some may be the product of palygorskite weathering and transformation of illite particularly at the surface horizons. Neoformation of palygorskite, as a result of calcite and gypsum precipitation, seems to be a major pathway for the occurrence of this mineral, especially on plateau physiographic units, although inheritance has less importance. Gypsiferous soils showed more pedogenic palygorskite as compared to calcareous soils. Three morphological forms of palygorskite, related to degree of weathering, were identified in the studied pedons. New great groups and subgroups of Ustepts (Aridic Gypsiustepts and Aridic–calcic Gypsiustepts) are suggested to be included in Soil Taxonomy based on the properties of some of the studied pedons. Dissolution and transport of anhydrite from outcrops, is considered the main source of pedogenic gypsum in these soils. Micromorphological studies, including thin section observations and SEM analyses indicated variable habits of gypsum crystals suggested a dynamic soil environment." @default.
• W2067160478 created "2016-06-24" @default.
• W2067160478 creator A5005001710 @default.
• W2067160478 creator A5008543256 @default.
• W2067160478 creator A5078042069 @default.
• W2067160478 date "2006-09-01" @default.
• W2067160478 modified "2023-10-18" @default.
• W2067160478 title "Pedogenesis and clay mineralogical investigation of soils formed on gypsiferous and calcareous materials, on a transect, southwestern Iran" @default.
• W2067160478 cites W1964300425 @default.
• W2067160478 cites W1965906628 @default.
• W2067160478 cites W1976017926 @default.
• W2067160478 cites W1979519167 @default.
• W2067160478 cites W1990059612 @default.
• W2067160478 cites W1990075902 @default.
• W2067160478 cites W1990720256 @default.
• W2067160478 cites W1999042142 @default.
• W2067160478 cites W2000159551 @default.
• W2067160478 cites W2001689835 @default.
• W2067160478 cites W2002108424 @default.
• W2067160478 cites W2009513684 @default.
• W2067160478 cites W2012327406 @default.
• W2067160478 cites W2014095295 @default.
• W2067160478 cites W2017620875 @default.
• W2067160478 cites W2019636295 @default.
• W2067160478 cites W2021869742 @default.
• W2067160478 cites W2030176397 @default.
• W2067160478 cites W2037026371 @default.
• W2067160478 cites W2038358080 @default.
• W2067160478 cites W2051001833 @default.
• W2067160478 cites W2056037346 @default.
• W2067160478 cites W2060082983 @default.
• W2067160478 cites W2060251567 @default.
• W2067160478 cites W2060791138 @default.
• W2067160478 cites W2062178505 @default.
• W2067160478 cites W2067180470 @default.
• W2067160478 cites W2070507230 @default.
• W2067160478 cites W2082256713 @default.
• W2067160478 cites W2091343636 @default.
• W2067160478 cites W2092755133 @default.
• W2067160478 cites W2092943486 @default.
• W2067160478 cites W2094714779 @default.
• W2067160478 cites W2095539356 @default.
• W2067160478 cites W2111019271 @default.
• W2067160478 cites W2114017769 @default.
• W2067160478 cites W2117249156 @default.
• W2067160478 cites W2121116596 @default.
• W2067160478 cites W2137707895 @default.
• W2067160478 cites W2138071946 @default.
• W2067160478 cites W2139268476 @default.
• W2067160478 cites W2150778642 @default.
• W2067160478 cites W2396916892 @default.
• W2067160478 cites W3009397686 @default.
• W2067160478 cites W4250212444 @default.
• W2067160478 doi "https://doi.org/10.1016/j.geoderma.2005.08.015" @default.
• W2067160478 hasPublicationYear "2006" @default.
• W2067160478 type Work @default.
• W2067160478 sameAs 2067160478 @default.
• W2067160478 citedByCount "94" @default.
• W2067160478 countsByYear W20671604782012 @default.
• W2067160478 countsByYear W20671604782013 @default.
• W2067160478 countsByYear W20671604782014 @default.
• W2067160478 countsByYear W20671604782015 @default.
• W2067160478 countsByYear W20671604782016 @default.
• W2067160478 countsByYear W20671604782017 @default.
• W2067160478 countsByYear W20671604782018 @default.
• W2067160478 countsByYear W20671604782019 @default.
• W2067160478 countsByYear W20671604782020 @default.
• W2067160478 countsByYear W20671604782021 @default.
• W2067160478 countsByYear W20671604782022 @default.
• W2067160478 countsByYear W20671604782023 @default.
• W2067160478 crossrefType "journal-article" @default.
• W2067160478 hasAuthorship W2067160478A5005001710 @default.
• W2067160478 hasAuthorship W2067160478A5008543256 @default.
• W2067160478 hasAuthorship W2067160478A5078042069 @default.
• W2067160478 hasConcept C123552892 @default.
• W2067160478 hasConcept C127313418 @default.
• W2067160478 hasConcept C150394285 @default.
• W2067160478 hasConcept C151730666 @default.
• W2067160478 hasConcept C155843905 @default.
• W2067160478 hasConcept C159390177 @default.
• W2067160478 hasConcept C159750122 @default.
• W2067160478 hasConcept C17409809 @default.
• W2067160478 hasConcept C178790620 @default.
• W2067160478 hasConcept C184269829 @default.
• W2067160478 hasConcept C185592680 @default.
• W2067160478 hasConcept C199289684 @default.
• W2067160478 hasConcept C2777787761 @default.
• W2067160478 hasConcept C2777844515 @default.
• W2067160478 hasConcept C2779429093 @default.
• W2067160478 hasConcept C2779870107 @default.
• W2067160478 hasConcept C2780873218 @default.
• W2067160478 hasConcept C40212044 @default.
• W2067160478 hasConcept C40724407 @default.
• W2067160478 hasConceptScore W2067160478C123552892 @default.
• W2067160478 hasConceptScore W2067160478C127313418 @default.
• W2067160478 hasConceptScore W2067160478C150394285 @default.
• W2067160478 hasConceptScore W2067160478C151730666 @default.
• W2067160478 hasConceptScore W2067160478C155843905 @default.

• next