FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4214869159> ?p ?o ?g. }

• W4214869159 endingPage "115780" @default.
• W4214869159 startingPage "115780" @default.
• W4214869159 abstract "The aim of this study was to investigate glauconite weathering in soils of temperate climate, with special attention paid to formation of iron oxyhydroxides at the expense of the glauconite. Five soil profiles developed on parent material in which glauconite was the main (if not the only) phyllosilicate and source of Fe were selected for the study. Basic physical and chemical properties of bulk (<2 mm) soil samples (color, texture, pH, and carbonate and soil organic carbon content) were determined. Clay fractions (<2 µm and <0.2 µm) and green pellets were separated from the studied soils and analyzed using X-ray diffractometry, Fourier-transform infrared spectroscopy, Mössbauer spectroscopy, and inductively coupled plasma - optical emission spectrometry. Thin sections prepared from selected undisturbed soil materials were observed under optical microscope. Three of the soils were acidic with pH ranging from 4.3 to 5.5 and the remaining two were alkaline with pH from 6.8 to 8.6. Parent glauconites from each profile showed quite similar chemical composition, except that in one case Fe(II) was much more abundant than in the others. In both acidic and alkaline soils, glauconite weathering products included Al-smectite-rich glauconite-smectite mixed-layered minerals (G-S), kaolinite, and Fe oxyhydroxides. G-S were likely formed by transformation of glauconite, whereas kaolinite and iron oxyhydroxides (i.e. goethite, lepidocrocite, and perhaps ferrihydrite) crystallized in the studied soils from substances dissolved from parent glauconites. Leaching of Fe and Mg from the glauconite structure and loss of K were indicated. In acidic soils the weathering products concentrated in the clay fractions, whereas in alkaline soils they occurred both in clays and in the glaucony pellets. Mössbauer spectroscopy indicated that fine crystalline and especially nanocrystalline iron oxyhydroxides are substantial products of glauconite weathering in all the studied clays. Formation of the Fe oxyhydroxides was controlled by hydrological conditions (and related redox activity) and by soil pH. Alkaline conditions seemed to favor goethite crystallization, whereas redox activity led to formation of lepidocrocite and likely ferrihydrite. Soil color was mostly controlled by the presence of glauconite. Only the relatively significant lepidocrocite content in a few of the studied soil horizons was marked by brown or rusty colors indicating high redox activity." @default.
• W4214869159 created "2022-03-05" @default.
• W4214869159 creator A5009628017 @default.
• W4214869159 creator A5011727209 @default.
• W4214869159 creator A5033339999 @default.
• W4214869159 creator A5045727242 @default.
• W4214869159 creator A5045908166 @default.
• W4214869159 creator A5067929745 @default.
• W4214869159 creator A5069095254 @default.
• W4214869159 date "2022-06-01" @default.
• W4214869159 modified "2023-10-11" @default.
• W4214869159 title "Formation of iron oxyhydroxides as a result of glauconite weathering in soils of temperate climate" @default.
• W4214869159 cites W1642724957 @default.
• W4214869159 cites W1980593832 @default.
• W4214869159 cites W1998786159 @default.
• W4214869159 cites W1999512079 @default.
• W4214869159 cites W2014749422 @default.
• W4214869159 cites W2026568442 @default.
• W4214869159 cites W2031588808 @default.
• W4214869159 cites W2036075068 @default.
• W4214869159 cites W2060133447 @default.
• W4214869159 cites W2088266104 @default.
• W4214869159 cites W2096604414 @default.
• W4214869159 cites W2124317801 @default.
• W4214869159 cites W2127197558 @default.
• W4214869159 cites W2138811779 @default.
• W4214869159 cites W2236827699 @default.
• W4214869159 cites W2309936762 @default.
• W4214869159 cites W2320116693 @default.
• W4214869159 cites W2326739351 @default.
• W4214869159 cites W2430797665 @default.
• W4214869159 cites W2886610040 @default.
• W4214869159 cites W2909931702 @default.
• W4214869159 cites W3039345509 @default.
• W4214869159 cites W4255412919 @default.
• W4214869159 doi "https://doi.org/10.1016/j.geoderma.2022.115780" @default.
• W4214869159 hasPublicationYear "2022" @default.
• W4214869159 type Work @default.
• W4214869159 citedByCount "4" @default.
• W4214869159 countsByYear W42148691592023 @default.
• W4214869159 crossrefType "journal-article" @default.
• W4214869159 hasAuthorship W4214869159A5009628017 @default.
• W4214869159 hasAuthorship W4214869159A5011727209 @default.
• W4214869159 hasAuthorship W4214869159A5033339999 @default.
• W4214869159 hasAuthorship W4214869159A5045727242 @default.
• W4214869159 hasAuthorship W4214869159A5045908166 @default.
• W4214869159 hasAuthorship W4214869159A5067929745 @default.
• W4214869159 hasAuthorship W4214869159A5069095254 @default.
• W4214869159 hasConcept C107872376 @default.
• W4214869159 hasConcept C127313418 @default.
• W4214869159 hasConcept C150394285 @default.
• W4214869159 hasConcept C159390177 @default.
• W4214869159 hasConcept C159750122 @default.
• W4214869159 hasConcept C17409809 @default.
• W4214869159 hasConcept C178790620 @default.
• W4214869159 hasConcept C185592680 @default.
• W4214869159 hasConcept C199289684 @default.
• W4214869159 hasConcept C2776386860 @default.
• W4214869159 hasConcept C2777787761 @default.
• W4214869159 hasConcept C2777975867 @default.
• W4214869159 hasConcept C2779256693 @default.
• W4214869159 hasConcept C2779899878 @default.
• W4214869159 hasConcept C2780804967 @default.
• W4214869159 hasConcept C40212044 @default.
• W4214869159 hasConcept C40724407 @default.
• W4214869159 hasConcept C504270822 @default.
• W4214869159 hasConceptScore W4214869159C107872376 @default.
• W4214869159 hasConceptScore W4214869159C127313418 @default.
• W4214869159 hasConceptScore W4214869159C150394285 @default.
• W4214869159 hasConceptScore W4214869159C159390177 @default.
• W4214869159 hasConceptScore W4214869159C159750122 @default.
• W4214869159 hasConceptScore W4214869159C17409809 @default.
• W4214869159 hasConceptScore W4214869159C178790620 @default.
• W4214869159 hasConceptScore W4214869159C185592680 @default.
• W4214869159 hasConceptScore W4214869159C199289684 @default.
• W4214869159 hasConceptScore W4214869159C2776386860 @default.
• W4214869159 hasConceptScore W4214869159C2777787761 @default.
• W4214869159 hasConceptScore W4214869159C2777975867 @default.
• W4214869159 hasConceptScore W4214869159C2779256693 @default.
• W4214869159 hasConceptScore W4214869159C2779899878 @default.
• W4214869159 hasConceptScore W4214869159C2780804967 @default.
• W4214869159 hasConceptScore W4214869159C40212044 @default.
• W4214869159 hasConceptScore W4214869159C40724407 @default.
• W4214869159 hasConceptScore W4214869159C504270822 @default.
• W4214869159 hasLocation W42148691591 @default.
• W4214869159 hasOpenAccess W4214869159 @default.
• W4214869159 hasPrimaryLocation W42148691591 @default.
• W4214869159 hasRelatedWork W1170235028 @default.
• W4214869159 hasRelatedWork W2022908735 @default.
• W4214869159 hasRelatedWork W2058657800 @default.
• W4214869159 hasRelatedWork W2070912856 @default.
• W4214869159 hasRelatedWork W2078383619 @default.
• W4214869159 hasRelatedWork W2087464113 @default.
• W4214869159 hasRelatedWork W2190608186 @default.
• W4214869159 hasRelatedWork W2293422472 @default.
• W4214869159 hasRelatedWork W2320106949 @default.
• W4214869159 hasRelatedWork W2774057186 @default.
• W4214869159 hasVolume "416" @default.

• next