FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2130111932> ?p ?o ?g. }

• W2130111932 endingPage "120" @default.
• W2130111932 startingPage "107" @default.
• W2130111932 abstract "Only a few paleoecological studies have attempted to use the geochemistry of lacustrine sediments to reconstruct the history of soil genesis. The geochemical signatures of modern soils must firstly be determined before using them to investigate lake sediments. Our study explores the geochemical variability between eight subalpine soil profiles from the internal zone of the Alps to find relevant sediment tracers for present-day soils. Based on the concentrations of secondary Al- and Fe-bearing phases, as well as major element and Rare Earth Element (REE) geochemistry, different subalpine soil types can be clearly differentiated in the study area. Although formed in similar geomorphological settings, the soil typologies are diverse: Podzol group soils are developed under old-growing coniferous forest, whereas Cambisols occur under present-day old-meadows. By applying PCA including pedological and geochemical parameters, we can clearly discriminate between Podzol and Cambisol samples, revealing differences that reflect the intensity of chemical weathering. In contrast, deep and surface samples can be distinguished using the degree of physical weathering. The proportions of organic-bound Al and Fe are significantly higher in Podzols, thus providing a sediment tracer to reconstruct the intensity and degree of podzolisation. The increase of Light REE fractionation from the C-horizons to the topsoil horizons is explained in terms of soil processes. The high-field-strength element Nb is used to estimate enrichment or depletion relative to the unweathered parent material. The resulting normalized REE patterns indicate that Podzol profiles are more depleted than Cambisols. Moreover, normalized REE patterns of A- and Bw-horizons are similar in the Cambisol profiles, whereas the E- and Bs-horizons of Podzols exhibit large variations. Normalized REE patterns may thus provide a precise tracer of the degree of weathering of materials. Hence, we suggest that REE behaviour and soil weathering are clearly related. This study also highlights the effects of millennial-scale agricultural practices on soils, e.g. the eventual depodzolization related to deforestation." @default.
• W2130111932 created "2016-06-24" @default.
• W2130111932 creator A5048937990 @default.
• W2130111932 creator A5059191365 @default.
• W2130111932 creator A5062154198 @default.
• W2130111932 creator A5083070341 @default.
• W2130111932 creator A5091664857 @default.
• W2130111932 date "2008-05-01" @default.
• W2130111932 modified "2023-09-25" @default.
• W2130111932 title "Distinguishing subalpine soil types using extractible Al and Fe fractions and REE geochemistry" @default.
• W2130111932 cites W1880555926 @default.
• W2130111932 cites W1967984089 @default.
• W2130111932 cites W1971987752 @default.
• W2130111932 cites W1975583031 @default.
• W2130111932 cites W1977039791 @default.
• W2130111932 cites W1985768846 @default.
• W2130111932 cites W1995442679 @default.
• W2130111932 cites W1999490855 @default.
• W2130111932 cites W2000033372 @default.
• W2130111932 cites W2005473240 @default.
• W2130111932 cites W2015940330 @default.
• W2130111932 cites W2018441231 @default.
• W2130111932 cites W2026719342 @default.
• W2130111932 cites W2028403630 @default.
• W2130111932 cites W2029401070 @default.
• W2130111932 cites W2032973003 @default.
• W2130111932 cites W2035867807 @default.
• W2130111932 cites W2036774733 @default.
• W2130111932 cites W2037224305 @default.
• W2130111932 cites W2043246222 @default.
• W2130111932 cites W2045004755 @default.
• W2130111932 cites W2048898834 @default.
• W2130111932 cites W2056944488 @default.
• W2130111932 cites W2066592876 @default.
• W2130111932 cites W2066659554 @default.
• W2130111932 cites W2067541981 @default.
• W2130111932 cites W2071033719 @default.
• W2130111932 cites W2077140115 @default.
• W2130111932 cites W2077715404 @default.
• W2130111932 cites W2080830474 @default.
• W2130111932 cites W2082112303 @default.
• W2130111932 cites W2082746960 @default.
• W2130111932 cites W2083304964 @default.
• W2130111932 cites W2087937118 @default.
• W2130111932 cites W2104573843 @default.
• W2130111932 cites W2105999179 @default.
• W2130111932 cites W2108400950 @default.
• W2130111932 cites W2110001507 @default.
• W2130111932 cites W2114268272 @default.
• W2130111932 cites W2155276151 @default.
• W2130111932 cites W2158724055 @default.
• W2130111932 cites W2160657028 @default.
• W2130111932 cites W2168745915 @default.
• W2130111932 cites W2169964073 @default.
• W2130111932 cites W2325621822 @default.
• W2130111932 doi "https://doi.org/10.1016/j.geoderma.2008.03.001" @default.
• W2130111932 hasPublicationYear "2008" @default.
• W2130111932 type Work @default.
• W2130111932 sameAs 2130111932 @default.
• W2130111932 citedByCount "36" @default.
• W2130111932 countsByYear W21301119322013 @default.
• W2130111932 countsByYear W21301119322014 @default.
• W2130111932 countsByYear W21301119322015 @default.
• W2130111932 countsByYear W21301119322016 @default.
• W2130111932 countsByYear W21301119322017 @default.
• W2130111932 countsByYear W21301119322018 @default.
• W2130111932 countsByYear W21301119322019 @default.
• W2130111932 countsByYear W21301119322020 @default.
• W2130111932 countsByYear W21301119322021 @default.
• W2130111932 countsByYear W21301119322022 @default.
• W2130111932 crossrefType "journal-article" @default.
• W2130111932 hasAuthorship W2130111932A5048937990 @default.
• W2130111932 hasAuthorship W2130111932A5059191365 @default.
• W2130111932 hasAuthorship W2130111932A5062154198 @default.
• W2130111932 hasAuthorship W2130111932A5083070341 @default.
• W2130111932 hasAuthorship W2130111932A5091664857 @default.
• W2130111932 hasConcept C114793014 @default.
• W2130111932 hasConcept C127313418 @default.
• W2130111932 hasConcept C142535954 @default.
• W2130111932 hasConcept C156634047 @default.
• W2130111932 hasConcept C159390177 @default.
• W2130111932 hasConcept C159750122 @default.
• W2130111932 hasConcept C17409809 @default.
• W2130111932 hasConcept C177921069 @default.
• W2130111932 hasConcept C199289684 @default.
• W2130111932 hasConcept C20529654 @default.
• W2130111932 hasConcept C2776501588 @default.
• W2130111932 hasConcept C2816523 @default.
• W2130111932 hasConcept C40724407 @default.
• W2130111932 hasConceptScore W2130111932C114793014 @default.
• W2130111932 hasConceptScore W2130111932C127313418 @default.
• W2130111932 hasConceptScore W2130111932C142535954 @default.
• W2130111932 hasConceptScore W2130111932C156634047 @default.
• W2130111932 hasConceptScore W2130111932C159390177 @default.
• W2130111932 hasConceptScore W2130111932C159750122 @default.
• W2130111932 hasConceptScore W2130111932C17409809 @default.
• W2130111932 hasConceptScore W2130111932C177921069 @default.
• W2130111932 hasConceptScore W2130111932C199289684 @default.

• next