FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1994282316> ?p ?o ?g. }

• W1994282316 endingPage "2943" @default.
• W1994282316 startingPage "2934" @default.
• W1994282316 abstract "In the grassland/forest ecotone of North America, many areas are experiencing afforestation and subsequent shifts in ecosystem carbon (C) stocks. Ecosystem scientists commonly employ a suite of techniques to examine how such land use changes can impact soil organic matter (SOM) forms and dynamics. This study employs four such techniques to compare SOM in grassland (Bromus inermis) and recently forested (∼35 year, Ulmus spp. and Quercus spp.) sites with similar soil types and long-term histories in Kansas, USA. The work examines C and nitrogen (N) parameters in labile and recalcitrant SOM fractions isolated via size and density fractionation, acid hydrolysis, and long-term incubations. Size fractionation highlighted differences between grassland and forested areas. N concentration of forested soils’ 63–212 μm fraction was higher than corresponding grassland soils’ values (3.0±0.3 vs. 2.3±0.3 mg gfraction−1, P<0.05), and N concentration of grassland soils’ 212–2000 μm fraction was higher than forested soils (3.0±0.4 vs. 2.3±0.2 mg gfraction−1, P<0.05). Similar trends were observed for these same fractions for C concentration; forested soils exhibited 1.3 times the C concentration in the 63–212 μm fraction compared to this fraction in grassland soils. Fractions separated via density separation and acid hydrolysis exhibited no differences in [C], [N], δ15N, or δ13C when compared across land use types. Plant litterfall from forested sites possessed significantly greater N concentrations than that from grassland sites (12.41±0.10 vs. 11.62±0.19 mg glitter−1). Long-term incubations revealed no differences in C or N dynamics between grassland and forested soils. δ13C and δ15N values of the smallest size and the heavier density fractions, likely representing older and more recalcitrant SOM, were enriched compared to younger and more labile SOM fractions; δ15N of forested soils’ 212–2000 μm fraction were higher than corresponding grassland soils (1.7±0.3‰ vs. 0.5±0.4‰). δ13C values of acid hydrolysis fractions likely reflect preferential losses of 13C-depleted compounds during hydrolysis. Though C and N data from size fractions were most effective at exhibiting differences between grassland and forested soils, no technique conclusively indicates consistent changes in SOM dynamics with forest growth on these soils. The study also highlights some of the challenges associated with describing SOM parameters, particularly δ13C, in SOM fractions isolated by acid hydrolysis." @default.
• W1994282316 created "2016-06-24" @default.
• W1994282316 creator A5074707367 @default.
• W1994282316 date "2006-09-01" @default.
• W1994282316 modified "2023-09-26" @default.
• W1994282316 title "Soil organic matter dynamics and land use change at a grassland/forest ecotone" @default.
• W1994282316 cites W140645639 @default.
• W1994282316 cites W1497615079 @default.
• W1994282316 cites W1579893055 @default.
• W1994282316 cites W1630902002 @default.
• W1994282316 cites W1773377806 @default.
• W1994282316 cites W1876752304 @default.
• W1994282316 cites W1935089707 @default.
• W1994282316 cites W1965578568 @default.
• W1994282316 cites W1970527729 @default.
• W1994282316 cites W1972824616 @default.
• W1994282316 cites W1978167707 @default.
• W1994282316 cites W1993152985 @default.
• W1994282316 cites W2004977609 @default.
• W1994282316 cites W2006371148 @default.
• W1994282316 cites W2006776514 @default.
• W1994282316 cites W2018471645 @default.
• W1994282316 cites W2019159344 @default.
• W1994282316 cites W2026649473 @default.
• W1994282316 cites W2028544257 @default.
• W1994282316 cites W2056533180 @default.
• W1994282316 cites W2066074198 @default.
• W1994282316 cites W2067264556 @default.
• W1994282316 cites W2070608792 @default.
• W1994282316 cites W2089328440 @default.
• W1994282316 cites W2091479940 @default.
• W1994282316 cites W2104151044 @default.
• W1994282316 cites W2109677123 @default.
• W1994282316 cites W2113057981 @default.
• W1994282316 cites W2125632305 @default.
• W1994282316 cites W2147716564 @default.
• W1994282316 cites W2159549625 @default.
• W1994282316 cites W2166694299 @default.
• W1994282316 cites W2166885058 @default.
• W1994282316 cites W2169825978 @default.
• W1994282316 cites W229434232 @default.
• W1994282316 cites W2329526992 @default.
• W1994282316 cites W29999919 @default.
• W1994282316 cites W3167916584 @default.
• W1994282316 cites W37735639 @default.
• W1994282316 cites W584984737 @default.
• W1994282316 cites W623623931 @default.
• W1994282316 cites W2001575946 @default.
• W1994282316 cites W2053005579 @default.
• W1994282316 doi "https://doi.org/10.1016/j.soilbio.2006.05.004" @default.
• W1994282316 hasPublicationYear "2006" @default.
• W1994282316 type Work @default.
• W1994282316 sameAs 1994282316 @default.
• W1994282316 citedByCount "67" @default.
• W1994282316 countsByYear W19942823162012 @default.
• W1994282316 countsByYear W19942823162013 @default.
• W1994282316 countsByYear W19942823162014 @default.
• W1994282316 countsByYear W19942823162015 @default.
• W1994282316 countsByYear W19942823162016 @default.
• W1994282316 countsByYear W19942823162017 @default.
• W1994282316 countsByYear W19942823162018 @default.
• W1994282316 countsByYear W19942823162019 @default.
• W1994282316 countsByYear W19942823162020 @default.
• W1994282316 countsByYear W19942823162021 @default.
• W1994282316 countsByYear W19942823162022 @default.
• W1994282316 countsByYear W19942823162023 @default.
• W1994282316 crossrefType "journal-article" @default.
• W1994282316 hasAuthorship W1994282316A5074707367 @default.
• W1994282316 hasConcept C110872660 @default.
• W1994282316 hasConcept C159390177 @default.
• W1994282316 hasConcept C159750122 @default.
• W1994282316 hasConcept C178790620 @default.
• W1994282316 hasConcept C182124840 @default.
• W1994282316 hasConcept C185592680 @default.
• W1994282316 hasConcept C18903297 @default.
• W1994282316 hasConcept C199877563 @default.
• W1994282316 hasConcept C2775835988 @default.
• W1994282316 hasConcept C2778091200 @default.
• W1994282316 hasConcept C39432304 @default.
• W1994282316 hasConcept C39464130 @default.
• W1994282316 hasConcept C48743137 @default.
• W1994282316 hasConcept C6557445 @default.
• W1994282316 hasConcept C86803240 @default.
• W1994282316 hasConcept C97428945 @default.
• W1994282316 hasConceptScore W1994282316C110872660 @default.
• W1994282316 hasConceptScore W1994282316C159390177 @default.
• W1994282316 hasConceptScore W1994282316C159750122 @default.
• W1994282316 hasConceptScore W1994282316C178790620 @default.
• W1994282316 hasConceptScore W1994282316C182124840 @default.
• W1994282316 hasConceptScore W1994282316C185592680 @default.
• W1994282316 hasConceptScore W1994282316C18903297 @default.
• W1994282316 hasConceptScore W1994282316C199877563 @default.
• W1994282316 hasConceptScore W1994282316C2775835988 @default.
• W1994282316 hasConceptScore W1994282316C2778091200 @default.
• W1994282316 hasConceptScore W1994282316C39432304 @default.
• W1994282316 hasConceptScore W1994282316C39464130 @default.
• W1994282316 hasConceptScore W1994282316C48743137 @default.
• W1994282316 hasConceptScore W1994282316C6557445 @default.

• next