FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2616961637> ?p ?o ?g. }

• W2616961637 endingPage "39" @default.
• W2616961637 startingPage "30" @default.
• W2616961637 abstract "Water-extractable organic matter (WEOM) is the most labile, dynamic, and bioavailable fraction of soil organic matter (SOM). WEOM is a very important component of soil because it is responsible for the mobilization and translocation of many elements and pollutants in the soil environment and plays a crucial role in the biogeochemistry of carbon (C) and nitrogen (N), mineral weathering as well as pedogenesis. The main objectives of this study were: 1) to determine the quantity and chemistry of WEOM in the surface horizons of High Arctic soils under different types of tundra vegetation in the eastern part of the Fuglebergsletta coastal plain in the Hornsund area of southwestern Spitsbergen; 2) to determine relationships between quantity of WEOM and physical and chemical soil properties; and 3) to verify the hypothesis that soil surface horizons covered with different types of tundra vegetation and showing different physical and chemical properties exhibit different quantity and quality of WEOM. Soil samples (uppermost 10 cm) in six replicates from surface horizons were randomly collected at sites differing in terms of tundra vegetation type (wet moss, ornithocoprophilous, lichen-heath, polygonal). The obtained results indicate that the highest concentration of water-extractable organic carbon (WEOC) and water-extractable total nitrogen (WETN) occurs in surface horizons of soils covered with wet moss and ornithocoprophilous tundra vegetation. Soils covered with lichen-heath and polygonal tundra vegetation exhibit a markedly and significantly lower concentration of WEOC and WETN. On average, WEOC constitutes maximally up to 8.0% of total soil organic carbon (SOC) and WETN constitutes maximally up to 1.5% of total nitrogen (Ntot) content in the studied soil surface horizons. The lowest proportion of WEOC to total SOC and WETN to Ntot occurs in soils containing the highest content of SOM. On the other hand, the highest proportion of WEOC to total SOC and WETN to Ntot is present in soils characterized by the lowest content of SOM. Concentration of WEOC and WETN is highly positively and significantly correlated to the content of SOC, Ntot, total phosphorus (Ptot), and the C/N ratio as well as negatively and significantly correlated to pH and ash content. Fourier-transform infrared attenuated total reflectance (FTIR-ATR) spectra indicate clear differences in the chemistry of WEOM between the studied soils. The WEOM in the surface horizons of soils under wet moss and ornithocoprophilous tundra vegetation is characterized by a prevalence of aromatic compounds over aliphatic compounds. On the other hand, WEOM in surface horizons of soils covered with polygonal tundra vegetation exhibits a prevalence of aliphatic compounds over aromatic compounds. WEOM in surface horizons of soils under lichen-heath tundra vegetation contains an almost equal concentration of aromatic compounds and aliphatic compounds." @default.
• W2616961637 created "2017-06-05" @default.
• W2616961637 creator A5069095254 @default.
• W2616961637 date "2017-11-01" @default.
• W2616961637 modified "2023-09-25" @default.
• W2616961637 title "Quantity and chemistry of water-extractable organic matter in surface horizons of Arctic soils under different types of tundra vegetation – A case study from the Fuglebergsletta coastal plain (SW Spitsbergen)" @default.
• W2616961637 cites W1491836404 @default.
• W2616961637 cites W1521951625 @default.
• W2616961637 cites W1881036256 @default.
• W2616961637 cites W1963106668 @default.
• W2616961637 cites W1970917249 @default.
• W2616961637 cites W1975062306 @default.
• W2616961637 cites W1983072551 @default.
• W2616961637 cites W1984749404 @default.
• W2616961637 cites W1985772484 @default.
• W2616961637 cites W1989512241 @default.
• W2616961637 cites W1995548542 @default.
• W2616961637 cites W1996440470 @default.
• W2616961637 cites W2000511773 @default.
• W2616961637 cites W2004663205 @default.
• W2616961637 cites W2008065727 @default.
• W2616961637 cites W2009858984 @default.
• W2616961637 cites W2016808374 @default.
• W2616961637 cites W2018553359 @default.
• W2616961637 cites W2019765698 @default.
• W2616961637 cites W2022710326 @default.
• W2616961637 cites W2022790455 @default.
• W2616961637 cites W2024060379 @default.
• W2616961637 cites W2028817957 @default.
• W2616961637 cites W2033794830 @default.
• W2616961637 cites W2035047192 @default.
• W2616961637 cites W2041735804 @default.
• W2616961637 cites W2045491783 @default.
• W2616961637 cites W2047034635 @default.
• W2616961637 cites W2047618978 @default.
• W2616961637 cites W2053057104 @default.
• W2616961637 cites W2053467509 @default.
• W2616961637 cites W2054532641 @default.
• W2616961637 cites W2059864707 @default.
• W2616961637 cites W2062113651 @default.
• W2616961637 cites W2065742803 @default.
• W2616961637 cites W2067246725 @default.
• W2616961637 cites W2073284340 @default.
• W2616961637 cites W2074481633 @default.
• W2616961637 cites W2075155440 @default.
• W2616961637 cites W2078788590 @default.
• W2616961637 cites W2080889480 @default.
• W2616961637 cites W2086285164 @default.
• W2616961637 cites W2086730780 @default.
• W2616961637 cites W2086980364 @default.
• W2616961637 cites W2089126796 @default.
• W2616961637 cites W2089536570 @default.
• W2616961637 cites W2090963808 @default.
• W2616961637 cites W2091368907 @default.
• W2616961637 cites W2097489502 @default.
• W2616961637 cites W2112826796 @default.
• W2616961637 cites W2117350830 @default.
• W2616961637 cites W2123981120 @default.
• W2616961637 cites W2125222250 @default.
• W2616961637 cites W2129216263 @default.
• W2616961637 cites W2132615315 @default.
• W2616961637 cites W2135283895 @default.
• W2616961637 cites W2137989725 @default.
• W2616961637 cites W2139429225 @default.
• W2616961637 cites W2141693896 @default.
• W2616961637 cites W2143871414 @default.
• W2616961637 cites W2152833033 @default.
• W2616961637 cites W2156696672 @default.
• W2616961637 cites W2157238615 @default.
• W2616961637 cites W2159549065 @default.
• W2616961637 cites W2162438714 @default.
• W2616961637 cites W2163462941 @default.
• W2616961637 cites W2166121390 @default.
• W2616961637 cites W2166915931 @default.
• W2616961637 cites W2167287371 @default.
• W2616961637 cites W2168034067 @default.
• W2616961637 cites W2329835996 @default.
• W2616961637 cites W2531599245 @default.
• W2616961637 cites W2591860017 @default.
• W2616961637 cites W2611117849 @default.
• W2616961637 cites W2611311183 @default.
• W2616961637 cites W2792163418 @default.
• W2616961637 cites W3130181153 @default.
• W2616961637 cites W4243307545 @default.
• W2616961637 cites W583849962 @default.
• W2616961637 doi "https://doi.org/10.1016/j.geoderma.2017.05.038" @default.
• W2616961637 hasPublicationYear "2017" @default.
• W2616961637 type Work @default.
• W2616961637 sameAs 2616961637 @default.
• W2616961637 citedByCount "16" @default.
• W2616961637 countsByYear W26169616372018 @default.
• W2616961637 countsByYear W26169616372019 @default.
• W2616961637 countsByYear W26169616372020 @default.
• W2616961637 countsByYear W26169616372021 @default.
• W2616961637 countsByYear W26169616372022 @default.
• W2616961637 countsByYear W26169616372023 @default.
• W2616961637 crossrefType "journal-article" @default.
• W2616961637 hasAuthorship W2616961637A5069095254 @default.

• next