FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2555782007> ?p ?o ?g. }

• W2555782007 endingPage "210" @default.
• W2555782007 startingPage "201" @default.
• W2555782007 abstract "Soil erosion, which will induce the redistribution of soil and associated soil organic carbon (SOC) on the Earth's surface, is of critically importance for biogeochemical cycling of essential elements and terrestrial carbon sequestration. Despite the importance of soil erosion, surprisingly few studies have evaluated the sources of eroded carbon (C). This study used natural abundance levels of the stable isotope signature (13C) and radioactive isotopes (137Cs and 210Pbex), along with elements ratio (C/N) based on a two end member mixing model to qualitatively and quantitatively identify the sources of sedimentary OC retained by check dam in the Qiaozigou small watershed in the Loess Plateau, China. Sediment profiles (0–200 cm) captured at natural depositional area of the basin was compared to possible source materials, which included: superficial Loess mineral soils (0–20 cm) from three land use types [i.e., grassland (Medicago sativa), forestland (Robinia pseudoacacia.), shrubland (Prunus sibirica), and gully land (Loess parent material.)]. The results demonstrated that SOC in sediments showed significantly negative correlation with pH (P < 0.01), and positive correlation with soil water content (SWC) (P < 0.05). The sedimentary OC was not derived from grasslands or gullies. Forestland and shrubland were two main sources of eroded organic carbon within the surface sediment (0–60 cm deep), except for that in the 20–40 cm soil layer. Radionuclides analyses also implied that the surface sediments retained by check-dams mainly originated from soils of forestland and shrubland. Results of the two end-member mixing model demonstrated that more than 50% SOC (mean probability estimate (MPE) 50.13% via 13C and 60.53% via C/N) in surface sediment (0–20 cm deep) derived from forestland, whereas subsurface sedimentary SOC (20–200 cm) mainly resulted from shrubland (MPE > 50%). Although uncertainties on the sources of SOC in deep soils exist, the soil organic δ13C and C/N is still an effective indicator for sources of sedimentary organic carbon in the deposition zone in the short term (<10 years)." @default.
• W2555782007 created "2016-11-30" @default.
• W2555782007 creator A5011250891 @default.
• W2555782007 creator A5022632563 @default.
• W2555782007 creator A5031043803 @default.
• W2555782007 creator A5040647242 @default.
• W2555782007 creator A5045682950 @default.
• W2555782007 creator A5074591122 @default.
• W2555782007 creator A5077794892 @default.
• W2555782007 creator A5084407437 @default.
• W2555782007 date "2017-02-01" @default.
• W2555782007 modified "2023-10-02" @default.
• W2555782007 title "Tracing the source of sedimentary organic carbon in the Loess Plateau of China: An integrated elemental ratio, stable carbon signatures, and radioactive isotopes approach" @default.
• W2555782007 cites W1124184334 @default.
• W2555782007 cites W1568554011 @default.
• W2555782007 cites W1624044426 @default.
• W2555782007 cites W1906938362 @default.
• W2555782007 cites W1965001273 @default.
• W2555782007 cites W1969593825 @default.
• W2555782007 cites W1970427282 @default.
• W2555782007 cites W1971359639 @default.
• W2555782007 cites W1972792902 @default.
• W2555782007 cites W1975302322 @default.
• W2555782007 cites W1981370070 @default.
• W2555782007 cites W1991161765 @default.
• W2555782007 cites W1993849512 @default.
• W2555782007 cites W1995673273 @default.
• W2555782007 cites W1996166331 @default.
• W2555782007 cites W1999401090 @default.
• W2555782007 cites W2000775960 @default.
• W2555782007 cites W2013651338 @default.
• W2555782007 cites W2018805647 @default.
• W2555782007 cites W2021319514 @default.
• W2555782007 cites W2024615693 @default.
• W2555782007 cites W2027244875 @default.
• W2555782007 cites W2037956243 @default.
• W2555782007 cites W2038576345 @default.
• W2555782007 cites W2039990206 @default.
• W2555782007 cites W2044930091 @default.
• W2555782007 cites W2046866959 @default.
• W2555782007 cites W2049207331 @default.
• W2555782007 cites W2055124987 @default.
• W2555782007 cites W2059122717 @default.
• W2555782007 cites W2068248597 @default.
• W2555782007 cites W2068368494 @default.
• W2555782007 cites W2073148418 @default.
• W2555782007 cites W2085869299 @default.
• W2555782007 cites W2088329813 @default.
• W2555782007 cites W2093644888 @default.
• W2555782007 cites W2098245583 @default.
• W2555782007 cites W2098836166 @default.
• W2555782007 cites W2099430001 @default.
• W2555782007 cites W2105968885 @default.
• W2555782007 cites W2107252480 @default.
• W2555782007 cites W2107325428 @default.
• W2555782007 cites W2109677123 @default.
• W2555782007 cites W2110854629 @default.
• W2555782007 cites W2113199636 @default.
• W2555782007 cites W2118070139 @default.
• W2555782007 cites W2124605197 @default.
• W2555782007 cites W2137980061 @default.
• W2555782007 cites W2149598290 @default.
• W2555782007 cites W2152151536 @default.
• W2555782007 cites W2152486065 @default.
• W2555782007 cites W2153238213 @default.
• W2555782007 cites W2157462758 @default.
• W2555782007 cites W2158700023 @default.
• W2555782007 cites W2164215496 @default.
• W2555782007 cites W2197287568 @default.
• W2555782007 cites W2234065431 @default.
• W2555782007 cites W2300904730 @default.
• W2555782007 cites W2344965000 @default.
• W2555782007 cites W2474949181 @default.
• W2555782007 cites W2521948331 @default.
• W2555782007 cites W2529756480 @default.
• W2555782007 doi "https://doi.org/10.1016/j.jenvrad.2016.10.022" @default.
• W2555782007 hasPubMedId "https://pubmed.ncbi.nlm.nih.gov/27843064" @default.
• W2555782007 hasPublicationYear "2017" @default.
• W2555782007 type Work @default.
• W2555782007 sameAs 2555782007 @default.
• W2555782007 citedByCount "14" @default.
• W2555782007 countsByYear W25557820072017 @default.
• W2555782007 countsByYear W25557820072018 @default.
• W2555782007 countsByYear W25557820072020 @default.
• W2555782007 countsByYear W25557820072022 @default.
• W2555782007 countsByYear W25557820072023 @default.
• W2555782007 crossrefType "journal-article" @default.
• W2555782007 hasAuthorship W2555782007A5011250891 @default.
• W2555782007 hasAuthorship W2555782007A5022632563 @default.
• W2555782007 hasAuthorship W2555782007A5031043803 @default.
• W2555782007 hasAuthorship W2555782007A5040647242 @default.
• W2555782007 hasAuthorship W2555782007A5045682950 @default.
• W2555782007 hasAuthorship W2555782007A5074591122 @default.
• W2555782007 hasAuthorship W2555782007A5077794892 @default.
• W2555782007 hasAuthorship W2555782007A5084407437 @default.
• W2555782007 hasConcept C107872376 @default.
• W2555782007 hasConcept C109007969 @default.
• W2555782007 hasConcept C110872660 @default.

• next