FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2055852911> ?p ?o ?g. }

• W2055852911 endingPage "1335" @default.
• W2055852911 startingPage "1320" @default.
• W2055852911 abstract "This study presents a Holocene sediment budget for the Valdaine Region, located at the edge of the southern French Pre-Alps. Holocene colluvial and alluvial deposition are quantified based on existing and new field data. Average sediment thickness values were calculated for different landscape units, and available chronological data were used to make a time-differentiated sediment budget. Total Holocene colluvial deposition in the Valdaine (334 km 2 ) amounts 167 × 10 6 m 3 , while alluvial deposition in the Roubion and Jabron catchments (in total 610 km 2 , including their catchment upstream the Valdaine) amounts 177 × 10 6 m 3 . Especially, colluvial deposition is high (0.75 × 10 6 g/m 2 ) compared with other catchments. Three major deposition periods (8500–2000 bc, 700 bc–ad 800 and ad 1200–2000) and two periods of relative hillslope stability with local fluvial incision (2000–700 bc and ad 800–1200) set the framework for a time-differentiated sediment budget. Results show that depositional phases relate to intense land use and hillslope stability and fluvial incision to land abandonment. Catchment averaged colluvial deposition increases from 13 × 10 −6 m 3 /m 2 /yr for 8500–2000 bc to 355 × 10 −6 m 3 /m 2 /yr for ad 1200–2000, while alluvial deposition increases from 16 to 147 × 10 −6 m 3 /m 2 /yr between the same time periods. A relationship with climatic fluctuations was not found because of the limited temporal resolution of the sediment budget. The derived sediment cascade model shows how alluvial sediments change from fine (silt and clay) to coarse (sand and gravel) after ad 1200. This went along with the establishment of a braided river pattern, indicating that the main source of sediment shifted to the mountainous headwaters. Further research including fingerprinting and modeling would be necessary to further understand the sediment budget and to more accurately quantify the different source areas and the export from the catchment." @default.
• W2055852911 created "2016-06-24" @default.
• W2055852911 creator A5023443606 @default.
• W2055852911 creator A5048926787 @default.
• W2055852911 creator A5063060710 @default.
• W2055852911 date "2014-08-14" @default.
• W2055852911 modified "2023-09-23" @default.
• W2055852911 title "Characterization and quantification of Holocene colluvial and alluvial sediments in the Valdaine Region (southern France)" @default.
• W2055852911 cites W1498592223 @default.
• W2055852911 cites W1555140092 @default.
• W2055852911 cites W1810361461 @default.
• W2055852911 cites W1964069208 @default.
• W2055852911 cites W1966937328 @default.
• W2055852911 cites W1969639156 @default.
• W2055852911 cites W1976019864 @default.
• W2055852911 cites W1979769626 @default.
• W2055852911 cites W1993858436 @default.
• W2055852911 cites W1999687518 @default.
• W2055852911 cites W2005280318 @default.
• W2055852911 cites W2008487994 @default.
• W2055852911 cites W2010889515 @default.
• W2055852911 cites W2021981486 @default.
• W2055852911 cites W2022113474 @default.
• W2055852911 cites W2028273171 @default.
• W2055852911 cites W2031095697 @default.
• W2055852911 cites W2039926974 @default.
• W2055852911 cites W2042170200 @default.
• W2055852911 cites W2043556716 @default.
• W2055852911 cites W2053643209 @default.
• W2055852911 cites W2054107324 @default.
• W2055852911 cites W2056651257 @default.
• W2055852911 cites W2057485127 @default.
• W2055852911 cites W2059094503 @default.
• W2055852911 cites W2059928953 @default.
• W2055852911 cites W2064401490 @default.
• W2055852911 cites W2069283248 @default.
• W2055852911 cites W2078901610 @default.
• W2055852911 cites W2079414175 @default.
• W2055852911 cites W2087930008 @default.
• W2055852911 cites W2088338595 @default.
• W2055852911 cites W2089889344 @default.
• W2055852911 cites W2112466769 @default.
• W2055852911 cites W2123522185 @default.
• W2055852911 cites W2126029485 @default.
• W2055852911 cites W2128804666 @default.
• W2055852911 cites W2143431615 @default.
• W2055852911 cites W2150350458 @default.
• W2055852911 cites W2151254470 @default.
• W2055852911 cites W2163706082 @default.
• W2055852911 cites W2165143671 @default.
• W2055852911 cites W3208656199 @default.
• W2055852911 cites W4238712749 @default.
• W2055852911 cites W4244508810 @default.
• W2055852911 cites W4249074704 @default.
• W2055852911 cites W4299736021 @default.
• W2055852911 doi "https://doi.org/10.1177/0959683614540946" @default.
• W2055852911 hasPublicationYear "2014" @default.
• W2055852911 type Work @default.
• W2055852911 sameAs 2055852911 @default.
• W2055852911 citedByCount "18" @default.
• W2055852911 countsByYear W20558529112014 @default.
• W2055852911 countsByYear W20558529112016 @default.
• W2055852911 countsByYear W20558529112017 @default.
• W2055852911 countsByYear W20558529112018 @default.
• W2055852911 countsByYear W20558529112019 @default.
• W2055852911 countsByYear W20558529112020 @default.
• W2055852911 countsByYear W20558529112022 @default.
• W2055852911 countsByYear W20558529112023 @default.
• W2055852911 crossrefType "journal-article" @default.
• W2055852911 hasAuthorship W2055852911A5023443606 @default.
• W2055852911 hasAuthorship W2055852911A5048926787 @default.
• W2055852911 hasAuthorship W2055852911A5063060710 @default.
• W2055852911 hasBestOaLocation W20558529115 @default.
• W2055852911 hasConcept C100970517 @default.
• W2055852911 hasConcept C109007969 @default.
• W2055852911 hasConcept C112959462 @default.
• W2055852911 hasConcept C113541313 @default.
• W2055852911 hasConcept C114793014 @default.
• W2055852911 hasConcept C126753816 @default.
• W2055852911 hasConcept C127313418 @default.
• W2055852911 hasConcept C140345934 @default.
• W2055852911 hasConcept C151730666 @default.
• W2055852911 hasConcept C17409809 @default.
• W2055852911 hasConcept C187320778 @default.
• W2055852911 hasConcept C205649164 @default.
• W2055852911 hasConcept C2816523 @default.
• W2055852911 hasConcept C32552466 @default.
• W2055852911 hasConcept C64297162 @default.
• W2055852911 hasConcept C69823785 @default.
• W2055852911 hasConcept C76886044 @default.
• W2055852911 hasConceptScore W2055852911C100970517 @default.
• W2055852911 hasConceptScore W2055852911C109007969 @default.
• W2055852911 hasConceptScore W2055852911C112959462 @default.
• W2055852911 hasConceptScore W2055852911C113541313 @default.
• W2055852911 hasConceptScore W2055852911C114793014 @default.
• W2055852911 hasConceptScore W2055852911C126753816 @default.
• W2055852911 hasConceptScore W2055852911C127313418 @default.
• W2055852911 hasConceptScore W2055852911C140345934 @default.

• next