FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2160278136> ?p ?o ?g. }

• W2160278136 endingPage "29" @default.
• W2160278136 startingPage "19" @default.
• W2160278136 abstract "Production and size of charred particles determine transport and deposition in lakes. Lack of such data is a principal obstacle to interpretation of past fire from charcoal profiles. Our two-part analysis includes a calibration study, to assess charred-particle production and transport during fire, and a study of charred particles in sediment. The calibration step establishes the magnitude and size distribution of particle accumulation from traps during a controlled burn of Pinus sylvewtris forest in west-central Siberia. This high-intensity fire consumed 3.71 kg m -2 of fuels and produced 0.0729 kg m -2 of airborne particles, for an emission factor of 0.02 kg kg -1 . Particle flux to the ground was 1 to 3 mm 2 cm -2 yr -1 inside the burn; it declined sharply within 5 m of the burn edge, and it was variable but without trend to a distance of 60 m. Particle-size distributions were conservative, with a slope of 2 on plots of log frequency versus log diameter, and sediment data suggest this slope may steepen as sources bcome more remote and as large particles are progressively lost due to settling. Deposition from the plume is similar to accumulation rates in sediment, with apparent upward bias in sediments as expected from broad geographic patterns in charcoal distributions. During the mid-Holocene charred-particle accumulation in lake sediments (10 1 mm 2 cm -2 yr -1 was greater than observed in particle traps within the experimental burn. Particles were larger, suggesting nearby sources. Rates decreased by 3800 BP to values lower than average rates in particle traps, and samples were depleted in large particles. Low rates and infrequent large particles indicate sources were distant. Accumulation rates and particle sizes were again high from 3400 to 2800 and from 1400 to 700 BP. Close correspondence between the accumulation rates during the experimental burn and in sediments and particle evidence for source area, as well as their agreement with particle-trap data from the experimental burn, suggest that, in this region, fire may have been more frequent and closer in the mid-Holocene than today. We cannot rule out the possibility, however, that changes in charred particle accumulation also reflect changes in supply of sediment to the core site." @default.
• W2160278136 created "2016-06-24" @default.
• W2160278136 creator A5006655316 @default.
• W2160278136 creator A5063550258 @default.
• W2160278136 creator A5084705730 @default.
• W2160278136 creator A5090220956 @default.
• W2160278136 date "1998-01-01" @default.
• W2160278136 modified "2023-10-16" @default.
• W2160278136 title "Relationships between charcoal particles in air and sediments in west-central Siberia" @default.
• W2160278136 cites W142745411 @default.
• W2160278136 cites W194496668 @default.
• W2160278136 cites W1966599239 @default.
• W2160278136 cites W1971890674 @default.
• W2160278136 cites W1977945389 @default.
• W2160278136 cites W1990892589 @default.
• W2160278136 cites W2002992535 @default.
• W2160278136 cites W2012186543 @default.
• W2160278136 cites W2014446516 @default.
• W2160278136 cites W2017496064 @default.
• W2160278136 cites W2022874689 @default.
• W2160278136 cites W2025776119 @default.
• W2160278136 cites W2050610996 @default.
• W2160278136 cites W2057315659 @default.
• W2160278136 cites W2067654444 @default.
• W2160278136 cites W2068701835 @default.
• W2160278136 cites W2075329931 @default.
• W2160278136 cites W2118735928 @default.
• W2160278136 cites W2121452538 @default.
• W2160278136 cites W2162159364 @default.
• W2160278136 cites W2280624662 @default.
• W2160278136 cites W313858095 @default.
• W2160278136 cites W37629021 @default.
• W2160278136 cites W4236005966 @default.
• W2160278136 cites W4246835989 @default.
• W2160278136 cites W648291773 @default.
• W2160278136 cites W993450107 @default.
• W2160278136 doi "https://doi.org/10.1191/095968398672501165" @default.
• W2160278136 hasPublicationYear "1998" @default.
• W2160278136 type Work @default.
• W2160278136 sameAs 2160278136 @default.
• W2160278136 citedByCount "262" @default.
• W2160278136 countsByYear W21602781362012 @default.
• W2160278136 countsByYear W21602781362013 @default.
• W2160278136 countsByYear W21602781362014 @default.
• W2160278136 countsByYear W21602781362015 @default.
• W2160278136 countsByYear W21602781362016 @default.
• W2160278136 countsByYear W21602781362017 @default.
• W2160278136 countsByYear W21602781362018 @default.
• W2160278136 countsByYear W21602781362019 @default.
• W2160278136 countsByYear W21602781362020 @default.
• W2160278136 countsByYear W21602781362021 @default.
• W2160278136 countsByYear W21602781362022 @default.
• W2160278136 countsByYear W21602781362023 @default.
• W2160278136 crossrefType "journal-article" @default.
• W2160278136 hasAuthorship W2160278136A5006655316 @default.
• W2160278136 hasAuthorship W2160278136A5063550258 @default.
• W2160278136 hasAuthorship W2160278136A5084705730 @default.
• W2160278136 hasAuthorship W2160278136A5090220956 @default.
• W2160278136 hasConcept C111368507 @default.
• W2160278136 hasConcept C114793014 @default.
• W2160278136 hasConcept C127313418 @default.
• W2160278136 hasConcept C151730666 @default.
• W2160278136 hasConcept C153294291 @default.
• W2160278136 hasConcept C173209714 @default.
• W2160278136 hasConcept C178790620 @default.
• W2160278136 hasConcept C185592680 @default.
• W2160278136 hasConcept C187320778 @default.
• W2160278136 hasConcept C187530423 @default.
• W2160278136 hasConcept C199289684 @default.
• W2160278136 hasConcept C205649164 @default.
• W2160278136 hasConcept C2775840915 @default.
• W2160278136 hasConcept C2778517922 @default.
• W2160278136 hasConcept C2816523 @default.
• W2160278136 hasConcept C39432304 @default.
• W2160278136 hasConcept C526406351 @default.
• W2160278136 hasConcept C60448018 @default.
• W2160278136 hasConcept C64297162 @default.
• W2160278136 hasConcept C68709404 @default.
• W2160278136 hasConcept C76886044 @default.
• W2160278136 hasConcept C87717796 @default.
• W2160278136 hasConcept C91586092 @default.
• W2160278136 hasConceptScore W2160278136C111368507 @default.
• W2160278136 hasConceptScore W2160278136C114793014 @default.
• W2160278136 hasConceptScore W2160278136C127313418 @default.
• W2160278136 hasConceptScore W2160278136C151730666 @default.
• W2160278136 hasConceptScore W2160278136C153294291 @default.
• W2160278136 hasConceptScore W2160278136C173209714 @default.
• W2160278136 hasConceptScore W2160278136C178790620 @default.
• W2160278136 hasConceptScore W2160278136C185592680 @default.
• W2160278136 hasConceptScore W2160278136C187320778 @default.
• W2160278136 hasConceptScore W2160278136C187530423 @default.
• W2160278136 hasConceptScore W2160278136C199289684 @default.
• W2160278136 hasConceptScore W2160278136C205649164 @default.
• W2160278136 hasConceptScore W2160278136C2775840915 @default.
• W2160278136 hasConceptScore W2160278136C2778517922 @default.
• W2160278136 hasConceptScore W2160278136C2816523 @default.
• W2160278136 hasConceptScore W2160278136C39432304 @default.
• W2160278136 hasConceptScore W2160278136C526406351 @default.

• next