FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2800774557> ?p ?o ?g. }

• W2800774557 abstract "A large quantity of radionuclides was released by the Fukushima Daiichi Nuclear Power Plant accident in March 2011, and those deposited on ground and vegetation could return to the atmosphere through resuspension processes. Although the resuspension has been proposed to occur with wind blow, biomass burning, ecosystem activities, etc., the dominant process in contaminated areas of Fukushima is not fully understood. We have examined the resuspension process of radiocesium (134,137Cs) based on long-term measurements of the atmospheric concentration of radiocesium activity (the radiocesium concentration) at four sites in the contaminated areas of Fukushima as well as the aerosol characteristic observations by scanning electron microscopy (SEM) and the measurement of the biomass burning tracer, levoglucosan. The radiocesium concentrations at all sites showed a similar seasonal variation: low from winter to early spring and high from late spring to early autumn. In late spring, they showed positive peaks that coincided with the wind speed peaks. However, in summer and autumn, they were correlated positively with atmospheric temperature but negatively with wind speed. These results differed from previous studies based on data at urban sites. The difference of radiocesium concentrations at two sites, which are located within a 1 km range but have different degrees of surface contamination, was large from winter to late spring and small in summer and autumn, indicating that resuspension occurs locally and/or that atmospheric radiocesium was not well mixed in winter/spring, and it was opposite in summer/autumn. These results suggest that the resuspension processes and the host particles of the radiocesium resuspension changed seasonally. The SEM analyses showed that the dominant coarse particles in summer and autumn were organic ones, such as pollen, spores, and microorganisms. Biological activities in forest ecosystems can contribute considerably to the radiocesium resuspension in these seasons. During winter and spring, soil, mineral, and vegetation debris were predominant coarse particles in the atmosphere, and the radiocesium resuspension in these seasons can be attributed to the wind blow of these particles. Any proofs that biomass burning had a significant impact on atmospheric radiocesium were not found in the present study." @default.
• W2800774557 created "2018-05-17" @default.
• W2800774557 creator A5008105817 @default.
• W2800774557 creator A5010993723 @default.
• W2800774557 creator A5018793104 @default.
• W2800774557 creator A5019135274 @default.
• W2800774557 creator A5033775542 @default.
• W2800774557 creator A5033871406 @default.
• W2800774557 creator A5034789926 @default.
• W2800774557 creator A5038396489 @default.
• W2800774557 creator A5038988063 @default.
• W2800774557 creator A5050044217 @default.
• W2800774557 creator A5058957688 @default.
• W2800774557 creator A5063436868 @default.
• W2800774557 creator A5064120942 @default.
• W2800774557 creator A5072388358 @default.
• W2800774557 creator A5084363059 @default.
• W2800774557 creator A5091071434 @default.
• W2800774557 date "2018-02-21" @default.
• W2800774557 modified "2023-10-18" @default.
• W2800774557 title "The seasonal variations of atmospheric 134,137Cs activity and possible host particles for their resuspension in the contaminated areas of Tsushima and Yamakiya, Fukushima, Japan" @default.
• W2800774557 cites W1485504984 @default.
• W2800774557 cites W1522196755 @default.
• W2800774557 cites W1964997230 @default.
• W2800774557 cites W1970401438 @default.
• W2800774557 cites W1986390324 @default.
• W2800774557 cites W1990019715 @default.
• W2800774557 cites W1990928167 @default.
• W2800774557 cites W2001372136 @default.
• W2800774557 cites W2007233299 @default.
• W2800774557 cites W2008877782 @default.
• W2800774557 cites W2013501942 @default.
• W2800774557 cites W2016441857 @default.
• W2800774557 cites W2017054490 @default.
• W2800774557 cites W2029804172 @default.
• W2800774557 cites W2032968004 @default.
• W2800774557 cites W2035037319 @default.
• W2800774557 cites W2035929537 @default.
• W2800774557 cites W2036289626 @default.
• W2800774557 cites W2038299205 @default.
• W2800774557 cites W2038363137 @default.
• W2800774557 cites W2043333771 @default.
• W2800774557 cites W2061809412 @default.
• W2800774557 cites W2069138454 @default.
• W2800774557 cites W2071202569 @default.
• W2800774557 cites W2087001557 @default.
• W2800774557 cites W2098816487 @default.
• W2800774557 cites W2105845169 @default.
• W2800774557 cites W2109886685 @default.
• W2800774557 cites W2110344328 @default.
• W2800774557 cites W2136291104 @default.
• W2800774557 cites W2155096269 @default.
• W2800774557 cites W2193068715 @default.
• W2800774557 cites W2260114138 @default.
• W2800774557 cites W2282969430 @default.
• W2800774557 cites W2318973710 @default.
• W2800774557 cites W2328681145 @default.
• W2800774557 cites W2332926040 @default.
• W2800774557 cites W2334286555 @default.
• W2800774557 cites W2344156302 @default.
• W2800774557 cites W2365025274 @default.
• W2800774557 cites W2528251355 @default.
• W2800774557 cites W4239430066 @default.
• W2800774557 doi "https://doi.org/10.1186/s40645-018-0171-z" @default.
• W2800774557 hasPublicationYear "2018" @default.
• W2800774557 type Work @default.
• W2800774557 sameAs 2800774557 @default.
• W2800774557 citedByCount "27" @default.
• W2800774557 countsByYear W28007745572018 @default.
• W2800774557 countsByYear W28007745572019 @default.
• W2800774557 countsByYear W28007745572020 @default.
• W2800774557 countsByYear W28007745572021 @default.
• W2800774557 countsByYear W28007745572022 @default.
• W2800774557 countsByYear W28007745572023 @default.
• W2800774557 crossrefType "journal-article" @default.
• W2800774557 hasAuthorship W2800774557A5008105817 @default.
• W2800774557 hasAuthorship W2800774557A5010993723 @default.
• W2800774557 hasAuthorship W2800774557A5018793104 @default.
• W2800774557 hasAuthorship W2800774557A5019135274 @default.
• W2800774557 hasAuthorship W2800774557A5033775542 @default.
• W2800774557 hasAuthorship W2800774557A5033871406 @default.
• W2800774557 hasAuthorship W2800774557A5034789926 @default.
• W2800774557 hasAuthorship W2800774557A5038396489 @default.
• W2800774557 hasAuthorship W2800774557A5038988063 @default.
• W2800774557 hasAuthorship W2800774557A5050044217 @default.
• W2800774557 hasAuthorship W2800774557A5058957688 @default.
• W2800774557 hasAuthorship W2800774557A5063436868 @default.
• W2800774557 hasAuthorship W2800774557A5064120942 @default.
• W2800774557 hasAuthorship W2800774557A5072388358 @default.
• W2800774557 hasAuthorship W2800774557A5084363059 @default.
• W2800774557 hasAuthorship W2800774557A5091071434 @default.
• W2800774557 hasBestOaLocation W28007745571 @default.
• W2800774557 hasConcept C107054158 @default.
• W2800774557 hasConcept C107872376 @default.
• W2800774557 hasConcept C112570922 @default.
• W2800774557 hasConcept C121332964 @default.
• W2800774557 hasConcept C125403950 @default.
• W2800774557 hasConcept C127313418 @default.
• W2800774557 hasConcept C127413603 @default.
• W2800774557 hasConcept C153294291 @default.

• next