FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4281675819> ?p ?o ?g. }

• W4281675819 endingPage "101353" @default.
• W4281675819 startingPage "101353" @default.
• W4281675819 abstract "The sensitivity of the optically stimulated luminescence (OSL) from quartz is thought to be mainly influenced by source rock (crystallization temperature and quartz defect types) and depositional history (irradiation/bleaching cycles). In this study, the OSL sensitivity of quartz of different grain sizes from loess (L1) and paleosol (S1) layers at the Xifeng section of the Chinese Loess Plateau was analyzed. The OSL sensitivity of the samples from the Xifeng section shows a distinct difference between glacial and interglacial cycles, which is consistent with the patterns observed from magnetic susceptibility (MS) and grain sizes. The highest OSL sensitivity is observed in S1, which is twelve times the lowest sensitivity observed in L1. Moreover, the contribution of the fast component of quartz OSL from the paleosol accounts for more than 90% of the total OSL signal. In contrast, the middle and slow components contribute more in loess, and a significant variation among different aliquots was observed. Comparison of the data obtained from loess sections from different regions, including Xifeng, Luochuan, Jingyuan and Shimao, show significant differences in the magnitudes of OSL sensitivity but a similar pattern between glacial and interglacial periods. The results of this study suggest that, except for the wildfire model proposed to interpret the high OSL sensitivity in paleosol (Zhang, 2018), the shift of wind pattern of westerly wind (i.e., transporting “dim” source from North Tibetan Plateau and northwesterly wind (i.e., transporting “bright” source from Alxa Arid Lands and the subsequent mixture from the different sources may partially contribute to the different OSL sensitivities observed for Xifeng and Luochuan. In contrast, the OSL sensitivity of Shimao samples from L1 was affected by the input from the Mu Us Desert, and those of Jingyuan may affected by the contribution from the Yellow River. • The fast components of the “bright” paleosol with high OSL sensitivity accounted for more than 90%, and the differences among aliquots were slight. In contrast, the same components for “dim” loess occupied below 90%, and the difference among aliquots was significant. • The spatial changes of OSL sensitivity vary more significantly during interglacial periods than that during glacial periods. • Wind pattern likely have potential cause for the variation of quartz OSL sensitivity in CLP." @default.
• W4281675819 created "2022-06-13" @default.
• W4281675819 creator A5044989027 @default.
• W4281675819 creator A5063922467 @default.
• W4281675819 date "2022-08-01" @default.
• W4281675819 modified "2023-10-17" @default.
• W4281675819 title "Variations in the sensitivity of the optically stimulated luminescence from quartz in the Xifeng section: A spatiotemporal comparison across the Chinese Loess Plateau since the last interglaciation" @default.
• W4281675819 cites W1940405548 @default.
• W4281675819 cites W1976170009 @default.
• W4281675819 cites W1982536433 @default.
• W4281675819 cites W1988459455 @default.
• W4281675819 cites W1989229638 @default.
• W4281675819 cites W1999837643 @default.
• W4281675819 cites W2000271298 @default.
• W4281675819 cites W2002750691 @default.
• W4281675819 cites W2003069161 @default.
• W4281675819 cites W2005141551 @default.
• W4281675819 cites W2007412053 @default.
• W4281675819 cites W2008642188 @default.
• W4281675819 cites W2028802527 @default.
• W4281675819 cites W2038269904 @default.
• W4281675819 cites W2044075045 @default.
• W4281675819 cites W2045686346 @default.
• W4281675819 cites W2047171063 @default.
• W4281675819 cites W2056945332 @default.
• W4281675819 cites W2062319077 @default.
• W4281675819 cites W2067080216 @default.
• W4281675819 cites W2068151697 @default.
• W4281675819 cites W2073168135 @default.
• W4281675819 cites W2082627559 @default.
• W4281675819 cites W2091983811 @default.
• W4281675819 cites W2092677927 @default.
• W4281675819 cites W2092889986 @default.
• W4281675819 cites W2094957047 @default.
• W4281675819 cites W2102934406 @default.
• W4281675819 cites W2111590126 @default.
• W4281675819 cites W2131218079 @default.
• W4281675819 cites W2140775872 @default.
• W4281675819 cites W2141350889 @default.
• W4281675819 cites W2158679230 @default.
• W4281675819 cites W2159826862 @default.
• W4281675819 cites W2170001276 @default.
• W4281675819 cites W2593844788 @default.
• W4281675819 cites W2727801677 @default.
• W4281675819 cites W2760822346 @default.
• W4281675819 cites W2770706896 @default.
• W4281675819 cites W2799514175 @default.
• W4281675819 cites W2966706888 @default.
• W4281675819 cites W3043490130 @default.
• W4281675819 cites W574357270 @default.
• W4281675819 cites W639513051 @default.
• W4281675819 doi "https://doi.org/10.1016/j.quageo.2022.101353" @default.
• W4281675819 hasPublicationYear "2022" @default.
• W4281675819 type Work @default.
• W4281675819 citedByCount "2" @default.
• W4281675819 countsByYear W42816758192022 @default.
• W4281675819 crossrefType "journal-article" @default.
• W4281675819 hasAuthorship W4281675819A5044989027 @default.
• W4281675819 hasAuthorship W4281675819A5063922467 @default.
• W4281675819 hasConcept C112698675 @default.
• W4281675819 hasConcept C114793014 @default.
• W4281675819 hasConcept C125800877 @default.
• W4281675819 hasConcept C127313418 @default.
• W4281675819 hasConcept C134306372 @default.
• W4281675819 hasConcept C144133560 @default.
• W4281675819 hasConcept C148869448 @default.
• W4281675819 hasConcept C151730666 @default.
• W4281675819 hasConcept C159390177 @default.
• W4281675819 hasConcept C17409809 @default.
• W4281675819 hasConcept C185515318 @default.
• W4281675819 hasConcept C192562407 @default.
• W4281675819 hasConcept C199289684 @default.
• W4281675819 hasConcept C2779870107 @default.
• W4281675819 hasConcept C2780030769 @default.
• W4281675819 hasConcept C2780129039 @default.
• W4281675819 hasConcept C2993008072 @default.
• W4281675819 hasConcept C33923547 @default.
• W4281675819 hasConcept C49040817 @default.
• W4281675819 hasConceptScore W4281675819C112698675 @default.
• W4281675819 hasConceptScore W4281675819C114793014 @default.
• W4281675819 hasConceptScore W4281675819C125800877 @default.
• W4281675819 hasConceptScore W4281675819C127313418 @default.
• W4281675819 hasConceptScore W4281675819C134306372 @default.
• W4281675819 hasConceptScore W4281675819C144133560 @default.
• W4281675819 hasConceptScore W4281675819C148869448 @default.
• W4281675819 hasConceptScore W4281675819C151730666 @default.
• W4281675819 hasConceptScore W4281675819C159390177 @default.
• W4281675819 hasConceptScore W4281675819C17409809 @default.
• W4281675819 hasConceptScore W4281675819C185515318 @default.
• W4281675819 hasConceptScore W4281675819C192562407 @default.
• W4281675819 hasConceptScore W4281675819C199289684 @default.
• W4281675819 hasConceptScore W4281675819C2779870107 @default.
• W4281675819 hasConceptScore W4281675819C2780030769 @default.
• W4281675819 hasConceptScore W4281675819C2780129039 @default.
• W4281675819 hasConceptScore W4281675819C2993008072 @default.
• W4281675819 hasConceptScore W4281675819C33923547 @default.
• W4281675819 hasConceptScore W4281675819C49040817 @default.
• W4281675819 hasLocation W42816758191 @default.

• next