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dc.contributor.authorLi, Jianwu
dc.contributor.authorSong, Zhaoliang
dc.contributor.authorRuan, Li
dc.contributor.authorYang, Lihui
dc.contributor.authorVan Zwieten, Lukas
dc.contributor.authorHu, Zhongchen
dc.contributor.authorHe, Shengjia
dc.contributor.authorChenwu, Wentao
dc.contributor.authorWang, Hailong
dc.date.accessioned2020-01-03T01:07:13Z
dc.date.available2020-01-03T01:07:13Z
dc.date.issued2019
dc.identifier.issn1439-0108
dc.identifier.doi10.1007/s11368-018-2012-5
dc.identifier.urihttp://hdl.handle.net/10072/390011
dc.description.abstractPurpose: The present study was conducted to understand the pedogenesis of soils developed on basalts and reveal the impact of Asian dust on soils in subtropical China. Materials and methods: Soils developed on basalts in Xinchang-Shengzhou Basin are classified as ultisol and sampled by genetic horizon. For grain size analysis, organic matter was removed from soil samples, and then soil samples were dispersed overnight and followed by ultrasonic treatment. Grain size was measured by a Laser Grain size Analyzer. For isotopic analysis, soil samples were first dried at room temperature and then combusted at 700 °C, digested using an HNO3 + HF mixture and dissolved in a 2 N HCl solution. Sr and Nd isotopes measured on a GV Isoprobe-T thermal ionization mass spectrometer (TIMS). Results and discussion: The grain size distribution with a significantly high content of the “basic dust fraction” (10–50 μm fraction) in the upper profiles (0–40 cm) indicates atmospheric deposition onto the surface layers of soils. The patterns of the grain size frequency curves in the upper layer imply that Asian dust has a great impact on soils. The grain size parameters also reflected the influence of Eolian deposits on soils. The 87Sr/86Sr and εNd values for soils show that the near-surface horizons are substantially impacted by dust. Conclusions: The grain size, its parameters, and Sr-Nd isotopes have been marked by Eolian characteristics for the upper layers of soil, while showing a dominant basaltic signature in the lower layers. Besides parent material, accumulation of Asian dust has played an important role in pedogenesis of soils in Southeast China.
dc.description.peerreviewedYes
dc.languageEnglish
dc.publisherSpringer
dc.relation.ispartofpagefrom232
dc.relation.ispartofpageto240
dc.relation.ispartofissue1
dc.relation.ispartofjournalJournal of Soils and Sediments
dc.relation.ispartofvolume19
dc.subject.fieldofresearchEarth Sciences
dc.subject.fieldofresearchEnvironmental Sciences
dc.subject.fieldofresearchAgricultural and Veterinary Sciences
dc.subject.fieldofresearchcode04
dc.subject.fieldofresearchcode05
dc.subject.fieldofresearchcode07
dc.subject.keywordsScience & Technology
dc.subject.keywordsLife Sciences & Biomedicine
dc.subject.keywordsSoil Science
dc.subject.keywordsEnvironmental Sciences & Ecology
dc.titleThe contribution of Asian dust in the pedogenesis of ultisols in Southeastern China determined by soil grain size
dc.typeJournal article
dc.type.descriptionC1 - Articles
dcterms.bibliographicCitationLi, J; Song, Z; Ruan, L; Yang, L; Van Zwieten, L; Hu, Z; He, S; Chenwu, W; Wang, H, The contribution of Asian dust in the pedogenesis of ultisols in Southeastern China determined by soil grain size, Journal of Soils and Sediments, 2019, 19 (1), pp. 232-240
dc.date.updated2020-01-03T01:04:46Z
gro.hasfulltextNo Full Text
gro.griffith.authorVan Zwieten, Lukas


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