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Grain-size and Sr–Nd isotopic compositions of dry- and wet-deposited dusts during the same dust-storm event in Harbin, China: implications for source, transport–deposition modes, dynamic mechanism and formation of eolian loess

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Abstract

A strong dust-storm event occurred in Harbin, China on May 11, 2011. The dry and wet dust deposits from this dust-storm event were examined in terms of grain-size and Sr–Nd isotopic compositions, along with scanning electron microscope. The dry-deposited dusts are characterized by bimodal grain-size distributions with fine mode of 3.6 μm and coarse mode of 28 μm, while the wet-deposited dusts are indicative of unimodal grain-size modes with a fine mode of 6 μm. These dust-storm depositions are derived from distal sources, for instance >1000 km away from dust sink spot, regardless of the occurrence of relatively coarse component with coarse mode at 28 μm for dry-deposited dusts. The Sr–Nd isotopic compositions of the dust-storm depositions are suggestive of the derivation from Horqin Sandy Land and, to a certain extent, Hunsandake Sandy Land, for both dry-deposited dust and wet-deposited dust. The fine mode (<10 μm) constituting fine tail and bimodality of grain-size distributions reflect the presence of fine particles as aggregates and/or adhering to larger grains, rather than fine grains having the derivation different from coarse grains. The fine particles may be transported and deposited by forming aggregates and/or by adhering to larger grains in low level. The fine grains are transported along with coarse grains during dust storms in spring, indicating dust storms being an important atmospheric circulation mode for the transportation of eolian dust. The fine and coarse particles in the CLP loess have the identical dust sources.

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References

  • Amit R, Enzel Y, Mushkin A, Gillespie A, Batbaatar J, Crouvi O, Vandenberghe J, An ZS (2014) Linking coarse silt production in Asian sand deserts and Quaternary accretion of the Chinese Loess Plateau. Geology 42(1):23–26

    Article  Google Scholar 

  • An Z (2000) The history and variability of the East Asian paleomonsoon climate. Quatern Sci Rev 19:171–187. doi:10.1016/S0277-3791(99)00060-8

    Article  Google Scholar 

  • An Z, Kukla GJ, Porter SC, Xiao J (1991) Magnetic susceptibility evidence of monsoon variation on the Loess Plateau of central China during the last 130,000 years. Quatern Res 36:29–36. doi:10.1016/0033-5894(91)90015-W

    Article  Google Scholar 

  • An FY, Ma HZ, Wei HC, Lai ZP (2012) Distinguishing aeolian signature from lacustrine sediments of the Qaidam Basin in northeastern Qinghai-Tibetan Plateau and its palaeoclimatic implications. Aeolian Res 4:17–30

    Article  Google Scholar 

  • Biscaye PE, Grousset PE, Revel M, Van der Gaast S, Zielinski GA, Vaars A, Kukla G (1997) Asian provenance of glacial dust (stage 2) in the GISP2 ice core, Summit, Greenland. J Geophys Res 102(C12):26765–26781

    Article  Google Scholar 

  • Che XD, Li GJ (2013) Binary sources of loess on the Chinese Loess Plateau revealed by U-Pb ages of zircon. Quatern Res 80:545–551

    Article  Google Scholar 

  • Chen LH, Miu X, Yu Z (1986) The applications of scanning electron microscope in geology. Science Press, Beijing

    Google Scholar 

  • Chen J, Li GJ, Yang JD, Rao WB, Lu HY, Balsam W, Sun YB, Ji JF (2007) Nd and Sr isotopic characteristics of Chinese deserts: implications for the provenances of Asian dust. Geochim Cosmochim Acta 71:3904–3914

    Article  Google Scholar 

  • Crouvi O, Amit R, Enzel Y, Porat N, Sandler A (2008) Sand dunes as a major proximal dust source for late Pleistocene loess in the Negev Desert, Israel. Quatern Res 70:275–282

    Article  Google Scholar 

  • Crouvi O, Amit R, Enzel Y, Gillespie AR (2010) Active sand seas and the formation of desert loess. Quatern Sci Rev 29:2087–2098

    Article  Google Scholar 

  • Crouvi O, Schepanski K, Amit R, Gillespie AR, Enzel Y (2012) Multiple dust sources in the Sahara Desert: the importance of sand dunes. Geophys Res Lett 39:L13401. doi:10.1029/2012GL052145

    Article  Google Scholar 

  • Derbyshire E, Meng XM, Kemp RA (1998) Provenance, transport and characteristics of modern aeolian dust in western Gansu Province, China, and interpretation of the Quaternary loess record. J Arid Environ 39:497–516

    Article  Google Scholar 

  • Enzel Y, Amit R, Crouvi O, Porat N (2010) Abrasion-derived sediments under intensified winds at the latest Pleistocene leading edge of the advancing Sinai–Negev erg. Quatern Res 74:121–131

    Article  Google Scholar 

  • Falkovich AH, Ganor E, Levin Z, Formenti P, Rudich Y (2001) Chemical and mineralogical analysis of individual mineral dust particles. J Geophys Res 106(D16):18029–18036

    Article  Google Scholar 

  • Feng JL, Zhu LP, Ju JT, Zhou LP, Zhen XL, Zhang W, Gao SP (2008) Heavy dust fall in Beijing, on April 16–17, 2006: geochemical properties and indications of the dust provenance. Geochem J 42:221–236

    Article  Google Scholar 

  • Gallet S, Jahn B, Torii M (1996) Geochemical characterization of the Luochuan loess paleosol sequence, China, and paleoclimatic implications. Chem Geol 133:67–88

    Article  Google Scholar 

  • Gallet S, Jahn BM, Lanoe BVV, Dia A, Rossello E (1998) Loess geochemistry and its implications for particle origin and composition of the upper continental crust. Earth Planet Sci Lett 156:157–172

    Article  Google Scholar 

  • Grousset FE, Biscaye PE (2005) Tracing dust sources and transport patterns using Sr, Nd and Pb isotopes. Chem Geol 222:149–167

    Article  Google Scholar 

  • Guo ZT, Ruddiman WF, Hao QZ, Wu HB, Qiao YS, Zhu RX, Peng SZ, Wei JJ, Yuan BY, Liu TS (2002) Onset of Asian desertification by 22 Myr ago inferred from loess deposits in China. Nature 416:159–163

    Article  Google Scholar 

  • Hao QZ, Guo ZT, Qiao YS, Xu B, Oldfield F (2010) Geochemical evidence for the provenance of middle Pleistocene loess deposits in southern China. Quatern Sci Rev 29:3317–3326

    Article  Google Scholar 

  • Honda M, Yabuki S, Shimizu H (2004) Geochemical and isotopic studies of aeolian sediments in China. Sedimentology 51(2):211–230

    Article  Google Scholar 

  • Jahn B, Gallet S, Han JM (2001) Geochemistry of the Xining, Xifeng and Jixian sections, Loess Plateau of China: eolian dust provenance and paleosol evolution during the last 140 ka. Chem Geol 178:71–94

    Article  Google Scholar 

  • Li GJ, Chen J, Ji JF, Yang JD, Conway TM (2009a) Natural and anthropogenic sources of East Asian dust. Geology 37(8):727–730. doi:10.1130/G30031A.1

    Article  Google Scholar 

  • Li XS, Han ZY, Chen YY, Cai YF, Yang DY (2009b) Characteristics and source of rain dust in Nanjing on March 11, 2006. Quatern Sci 29(1):43–54 (in Chinese with English abstract)

    Google Scholar 

  • Li GJ, Pettke T, Chen J (2011) Increasing Nd isotopic ratio of Asian dust indicates progressive uplift of the north Tibetan Plateau since the middle Miocene. Geology 39(3):199–202. doi:10.1130/G31734.1

    Article  Google Scholar 

  • Lim J, Matsumoto E (2006) Bimodal grain-size distribution of aeolian quartz in a maar of Cheju Island, Korea, during the last 6500 years: its flux variation and controlling factor. Geophys Res Lett 33:L21816. doi:10.1029/2006GL027432

    Article  Google Scholar 

  • Lim J, Matsumoto E (2008a) Fine aeolian quartz records in Cheju Island, Korea, during the last 6500 years and pathway change of the westerlies over east Asia. J Geophys Res 113:D08106. doi:10.1029/2007JD008501

    Google Scholar 

  • Lim J, Matsumoto E (2008b) Estimation of aeolian dust flux on Cheju Island, Korea, during the Mid-to Late Holocene. Quatern Int 176–177:104–111

    Article  Google Scholar 

  • Liu TS (1985) Loess and environment. China Ocean Press, Beijing

    Google Scholar 

  • Liu CQ, Masuda A, Okada A, Yabuki S, Fan ZL (1994) Isotope geochemistry of Quaternary deposits from the arid lands in northern China. Earth Planet Sci Lett 127:25–38

    Article  Google Scholar 

  • Maher BA, Mutch TJ, Cunningham D (2009) Magnetic and geochemical characteristics of Gobi Desert surface sediments: implications for provenance of the Chinese Loess Plateau. Geology 37(3):279–282. doi:10.1130/G25293A.1

    Article  Google Scholar 

  • McTainsh GH, Nickling WG, Lynch AW (1997) Dust deposition and particle size in Mali, West Africa. Catena 29:307–322

    Article  Google Scholar 

  • Porter SC (2001) Chinese loess record of monsoon climate during the last glacial-interglacial cycle. Earth Sci Rev 54:115–128. doi:10.1016/S0012-8252(01)00043-5

    Article  Google Scholar 

  • Prins MA, Vriend M, Nugteren G, Vandenberghe J, Lu HY, Zheng H, Weltje GJ (2007) Late Quaternary Aeolian dust input variability on the Chinese Loess Plateau: inferences from unmixing of loess grain-size records. Quatern Sci Rev 26:230–242

    Article  Google Scholar 

  • Pullen A, Kapp P, McCallister AT, Chang H, Gehrels GE, Garzione CN, Heermance RV, Ding L (2011) Qaidam Basin and northern Tibetan Plateau as dust sources for the Chinese Loess Plateau and paleoclimatic implications. Geology 39(11):1031–1034. doi:10.1130/G32296.1

    Article  Google Scholar 

  • Pye K (1995) The nature, origin and accumulation of loess. Quatern Sci Rev 14:653–667

    Article  Google Scholar 

  • Pye K, Zhou LP (1989) Late Pleistocene and Holocene Aeolian dust deposition in North China and the Northwest Pacific Ocean. Palaeogeogr Palaeoclimatol Palaeoecol 73:11–23

    Article  Google Scholar 

  • Qian P, Zhou LM, Zheng XM (2014) Magnetic properties of airborne particulate matter in shanghai during dust storm events and the implications for heavy metal contaminant sources. Environ Earth Sci 72:4167–4178

    Article  Google Scholar 

  • Qiang M, Lang L, Wang Z (2010) Do fine-grained components of loess indicate westerlies: insights from observations of dust storm deposits at Lenghu (Qaidam Basin, China). J Arid Environ 74:1232–1239

    Article  Google Scholar 

  • Rea DK (1994) The paleoclimatic record provided by eolian deposition in the deep sea: the geologic history of wind. Rev Geophys 32:159–195

    Article  Google Scholar 

  • Rea DK, Hovan SA (1995) Grain size distribution and depositional processes of the mineral component of abyssal sediments: lessons from the North Pacific. Paleoceanography 10(2):251–258

    Article  Google Scholar 

  • Rea DK, Leinen M, Janecek TR (1985) Geological approach to the long term history of atmospheric circulation. Science 227:721–725

    Article  Google Scholar 

  • Roe G (2009) On the interpretation of Chinese loess as a paleoclimate indicator. Quatern Res 71:150–161

    Article  Google Scholar 

  • Singer A, Ganor E, Dultz S, Fischer W (2003) Dust deposition over the Dead Sea. J Arid Environ 53:41–59

    Article  Google Scholar 

  • Sun DH (2004) Monsoon and westerly circulation changes recorded in the late Cenozoic aeolian sequences of Northern China. Glob Planet Change 41:63–80

    Article  Google Scholar 

  • Sun DH, Lu HY, Rea D, Sun YB, Wu SG (2000) Bimode grain-size distribution of Chinese loess and its paleoclimate implication. Acta Sedimentol Sin 18(3):327–335 (in Chinese with English abstract)

    Google Scholar 

  • Sun DH, An ZS, Su RX, Wu XH, Wang SM, Sun QL (2001) Mathematical approach to sedimentary component partitioning of polymodal sediments and its applications. Prog Nat Sci 11(5):374–382

    Google Scholar 

  • Sun DH, Bloemendal J, Rea DK, Vandenberghe J, Jiang FC, An ZS, Su RX (2002) Grain-size distribution function of polymodal sediments in hydraulic and aeolian environments, and numerical partitioning of the sedimentary components. Sediment Geol 152:263–277

    Article  Google Scholar 

  • Sun DH, An ZS, Su RX, Lu HY, Sun YB (2003) Eolian sedimentary records for the evolution of monsoon and westerly circulations of northern China in the last 2.6 Ma. Sci China Ser D 46(10):1049–1059

    Article  Google Scholar 

  • Sun DH, Bloemendal J, Rea DK, An ZS, Vandenberghe J, Lu HY, Su RX, Liu DS (2004) Bimodal grain-size distribution of Chinese loess, and its palaeoclimatic implications. Catena 55:325–340

    Article  Google Scholar 

  • Sun DH, Su RX, Bloemendal J, Lu HY (2008a) Grain-size and accumulation rate records from Late Cenozoic aeolian sequences in northern China: implications for variations in the East Asian winter monsoon and westerly atmospheric circulation. Paleogeogr Paleoclimatol Palaeoecol 264:39–53

    Article  Google Scholar 

  • Sun YB, Tada R, Chen J, Liu QS, Toyoda S, Tani A, Ji JF, Isozaki Y (2008b) Tracing the provenance of fine-grained dust deposited on the central Chinese Loess Plateau. Geophys Res Lett 35:L01804. doi:10.1029/2007GL031672

    Google Scholar 

  • Tsoar H, Pye K (1987) Dust transport and the question of desert loess formation. Sedimentology 34:139–153

    Article  Google Scholar 

  • Wan DJ, Mu GJ, Jin ZD, Lei JQ (2013) The effects of oasis on aeolian deposition under different weather conditions: a case study at the southern margin of the Taklimakan desert. Environ Earth Sci 68:103–114

    Article  Google Scholar 

  • Xie YY, Meng J, Guo LF (2014) REE geochemistry of modern eolian dust deposits in Harbin city, Heilongjiang province, China: implications for provenance. Catena 123:70–78

    Article  Google Scholar 

  • Yang JD, Li GJ, Rao WB, Ji JF (2009) Isotopic evidences for provenance of East Asian Dust. Atmos Environ 43:4481–4490

    Article  Google Scholar 

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Acknowledgments

This study was financially supported by the National Natural Science Foundation of China (Grant: 41471070). The authors would like to express their appreciation to Prof. Youbin Sun for his help in grain-size analysis. Thanks also go to Mrs. Mu Liu for measuring Sr and Nd isotopic composition, and to Mrs. Hong Zhang and Yuxi Xie for their assistance in sampling.

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  1. College of Geographic Science, Harbin Normal University, Harbin, 150025, China

    Yuanyun Xie, Yunping Chi, Jie Meng, Linfeng Guo & Yanru Wang

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  1. Yuanyun Xie
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Correspondence to Yuanyun Xie.

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Xie, Y., Chi, Y., Meng, J. et al. Grain-size and Sr–Nd isotopic compositions of dry- and wet-deposited dusts during the same dust-storm event in Harbin, China: implications for source, transport–deposition modes, dynamic mechanism and formation of eolian loess. Environ Earth Sci 74, 6489–6502 (2015). https://doi.org/10.1007/s12665-015-4747-2

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