Environmental Geology

, Volume 53, Issue 8, pp 1767–1775 | Cite as

The influence of dry lakebeds, degraded sandy grasslands and abandoned farmland in the arid inlands of northern China on the grain size distribution of East Asian aeolian dust

Original Article

Abstract

Dry lakes, degraded sandy grasslands, abandoned farmland and mobile dunes which are widely distributed throughout the arid areas of northern China have been investigated in this work. Gain-size distribution of the surface sediments of Manas lake in Junggar basin, Juyan lake in the Alxa plateau, Zhuye lake in Minqin basin and most deserts (such as Mu Us desert, Otindag desert, Horqin desert and Hulun Buir desert) in China have been analyzed. The results show clay with particle sized <10 μm on the surface sediments of dry lakebed and sandy grassland developed from dry lakebed, respectively, account for >60% and ∼50% of the total mass. Since the tiny particles on the surface of abandoned farmland are blown away easily and rapidly, the content of clay particles in Minqin basin is <14%. The grain-size distribution of mobile dunes in northern China mainly consists of particles >63 μm and few particles <10 μm. Consequently, although sand/dust storms originate primarily in the western deserts, the gobi areas of the Alxa plateau, the north and east of Hexi Corridor and in central Mongolia, the widely distributed dry lakebeds, sandy grasslands and abandoned farmland adjacent to the deserts also contribute to aeolian dusts. Hence, the material sources for sand dust storm in East Asia include inland deserts, but also dry lakes, sandy grasslands and abandoned farmland, which are widely distributed throughout the arid inlands of northern China.

Keywords

Dry lakebeds Sand/dust storm East Asia Grain size distribution Northern China 

References

  1. Cheng WM, Zhou CH, Li JX (2001) Evolution of Manas lake landscape in Xinjiang and its ECO-environmental effect (in Chinese). Quaternary Sci 21(6):560–565Google Scholar
  2. Chung YS, Kim HS, Dulam J, Harirs J (2003) On heavy dustfall observed with explosive sandstorm in Chongwon-Chongju, Korea in 2002. Atmos Environ 37(24):3425–3433CrossRefGoogle Scholar
  3. Darmenova K, Sokolik IN, Darmenov A (2005) Characterization of east Asian dust outbreaks in the spring of 2001 using ground-based and satellite data J Geophys Res 110(D2): D02204CrossRefGoogle Scholar
  4. Ding ZL, Sun JM, Rutter NW, Rokosh D, Liu TS (1999) Changes in sand content of loess deposits along a north–south transect of the Chinese Loess plateau and the implications for desert variations. Quaternary Res 52(1):56–62CrossRefGoogle Scholar
  5. Duce RA, Unni CK, Ray BJ, Prospero JM, Merrill JT (1980) Long-range atmospheric transport of soil dust from Asia to the tropical North Pacific: temporal variability. Science 209(4464):1522–1524CrossRefGoogle Scholar
  6. Jaffe D, Anderson T, Covert D, Kotchenruther R, Trost B, Danielson J, Simpson W, Berntsen T, et al (1999) Transport of Asian air pollution to North America. Geophys Res Lett 26(6):711–714CrossRefGoogle Scholar
  7. Kurtz AC, Derry LA, Chadwick OA (2001) Accretion of Asian dust to Hawaiian soils: isotopic, elemental, and mineral mass balances. Geochim Cosmochim Acta 12(65):1971–1983CrossRefGoogle Scholar
  8. Liu TS, Gu XF, An ZS, Fan YX (1981) The dust fall in Beijing, China on April 18,1980. Geol Soc Am Spec Pap 186:149–157Google Scholar
  9. Ma JZ, Wang XS, Edmunds WM (2005) The characteristics of ground-water resources and their changes under the impacts of human activity in the arid Northwest China—a case study of the Shiyang River basin. J Arid Environ 61(2):277–295CrossRefGoogle Scholar
  10. McKendry IG, Hacker JP, Stull R, Sakiyama S, Mignacca D, Reid K (2001) Long-range transport of Asian dust to the Lower Fraser Valley, British Columbia, Canada. J Geophys Res 106(D16):18361–18370CrossRefGoogle Scholar
  11. Sun JM, Liu TS, Lei ZF (2000) Source of heavy dust fall in Beijing, China on April 16,1998. Geogr Res Lett 27(14):2105–2108CrossRefGoogle Scholar
  12. Tsoar H, Pye K (1987) Dust transport and question of desert loess formation. Sedimentology 34(1):139–153CrossRefGoogle Scholar
  13. Wang SM, Dou HS (eds) (1998) Chinese lakes, Science Press, BeijingGoogle Scholar
  14. Wang GX, Cheng GD (1999) Water resource development and its influence on the environment in arid, areas of China—the case of the Hei River basin. J Arid Environ 43(2):121–131CrossRefGoogle Scholar
  15. Wang G, Cheng G (2000) The characteristics of water resources and the changes of the hydrological process and environment in the arid zone of northwest China. Environ Geol 39(7):783–790CrossRefGoogle Scholar
  16. Wang NA, Zhao Q, Hu G, Kan YS (2003) Climatic and humanistic background of desertification process in the recent 2000 years in Hexi Corridor (in Chinese). China J Desert Res 23(1):95–100Google Scholar
  17. Zdanowicz C, Hall G, Vaive J, Amelin Y, Percival J, Girard I, Biscaye P, Bory A (2006) Asian dustfall in the St. Elias Mountains, Yukon, Canada. Geochim Cosmochim Acta 70(14):3493–3507CrossRefGoogle Scholar
  18. Zhang XY (2001) Source distributions, emission, transport, deposition of Asian dust and loess accumulation (in Chinese). Quarternary Sci 21(1):29–40Google Scholar
  19. Zhang DE, Lu F (1999) Winter sandstorm events in extensive Northern China (in Chinese). Quaternary Sci 5:441–447Google Scholar
  20. Zhang XY, Arimoto R, An ZS (1997) Dust emission from Chinese desert sources linked to variations in atmospheric circulation. J Geophys Res 102(D23):28041–28047CrossRefGoogle Scholar
  21. Zhang J, Wu Y, Liu CL, Shen ZB, Yu ZG, Zhang Y (2001) Aerosol characters from desert region of Northwest China and the Yellow Sea in spring and summer: observations at Minqin, Qingdao, and Qianliyan in 1995–1996. Atmos Environ 35(29):5007–5018CrossRefGoogle Scholar
  22. Zhang Q, Zhao CS, Tie XX, Wei Q, Huang MY, Li GH, Ying ZM, Li CC (2006) Characterizations of aerosols over the Beijing region: a case study of aircraft measurements. Atmos Environ 40(24):4513–4527CrossRefGoogle Scholar
  23. Zhou ZJ (2001) Blowing-sand and sandstorm in China in recent 45 years (in Chinese). Quaternary Sci 21(1):9–17Google Scholar
  24. Zhou M, Okada K, Qian F, Wu PM, Su L, Casateto BE, Shimohara T (1996) Characteristics of dust-storm particles and their long-range transport from China to Japan—case studies in April 1993. Atmos Res 40(1):19–31CrossRefGoogle Scholar

Copyright information

© Springer-Verlag 2007

Authors and Affiliations

  1. 1.Institute of Geology and Geophysics, Graduate SchoolChinese Academy of SciencesBeijingChina
  2. 2.Department of GeologyNorthwest UniversityXi’anChina
  3. 3.Xi’an Institute of Geology and Mineral ResourcesChina Geological SurveyXi’anChina

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