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Grain-size distribution of surface sediments of climbing and falling dunes in the Zedang valley of the Yarlung Zangbo River, southern Tibetan plateau

  • Jiaqiong Zhang
  • Chunlai ZhangEmail author
  • Qing Li
  • Xinghui Pan
Article

Abstract

Climbing and falling dunes are widespread in the wide valleys of the middle reaches of the Yarlung Zangbo River. Along a sampling transect running from northeast to southwest through 10 climbing dunes and two falling dunes in the Langsailing area, the surface sediments were sampled to analyse the grain-size characteristics, to clarify the transport pattern of particles with different grain sizes, and to discuss the effects of terrain factors including dune slope, mountain slope, elevation and transport distance to sand transport. Sand dunes on both sides of the ridge are mainly transverse dunes. Fine and medium sands were the main particles, with few very fine and coarse particles in the surface sediments. Particles \({>}4.00\varPhi \) were blown upslope by suspension, particles \(1.00{-}4.00\varPhi \) were mainly transported upslope by saltation with opposite change tendency, and particles \({<}1.00\varPhi \) mainly moved by creep were found almost exclusively at the bottom of the slopes. As terrain factors, elevation and transport distance were more important factors influencing the distribution of grain size and particle fraction on dunes. Local winds observation might be helpful for the transport mechanism study of particles on climbing and falling dunes, while the wind data from nearby weather station was hardly helpful.

Keywords

Climbing and falling dunes grain-size distribution sand transport pattern wide river valleys terrain factors 

Notes

Acknowledgements

This work was funded by the Strategic Priority Research Program of Chinese Academy of Sciences (XDA20040202), the National Basic Research Program of China (2013CB956001) and the National Natural Science Foundation of China (40871015). The wind data used in this study was parts of data from forcing dataset developed by Data Assimilation and Modeling Center for Tibetan Multi-spheres, Institute of Tibetan Plateau Research, Chinese Academy of Sciences. Authors sincerely appreciate Dr. Geoff Hart for the language editing.

Supplementary material

12040_2018_1030_MOESM1_ESM.pdf (173 kb)
Supplementary material 1 (pdf 172 KB)

References

  1. Al-Enezi A, Pye K, Misak R and Al-Hajraf S 2008 Morphologic characteristics and development of falling dunes, northeast Kuwait; J. Arid Environ. 72(4) 423–439.CrossRefGoogle Scholar
  2. Bagnold R A 1937 The size-grading of sand by wind; Proc. Roy. Soc. London A: Math. Phys. Sci. 163(913) 250–264.CrossRefGoogle Scholar
  3. Bao K S, Jia L, Lu X G and Wang G 2010 Grain-size characteristics of sediment in Daniugou peatland in Changbai mountains, northeast China: Implications for atmospheric dust deposition; Chin. Geogr. Sci. 20(6) 498–505 (in Chinese).CrossRefGoogle Scholar
  4. Barrineau C P and Ellis J 2013 Sediment transport and wind flow around hummocks; Aeolian Res. 8 19–27.CrossRefGoogle Scholar
  5. Bullard J E and Nash D 1998 Linear dune pattern variability in the vicinity of dry valleys in the southwest Kalahari; Geomorphology 23(1) 35–54.CrossRefGoogle Scholar
  6. Chojnacki M, Moersch J E and Burr D M 2010 Climbing and falling dunes in Valles Marineris, Mars; Geophys. Res. Lett. 37 L08201.CrossRefGoogle Scholar
  7. Folk R L and Ward W C 1957 Brazos River bar, a study in the significance of grain-size parameters; J. Sedim. Res. 27(1) 3–26.CrossRefGoogle Scholar
  8. Goossens D and Offer Z Y 1997 Aeolian dust erosion on different types of hills in a rocky desert: Wind tunnel simulations and field measurements; J. Arid Environ. 37(2) 209–229.CrossRefGoogle Scholar
  9. Hayward R K, Mullins K F, Fenton L K, Hare T M, Titus N T, Bourke M C, Colaprete A and Christensen P R 2007 Mars global digital dune database and initial science results. J. Geophys. Res. 112 E11007,  https://doi.org/10.1029/2007JE002943 CrossRefGoogle Scholar
  10. Iversen J D and Rasmussen R R 1999 The effect of wind speed and bed slope on sand transport; Sedimentology 46 723–731.CrossRefGoogle Scholar
  11. Lancaster N 1995 Geomorphology of desert dunes; Routledge, London, 290p.Google Scholar
  12. Lancaster N and Tchakerian V P 1996 Geomorphology and sediments of sand ramps in the Mojave desert; Geomorphology 17(1–3) 151–165.CrossRefGoogle Scholar
  13. Lewis A D 1936 Sand dunes of the Kalahari within the borders of the Union; South Afr. Geogr. J. 19(1) 22–32.CrossRefGoogle Scholar
  14. Li S, Wang Y, Hasi, Yang P, Jin H L and Zhang J S 1997 Classification and development of aeolian sand landform in the Yarlung Zangbo valley; J. Desert Res. 17(4) 342–350 (in Chinese).Google Scholar
  15. Li S, Don G R, Shen J Y, Yang P, Liu X W, Wang Y, Jin H L and Wang Q 1999 Formation mechanisms and development pattern of aeolian sand landform in the Yarlung Zangbo river valley; Sci. China. Ser. D: Earth Sci. 42(3) 272–284.CrossRefGoogle Scholar
  16. Liu X, Li S and Shen J 1999 Wind tunnel simulation experiment of mountain dunes; J. Arid Environ. 42(1) 49–59.CrossRefGoogle Scholar
  17. Livingstone I, Bullard J E, Wiggs G F S and Thomas D S T 1999 Grain-size variation on dunes in the southwest Kalahari, southern Africa; J. Sedim. Res. 69(3) 546–552.CrossRefGoogle Scholar
  18. Loope D B, Swinehart J B and Mason J 1995 Dune-dammed palaeovalleys of the Nebraska Sand Hills: Intrinsic vs. climatic controls on the accumulation of lake and marsh sediments; Geol. Soc. Am. Bull. 107(4) 396–406.CrossRefGoogle Scholar
  19. Luo C X, Zheng Z, Zou H X, Pan A D, Fang G, Bai J J, Li J and Yang M X 2013 Palaeoenvironmental significance of grain-size distribution of river flood deposits: A study of the archaeological sites of the Apengjiang River Drainage, upper Yangtze region, Chongqing, China; J. Archaeol. Sci. 40(2) 827–840.CrossRefGoogle Scholar
  20. Pan M H, Wu Y Q, Zheng Y H and Tan L H 2014 Holocene aeolian activity in the Dinggye area (Southern Tibet, China); Aeolian Res. 12 19–27.CrossRefGoogle Scholar
  21. Pye K 1987 Aeolian dust and dust deposits; Academic Press, London.Google Scholar
  22. Rajamanickam G V and Gujar A R 1997 Grain-size studies on the nearshore sediments of Jaigad, Ambwah and Varvada Bays, Maharashtra; J. Geol. Soc. India 49(5) 567–576.Google Scholar
  23. Shao Y 2008 Physics and modelling of wind erosion; Springer, London.Google Scholar
  24. Smith B J, Wright J S and Whalley W B 1991 Simulated aeolian abrasion of Pannonian sands and its implications for the origins of Hungarian loess; Earth Surf. Process. Landforms 16(8) 745–752.CrossRefGoogle Scholar
  25. Tanaka K L, Skinner Jr J A, Hare T M, Joyal T and Wenker A 2003 Resurfacing history of the northern plains of Mars based on geologic mapping of Mars global surveyor data; J. Geophys. Res. Planet. 108(E4) 401–403.Google Scholar
  26. Tsoar H 1983 Wind tunnel modeling of echo and climbing dunes; In: Eolian sediments and processes (eds) Brookfield M E and Ahlbrandt T S, Elsevier, Amsterdam, pp. 247–259.CrossRefGoogle Scholar
  27. Tsoar H 1986 Two-dimensional analysis of dune profiles and the effect of Grain-size on sand dune morphology; In: Physics of desertification (eds) El-Baz F, Hassan M H A and Martinus Nijhof, The Hague, pp. 94–108.Google Scholar
  28. Tsoar H, White B and Berman E 1996 The effect of slopes on sand transport-numerical modeling; Landscape Urban Plan. 34(3–4) 171–181.CrossRefGoogle Scholar
  29. USDA 1951 United States Department of Agriculture (USDA) soil survey manual; U.S. Department of Agricultural Handbook No. 18, Washington DC.Google Scholar
  30. Van Der Wal D 1998 The impact of the grain-size distribution of nourishment sand on Aeolian sand transport; J. Coast. Res. 14(2) 620–631.Google Scholar
  31. Wang X M, Dong Z B, Zhang J W, Qu J J and Zhao A G 2003 Grain-size characteristics of dune sands in the central Taklimakan Sand Sea; Sedim. Geol. 161(1–2) 1–14.CrossRefGoogle Scholar
  32. Wasson R J 1984 Late Quaternary palaeoenvironments in the desert dune fields of Australia; In: Late cainozoic palaeoclimates of the southern hemisphere (ed.) Vogel J C, Balkema, Rotterdam, pp. 419–432.Google Scholar
  33. Watson A 1986 Grain-size variations on a longitudinal dune and a barchan dune; Sedim. Geol. 46 49–66.CrossRefGoogle Scholar
  34. White B and Tsoar H 1998 Slope effect on saltation over a climbing sand dune; Geomorphology 22(2) 159–180.CrossRefGoogle Scholar
  35. Zhang J Q, Zhang C L, Zhou N and Ma X J 2011 Spatial pattern of grain-size distribution in surface sediments as a result of variations in the aeolian environment in China’s Shapotou railway protective system. Aeolian Res. 3 295–302.CrossRefGoogle Scholar
  36. Zheng Y H, Wu Y Q, Li S, Tan L H, Gou S W and Zhang H Y 2009 Grain-size characteristics of sediments formed since 8600 yr BP in middle reaches of Yarlung Zangbo River in Tibet and their paleoenvironmental significance; Chin. Geogr. Sci. 19(2) 113–119 (in Chinese).CrossRefGoogle Scholar
  37. Zhou N, Zhang C L and Liu Y G 2012 Variation of grain sizes on a mountain climbing dune in Mainling wide valley, Yarlung Zangbo river; Geogr. Res. 31(1) 2–14 (in Chinese).Google Scholar
  38. Zimbelman J R and Williams S H 2007 Eolian dunes and deposits in the western United States as analogs to wind-related features on Mars; In: The geology of mars: evidence from earth-based analogs (ed.) Chapman M, Cambridge Planetary Science Series, Cambridge University Press, Washington, USA, pp. 232–257.CrossRefGoogle Scholar

Copyright information

© Indian Academy of Sciences 2018

Authors and Affiliations

  • Jiaqiong Zhang
    • 1
  • Chunlai Zhang
    • 2
    Email author
  • Qing Li
    • 2
  • Xinghui Pan
    • 3
  1. 1.State Key Laboratory of Soil Erosion and Dryland Farming on the Loess Plateau, Institute of Soil and Water ConservationNorthwest A&F UniversityYanglingPeople’s Republic of China
  2. 2.State Key Laboratory of Earth Surface Processes and Resource Ecology, MOE Engineering Research Center of Desertification and Blown-Sand Control, Faculty of Geographical ScienceBeijing Normal UniversityBeijingPeople’s Republic of China
  3. 3.Hydrology and Water Resources Survey Bureau of WeifangWeifangPeople’s Republic of China

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