Abstract
Through analysis of satellite images from Google Earth, this article expounds the characteristics of large-scale geomorphic patterns of the complex longitudinal sand ridge zone in the Taklimakan Desert, and reduces the large-scale geomorphic patterns to six types: parallel pattern, “日” character-shaped and “乡” character-shaped pattern, comb-shaped pattern, fork-shaped pattern, toe-shaped pattern and miscellaneous pattern. And according to the large-scale geomorphic pattern type (or composition of pattern types) as well as some other factors, the article divides the complex longitudinal sand ridge zone into 55 subzones. Lastly, aiming at the genetic problems of the large-scale geomorphic patterns, the article suggests three connective types of the sand ridges in the complex longitudinal sand ridge zone, i.e., connecting or intersecting after natural elongation, connecting in a narrow place and connecting with the aid of intermediary.
Similar content being viewed by others
References
Tarim Oil Subsidiary of Chinese National Petroleum Company. Tarim Oil Desert Highway (in Chinese). Beijing: Petroleum Industry Press, 1996. 78–223
Li H P, Chen G T. Retrograde evolution of barchan on interdune corridor of complex ridges in central Taklimakan Desert (in Chinese). J Desert Res, 1999, 19(2): 134–138
Li H P, Chen G T, Xue D Q. Wind field over complex dune-chains and the dynamic features of the dunes overlying on the dune-chains in the hinterland of Taklimakan Desert (in Chinese). Arid Land Geogr, 2001, 24(1): 80–85
Wang X M, Dong Z B, Qu J J. Morphologic parameters of the simple transverse dunes in Taklimakan Desert (in Chinese). J Lanzhou Univ (Nat Sci), 2002, 38(6): 110–116
Zhang J W, Chen G T, Chen F H, et al. Dynamic processes of linear dunes in central Taklimakan Desert (in Chinese). J Desert Res, 1999, 19(2): 128–133
Dong Z B, Chen G T, Yan C Z, et al. The sand dune movement along the Tarim Desert Oil-transportation Highway (in Chinese). J Desert Res, 1998, 18(4): 328–333
Li Z Z, Guan Y Z, Sun Z, et al. Grain size characteristics and their distribution on longitudinal dunes in the interior of Taklimakan Desert (in Chinese). Arid Zone Res, 1996, 13(2): 37–43
Li Z Z, Guan Y Z, Sun Z, et al. Geomorphic characteristics of Barchan along the Tarim Desert Oil-transporting Highway (in Chinese). J Xinjiang Univ (Nature Science), 1998, 15(1): 80–90
Chen G T, Li Z S, Dong Z B, et al. Grain size parameters along the transection of a complex longitudinal dune in the center of Taklimakan Desert (in Chinese). J Arid Land Resour Environ, 1998, 12(1): 21–28
Li S Y, Wang D, Lei J Q. Spatial distribution of sand drift disasters on road surface in the hinterland of the Taklimakan Desert (in Chinese). Arid Land Geogr, 2005, 28(1): 93–97
Lei J Q, Wang X Q, Wang D. The formation of the blown sand disaster to the Tarim Desert Highway, Xinjiang, China (in Chinese). Arid Zone Res, 2003, 20(1): 1–6
Qian Y B, Wang X Q, Huang Q, et al. Study on blown sand hazard along the Tarim Desert Highway (in Chinese). J Arid Land Resour Environ, 2000, 14(3): 28–34
Wang X Q, Lei J Q. Relationship between the alignment of routes and degrees of wind-sand hazard in the drifting-sand region—a case study of Tarim Desert Highway (in Chinese). Arid Land Geogr, 2000, 23(3): 221–226
Wang X Q, Lei J Q, Huang Q. Study on spatial distribution of wind-sand hazard along the Tarim Desert Highway, China (in Chinese). J Desert Res, 2000, 20(4): 438–442
Wang X Q, Huang Q, Lei J Q. Sand disaster of Tarim Desert Highway crossing over the area of compound longitudinal dunes (in Chinese). Arid Zone Res, 1998, 15(3): 48–51
Wang D, Lei J Q, Xu J R, et al. Differences of blown sand disaster in the shelter system in different positions on the sand ridges along No. 1 Desert Highway in the hinterland of Taklimakan Desert (in Chinese). J Arid Land Res Environ, 2004, 18(5): 29–33
Dong Z B, Chen G T, He X D, et al. Controlling blown sand along the highway crossing the Taklimakan Desert. J Arid Environ, 2004, 57: 329–344
Wang X M, Dong Z B, Qu J J, et al. Dynamic processes of a simple linear dune—a study in the Taklimakan Sand Sea, China. Geomorphology, 2003, 52: 233–241
Wang X M, Dong Z B, Zhang J W, et al. Formation of the complex linear dunes in the central Taklimakan Sand Sea, China. Earth Surf Proc Land, 2004, 29: 677–686
Zhu Z D, Chen Z P, Wu Z, et al. Study on the Geomorphology of Wind-drift Sands in the Taklimakan Desert (in Chinese). Beijing: Science Press, 1981. 27–70
Livingstone I, Wiggs G F S, Weaver C M. Geomorphology of desert sand dunes—a review of recent progress. Earth-Sci Rev, 2007, 80: 239–257
Tsoar H, Blumberg D G, Stoler Y. Elongation and migration of sand dunes. Geomorphology, 2004, 57: 293–302
Li Z Z, Zhou Y, Luo R Y. Recent advances in aeolian geomorphology (in Chinese). Arid Zone Res, 1999, 16(2): 61–66
Qian G Q, Dong Z B, Luo W Y, et al. Wind tunnel simulation of the threshold wind velocity in the lee-side of transverse dunes (in Chinese). Arid Land Geogr, 2007, 30(1): 66–70
He D L. Problems on formation mechanism of aeolian landform (in Chinese). J Desert Res, 1985, 5(1): 33–37
Wu Z. Approach to the genesis of the Taklimakan Desert (in Chinese). Acta Geogr Sin, 1981, 36(3): 280–291
Wu Z. Geomorphology of Wind-drift Sand (in Chinese). Beijing: Science Press, 1987.127–141
Zhu Z D, Wu Z, Liu S, et al. Introduction of Desert in China (in Chinese). Beijing: Science Press, 1980. 42
Babayev A T, Glenov C K (Translated by Han Z W). Geomorphology of Desert (in Chinese). Lanzhou: Gansu Culture Press, 1998. 32–37
Author information
Authors and Affiliations
Corresponding author
Additional information
Supported by Major Orientation Foundation of the Knowledge Innovation Program of the Chinese Academy of Sciences (Grant No. KZCX3-SW-342)
About this article
Cite this article
Yue, J., Lei, J. & Mu, G. Preliminary studies on the large-scale geomorphic patterns of the complex longitudinal sand ridge zone in the Taklimakan Desert. Chin. Sci. Bull. 53 (Suppl 2), 177–189 (2008). https://doi.org/10.1007/s11434-008-6021-4
Received:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1007/s11434-008-6021-4