Dynamics and Numerical Modeling of Sandy Desert Morphology Caused by Aeolian Transport of Sand Particles

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Wind caused the much sediment fluxes leading to both erosion and deposits in the sandy desertification area, and the much kind of beautiful sandy desert morphologies are formed. This is really crucial to the development of the dynamic behaviour of aeolian transport of sand particles. The sand desert morphologies are representing significant information archives for understanding the desertification problem. Dynamics and numerical modeling provides an essential tool for studying the aeolian transport of sand particle and morphology of sand desert such as ripple and dune. In this study, the mathematical models based on the dynamics are analyzed by considering the several keys as saltation, creep, suspension, avalanche and its threshold condition etc. for sand morphology forming processes. Then due to sand flow field real characteristics, the establishing process of stream flow field are analyzed, and the implication relationships as well as the coupling process between uniform stream flow field and the sand flow field are analyzed. Finally, the sand flow field models is discretized, and different kinds of sandy desert morphology are simulated by considering the sand particle size and mass in fixed, semi-fixed and free sand flow field area.

Info:

Periodical:

Key Engineering Materials (Volumes 462-463)

Edited by:

Ahmad Kamal Ariffin, Shahrum Abdullah, Aidy Ali, Andanastuti Muchtar, Mariyam Jameelah Ghazali and Zainuddin Sajuri

Pages:

1038-1043

DOI:

10.4028/www.scientific.net/KEM.462-463.1038

Citation:

X. Abdikerem et al., "Dynamics and Numerical Modeling of Sandy Desert Morphology Caused by Aeolian Transport of Sand Particles", Key Engineering Materials, Vols. 462-463, pp. 1038-1043, 2011

Online since:

January 2011

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Price:

$38.00

[1] H.J. Herrmann and G. Sauermann: Physica A. Vol, 283 (2000), p.24.

[2] R. A. Bagnold. The physics of blown sand and desert dunes. Methuen, London, (1941).

[3] K. Pye and H. Tsoar. Aeolian sand and sand dunes. Unwin Hyman, London, (1990).

DOI: 10.1007/978-94-011-5986-9_6

[4] N. Lancaster. Geomorphology of desert dunes. Routledge, London, (1995).

[5] Gerd SAUERMANN, Klaus KROY and Hans J. HERRMANN: 2iem Atelier International  Formation et Migration des Dunes , Nouakchott, ´ evrier 2001. p.7.

[6] Xamxinur Abdikerem, Zhonghua Xu and Mamtimin Geni: Advanced Materials Research Vols. 33-37 (2008) p.1055.

DOI: 10.4028/www.scientific.net/amr.33-37.1055

[7] Xamxinur Abdikerem, Akbar Eziz, AbuduKelimu Abudureheman and Mamtimin Geni: Advanced Materials Research Vols. 33-37 (2008).

DOI: 10.4028/www.scientific.net/amr.33-37.1069

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