Movement of a small slipfaceless dome dune in the Namib Sand Sea, Namibia

被引:35
作者
Bristow, CS
Lancaster, N
机构
[1] Univ London Birkbeck Coll, Sch Earth Sci, London WC1E 7HX, England
[2] Desert Res Inst, Reno, NV USA
关键词
sand transport; dune migration; Namib Sand Sea; dome dune;
D O I
10.1016/j.geomorph.2003.09.015
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
The migration of a small slipfaceless dome dune close to the northern edge of the Namib Sand Sea has been measured by topographic survey. The dune dimensions are 45-m wide and 1-m high with a volume of 551 m(3) that has been calculated as the difference between the dune's surface elevation and an interdune surface extrapolated from measurements around the edge of the dune. The migration direction, 64degrees, and distance moved, 90 m, are measured against stakes set out in 1976. The dune has moved about 90 m between 1976 and 1999. This is an average linear migration rate of around 4 m year, and is equivalent to an annual sand transport rate of about 1.2 tonnes m(-1) year(-1). The calculated total potential sand flow in this part of the Namib Desert is 119 tonnes m(-1) year(-1), and the resultant potential sand flow is 63 tonnes m(-1) year(-1). The dune migration is therefore about 1% of the total potential sandflow and 2% of the resultant indicating that dune migration is only a small part of total potential sand transport. The results suggest that small slipfaceless dome dunes are very inefficient at trapping sand, and that winds blowing across the interdune in this area are undersaturated with sand. (C) 2003 Elsevier B.V. All rights reserved.
引用
收藏
页码:189 / 196
页数:8
相关论文
共 12 条
[1]  
[Anonymous], 1941, PHYS BLOWN SAND DESE
[2]  
[Anonymous], 1974, GEOL RUNDSCH, DOI DOI 10.1007/BF01821323
[3]  
Besler H., 1975, WURZBURGER GEOGRAPHI, V43, P135
[4]  
Besler H., 1980, STUTTGARTER GEOGRAPH, V96
[5]   The sedimentary structure of linear sand dunes [J].
Bristow, CS ;
Bailey, SD ;
Lancaster, N .
NATURE, 2000, 406 (6791) :56-59
[6]  
Cooke R.U., 1993, DESERT GEOMORPHOLOGY, DOI 10.1016/0013-7952(93)90027-a
[7]   WINDS AND SAND MOVEMENTS IN THE NAMIB SAND SEA [J].
LANCASTER, N .
EARTH SURFACE PROCESSES AND LANDFORMS, 1985, 10 (06) :607-619
[8]  
Lancaster N., 1983, EOLIAN SEDIMENTS PRO, P261
[9]   MONITORING SURFACE CHANGE ON A NAMIB LINEAR DUNE [J].
LIVINGSTONE, I .
EARTH SURFACE PROCESSES AND LANDFORMS, 1989, 14 (04) :317-332
[10]  
MCKEE ED, 1979, 188 GEOL SOC AM, P64