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南京大学海岸与海岛开发国家试点实验室,新疆师范大学地理系,中国科学院兰州沙漠研究所
Published:1998
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[1]李志忠,关有志,孙忠,陈广庭.塔里木沙漠石油公路沿线新月形沙丘的地貌特征[J].新疆大学学报(自然科学版),1998(01).
李志忠, 关有志, 孙忠, et al. 塔里木沙漠石油公路沿线新月形沙丘的地貌特征[J]. Journal of Xinjiang University (Natural Science Edition in Chinese and English), 1998, (1).
新月形沙丘是塔里木沙漠石油公路沿线分布最广泛的沙丘类型,也是对公路造成沙害的主要沙丘类型.本文探讨了公路沿线新月形沙丘的形态特征、粒度分布和运动规律.研究表明,公路沿线新月形沙丘的空间尺度较小,沙丘高度、背风坡长和迎风坡长三者之间的相关性较好;表层沙样的平均粒径由迎风坡到背风坡变细,而分选性在沙丘各部位的差别不大;所有沙丘均朝SW方向迁移,与公路沿线年合成风向一致,沙丘平均迁移速度为6~8米/年.
Barchans are not only the most widespread dune type but also the main cause of blown-sand disaster along Tarim Desert Oil-transporting Highway in the southern of Xinjiang
China.We inquiered into the morphological feature
grain-size distribution and moving law of the barchans along the Highway in this paper.The results can be concluded as follows. 1)The dimension of the barchans along the Highway is smaller than that of barchans in other deserts over the world
which has relation to little saturated sand flow
development on short time and narrow moving space existed both sides of most the Highway.We fornd that there are good relations among dune height (H)
leeward slope length (Lb) and windward slope length (Ly).And
these relations are almost no difference during the dune migration. 2)The analysis of trend surface of grain texture parameters on the surface of the dune revealed that values of mean grain-size (Md) is accorded with the model of puadratic trend-surface
and that of standard deviation(δ 1)with that of puartic trend-surface.That is
the sand grain-size on the surface of the dune become finer from windward slope to leeward slope
and sorting degree on the whole surface of the dunes are about the same.In a word
distrebution of grain texture paramters has relation to relative transporting energy of wind on the surface of the dune
and to background of sand source where dunes are located. 3)All the barchans are moving in the same direction as SW
which coincide with the direction of NE compound wind recorded by the weather station nearby the Highway. The mean moving velocity of the barcchans is about 6-8m/year.But
there are some changes in the velocity under the influence of dune height
compound shape as well as ground conditions.
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