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高寒沙地地表风沙沉积物粒度特征的时空变化

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本文拟以青海湖流域湖东沙地不同恢复年限的沙丘为研究对象,通过分析风沙沉积物在不同沙丘地貌部位的粒度分布特征,探讨治沙措施影响下风沙流携沙粒度的时空变化规律.结果表明:(1)流动沙丘表层沉积物粗粒物质较多,自然固定沙丘、不同年份建植沙棘沙丘表层沉积物则以细砂为主.(2)流动沙丘迎风坡细粒含量最高,而植被覆盖沙丘背风坡与坡顶风沙沉积物的细粒物质含量高于迎风坡,这与本区的风况密切相关.(3)随着沙丘植被条件的转好,平均粒径不断减小;分选系数逐渐增大;偏度逐渐向正偏靠拢;沙丘峰态均属于中等峰态;分形维数变化无规律.总体而言,沙丘恢复年限越长对沉积物粒径影响越大.
Spatiotemporal Variation of Particle Size Characteristics of Surface Aeolian Sediments in Alpine Desert
In this paper,we plan to study the dunes with different recovery years of sand land in the east of sand land,and discuss the spatial and temporal change law of sand flow under the influence of sand control meas-ures,by analyzing the particle size distribution characteristics of wind sand sediments in different sand dune land-forms.The results showed that:(1)there were more coarse-grained substances in the surface sediments of mobile sand dunes,while the surface sediments of naturally fixed sand dunes and seabuckthorn sand dunes planted in dif-ferent years were mainly fine sand.(2)The windward slope of mobile sand dunes had the highest content of fine particles,while the vegetation covered sand dunes had a higher content of fine particles in the windward slope and top sand sediment than in the windward slope,which was closely related to the wind conditions in this area.(3)With the improvement of vegetation conditions in sand dunes,the average particle size continued to decrease;The sorting coefficient gradually increased;The skewness gradually approached the positive skewness;The peak shape of sand dunes belonged to the moderate peak shape;The fractal dimension changed irregularly.Overall,the longer the restoration period of sand dunes,the greater the impact on sediment particle size.

Sand sedimentParticle size parameterVegetation restorationFractal dimension

金耀涛、田丽慧、张登山、李耀、陈冬冬、刘蕊娜

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青海大学省部共建三江源生态与高原农牧业国家重点实验室,青海 西宁 810016

风沙沉积物 粒度参数 植被恢复 分形维数

2024

青海农林科技
青海省农林科学院 青海省林学会 青海省农学会

青海农林科技

影响因子:0.183
ISSN:1004-9967
年,卷(期):2024.(4)