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国家自然科学基金(41201003)

作品数:2 被引量:8H指数:2
相关作者:高艳红安志山牛清河屈建军杨根生更多>>
相关机构:中国科学院更多>>
发文基金:国家自然科学基金中国博士后科学基金国家重点基础研究发展计划更多>>
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Computational fluid dynamics evaluation of the effect of different city designs on the wind environment of a downwind natural heritage site被引量:4
2014年
Disturbance in wind regime and sand erosion deposition balance may lead to burial and eventual vanishing of a site.This study conducted 3D computational fluid dynamics(CFD)simulations to evaluate the effect of a proposed city design on the wind environment of the Crescent Spring,a downwind natural heritage site located in Dunhuang,Northwestern China.Satellite terrain data from the Advanced Spaceborne Thermal Emission and Reflection Radiometer(ASTER)Digital Elevation Model(DEM)were used to construct the solid surface model.Steady-state Reynolds Averaged Navier-Stokes equations(RANS)with shear stress transport(SST)k-ωturbulence model were then applied to solve the flow field problems.Land-use changes were modeled implicitly by dividing the underlying surface into different areas and by applying corresponding aerodynamic roughness lengths.Simulations were performed by using cases with different city areas and building heights.Results show that the selected model could capture the surface roughness changes and could adjust wind profile over a large area.Wind profiles varied over the greenfield to the north and over the Gobi land to the east of the spring.Therefore,different wind speed reduction effects were observed from various city construction scenarios.The current city design would lead to about 2 m/s of wind speed reduction at the downwind city edge and about 1 m/s of wind speed reduction at the north of the spring at 35-m height.Reducing the city height in the north greenfield area could efficiently eliminate the negative effects of wind spee.By contrast,restricting the city area worked better in the eastern Gobi area compared with other parts of the study area.Wind speed reduction in areas near the spring could be limited to 0.1 m/s by combining these two abatement strategies.The CFD method could be applied to simulate the wind environment affected by other land-use changes over a large terrain.
BenLi LIUJianJun QUQingHe NIUJunZhan WANGKeCun ZHANG
库姆塔格沙漠东部复杂地貌地表沉积物化学元素组成初步研究被引量:4
2014年
通过对库姆塔格沙漠东部的沙漠、戈壁、绿洲、湿地、干河床等地貌单元地表沉积物化学元素的分析,研究了不同类型沉积物常量、微量元素的UCC标准值、Ba-Sr含量比值、化学蚀变指数等特征。结果表明:各类型沉积物的元素特征差异显著,但都处于低等风化阶段。库姆塔格沙漠东北端的平沙地、灌丛沙地与北侧戈壁地表沉积物元素特征相近,物源是北山;沙漠东缘沙物质有相近的主元素含量和Ba-Sr含量比值,化学风化特征和Fe、Mg含量自北向南呈现渐变趋势,表明受到偏北风的搬运混合作用,其可能的物源包括南部阿尔金山洪冲积物、东侧的干河床和戈壁。沙漠与敦煌绿洲间的戈壁地带化学风化微弱,区域差异不明显,但不同部位沙物质的元素含量有近源性。鸣沙山西侧的沙物质元素不同于库姆塔格沙漠,而与之相近的党河漫滩相近,因此其最有可能的物源是党河。
柳本立屈建军杨根生牛清河安志山高艳红
关键词:库姆塔格沙漠化学元素风化
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