1、

Centrifuge Modeling Test to Working Mechanism of Reinforced Aeolian Sand Retaining Wall

加筋风积沙挡墙工作机理的离心模型试验

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2、

Types of lakes: tectonic lake, crater lake, fluvial lake, dammed lake, glacier lake, karst lake, Aeolian lake, impact crater lake and artificial lake.

湖泊分类:构造湖、火山口湖、冲积残留湖、堰塞湖、冰川湖、喀斯特湖、风成湖、陨石撞击湖和人工湖。

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3、

Characteristics of Grain Size Parameters of Modern Coastal Aeolian Sands in Temperate Coastal Region in China

海岸现代风成砂粒度参数特征的研究&以中国温带海岸为例

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4、

Progress in aeolian sand ripple research& A review

风成沙纹的研究进展

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5、

Analysis of Lift-off Sand Particles Spin in Aeolian Saltation

沙粒起跳自旋的分析

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6、

Large-eddy Simulation of Three Dimensional Turbulent Aeolian Motion and Numerical Simulation of Evolution of Sand Ripples; Uplift and erosion at last produced the desert landscape we see today.

三维湍流风沙运动的大涡模拟及沙漠地貌的数值模拟最后,地表抬升和侵蚀作用产生了我们今日所见的沙漠风貌。

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7、

Research Achievements in Aeolian Physics in China for the Last Five Decades(ⅰ)

中国风沙物理研究五十年(Ⅰ)

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8、

Ever since the Miocene time, aeolian dust has been falling down over Northwestern China, forming the Loess Plateau.

中国西北地区,从中新世以来就有持续不断的风尘沉积。

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9、

As a result, the reason of having two peak value in the aeolian sand tamping curve is that aeolian sand is not a sticky material; it is also the reason that the aeolian sand granule has special movement rule while impacting.

结果表明:风积沙无粘性是导致其压实曲线呈双峰值的原因,也是其颗粒在压实时有着特殊运动规律的原因。

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10、

This paper studies physical and mechanical property of Aeolian soil, and puts forward a variety of Aeolian soil improvement programs, then analyzes the programs.

本文系统的研究了风积土的物理力学性质,提出了风积土的多种改良方案,并进行分析比较,进而探讨了改良方案在工程中的实际应用。

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11、

Luohe formation mainly develops aeolian deposit, alluvial fan and braided deposit.

洛河组主要发育风成沉积、冲(洪)积扇、辫状河沉积;

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12、

A research of aeolian landform in northern China based on remote sensing imagery;

以往关于库姆塔格沙漠风沙地貌的认识主要基于遥感影像判读。

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13、

Problems on Formation Mechanism of Aeolian Landform

风沙地貌形成机制的几个问题

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14、

Division of Aeolian Landform Configuration in Northern Badain Jaran Desert

巴丹吉林沙漠北部风沙地貌形态类型的分区研究

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15、

Study on Formation and Development of Aeolian Landform and Trend of Environmental Change at Lower Reach of the Keriya River, Taklimakan Desert

塔克拉玛干沙漠克里雅河下游地区风沙地貌的形成发育与环境变化趋势的初步研究

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16、

Barchan dunes is a fundamental pattern of aeolian landform. Generally speaking, it is moulded by non saturated wind sand flow which is the high concentration.

新月形沙丘是风沙地貌基本形态之一,一般为高浓度非饱和风沙流所塑造。

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17、

The periglacial Aeolian landform and deposition is the desert physiognomy formed by the blown sand under cold and arid environment, always accompanied with the impact of glaciers and freezing and thawing.

冰缘风沙地貌与沉积是在冰缘寒冷干旱气候环境中,伴有冰川或冻融作用影响,主要由风沙作用形成的荒漠地貌。

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18、

Uring the Quaternary the basic condition of the aeolian landform such as wind force, wind direction, sand sources and landscape in the northern China had changed simultaneously with the uplifting pluse of Qing-Zang plateau.

第四纪期间中国北方风沙地貌发育的基本条件如风力、风向、沙源、地形等随青藏高原的逐步隆升均发生相应变化。

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19、

The characteristics of Aeolian Sandy landform in ancient Yellow River course area at Northern Henan Province

豫北黄河古道区风沙地貌特征豫北黄河故道湿地鸟类自然保护区鸟类区系调查

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20、

Uplift test study on reinforced aeolian sand ( ii)& analysis and calculation of uplift bearing capacity

加筋风砂土抗拔试验研究(II)&抗拔载荷能力计算分析

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