Please wait a minute...
img

Wechat

Adv search
JOURNAL OF DESERT RESEARCH  2012, Vol. 32 Issue (2): 323-330    DOI:
Desert and Desertification     
Transition Model of Saltation Bombardment
ZHAO Jian-hua1,2, ZHANG Qiang1,2, LONG Xiao2
1.Lanzhou (Open) Key Laboratory of Arid Climate Change and Reducing Disaster of Gansu Province (China Meteorological Administrator), Lanzhou Institute of Arid Meteorology, CMA, Lanzhou 730020, China;
2.College of Atmospheric Sciences, Lanzhou University, Lanzhou 730000, China
Download:  PDF (3213KB) 
Export:  BibTeX | EndNote (RIS)      
Abstract  Dust emission by saltation bombardment is the most important dust emission way. Lu H and Shao YP ever presented a wonderful model of volume removal to predict dust emission rate. In consideration of its deficiency, we, however, from another point of view, brings forward a transition model to predict dust emission. The transition model of dust emission is an analogy of electron transition, which results from a detailed analysis of the stress transferring process on sand bed. According to this transition model, a particle on the bed will be released if energy transferred to it from the impacting particle through the bed, is bigger than the "transition" energy, which is the least energy to eject a particle into air, and the remained energy of the ejected particle is converted to its initial kinetic energy. Thus the expressions of the number of ejected particles, their velocity distributions and the shapes of bombardment crater in two-dimension and three-dimension situations are then easily obtained based on the transition model. And the dust emission by saltation bombardment then becomes an issue to research into the transition energy and the energy distribution around the point where collision happens. In this paper we introduce two methods, namely, the method of absorption coefficient and the method of transport equation, to approximate the energy distribution. The images of the two-dimension craters by the two methods show that the crater is big (or small) as to big-sized (or small-sized) particles and a big (or small) number of ejected particles, and collapse may appear with the crater's formation. And of the method of absorption coefficient, the crater expands with the increase of absorption coefficient at the outset, but shrinks when absorption coefficient is bigger than a certain value. Of the method of transport equation, the crater always seems to expand with kt, an important parameter of this method.
Key words:  dust emission by saltation bombardment      number of ejected particles      bombardment crater     
Received:  26 August 2011      Published:  20 March 2012
ZTFLH: 

P445.4

 
Articles by authors
ZHAO Jian-hua
ZHANG Qiang
LONG Xiao

Cite this article: 

ZHAO Jian-hua, ZHANG Qiang, LONG Xiao. Transition Model of Saltation Bombardment. JOURNAL OF DESERT RESEARCH, 2012, 32(2): 323-330.

URL: 

http://www.desert.ac.cn/EN/     OR     http://www.desert.ac.cn/EN/Y2012/V32/I2/323

[1]屈建军,井哲帆,张克存,等.HDPE蜂巢式固沙障研制与防沙效应实验研究[J].中国沙漠,2008,28(4):599-604.

[2]杨兴华,何清,艾力\5买买提明.塔克拉玛干沙漠塔中地区春夏季风蚀起沙研究[J].中国沙漠,2010,30(4):770-776.

[3]周悦,牛生杰,邱玉珺.半干旱区沙尘天气近地层湍流通量及起沙研究[J].中国沙漠,2010,30(5):1194-1199.

[4]夏训诚,杨根生.中国西北地区沙尘暴灾害及防治[M].北京:中国环境科学出版社,1996:1-242.

[5]钱正安,贺慧霞,瞿章,等.我国西北地区沙尘暴的分级标准和个例谱及其统计特征[C]//中国沙尘暴研究.北京:气象出版社,1997:1-10.

[6]Brazel A J.The relationship of weather types to dust storm generation in Arizona (1965—1980)[J].Journal of Climate,1986,6:255-275.

[7]Patricia M P,Nancy L B,Edward H B.An observational study of the “interstate 5” dust storm case[J].Bulletin of the American Meteorological Society,1996,77(4):693-720.

[8]胡隐樵,光田宇.强沙尘暴发展与干飑线——黑风暴形成的一个机理分析[J].高原气象,1996,15(2):178-185.

[9]胡隐樵,光田宁.强沙尘暴微气象特征和局地触发机制[J].大气科学,1997,21(5):581-589.

[10]岳平,牛生杰,张强,等.夏季强沙尘暴内部热力动力特征的个例研究[J].中国沙漠,2008,28(3):509-514.

[11]王敏仲,魏文寿,杨莲梅,等.塔里木盆地一次东灌型沙尘暴环流动力结构分析[J].中国沙漠,2008,28(2):370-376.

[12]陈艳,宿海良,张婉莹,等.一次强沙尘暴天气的成因分析[J].中国沙漠,2009,29(4):757-765.

[13]李彰俊,孙照渤,姜学恭.蒙古气旋天气过程中的沙尘传输特征[J].中国沙漠,2008,28(5):927-930.

[14] 姜学恭,李彰俊,程丛兰,等.地面加热对沙尘暴数值模拟结果的影响研究[J].中国沙漠,2010,30(1):182-192.

[15]李彰俊,郝璐,李兴华.积雪覆盖度对沙尘暴的影响分析[J].中国沙漠,2008,28(2):338-343.

[16]贺大梁,刘大有.跃移沙粒起跳的受力机制[J].中国沙漠,1989,9(2):14-21.

[17]董治宝.风沙启动形式与起动假说[J].干旱气象,2005,23(2):64-69.

[18]屈建军,焉穆弘,董光荣,等.沙尘暴起电的风洞模拟实验研究[J].中国科学(D辑),2003,33(6):593-601.

[19]黄宁,郑晓静.风沙流中沙粒带电现象的实验测试[J].科学通报,2000,45(20):2232-2235.

[20]赵建华,张强,袁铁,等.沙粒启动机制的理论分析[J].中国沙漠,2005,25(6):853-862.

[21]Shao Y.A model for mineral dust emission[J].Journal of Geophysical Research,2001,106(20):239-254.

[22]Shao Y,Raupach M R.The overshot and equilibration of saltation[J].Journal of Geophysical Research,1993,97:20559-20564.

[23]Lu H,Shao Y P.A new model for dust emission by saltation bombardment[J].Journal of Geophysical Research,1999,104:16827-16842.

[24]Rice M A,Willetts B B,McEwan I K.Observations of collisions of saltating grains with a granular bed from high-speed cine-film[J].Sedimentology,1996,43:21-31.

[25]沈养中,孟胜国.结构力学[M].北京:科学出版社,2009:1-62

[26]孙其诚,金峰,王光谦,等.二维颗粒体系单轴压缩形成的力链结构[J].物理学报,2010,59(1):30-37.

[27]孙其诚,王光谦.静态堆积颗粒中的力链分布[J].物理学报,2008,57(8):4666-4674.

[28]陆坤权,刘奇星.颗粒物质(上)[J].物理,2004,33(9):629-635.

[29]Goldenberg C,Goldhirsch I.Friction enhances elasticity in granular solids[J].Nature,2005,435(7039):188-191.

[30]Atman A P F,Brunet P,Geng J,et al.Sensitivity of the stress response function to packing preparation[J].Journal of Physics:Condensed Matter,2005,17:2391-2403.

[31]褚圣麟.原子物理学[M].北京:高等教育出版社,2002:22-35.

[32]张胜业,潘玉玲.应用地球物理学原理[M].武汉:中国地质大学出版社,2004:315.

[33]粱昆淼.数学物理方法[M].北京:高等教育出版社,2000:409.
No Suggested Reading articles found!