Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1029/2020GL088644 |
Aeolian Creep Transport: Theory and Experiment | |
Wang, Peng; Zhang, Jie; Dun, Hongchao; Herrmann, Hans J.; Huang, Ning | |
通讯作者 | Huang, N |
来源期刊 | GEOPHYSICAL RESEARCH LETTERS
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ISSN | 0094-8276 |
EISSN | 1944-8007 |
出版年 | 2020 |
卷号 | 47期号:15 |
英文摘要 | Aeolian sand transport drives geophysical phenomena, such as bedform evolution and desertification. Creep plays a crucial, yet poorly understood, role in this process. We present a model for aeolian creep, making quantitative predictions for creep fluxes, which we verify experimentally. We discover that the creep transport rate scales like the Shields number to the power 5/2, clearly different from the laws known for saltation. We derive this 5/2 power scaling law from our theory and confirm it with meticulous wind tunnel experiments. We calculate the creep flux and layer thickness in steady state exactly and for the first time study the relaxation of the flux toward saturation, obtaining an analytic expression for the relaxation time. Plain Language Summary The sand transport of granular beds under the action of turbulent wind-sheared flows is of major importance for the bedforms evolution and desertification processes. Up to now, the saltation transport is well understood and predictable but not the creep transport and relevant scaling laws. In this study, a theory for the aeolian creep transport is developed and verified through wind tunnel experiments. We propose for the first time a scaling law with the Shields number for the creep transport rate. Our novel model allows predictions of the aeolian creep transport rate and shows that it captures the relaxation process in actual creep transport. Such theoretical model provides key tools for the study of aeolian creep but could not previously be studied in such detail. Our study provides a better understanding for the phenomenon that the bed surface itself appeared to be "fluidized" in aeolian sand transport. |
英文关键词 | aeolian sand transport creep saltation scaling laws wind tunnel relaxation process |
类型 | Article |
语种 | 英语 |
开放获取类型 | Other Gold |
收录类别 | SCI-E |
WOS记录号 | WOS:000560376100013 |
WOS关键词 | PARTICLE-SIZE ; SAND ; SALTATION ; GRAINS ; MODEL ; BED |
WOS类目 | Geosciences, Multidisciplinary |
WOS研究方向 | Geology |
来源机构 | 兰州大学 |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/325663 |
作者单位 | [Wang, Peng; Zhang, Jie; Dun, Hongchao; Huang, Ning] Lanzhou Univ, Coll Civil Engn & Mech, Key Lab Mech Disaster & Environm Western China, Lanzhou, Peoples R China; [Wang, Peng] Lanzhou Univ Technol, Sch Sci, Lanzhou, Peoples R China; [Herrmann, Hans J.] PMMH ESPCI, Paris, France; [Herrmann, Hans J.] Univ Fed Ceara, Dept Fis, Fortaleza, Ceara, Brazil |
推荐引用方式 GB/T 7714 | Wang, Peng,Zhang, Jie,Dun, Hongchao,et al. Aeolian Creep Transport: Theory and Experiment[J]. 兰州大学,2020,47(15). |
APA | Wang, Peng,Zhang, Jie,Dun, Hongchao,Herrmann, Hans J.,&Huang, Ning.(2020).Aeolian Creep Transport: Theory and Experiment.GEOPHYSICAL RESEARCH LETTERS,47(15). |
MLA | Wang, Peng,et al."Aeolian Creep Transport: Theory and Experiment".GEOPHYSICAL RESEARCH LETTERS 47.15(2020). |
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