An improved model to estimate annual sand transport rate by sand-driving winds

被引:2
|
作者
Xiao, Nan [1 ]
Dong, Zhibao [1 ]
Wang, Jiaqi [2 ]
Liu, Zhengyao [1 ,3 ]
Tuo, Yu [1 ]
Feng, Miaoyan [1 ]
Zhu, Chunming [1 ]
机构
[1] Shaanxi Normal Univ, Sch Geog & Tourism, 620 West Changan Ave, Xian 710119, Peoples R China
[2] Inner Mongolia Extra High Voltage Power Supply Bu, Jinchuan Econ Tech Dev Zone, 2 Huijin Rd, Hohhot 010050, Peoples R China
[3] Shaanxi Inst Geoenvironm Monitoring, 100 Yanta North Rd, Xian 710054, Peoples R China
基金
中国国家自然科学基金;
关键词
Sand transport rate; Sand-driving winds; Drift potential; Weibull probability distribution; The Badain Jaran Sand Sea; POWER-GENERATION; DESERTIFICATION; DUNES; SPEED; PARTICLES; PLATEAU;
D O I
10.1016/j.catena.2020.104945
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Some of the surface on Earth, Mars, Venus, and Titan is covered by ripples, dunes, and other features formed by sand-driving winds. Many developing countries in arid and semiarid areas are caught in a dilemma between the threat of sandy desertification and the development of wind energy. The estimation for the probability of sand-driving winds has been rarely studied. The ability of two-parameter Weibull probability distribution to estimate sand-driving winds is questioned. Sand transport rate is used only for the evaluation of short-term aeolian activities. Drift potential (DP) is an accessible way of evaluating potential sand transport volume by sand-driving winds. However, the relationship among annual sand transport volume, DP and wind energy has been rarely studied. Sand-driving winds can be divided into gentle winds and strong winds, but it is hard to distinguish them and to quantify their effects on aeolian geomorphology. A function was constructed from expressions of sand transport rate and the two-parameter Weibull probability distribution to improve the estimation of sand-driving winds. On this basis, annual sand transport volume was accurately evaluated by sand-driving winds. This is applicable to arid and semiarid areas worldwide. The relationship among annual sand transport volume, DP and wind energy was analyzed from the perspective of dimensional analysis. Gentle winds and strong winds are distinguished by transport wind velocity at which aeolian activities on a sandy underlying surface reach the erosion-deposition balance, and which corresponds to annual maximum sand transport rate. On a sandy underlying surface strong winds control deposition, while gentle winds dominate wind erosion. The transport wind velocity is nearly constant, weakly related to the probability distribution of sand-driving winds. These results provide a basis for an improved understanding of aeolian activities as an important planetary surface process, sand control engineering, and wind energy development.
引用
收藏
页数:10
相关论文
共 50 条
  • [1] An improved approach to estimate sand-driving winds
    Xiao, Nan
    Dong, Zhibao
    Xiao, Shun
    Wang, Jiaqi
    Liu, Zhengyao
    Sarina
    Tuo, Yu
    Zhu, Chunming
    Feng, Miaoyan
    [J]. JOURNAL OF CLEANER PRODUCTION, 2021, 285
  • [2] Characteristics of sand-driving wind regime and sediment transport in northeast edge of Ulan Buh Desert
    Luo, Fengmin
    Gao, Junliang
    Xin, Zhiming
    Bian, Kai
    Hao, Yuguang
    Liu, Fang
    [J]. Nongye Gongcheng Xuebao/Transactions of the Chinese Society of Agricultural Engineering, 2019, 35 (04): : 145 - 152
  • [3] On the rate of aeolian sand transport
    Sorensen, M
    [J]. GEOMORPHOLOGY, 2004, 59 (1-4) : 53 - 62
  • [4] Improved analytical model for the relaxation process of aeolian sand transport
    Bin Yang
    Yuxin Liu
    Bo Zhang
    Yuanwei Lin
    Yang Zhang
    [J]. The European Physical Journal E, 2021, 44
  • [5] Improved analytical model for the relaxation process of aeolian sand transport
    Yang, Bin
    Liu, Yuxin
    Zhang, Bo
    Lin, Yuanwei
    Zhang, Yang
    [J]. EUROPEAN PHYSICAL JOURNAL E, 2021, 44 (09):
  • [6] A transport-rate model of wind-blown sand
    Ping Lü *
    [J]. Sciences in Cold and Arid Regions, 2009, 1 (02) : 165 - 169
  • [7] A model of the sand transport rate that accounts for temporal evolution of the bed
    Wang, Xuesong
    Zhang, Chunlai
    Zou, Xueyong
    [J]. GEOMORPHOLOGY, 2021, 378
  • [8] A transport-rate model of wind-blown sand
    Lu, Ping
    Dong, ZhiBao
    [J]. SCIENCES IN COLD AND ARID REGIONS, 2009, 1 (02): : 165 - 169
  • [9] SEDIMENT TRANSPORT RATE FOR NONUNIFORM SAND
    WANG, SQ
    ZHANG, R
    [J]. SEDIMENT TRANSPORT MODELING: PROCEEDINGS OF AN INTERNATIONAL SYMPOSIUM, 1989, : 588 - 593
  • [10] Blown-sand transport rate
    Ni, JR
    Li, ZS
    Mendoza, C
    [J]. EARTH SURFACE PROCESSES AND LANDFORMS, 2004, 29 (01) : 1 - 14