Volume 37 Issue 5
Oct.  2023
Turn off MathJax
Article Contents
HUANG N, YANG B, HE W, et al. Measurement of wall shear stress in wind-blown sand environment[J]. Journal of Experiments in Fluid Mechanics, 2023, 37(5): 93-100 doi: 10.11729/syltlx20230074
Citation: HUANG N, YANG B, HE W, et al. Measurement of wall shear stress in wind-blown sand environment[J]. Journal of Experiments in Fluid Mechanics, 2023, 37(5): 93-100 doi: 10.11729/syltlx20230074

Measurement of wall shear stress in wind-blown sand environment

doi: 10.11729/syltlx20230074
  • Received Date: 2023-05-22
  • Accepted Date: 2023-07-24
  • Rev Recd Date: 2023-07-18
  • Available Online: 2023-11-06
  • Publish Date: 2023-10-30
  • As a key driving force of aeolian sand movement, wall shear stress is of importance in the study of aeolian sand movement. However, at present, the experimental measurement of the surface shear force in the wind-blown sand environment is extremely scarce, which has become a bottleneck for the further development of the wind-blown sand research. This paper introduces a method based on the hot-film technology for accurate measurement of the wall shear stress in the wind-blown sand environment. The wall shear stress was measured under conditions without sand using hot-film probes and two-dimensional hot-wire probes, respectively. The result shows that the hot-film probe has a good response to the wall shear stress, and the difference between the measurement results of the friction velocity of these two probes is less than 6.6%. The measurement results of the hot-film probe for the wall shear stress of flow around the square column are in good agreement with the OpenFOAM numerical simulation results, which further proves the effectiveness of the hot-film probe for the measurement of the wall shear stress. In addition, the particle impact test results of the hot film probes show that the influence of particle impact on the hot-film signal is negligible, so the hot-film probe can be used to effectively measure the wall shear stress in the wind-blown sand environment. Based on this technology, the spatial distribution characteristics of the wall shear stress along the flow direction in the wind-blown sand environment were tested. And for the first time, the spatial distribution of the wall shear stress in the wind-blown sand environment was obtained by means of actual measurement. In view of the high-frequency response capability of the hot-film probe, this technology will play an important role in the experimental research on the mechanism of aeolian sand movement in the turbulent boundary layer.
  • loading
  • [1]
    DUPONT S, BERGAMETTI G, MARTICORENA B, et al. Modeling saltation intermittency[J]. Journal of Geophysical Research: Atmospheres, 2013, 118(13): 7109–7128. doi: 10.1002/jgrd.50528
    [2]
    BAGNOLD R A. The physics of blown sand and desert dunes[M]. New York: W. Morrow & company, 1941.
    [3]
    AGOSTINI L, LESCHZINER M. The connection between the spectrum of turbulent scales and the skin-friction statistics in channel flow at Reτ ≈ 1000[J]. Journal of Fluid Mechanics, 2019, 871: 22–51. doi: 10.1017/jfm.2019.297
    [4]
    DUAN Y C, ZHONG Q, WANG G Q, et al. Contributions of different scales of turbulent motions to the mean wall-shear stress in open channel flows at low-to-moderate Reynolds numbers[J]. Journal of Fluid Mechanics, 2021, 918: A40. doi: 10.1017/jfm.2021.236
    [5]
    JACOB C, ANDERSON W. Conditionally averaged large-scale motions in the neutral atmospheric boundary layer: insights for aeolian processes[J]. Boundary-Layer Meteo-rology, 2017, 162(1): 21–41. doi: 10.1007/s10546-016-0183-4
    [6]
    RICHTER D H, SULLIVAN P P. Modification of near-wall coherent structures by inertial particles[J]. Physics of Fluids, 2014, 26(10): 103304. doi: 10.1063/1.4900583
    [7]
    RANA S, ANDERSON W, DAY M. Turbulence-based model for subthreshold aeolian saltation[J]. Geophysical Research Letters, 2020, 47(15): e2020GL088050. doi: 10.1029/2020GL088050
    [8]
    LI G, ZHANG J, HERRMANN H J, et al. Study of aerodynamic grain entrainment in aeolian transport[J]. Geophysical Research Letters, 2020, 47(11): e2019GL086574. doi: 10.1029/2019GL086574
    [9]
    COMOLA F, KOK J F, CHAMECKI M, et al. The intermittency of wind-driven sand transport[J]. Geophysical Research Letters, 2019, 46(22): 13430–13440. doi: 10.1029/2019GL085739
    [10]
    YIN X, JIANG C, SHAO Y P, et al. Large-eddy-simulation study on turbulent particle deposition and its dependence on atmospheric-boundary-layer stability[J]. Atmospheric Che-mistry and Physics, 2022, 22(7): 4509–4522. doi: 10.5194/acp-22-4509-2022
    [11]
    TAN L H, AN Z S, ZHANG K, et al. Intermittent aeolian saltation over a Gobi surface: threshold, saltation layer height, and high-frequency variability[J]. Journal of Geophysical Research: Earth Surface, 2020, 125(1): e2019JF005329. doi: 10.1029/2019JF005329
    [12]
    ZHENG X J, JIN T, WANG P. The influence of surface stress fluctuation on saltation sand transport around threshold[J]. Journal of Geophysical Research: Earth Surface, 2020, 125(5): e2019JF005246. doi: 10.1029/2019JF005246
    [13]
    KAWAMURA R. Study on sand movement by wind[J]. Annual Report Institute Science and Technology, 1951, 5(3): 95–112.
    [14]
    LETTAU K. Experimental and micro-meteorological field studies of dune migration[M]. LETTAU H H, LETTAU K, Exploring in the World's driest climate. Madison: University of Wisconsin-Madison, 1978: 110-147.
    [15]
    SØRENSEN M. On the rate of aeolian sand transport[J]. Geomorphology, 2004, 59(1-4): 53–62. doi: 10.1016/j.geomorph.2003.09.005
    [16]
    SLINN W G N. Predictions for particle deposition to vegetative canopies[J]. Atmospheric Environment (1967), 1982, 16(7): 1785–1794. doi: 10.1016/0004-6981(82)90271-2
    [17]
    ZHANG J, SHAO Y. A new parameterization of particle dry deposition over rough surfaces[J]. Atmospheric Chemistry and Physics, 2014, 14(22): 12429–12440. doi: 10.5194/acp-14-12429-2014
    [18]
    PRESTON J H. The determination of turbulent skin friction by means of pitot tubes[J]. The Journal of the Royal Aeronautical Society, 1954, 58(518): 109–121. doi: 10.1017/s0368393100097704
    [19]
    IRWIN H P A H. A simple omnidirectional sensor for wind-tunnel studies of pedestrian-level winds[J]. Journal of Wind Engineering and Industrial Aerodynamics, 1981, 7(3): 219–239. doi: 10.1016/0167-6105(81)90051-9
    [20]
    FAGE A, FALKNER V M. On the relation between heat transfer and surface friction for laminar flow[R]. Aeronautical Research Communications Report Memoran-dum, Report No. 1408, 1931.
    [21]
    LUDWIEG H. Instrument for measuring the wall shearing stress of turbulent boundary layers[R]. NACA Technical Memorandum 1284, 1950.
    [22]
    LIEPMANN H W, SKINNER G T. Shearing-stress measurements by use of a heated element[R]. NACA Technical Note 3268, 1954.
    [23]
    BELLHOUSE B J, SCHULTZ D L. The measurement of fluctuating skin friction in air with heated thin-film gauges[J]. Journal of Fluid Mechanics, 1968, 32(4): 675–680. doi: 10.1017/s0022112068000959
    [24]
    SUN B Y, WANG P B, LUO J, et al. A flexible hot-film sensor array for underwater shear stress and transition measurement[J]. Sensors, 2018, 18(10): 3469. doi: 10.3390/s18103469
    [25]
    WALTER B, GROMKE C, LEONARD K, et al. Spatially resolved skin friction velocity measurements using Irwin sensors: A calibration and accuracy analysis[J]. Journal of Wind Engineering and Industrial Aerodynamics, 2012, 104-106: 314–321. doi: 10.1016/j.jweia.2012.02.018
    [26]
    SHAO Y P, LU H. A simple expression for wind erosion threshold friction velocity[J]. Journal of Geophysical Research: Atmospheres, 2000, 105(D17): 22437–22443. doi: 10.1029/2000JD900304
  • 加载中

Catalog

    通讯作者: 陈斌, bchen63@163.com
    • 1. 

      沈阳化工大学材料科学与工程学院 沈阳 110142

    1. 本站搜索
    2. 百度学术搜索
    3. 万方数据库搜索
    4. CNKI搜索

    Figures(11)

    Article Metrics

    Article views (128) PDF downloads(61) Cited by()
    Proportional views
    Related

    /

    DownLoad:  Full-Size Img  PowerPoint
    Return
    Return