孟强, 张久洋, 2023. 基于SHPB试验的海冰动态力学性能研究[J]. 海岸工程, 42(3): 277-287. doi: 10.12362/j.issn.1002-3682.20220730001.
    引用本文: 孟强, 张久洋, 2023. 基于SHPB试验的海冰动态力学性能研究[J]. 海岸工程, 42(3): 277-287. doi: 10.12362/j.issn.1002-3682.20220730001.
    MENG Q, ZHANG J Y, 2023. Research on dynamic mechanical properties of sea ice based on SHPB test[J]. Coastal Engineering, 42(3): 277-287. doi: 10.12362/j.issn.1002-3682.20220730001
    Citation: MENG Q, ZHANG J Y, 2023. Research on dynamic mechanical properties of sea ice based on SHPB test[J]. Coastal Engineering, 42(3): 277-287. doi: 10.12362/j.issn.1002-3682.20220730001

    基于SHPB试验的海冰动态力学性能研究

    Research on Dynamic Mechanical Properties of Sea Ice Based on SHPB Test

    • 摘要: 为研究海冰在高应变率下的动态力学特性,使用分离式霍普金斯压杆(split Hopkinson pressure bar,SHPB)装置,对2种海冰试件进行动态冲击试验,并采用三波法对试验数据进行处理,得到了海冰试件的应力-应变关系以及能量耗散规律,并对海冰破碎能耗特性进行总结。试验结果表明:在应变率为53.2~229.6 s−1的区间内,海冰的动态抗压强度为17.1~40.0 MPa,相同气压下,1.0长径比海冰试件的应变率与峰值应力均小于0.5长径比的海冰试件;海冰试件受压应力作用,最终表现出塑性压剪破坏特征;应变率较小时,由于冰的黏性,海冰破坏后仍保持一个整体,随着应变率增大,试件断裂破碎为不同大小的碎块;2种长径比试件应变率对海冰的动态破坏的能量吸收率ω均具有较大的影响,但能量吸收率ω与应变率的关系曲线表现出不同的趋势。

       

      Abstract: In order to study the dynamic mechanical properties of sea ice at high strain rate, a device of split Hopkins pressure bar (SHPB) is used to conduct dynamic impact tests on 2 kinds of sea ice specimens and a three-wave method is used to process the test data. Thus, the stress-strain relationship and the energy dissipation law of the sea ice specimens are obtained and the energy consumption characteristics of sea ice breaking are summarized. The results of the test show that the dynamic compressive strength of the sea ice is 17.1−40.0 MPa within a range of strain rate of 53.2−229.6 s−1. Under the same air pressure, the sea ice specimen with an aspect ratio of 1.0 is smaller in both the strain rate and the peak stress than the specimen with an aspect ratio of 0.5. Under the action of the compressive stress the sea ice specimens show finally the characteristics of plastic pressure shear failure. When the strain rate is small, the sea ice remains as a whole after its destruction due to the viscosity of the ice. With the increasing of strain rate, the specimens are fractured and broken into pieces of blocks with different sizes. The strain rates of the specimens with the two aspect ratios influence greatly on the energy absorption rate ω of the sea ice dynamic destruction. However, the relationship curve between the energy absorption rate ω and the strain rate shows a different trend.

       

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