扰动条件下细粉质砂土浆体流场PIV试验研究
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TU43

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国家自然科学基金面上(41976049;52004081)中国冶金地质总局山东局青年科技(SDYJ-QNKY202008);河南省高等学校重点科研项目(21A440005)


The flow field of fine silty mortar under perturbation condition by PIV
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    摘要:

    基于高速粒子图像测速技术(PIV)对粉细质砂土浆体在扰动条件下颗粒流场的流动规律以及颗粒分选现象进行研究,PIV测试实验采用黄河三角洲地区分布的细粉质土层为实验级配土样,通过对扰动条件下浆体流场变化的PIV实验结果与颗粒迁移受力情况分析,建立扰动条件下细粉质颗粒分选流膜理论模型,研究结果表明,随着F扰动逐渐增大,当流场中颗粒在F扰动逐渐大于G自重时,侧边μ孔隙逐渐增大,沉积土层逐渐液化,而PIV观测的浆体流场结构,随着人工扰动力增强,扰动力上升方向与自由面之间形成负涡量涡旋区域后,且涡旋区域伴随主循环逐步扩大,由上部逐步下沉形成完整主循环涡旋结构,根据PIV流线测试可知颗粒迁移路径形成的区域呈现上宽下窄分布;对静置后的土层取样进行颗粒级配、塑液限、压缩性等实验分析,扰动后的土体呈现分层沉积,粒度特性呈上粗下细,粒径是造成颗粒扰动后分层沉积的主要原因,黏度造成黏粒颗粒在扰动迁移运动过程中粘聚富集,压缩性表明在流动过程中的土体结构变化规律呈上扰下固;本文通过试验现象以及力学分析建立浆体流膜分选理论分析模型,与PIV测试试验结果分析较为吻合,能够有效解释扰动条件下粉细质砂浆体流场运动及颗粒分选规律,并为相关工程提供理论基础。

    Abstract:

    Based on high-speed particle image velocimetry technology(PIV), the flow law of particle flow field and the phenomenon of particle separation in powder mortar body under disturbance were studied. In PIV test, the fine-grained soil layer distributed in the Yellow River Delta area is taken as the test graded soil sample. By analyzing the experimental results of particle image velocimetry (PIV) of slurry flow field changes and particle migration stress under disturbance, the theoretical model of fine particle separation flowing film under disturbance was established. The results show that with the increasing F disturbance, when F disturbance is greater than G, the lateral pores gradually increase and the sedimentary soil layer gradually liquefies. With the enhancement of artificial disturbance force, the slurry flow field structure observed by PIV forms a negative vortex zone between the rising direction of disturbance force and the free surface, which gradually expands with the main cycle and sinks from the upper part, forming a complete main cycle vortex structure. According to the streamline test of particle image velocimetry, the area formed by particle migration path presents a wide distribution at the top and narrow distribution at the bottom. Experimental analysis on particle size distribution, plastic liquid limit and compressibility shows that the disturbed soil presents layered deposition, with coarse particle size at the top and fine particle size at the bottom, which is the main reason for layered deposition after particle disturbance. Cohesion makes cohesive soil particles agglomerate and enrich in the process of disturbance and migration, and compressibility indicates that the change rule of soil structure in the process of flow is upward disturbance and downward consolidation. Through experimental phenomena and mechanical analysis, the theoretical analysis model of slurry membrane separation is established in this paper, which is in good agreement with PIV test results. It can effectively explain the flow field motion and particle separation law of fine-grained mortar under disturbance conditions, and provide theoretical basis for related projects.

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袁延召,许国辉,张巍巍. 扰动条件下细粉质砂土浆体流场PIV试验研究[J]. 科学技术与工程, 2022, 22(11): 4481-4488.
Yuan Yanzhao, Xu Guohui, Zhang Weiwei. The flow field of fine silty mortar under perturbation condition by PIV[J]. Science Technology and Engineering,2022,22(11):4481-4488.

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  • 收稿日期:2021-08-09
  • 最后修改日期:2022-04-06
  • 录用日期:2021-11-10
  • 在线发布日期: 2022-04-20
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