Darbois Texier B, Seguin A
Université Paris-Saclay, CNRS, Laboratoire FAST, 91405 Orsay, France.
Phys Rev E. 2022 Jul;106(1-1):014906. doi: 10.1103/PhysRevE.106.014906.
We measure and analyze the drag force experienced by a rigid rod that penetrates vertically into a granular medium and partially withdraws before sinking again. The drag during the successive reintrusions is observed to be significantly smaller than the force experienced in the first run. Two force regimes are evidenced depending on how the reintrusion depth compares with the withdrawal distance Δ. These two regimes are characterized by a force curve of positive and negative curvature and are separated by an inflection point, which is characterized experimentally. We approach the difference between the first intrusion and the following reintrusions by considering a modification in the stress field of the granular material after the partial extraction of the rod. A theoretical model for the stress modification is proposed and allows to rationalize all the experiments realized for different withdrawal distances Δ. This framework introduces a crossover length λ above which the stress modification in the granular medium is maintained and that is shown to depend linearly on Δ. Finally, the model provides a prediction for the location of the inflection points in reasonable agreement with observations.
我们测量并分析了一根刚性杆垂直插入颗粒介质并在再次下沉之前部分抽出时所受到的阻力。观察到在连续再次侵入过程中的阻力明显小于首次插入时所经历的力。根据再次侵入深度与抽出距离Δ的比较情况,可证明存在两种力的状态。这两种状态的特征是力曲线具有正曲率和负曲率,并且由一个拐点分隔开,该拐点通过实验确定其特征。我们通过考虑杆部分抽出后颗粒材料应力场的变化来探讨首次侵入与后续再次侵入之间的差异。提出了一个应力变化的理论模型,该模型能够合理地解释针对不同抽出距离Δ所进行的所有实验。这个框架引入了一个交叉长度λ,在该长度以上颗粒介质中的应力变化得以维持,并且表明该交叉长度与Δ呈线性关系。最后,该模型对拐点位置的预测与观测结果合理吻合。