Microrollers flow uphill as granular media

被引:3
作者
Wilson-Whitford, Samuel R. [1 ]
Gao, Jinghui [1 ]
Roffin, Maria Chiara [1 ,2 ]
Buckley, William E. [1 ]
Gilchrist, James F. [1 ]
机构
[1] Lehigh Univ, Dept Chem & Biomol Engn, Bethlehem, PA 18015 USA
[2] Nottingham Trent Univ, Sch Sci & Technol, Dept Phys, Nottingham NG11 8NS, England
基金
美国国家科学基金会;
关键词
RHEOLOGY;
D O I
10.1038/s41467-023-41327-1
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Pour sand into a container and only the grains near the top surface move. The collective motion associated with the translational and rotational energy of the grains in a thin flowing layer is quickly dissipated as friction through multibody interactions. Alternatively, consider what will happen to a bed of particles if one applies a torque to each individual particle. In this paper, we demonstrate an experimental system where torque is applied at the constituent level through a rotating magnetic field in a dense bed of microrollers. The net result is the grains roll uphill, forming a heap with a negative angle of repose. Two different regimes have been identified related to the degree of mobility or fluidisation of the particles in the bulk. Velocimetry of the near surface flowing layer reveals the collective motion of these responsive particles scales in a similar way to flowing bulk granular flows. A simple granular model that includes cohesion accurately predicts the apparent negative coefficient of friction. In contrast to the response of active or responsive particles that mimic thermodynamic principles, this system results in macroscopic collective behavior that has the kinematics of a purely dissipative granular system.
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页数:6
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