Boosting migration of large particles by solute contrasts

被引:254
作者
Abecassis, B. [1 ,2 ]
Cottin-Bizonne, C. [1 ]
Ybert, C. [1 ]
Ajdari, A. [2 ]
Bocquet, L. [1 ,3 ]
机构
[1] Univ Lyon 1, Lab PMCN, CNRS, UMR 5586, F-69622 Villeurbanne, France
[2] CNRS, ESPCI, UMR Gulliver 7083, F-75005 Paris, France
[3] Tech Univ Munich, Dept Phys, D-85748 Garching, Germany
关键词
D O I
10.1038/nmat2254
中图分类号
O64 [物理化学(理论化学)、化学物理学];
学科分类号
070304 [物理化学]; 081704 [应用化学];
摘要
Brownian diffusion is a keystone concept in a large variety of domains, from physics, chemistry to biology(1). Diffusive transport controls situations as diverse as reaction-diffusion processes in biology and chemistry(2-4), Brownian ratchet processes(5-7), dispersion in microfluidic devices(8,9) or even double-diffusive instability and salt-fingering phenomena in the context of ocean mixing(10). Although these examples span a broad range of length scales, diffusive transport becomes increasingly inefficient for larger particles. Applications, for example, in microfluidics, usually have recourse to alternative driving methods involving external sources to induce and control migration. Here, we demonstrate experimentally a strongly enhanced migration of large particles, achieved by slaving their dynamics to that of a fast carrier species, a dilute salt. The underlying fast salt diffusion leads to an apparent diffusive-like dynamics of the large particles, which is up to two orders of magnitude faster than their natural 'bare' diffusion. Moreover both spreading and focusing of the particle assembly can be achieved on demand. A model description shows a remarkable quantitative agreement with all measured data. Applications of this process are illustrated in microfluidics for filtering and concentrating operations, as well as in conjunction with standard hydrodynamic focusing. In a wider perspective, this mechanism can affect a broad range of scales and phenomena, from biological transport to the dispersion of sediments and pollutants in oceanographic situations.
引用
收藏
页码:785 / 789
页数:5
相关论文
共 31 条
[1]
Giant amplification of interfacially driven transport by hydrodynamic slip: Diffusio-osmosis and beyond [J].
Ajdari, Armand ;
Bocquet, Lyderic .
PHYSICAL REVIEW LETTERS, 2006, 96 (18)
[2]
ANDERSON JL, 1989, ANNU REV FLUID MECH, V21, P61
[3]
[Anonymous], 2000, AM J CARDIOL
[4]
Extreme accumulation of nucleotides in simulated hydrothermal pore systems [J].
Baaske, Philipp ;
Weinert, Franz M. ;
Duhr, Stefan ;
Lemke, Kono H. ;
Russell, Michael J. ;
Braun, Dieter .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2007, 104 (22) :9346-9351
[5]
Berg HC., 2003, E. coli in motion
[6]
The role of pair dispersion in turbulent flow [J].
Bourgoin, M ;
Ouellette, NT ;
Xu, HT ;
Berg, J ;
Bodenschatz, E .
SCIENCE, 2006, 311 (5762) :835-838
[7]
PATTERN-FORMATION OUTSIDE OF EQUILIBRIUM [J].
CROSS, MC ;
HOHENBERG, PC .
REVIEWS OF MODERN PHYSICS, 1993, 65 (03) :851-1112
[8]
Salt-pump mechanism for contaminant intrusion into coastal aquifers [J].
Dror, I ;
Amitay, T ;
Yaron, B ;
Berkowitz, B .
SCIENCE, 2003, 300 (5621) :950-950
[9]
Why molecules move along a temperature gradient [J].
Duhr, Stefan ;
Braun, Dieter .
PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA, 2006, 103 (52) :19678-19682
[10]
DIFFUSIOPHORESIS OF LATEX-PARTICLES IN ELECTROLYTE GRADIENTS [J].
EBEL, JP ;
ANDERSON, JL ;
PRIEVE, DC .
LANGMUIR, 1988, 4 (02) :396-406