Abstract

An ion-exchange-resin-based microfluidic pump is introduced that utilizes trace amounts of ions to generate fluid flows. We show experimentally that our pump operates in almost deionized water for periods exceeding 24 h and induces fluid flows of μm s-1 over hundreds of μm. This flow displays a far-field, power-law decay which is characteristic of two-dimensional (2D) flow when the system is strongly confined and of three-dimensional (3D) flow when it is not. Using theory and numerical calculations we demonstrate that our observations are consistent with electroosmotic pumping driven by μmol L-1 ion concentrations in the sample cell that serve as 'fuel' to the pump. Our study thus reveals that trace amounts of charge carriers can produce surprisingly strong fluid flows; an insight that should benefit the design of a new class of microfluidic pumps that operate at very low fuel concentrations.

Highlights

  • An ion-exchange-resin-based microfluidic pump is introduced that utilizes trace amounts of ions to generate fluid flows

  • Our results indicate that ion-exchange-resin-based microfluidic pumps have a surprisingly small lower bound to the ion concentration under which they can operate, which we chart in this paper

  • The striking feature of this pump is that it operates in mmol LÀ1 ionic concentrations for periods exceeding 24 h and yet manages to produce fluid flows with speeds of several mm sÀ1 over hundreds of mm, without strongly modifying its environment

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Summary

Experiments

We describe the experimental setup for a single ion-exchange-resin pump and characterization of the tracer properties used in our velocimetry measurements. We provide quantification of a wide range of resin pumps and tracers to show the generality of our findings. We study the impact of added salt on the pumping

Tracer characterization
Velocimetry for the ion-exchange-resin pump
An inverted pump
General considerations
Electrokinetic equations
Finite-element model of the pump
Tracer speed
Parameter choices
Finite-element results
Analytical calculations
À 2a þ DHþ DClÀ
Discussion and outlook
Full Text
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