Understanding the Efficiency of Autonomous Nano- and Microscale Motors

We analyze the power conversion efficiency of different classes of autonomous nano- and micromotors. For bimetallic catalytic motors that operate by a self-electrophoretic mechanism, there are four stages of energy loss, and together they result in a power conversion efficiency on the order of 10^–9. The results of finite element modeling agree well with experimental measurements of the efficiency of catalytic Pt–Au nanorod motors. Modifications of the composition and shape of bimetallic catalytic motors were predicted computationally and found experimentally to lead to higher efficiency. The efficiencies of bubble-propelled catalytic micromotors, magnetically driven flagellar motors, Janus micromotors driven by self-generated thermal gradients, and ultrasonically driven metallic micromotors are also analyzed and discussed

Particle Zeta Potentials Remain Finite in Saturated Salt Solutions

The zeta potential of a particle characterizes its motion in an electric field and is often thought to be negligible at high ionic strength (several moles per liter) due to thinning of the electrical double layer (EDL). Here, we describe zeta potential measurements on polystyrene latex (PSL) particles at monovalent salt concentrations up to saturation (∼5 M NaCl) using electrophoresis in sinusoidal electric fields and high-speed video microscopy. Our measurements reveal that the zeta potential remains finite at even the highest concentrations. Moreover, we find that the zeta potentials of sulfated PSL particles continue to obey the classical Gouy–Chapman model up to saturation despite significant violations in the model’s underlying assumptions. By contrast, amidine-functionalized PSL particles exhibit qualitatively different behaviors such as zero zeta potentials at high concentrations of NaCl and KCl and even charge inversion in KBr solutions. The experimental results are reproduced and explained by Monte Carlo simulations of a simple lattice model of the EDL that accounts for effects due to ion size and ion–ion correlations. At high salt conditions, the model suggests that quantitative changes in the magnitude of surface charge can result in qualitative changes in the zeta potentialmost notably, charge inversion of highly charged surfaces. These findings have important implications for electrokinetic phenomena such as diffusiophoresis within salty environments such as oceans, geological reservoirs, and living organisms

Particle Deposition on Microporous Membranes Can Be Enhanced or Reduced by Salt Gradients

Colloidal particle deposition on membranes is a continuing scientific and technological challenge. In this paper we examine the role of a previously unexplored phenomenondiffusiophoretic particle transport toward a membranein relation to fouling. Diffusiophoresis is an electrokinetic transport mechanism that arises in salt gradients, especially when the ions have different diffusion coefficients. Through experiments conducted with salt diffusing across microdialysis membranes, with no advection, we show experimentally that diffusiophoresis induces colloidal deposition on the surface of microporous surfaces. We used transient salt (NaCl, KCl, LiCl) gradients and fundamental electrokinetic modeling to assess the role of diffusiophoresis in colloidal fouling. Based on (i) difference in diffusion coefficients of ions, (ii) zeta potential on the particles, and (iii) ionic gradient applied across the walls of the membrane, colloidal fouling could be both quantitatively and qualitatively predicted. Our understanding enabled us to stop particle deposition by adding calcium carbonate outside the membrane, which generates a stronger electric field in a direction opposite to that created by salt diffusing from the membrane. We propose that accounting for this diffusiophoretic mode of particle deposition is important in understanding membrane fouling

Enhanced Transport into and out of Dead-End Pores

Dead-end micro- and nanoscale channels are ubiquitous in nature and are found in geological and biological systems subject to frequent disruptions. Achieving fluid flows in them is not possible through conventional pressure-driven mechanisms. Here we show that chemically driven convective flows leading to transport in and out of dead-end pores can occur by the phenomenon of “transient diffusioosmosis”. The advective velocity depends on the presence of an <i>in situ</i>-generated transient ion gradient and the intrinsic charge on the pore wall. The flows can reach speeds of 50 μm/s and cause extraction of otherwise-trapped materials. Our results illustrate that chemical energy, in the form of a transient salt gradient, can be transduced into mechanical motion with the pore wall acting as the pump. As discussed, the phenomena may underlie observed transport in many geological and biological systems involving tight or dead-end micro- and nanochannels

Enhanced Transport into and out of Dead-End Pores

Dead-end micro- and nanoscale channels are ubiquitous in nature and are found in geological and biological systems subject to frequent disruptions. Achieving fluid flows in them is not possible through conventional pressure-driven mechanisms. Here we show that chemically driven convective flows leading to transport in and out of dead-end pores can occur by the phenomenon of “transient diffusioosmosis”. The advective velocity depends on the presence of an <i>in situ</i>-generated transient ion gradient and the intrinsic charge on the pore wall. The flows can reach speeds of 50 μm/s and cause extraction of otherwise-trapped materials. Our results illustrate that chemical energy, in the form of a transient salt gradient, can be transduced into mechanical motion with the pore wall acting as the pump. As discussed, the phenomena may underlie observed transport in many geological and biological systems involving tight or dead-end micro- and nanochannels

Enhanced Transport into and out of Dead-End Pores

Dead-end micro- and nanoscale channels are ubiquitous in nature and are found in geological and biological systems subject to frequent disruptions. Achieving fluid flows in them is not possible through conventional pressure-driven mechanisms. Here we show that chemically driven convective flows leading to transport in and out of dead-end pores can occur by the phenomenon of “transient diffusioosmosis”. The advective velocity depends on the presence of an <i>in situ</i>-generated transient ion gradient and the intrinsic charge on the pore wall. The flows can reach speeds of 50 μm/s and cause extraction of otherwise-trapped materials. Our results illustrate that chemical energy, in the form of a transient salt gradient, can be transduced into mechanical motion with the pore wall acting as the pump. As discussed, the phenomena may underlie observed transport in many geological and biological systems involving tight or dead-end micro- and nanochannels

Enhanced Transport into and out of Dead-End Pores

Dead-end micro- and nanoscale channels are ubiquitous in nature and are found in geological and biological systems subject to frequent disruptions. Achieving fluid flows in them is not possible through conventional pressure-driven mechanisms. Here we show that chemically driven convective flows leading to transport in and out of dead-end pores can occur by the phenomenon of “transient diffusioosmosis”. The advective velocity depends on the presence of an <i>in situ</i>-generated transient ion gradient and the intrinsic charge on the pore wall. The flows can reach speeds of 50 μm/s and cause extraction of otherwise-trapped materials. Our results illustrate that chemical energy, in the form of a transient salt gradient, can be transduced into mechanical motion with the pore wall acting as the pump. As discussed, the phenomena may underlie observed transport in many geological and biological systems involving tight or dead-end micro- and nanochannels

Enhanced Transport into and out of Dead-End Pores

Dead-end micro- and nanoscale channels are ubiquitous in nature and are found in geological and biological systems subject to frequent disruptions. Achieving fluid flows in them is not possible through conventional pressure-driven mechanisms. Here we show that chemically driven convective flows leading to transport in and out of dead-end pores can occur by the phenomenon of “transient diffusioosmosis”. The advective velocity depends on the presence of an <i>in situ</i>-generated transient ion gradient and the intrinsic charge on the pore wall. The flows can reach speeds of 50 μm/s and cause extraction of otherwise-trapped materials. Our results illustrate that chemical energy, in the form of a transient salt gradient, can be transduced into mechanical motion with the pore wall acting as the pump. As discussed, the phenomena may underlie observed transport in many geological and biological systems involving tight or dead-end micro- and nanochannels

Enhanced Transport into and out of Dead-End Pores

Dead-end micro- and nanoscale channels are ubiquitous in nature and are found in geological and biological systems subject to frequent disruptions. Achieving fluid flows in them is not possible through conventional pressure-driven mechanisms. Here we show that chemically driven convective flows leading to transport in and out of dead-end pores can occur by the phenomenon of “transient diffusioosmosis”. The advective velocity depends on the presence of an <i>in situ</i>-generated transient ion gradient and the intrinsic charge on the pore wall. The flows can reach speeds of 50 μm/s and cause extraction of otherwise-trapped materials. Our results illustrate that chemical energy, in the form of a transient salt gradient, can be transduced into mechanical motion with the pore wall acting as the pump. As discussed, the phenomena may underlie observed transport in many geological and biological systems involving tight or dead-end micro- and nanochannels

Enhanced Transport into and out of Dead-End Pores

Dead-end micro- and nanoscale channels are ubiquitous in nature and are found in geological and biological systems subject to frequent disruptions. Achieving fluid flows in them is not possible through conventional pressure-driven mechanisms. Here we show that chemically driven convective flows leading to transport in and out of dead-end pores can occur by the phenomenon of “transient diffusioosmosis”. The advective velocity depends on the presence of an <i>in situ</i>-generated transient ion gradient and the intrinsic charge on the pore wall. The flows can reach speeds of 50 μm/s and cause extraction of otherwise-trapped materials. Our results illustrate that chemical energy, in the form of a transient salt gradient, can be transduced into mechanical motion with the pore wall acting as the pump. As discussed, the phenomena may underlie observed transport in many geological and biological systems involving tight or dead-end micro- and nanochannels