This study explores how electroosmosis and buoyancy forces affect flow regimes in electrokinetic systems within rectangular capillaries and how these regimes shape concentration profiles under varying temperature and non-symmetric conditions caused by uneven wall convection. The advective impact of Joule heating and convection on solute migration is investigated, with emphasis on determining which force dominates and how non-symmetric environments influence flow regimes and dispersion—key considerations for designing efficient electrokinetic devices and effective soil-remediation protocols. Using generalized (Robin-type) boundary conditions, the study introduces a skewness parameter 𝑅2 to help predict flow reversal behavior and mixing issues based on system parameters. The analysis applies heat-transfer modeling, solves the Navier–Stokes equation for buoyancy-driven cases limited by 𝑅2, and solves the molar species continuity equation to obtain concentration profiles across scenarios of 𝑅2 values and Joule heating. The area-averaging method is used for the advective case and limiting scenarios (including insulation and uneven environments) are reported, along with reverse-flow conditions and their mixing impact on concentration profiles.
more »
« less
Impact and Role of Temperature on Electrostatic Potentials and Velocity Profiles Prediction
Electrostatic potential profiles are vital for understanding and controlling electroosmosis as well as particle mixing. The shape and magnitude of this profile—particularly a key parameter called the zeta potential (ζ)—directly dictate the speed and direction of fluid flow when an electric field is applied. The role of temperature in modifying this important parameter has not been analyzed from a mathematical approach, and it is relevant for improving the design of microfluidic devices and technologies involving capillary electrophoresis for non-isothermal systems. In this study, two electrophoretic cell geometries are investigated under non-isothermal conditions. A heat-transport model (with heat generation and Dirichlet boundary conditions) is coupled into the Poisson–Boltzmann equation to obtain zeta potential profiles for different temperature distributions. In addition, the Navier–Stokes equation for the electroosmotic case is solved to obtain velocity profiles, including examples of flow reversal under temperature development. Numerical analysis for rectangular and cylindrical geometries indicates that large temperature gradients produce significant zeta-potential changes and can induce multiple flow reversals; effects are more pronounced at high Joule-heating values, while small temperature differences yield approximately linear electrostatic potential behavior and typical laminar profiles.
more »
« less
- Award ID(s):
- 2345379
- PAR ID:
- 10662908
- Publisher / Repository:
- American Institute of Chemical Engineers (AIChE)
- Date Published:
- Edition / Version:
- 1
- Page Range / eLocation ID:
- 1-2
- Subject(s) / Keyword(s):
- zeta potential joule heating flow reversal
- Format(s):
- Medium: X Size: 128KB Other: pdf
- Size(s):
- 128KB
- Location:
- Boston, MA, USA
- Sponsoring Org:
- National Science Foundation
More Like this
-
-
Available data on insulating, semiconducting, and metallic solids verify our new model that incorporates steady-state heat flow into a macroscopic, thermodynamic description of solids, with agreement being best for isotropic examples. Our model is based on: (1) mass and energy conservation; (2) Fourier’s law; (3) Stefan–Boltzmann’s law; and (4) rigidity, which is a large, yet heretofore neglected, energy reservoir with no counterpart in gases. To account for rigidity while neglecting dissipation, we consider the ideal, limiting case of a perfectly frictionless elastic solid (PFES) which does not generate heat from stress. Its equation-of-state is independent of the energetics, as in the historic model. We show that pressure-volume work (PdV) in a PFES arises from internal interatomic forces, which are linked to Young’s modulus (Ξ) and a constant (n) accounting for cation coordination. Steady-state conditions are adiabatic since heat content (Q) is constant. Because average temperature is also constant and the thermal gradient is fixed in space, conditions are simultaneously isothermal: Under these dual restrictions, thermal transport properties do not enter into our analysis. We find that adiabatic and isothermal bulk moduli (B) are equal. Moreover, Q/V depends on temperature only. Distinguishing deformation from volume changes elucidates how solids thermally expand. These findings lead to simple descriptions of the two specific heats in solids: ∂ln(cP)/∂P = −1/B; cP = nΞ times thermal expansivity divided by density; cP = cVnΞ/B. Implications of our validated formulae are briefly covered.more » « less
-
Abstract Improved modeling of permafrost active layer freeze‐thaw plays a crucial role in understanding the response of the Arctic ecosystem to the accelerating warming trend in the region over the past decades. However, modeling the dynamics of the active layer at diurnal time scale remains challenging using the traditional models of freeze‐thaw processes. In this study, a physically based analytical model is formulated to simulate the thaw depth of the active layer under changing boundary conditions of soil heat flux. Conservation of energy for the active layer leads to a nonlinear integral equation of the thaw depth using a temperature profile approximated from the analytical solution of the heat transfer equation forced by ground heat flux. Temporally variable ground heat flux is estimated using non‐gradient models when field observations are not available. Validation of the proposed model conducted against field data obtained from three Arctic forest and tundra sites demonstrates that the model is able to simulate both thaw depth and soil temperature profiles accurately. The model has the potential to estimate regional variability of the thaw depth for permafrost related applications.more » « less
-
The tempering response in the heat-affected zone (HAZ) of low alloy steels during temper bead welding is heavily dependent on the experienced thermal history. Past work has developed quantification approaches for isothermal tempering conditions and single non-isothermal tempering cycles, whereas the temper bead welding processes impart multiple non-isothermal cycles throughout the HAZ. This work outlines a novel methodology for tempering response quantification that allows for prediction of the HAZ hardness in multipass welding. The quantification approach utilizes a modification of the Grange-Baughman tempering parameter that converts non-isothermal cycles into an equivalent isothermal cycle and correlate this with the resulting hardness. This relationship can be utilized to evaluate hardness distributions throughout the HAZ of low alloy steel temper bead weldments based on the experienced thermal histories. It was shown that, in contrast with conventional heat treatment, the temper bead welding in Grade 22 steel results in nucleation of high density, finely dispersed Fe-Cr rich carbides. The proposed methodology was applied for evaluation of the HAZ hardness in a particular heat of Grade 22 steel, resulting from multiple tempering reheats, and was experimentally validated using a three-layer weld overlay. It was found that the peak temperature of weld tempering cycles was the most significant factor in controlling HAZ hardness.more » « less
-
Abstract We introduce a non-isothermal phase-field crystal model including heat flux and thermal expansion of the crystal lattice. The fundamental thermodynamic relation between internal energy and entropy, as well as entropy production, is derived analytically and further verified by numerical benchmark simulations. Furthermore, we examine how the different model parameters control density and temperature evolution during dendritic solidification through extensive parameter studies. Finally, we extend our framework to the modeling of open systems considering external mass and heat fluxes. This work sets the ground for a comprehensive mesoscale model of non-isothermal solidification including thermal expansion within an entropy-producing framework, and provides a benchmark for further meso- to macroscopic modeling of solidification.more » « less
An official website of the United States government

