Molecular dynamics simulations of the effect of static electric field on progressive ice formation

Author:

Shang Ruiqi12ORCID,Wu Tongyu1ORCID,Meguid S. A.1ORCID

Affiliation:

1. Mechanics and Aerospace Design Laboratory, University of Toronto 1 , Toronto, Ontario M5S 3G8, Canada

2. The Institute of Advanced Technologies in Energy and Electrical Engineering, Shenzhen International Graduate School, Tsinghua University 2 , Shenzhen, Guangdong, People’s Republic of China

Abstract

Ice accumulation under static electric fields presents a significant hazard to transmission lines and power grids. Contemporary computational studies of electrofreezing predominantly probed excessive electric fields (109 V/m) that are significantly higher than those typically encountered in proximity to transmission lines. To elucidate the influence of realistic electric fields (105 V/m) on ice crystallization, we run extensive molecular dynamics (MD) simulations across dual ice–water coexistence systems. Three aspects of work were accordingly examined. First, we investigated the influence of the effect of static electric fields, with a strength of 105 V/m, along three orthogonal axes on the phase transition during the encountered freezing and melting processes. Second, we established the mechanism of how the direction of an electric field, the initial ice crystallography, and the adjacent crystal planes influence the solidification process. Third, the results of our MD simulations were further post-processed to determine the dipole moment, radial distribution, and angle distribution resulting from the static electric field. Our results indicate that while weak electric fields do not cause complete polarization of liquid water molecules, they can induce a transition to a more structured ice-like geometry of the water molecules at the ice–water interphase region, particularly when applied perpendicular to the ice–water interphase. Notably, the interface adjacent to cubic ice exhibits a greater response to the electric fields than that adjacent to hexagonal ice. This is attributable to the intrinsic differences in their original hydrogen bonding networks.

Funder

Natural Sciences and Engineering Research Council of Canada

Publisher

AIP Publishing

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