Abstract

We derived theoretical formulations for the fluid threshold of conducting and insulating sand particles under an imposed electric field. Our analysis reveals a non-monotonic dependency of the fluid threshold on particle diameter, imposed electric field, and surface charge density. For conducting particles, electrostatic forces lead to a reduction of the fluid threshold by up to 31%. In contrast, for negatively charged insulating particles, electrostatic forces enhance the fluid threshold by up to 76%. Unexpectedly, electrostatic forces either enhance or inhibit the fluid threshold by up to 30%, depending on the imposed electric field and surface charge density.

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