The Multi-Species Farley-Buneman Instability in the Solar Chromosphere
Chad A. Madsen, Yakov S. Dimant, Meers M. Oppenheim, Juan M. Fontenla

TL;DR
This paper develops a multi-ion species theory of the Farley-Buneman Instability in the solar chromosphere, suggesting it could significantly contribute to electron heating by converting neutral flow energy into thermal energy.
Contribution
It extends previous single-ion models to include multiple ion species, providing new predictions for instability trigger velocities in the chromosphere.
Findings
FBI may be triggered at electron drift velocities as low as 4 km/s
Neutral flows can generate sufficient electric fields to induce FBI in the chromosphere
FBI could be a key mechanism for electron heating in the quiet Sun
Abstract
Empirical models of the solar chromosphere show intense electron heating immediately above its temperature minimum. Mechanisms such as resistive dissipation and shock waves appear insufficient to account for the persistence and uniformity of this heating as inferred from both UV lines and continuum measurements. This paper further develops the theory of the Farley-Buneman Instability (FBI) which could contribute substantially to this heating. It expands upon the single ion theory presented by Fontenla (2005) by developing a multiple ion species approach that better models the diverse, metal-dominated ion plasma of the solar chromosphere. This analysis generates a linear dispersion relationship that predicts the critical electron drift velocity needed to trigger the instability. Using careful estimates of collision frequencies and a one-dimensional, semi-empirical model of the…
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