Charge injection into the atmosphere by explosive volcanic eruptions through triboelectrification and fragmentation charging

TL;DR

This study uses a shock-tube to simulate volcanic jets, demonstrating size-dependent bipolar charging and highlighting the significant role of triboelectric and fragmentation charging in near-vent electrification and lightning.

Contribution

It provides experimental evidence for size-dependent bipolar charging and clarifies the roles of triboelectric and fragmentation mechanisms in volcanic electrification without ice.

Findings

Size-dependent bipolar charging observed in volcanic jet simulations

Triboelectric charging plays a significant role in near-vent electrification

Particles remain moderately electrified, potentially driving near-vent lightning

Abstract

Volcanic eruptions are associated with a wide range of electrostatic effects. Increasing evidence suggests that high-altitude discharges (lightning) in maturing plumes are driven by electrification processes that require the formation of ice (analogous to processes underpinning meteorological thunderstorms). However, electrical discharges are also common at or near the volcanic vent. A number of "ice-free" electrification mechanisms have been proposed to account for this activity: fractocharging, triboelectric charging, radioactive charging, and charging through induction. Yet, the degree to which each mechanism contributes to a jet's total electrification and how electrification in the gas-thrust region influences electrostatic processes aloft remains poorly constrained. Here, we use a shock-tube to simulate overpressured volcanic jets capable of producing spark discharges in the absence of ice. These discharges may be representative of the continual radio frequency (CRF) emissions observed at a number of eruptions. Using a suite of electrostatic sensors, we demonstrate the presence of size-dependent bipolar charging (SDBC) in a discharge-bearing flow for the first time. SDBC has been readily associated with triboelectric charging in other contexts and provides direct evidence that contact and frictional electrification play significant roles in electrostatic processes in the vent and near-vent regions of an eruption. Additionally, we find that particles leaving the region where discharges occur remain moderately electrified. This degree of electrification may be sufficient to drive near-vent lightning higher in the column. Thus, near-vent discharges may be underpinned by the same electrification mechanisms driving CRF, albeit involving greater degrees of charge separation.