# Spectra and physical properties of Taurid meteoroids

## TL;DR

This study analyzes the spectral, orbital, and physical properties of Taurid meteoroids from video observations, revealing their cometary origin, heterogeneity, and low material strength, with implications for understanding their source and composition.

## Contribution

It provides the first comprehensive spectral and physical characterization of Taurid meteoroids, including the widest spectral classification to date, and links their properties to cometary origins.

## Key findings

- Taurid meteoroids show heterogeneous spectral and physical properties.
- They break up under low dynamic pressures of 0.02 - 0.10 MPa.
- Spectral analysis indicates a cometary origin with diverse compositions.

## Abstract

Taurids are an extensive stream of particles produced by comet 2P/Encke, which can be observed mainly in October and November as a series of meteor showers rich in bright fireballs. Several near-Earth asteroids have also been linked with the meteoroid complex, and recently the orbits of two carbonaceous meteorites were proposed to be related to the stream, raising interesting questions about the origin of the complex and the composition of 2P/Encke. Our aim is to investigate the nature and diversity of Taurid meteoroids by studying their spectral, orbital, and physical properties determined from video meteor observations. Here we analyze 33 Taurid meteor spectra captured during the predicted outburst in November 2015 by stations in Slovakia and Chile, including 14 multi-station observations for which the orbital elements, material strength parameters, dynamic pressures, and mineralogical densities were determined. It was found that while orbits of the 2015 Taurids show similarities with several associated asteroids, the obtained spectral and physical characteristics point towards cometary origin with highly heterogeneous content. Observed spectra exhibited large dispersion of iron content and significant Na intensity in all cases. The determined material strengths are typically cometary in the $K_B$ classification, while $P_E$ criterion is on average close to values characteristic for carbonaceous bodies. The studied meteoroids were found to break up under low dynamic pressures of 0.02 - 0.10 MPa, and were characterized by low mineralogical densities of 1.3 - 2.5 g cm$^{-3}$. The widest spectral classification of Taurid meteors to date is presented.