Cometary Origin of the Zodiacal Cloud and Carbonaceous Micrometeorites
David Nesvorny, Peter Jenniskens, Harold F. Levison, William F., Bottke, David Vokrouhlicky

TL;DR
This paper models the zodiacal cloud's origin, emphasizing the dominant role of Jupiter-family comets, and links cometary debris to the primitive carbonaceous micrometeorites found on Earth.
Contribution
It introduces a quantitative model of the zodiacal cloud based on comet and asteroid dynamics, highlighting the dominance of JFCs and their disruption as the primary dust source.
Findings
85-95% of mid-infrared emission from JFCs
<10% dust from long period comets
Most micrometeorites are primitive carbonaceous
Abstract
The zodiacal cloud is a thick circumsolar disk of small debris particles produced by asteroid collisions and comets. Here, we present a zodiacal cloud model based on the orbital properties and lifetimes of comets and asteroids, and on the dynamical evolution of dust after ejection. The model is quantitatively constrained by IRAS observations of thermal emission, but also qualitatively consistent with other zodiacal cloud observations. We find that 85-95% of the observed mid-infrared emission is produced by particles from the Jupiter-family comets (JFCs) and 10% by dust from long period comets. Asteroidal dust is found to be present at 10%. We suggest that spontaneous disruptions of JFCs, rather than the usual cometary activity driven by sublimating volatiles, is the main mechanism that librates cometary particles into the zodiacal cloud. Our results imply that JFC particles…
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