The findings could help identify smaller near-Earth objects - such as the Chelyabinsk meteor that exploded over Russia in 2013 - before they blast through Earth's atmosphere, according to study co-author Hanying Wei, a researcher in earth, planetary and space sciences at the University of California at Los Angeles (UCLA).
Smaller space rocks and ultrafine dust often trail the massive near-Earth objects that circle the Sun.
Even if the main asteroid never comes close to the planet, Earth's gravitational pull can peel the smaller orbitals off and bring them directly toward the planet.
When meteoroids randomly collide with the medium-size rocky bodies in the dust cloud around an asteroid, even tiny particles can pulverise the much larger objects, creating an ultrafine haze of dust.
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The researchers wondered whether the presence of this fine dust, a byproduct of these catastrophic collisions, could help identify asteroids with large amounts of debris as well as the smaller near-Earth objects trailing them.
Photons ping the surface of the fine dust particles, knocking off electrons and leaving the dust positively charged, Wei said.
Several spacecraft in the solar system have onboard magnetometers that can detect these magnetic signatures of collision.
By using data from multiple spacecraft on the size and scale of the magnetic field perturbations, along with previously derived data on the speed and characteristics of known interstellar bodies, the team can calculate the size and shape of a trailing debris cloud.
These asteroids circle the Sun year after year, the researchers can map how the debris trail changes over time. From there, existing simulations can reveal whether Earth is in the path of rocky debris, Lai told 'Live Science'.
In contrast, Asteroid 308635, which circles the Sun every 455 days, does not carry much rocky debris in its wake.