David
Polishook – Research Projects
Flybys of
Near-Earth Asteroids Applying
tidal forces, the Earth can modify asteroids that pass very close to it: the asteroid
can spin-up, shakes can roll boulders and rocks, sub-surface material can be
exposed, and its entire shape can change. Only by
observing asteroids before and after their flybys, and measure the change (or
non-change) in their parameters we can study the strength and elasticity of
the internal structure. This allows us to predict what will happen to a
future impactor before colliding with the Earth and
what measures should be taken in order to destroy or deflect it. Image: The changed orbit of 2012
DA14, during its flyby on February 15, 2013. Polishook et al. 2012, Icarus 221. |
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Asteroids
disintegration by rotational fission The newly discovered category of
asteroid pairs consists of gravitationally unbound pairs that once
belonged to a single body. Studies showed that asteroid pairsÕ progenitors were
spun-up by the YORP effect, until they gain sufficient angular momentum to
cross the breakup limit for a strength-less object, known as the Òrubble pile
spin barrierÓ, and these asteroids split into two components. The study of asteroid pairs and
the way asteroids can disintegrate has manifold applications: while it
teaches us on their internal structure, it can also demonstrate the strong
forces that shaped the early solar system at the early stages of planet
formation. Image: Rotation
periods of asteroid pairs is correlated to the size ratio between the small
and large members of each pair. Polishook 2014. Accepted
to Icarus. arXiv:1406.3359 – spin axes of asteroid pairs were modified
by the YORP effect suggesting the YORP effect spin them up and not collisions.
Also – the first linkage found that asteroid pairs have low density values as expected from Òrubble-pileÓ
asteroids. Polishook et al. 2014. Icarus 233 – the
secondary member of a pair might split due to a secondary fission. Pravec, Vokrouhlicky, Polishook, et al. 2010. Nature 466, and its Press Release
– asteroid pairs are formed by the rotational-fission mechanism. Polishook et al. 2011. Icarus 212 – binary
asteroids with high separation were formed by the YORP effect. Vokrouhlicky, Durech, Polishook, et al., 2011, AJ 142 – the spin
state of the youngest asteroid pair 6070 Rheinland. |
Thermal forces
modify asteroids Re-emission of sunlight from
atmosphere-less bodies can modify their orbit (the Yarkovsky
effect), impose a torque on their spin, and change their rotational axis.
This mechanism has significant role in transporting small bodies in the Solar
System, forming near-Earth asteroids; splitting fractured bodies by spinning
them up; determining the special and size distribution of small bodies in the
Solar System through its history. We study the
parameters relevant for this mechanism, such as size and spin, and its
effects on asteroids such as spin distribution and formation of binaries. Image: The effect
of asteroidÕs spin on the YarkovskyÕs efficiency. Polishook et al. 2011. Icarus 212 – binary
asteroids with high separation were formed by the YORP effect. Polishook et al. 2010.
DPS meeting #42, p. 1055 – Yarkovsky
effect dependent on asteroidÕs spin. Polishook & Brosch 2009, Icarus
199 – Spin distribution of small main-belt asteroids is
controlled by the YORP effect. |
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Space Weathering Surfaces of atmosphere-less
bodies are modified with time by the Òspace weatheringÓ effect. This mechanism,
caused by solar wind, cosmic rays and micrometeorite bombardment alter the
top layer on planetary surfaces, causing it to display a ÒweatheredÓ, darker
and redder reflectance spectrum. Space weathering mechanism is not yet
understood: different bodies and materials present different amount of
weathering, and current estimations of its timescale differ dramatically from
one another, and range between 104 to 109 years. The effect of space
weathering on asteroids obscures their true nature. Understanding it will
help us determine their true composition, origins, and their role in planet
formation. Image: lunar sample
that shows the formation of a ÒweatheredÓ coating on the surface. Clark et
al. 2002 Asteroids III, 585-599. Polishook et al. 2014. Icarus 233 - Fresh
Surfaces Observed in the Main Belt on asteroid pairs! Polishook et al. 2009, M&PS 44 – looking for fresh surfaces by
rotational spectroscopy. |
Mining Astronomy Asteroidal
data were ÒminedÓ from the Palomar Transients Factory (PTF),
a survey with exceptionally wide field of view (7.2 square
degrees) on a 48ÕÕ telescope, dedicated for transient search. Our
pipeline detects asteroids in the PTF images, constructs their lightcurves, and calculates their rotation periods. The
pipeline was tested on data from four nights covering an area of ~21 deg2,
and was able to detect 624 asteroids, of which 145 were previously unknown.
Rotation periods for 173 asteroids were derived. 3 of the asteroids are
probably binary asteroids. We estimate that implementing our search for all
existing high-cadence PTF data will provide rotation periods for thousands of
asteroids. Image: Asteroids tracks on the PTFÕs
large field of view. Polishook et
al., 2012, MNRAS 421. |
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