Wei Zhu(祝伟)
I'm now an Assistant Professor in the Department of Astronomy at Tsinghua University in Beijing.
Wei Zhu (祝伟)
2019 May 9, Group Meeting
0.4 \(R_\oplus\)
0.9 \(R_\oplus\)
1.0 \(R \oplus\)
0.5 \(R \oplus\)
11 \(R \oplus\)
9 \(R \oplus\)
4.0 \(R \oplus\)
3.9 \(R \oplus\)
Mars' low mass places challenges on solar system formation theories \( \rightarrow \) grand tack model (Walsh et al. 2011)
Image credit: Lunine et al. (2009)
Planetesimal formation
Run-away
growth
Pebble
accretion
Oligarchic
growth
Giant impact
phase
If formation stops after oligarchic growth (i.e., at isolation mass), then planets should have similar sizes and regular spacings.
Terrestrial
planet form
Image credit: Lissauer et al. (2011)
HATNet
Keck
KMTNet
Kepler
See also Millholland, Wang, & Laughlin (2017) for the claim of mass similarity
Peas in a Pod: Planets in a Kepler Multi-planet System Are Similar in Size and Regularly Spaced
Data
One bootstrap trial
Weiss et al. (2018)
Statistical distribution
Radius of inner planet
Radius of outer planet
Radius of inner planet
Radius of outer planet
Data
One bootstrap trial
Weiss et al. (2018)
Statistical distribution
Inner period ratio
Outer period ratio
Inner period ratio
Outer period ratio
Image credit: Lunine et al. (2009)
Planetesimal formation
Run-away
growth
Pebble
accretion
Oligarchic
growth
Giant impact
phase
If formation stops after oligarchic growth (i.e., at isolation mass), then planets should have similar sizes and regular spacings.
Terrestrial
planet form
Stellar photometric noise over 6-hr integration (\( {\rm CDPP}_{\rm 6hr}\))
Kepler
K2
Conclusion:
Strong (weak) detection \(\approx\) large (small) planet
\[ \downarrow \]
Large planets should almost always have small companions
Data used in Weiss et al. (2018)
All planet triplets
Image credit: Lunine et al. (2009)
Planetesimal formation
Run-away
growth
Pebble
accretion
Oligarchic
growth
Giant impact
phase
If formation stops after oligarchic growth (i.e., at isolation mass), then planets should have similar sizes and regular spacings.
Terrestrial
planet form
Image credit: Lunine et al. (2009)
Planetesimal formation
Run-away
growth
Pebble
accretion
Oligarchic
growth
Giant impact
phase
Terrestrial
planet form
Given an initial mass contrast, what is the final?
(too big to fail in planet formation?)
HATNet
Keck
KMTNet
Kepler
Hot Jupiters
(~1%)
Cold Jupiters
(~10%)
Cold Neptunes
Super Earths
(30%)
Data from NASA Exoplanet Archive
By Wei Zhu(祝伟)
Presentation at Norm Murray group meeting
I'm now an Assistant Professor in the Department of Astronomy at Tsinghua University in Beijing.