Author biography
1 The Scientific Legacy of Giant-planet Research
2 The Planet-forming Environment
3 Microscopic to Macroscopic: Grain Growth and Pebble Formation
4 From Pebbles to Planetesimals
Sarah Dodson-Robinson received her PhD in Astronomy & Astrophysics from University of California at Santa Cruz in 2008, then took a Spitzer Postdoctoral Fellowship at NASA Exoplanet Science Institute. She is now an Associate Professor of Physics and Astronomy at University of Delaware. In 2013, she won the American Astronomical Society’s Annie Jump Cannon award for her contributions to the study of planet formation. Dr. Dodson-Robinson conducts numerical simulations of the chemical and dynamical evolution of planet-forming disks and participates in observational studies of debris disks. She also develops and tests methods for distinguishing exoplanet discoveries from stellar noise.
Sarah Dodson-Robinson undertaking is all the more remarkable as a
tour de force because this is only volume one of two. She follows
giant-planet formation through the gas-dominated stages of cloud
contraction into protoplanetary discs, condensation to dust and
pebbles, and then into rubble-pile planetesimals. The effects of
self-gravity, mutual gravitational interactions, and orbital
migration are deferred until the second volume, although the final
chapter steps across that threshold in discussing the Martian
hafnium and tungsten isotopic record as tracers of the timing of
embryo growth. Even though the theme is giant-planet origins,
inevitably there is much of relevance to rocky planets, meteorites,
and the Kuiper Belt too. All chapters, after the entertaining
introductory history-of-ideas chapter, abound in generally rather
complicated equations. Dodson-Robinson writes well and engagingly,
especially given the burden of all the equations. This is not a
book for the mathematically faint of heart, but there are boxes
that take the reader aside for a generally more 'friendly' chat. I
particularly appreciated the four pages of Box 3.1 that describe
and summarize the size progression of giant planet fore-runners
including the stages of planetesimal collisions and/or pebble
accretion and then gas accretion that will feature in Volume 2.
Citations of peer-reviewed papers abound in the text, and each
chapter concludes with several pages of references so that this
book would provide a good entry into the field for new researchers.
I would expect it to have a decade long useful life in
institutional libraries. It is well illustrated, mostly in
colour.
David Rothery, The Observatory, October 2022
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