Tides,
Orbit, and Gravity of the Moon

I am intersted in novel tidal and orbital dynamics processes
applied to the early Moon (PDF).
Such processes can tell us about the orientation, gravity field,
orbital state, and possibly the global geology and geochemisty of the
Moon we see today. I am also interested in how accretional
processes in the debris disk after the giant impact may have affected
the evolution of the Moon.
Above: one component of the lunar tidal
potential.
Lunar Paleomagnetism

Planetary magnetism is an excellent means of understanding the thermal
history and internal workings of a body. By studying the magnetic
remanence in lunar samples brought back by the Apollo missions we hope
to determine if the Moon's interior ever developed a magnetic
dynamo. Much of the work on lunar magnetism stopped by the mid
1980s, but there are good reasons to continue its study. In
particular, the remanence in very old samples has not been fully
explored. Also, instrument sensitivty and measurement techniques
are now much better, and much less sample material is required to
obtain useful results.
Above (left to right): Source boulder for 78235/6, 78236 in the lab on
a 3 mm diameter quartz rod,
a mosaic I pieced together showing the small source crater for 78155,
and 78155 in the lab on a 2.5 cm diameter quartz disc.
Lunar
Basins: Geology, Geochemistry, and Geophysics


Thorium is a great tracer element for understanding the thermal and
chemical evolution of the lunar crust. It is also easily measured
from orbit. I am interested in what thorium in the
farside South Pole-Aitken basin tells us about global lunar evolution (PDF). I am also intersted in
what controls the appearance of structural features of the largest
basins in general. What can the largest basins tell us about
large-scale properties of the bodies they impact?
Above: topography, thorium, and a
multispectral image of the lunar South Pole-Aitken basin.
Engineering
and Space Flight
From time to time I work on engineering ideas that are aimed at increasing
science
return from
robotic or human space flight. Several examples include concepts
to explore asteroids (PDF),
concepts to explore the lunar poles (PDF, PDF), lunar sample return
techniques (PDF), and illumination conditions
at lunar polar landing sites (PDF).
Above (left to right): Press from
Ciel et Espace and New Scientist magazines, illumination map of the
lunar poles, and my concept to explore the lunar poles from a commonly
proposed
NASA landing site.