This week, Jasmeer Sangha talks about his work extending his simulations to include many different species of planetary volatiles bouncing around on the moon. While water was known to be present, it was LCROSS (depicted above in this artist's concept image from Northrop Grumman) that discovered a wide range of different compounds in the PSRs.
by Jasmeer Sangha
This semester I chose to extend
my research past just water molecules and shift focus towards results brought
back from LCROSS, the Lunar Crater Observation and Sensing Satellite. The LCROSS
mission launched in 2009 and scientists found more than just water on the moon.
The mission objective was to have the Centaur, a rocket stage, launch itself into
the moon. It was decided that Cabeus, a large crater near the lunar south pole,
would be the Centaur’s destination. Cabeus is a permanently shadowed region which
allows freezing temperatures to trap particles in a layer a frost. The debris cloud made by the impact would be analyzed by LCROSS, orbiting up above, to discern the frost's composition.
From this experiment, it has been shown that carbon, nitrogen, and sulfur compounds
were present in Cabeus, yet water was the dominant constituent, outnumbering
all other compounds 5 to 1.
Though
we know what is in Cabeus crater we are unsure as to how it got there. My
previous work focused on the mechanism of traveling water molecules along the
surface. The program randomly spawned particles on the surface of the moon and
followed there lives until they were trapped in a dark hole for eternity, cooked
by the Sun’s rays, or lost to space - what lovely ways to go out, right? The results would show us how water ice is
distributed on the surface.
Thus,
from observations we know where the water is located and from simulations we know
how it made it there. Yet we still haven’t on touched on why there are these
volatiles jumping around on the moon’s surface. My new research aims to fill
this gap. It has been hypothesized that these volatiles were a result of a
combination of comets and asteroid impacts alongside solar wind deposits. The
solar winds consist mainly of alpha particles, protons and electrons. These are
stripped down hydrogen and helium particles which could recombine with heavier
elements to create water, ammonia and methane. Alternatively, comets and
asteroids often carry frozen volatiles on their surface that could easily
populate surrounding areas after impact.
My previous work has been
modified to simulate the travelling patterns of the other molecular substances
found in Cabeus crater. Each molecule type has very different properties to
consider: mass, dissociation energy and residence time being the most relevant. In
extreme cases, a change in mass can cause particles to be too heavy to make
large enough jumps into polar regions or so light that they fly off into space
with any influx of energy. Dissociation energy is linked to the robustness of
these molecules: their ability to stay together while being bombarded by
radiation from the sun. If a molecule is weekly bonded, it would be destroyed
before it could make progress towards any PSRs. Finally, residence time tells
us how long a particle will stick to a surface between hops: its easy to see
how small bouncy balls would have more interesting adventures compared to
Velcro. After considering these properties, the results spit out of the other
end can be compared to the observations from LCROSS. This comparison will allow
us to narrow down a list of candidates that could have made the deposits on our
Moon.
It is always exciting to start
new projects and this section of my research has not disappointed. Tweaking
small aspects of my code and watching as it creates a cascade of different
results reminds me of why I started this journey into physics. Tinkering with
marble tracks as a child, exploring Python toolboxes as a student, explaining
the simplicity yet complexity of planetary motion to muggles were always play
outside of work. I am lucky to have this opportunity to find play in the work I
am doing now, to be putting together this jigsaw or at least telling the
community, “Hey, I think this piece fits here!”
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