In situ optical measurement of the interplanetary dust concentration from Earth’s orbit
Abstract
The amount of interplanetary dust impacting the Earth’s atmosphere is still not well estimated, in terms of
total mass, size distribution, and concentration of particles. We propose to apply the counting techniques used
in the Earth’s atmosphere for determining the concentration of liquid and solid aerosols, to the detection of
these interplanetary particles. The main differences with the Earth’s atmosphere measurements are the very low
concentrations, the high speed of the particles (at least several km/s) and the space conditions.
We have developed recently an innovative design of aerosols counter, called LOAC, which provides the concen-
trations for 19 size classes of particles in the 0.2-50 micrometer range, and also an estimate of their typology (or
their light absorbing properties). The particles are injected through a laser beam via a pumping system, and two
photodiodes record the light scattered. This instrument combines the measurements at two different angles, the
first at around 15° being insensitive to the refractive index and porosity of the particles, and the second one around
60° being very sensitive to the nature of the particles. LOAC is used in routine since 5 years on the ground and
from all kinds of balloons for the troposphere (mainly pollution) and stratosphere monitoring, and is also involved
in various international campaigns.
An updated version of LOAC is in development for space applications, essentially for in situ measurements
planetary atmospheres. LOAC can also be modified for the detection of high velocity particles, by using a light
source of several cm long instead of a laser beam. No pump is needed, since the particles will cross an open cell
oriented at a constant angle from the motion of the instrument. This instrument could perform measurements in
Earth orbit, onboard a micro-satellite or on the International Space Station.
We will present this new concept of instrument, and how the measurements can be used to better constrain the
nature and flux of the incoming interplanetary materia