REM Experiment
The ESA-ESTEC REM on STRV-Ib completes the
suite of radiation measurement instruments flown on
the STRV-I mission. The GTO radiation environment
is mainly composed of electrons of a few MeV energy,
protons of up to several hundred MeV energy and
energetic heavy ions. The REM maps this environment
with good spatial resolution and over an extended
period, including the south Atlantic anomaly and
directionalites in the environment.
REM is a simple system consisting of two independent
shielded silicon detectors with different types of
shielding. Energetic particles impacting on the
detectors generate pulses which are counted, and the
number impacting in a set time are stored. By
separating pulses according to their magnitude (-E)
which depends on energy, the particle type and energy
data can be derived. Each detector has sixteen channels
of discrimination on pulse magnitude. The detectors
used are 300Tm silicon diode detectors. The "electron
detector" is 25 mm2 with a 3 mm aluminium shield.
while the larger "proton detector" of 150 mm: is
shielded by 3 mm of aluminium and an additional 0.75
mm of tantalum. The extra tantalum considerably
reduces the electron and bremsstrahlung penetration
and so makes this detector better at monitoring protons.
The electron detector shield stops protons of energies
below 24MeV and has an electron cut off around
1.4MeV. The proton detector has a cut off energy of
35MeV and suppresses incident electrons by a factor
-200. Despite the simplicity, by flying the experiment
in GTO and operating the experiment over an extended
period. with good time resolution, signif']cant data can
be generated. Additionally, knowledge of the pointing
direction can be used to investigate directionality in the
environment.
A copy of the REM is also mounted externally on MIR.
Both REM models have been operating simultaneously
during 1995. The correlation of the two instrument
data sets will prove highly valuable in the context of
modelling the environment. The results can also be
correlated with those made by complementary
experiments on the STRV-1 satellites and on other
spacecraft. Calibration is important to verify the
expected performance of the detectors and has been
performed in particle accelerators, complemented by
numerical simulations.
The instrument is operated continuously around an orbit
and under software control changes sampling rate
depending on time from perigee. To date, REM has
provided good quality data with few major problems.
Initial problems with the on-board processing software
were solved by uploading a modification to the
software. Similarly, accumulation times have been
optimised. Dead time corrections have also given some
problems but this is felt to have been solved. Some
noise at the most sensitive -E channels is also seen.
Extraction of particle spectra has taken longer than
expected due to the need to perform careful numerical
simulations before applying it to the counts data. The
counts data illustrate in qualitative terms the highly
dynamic nature of the outer, electron belt and the
relative stability of the proton belt. Correlations with
the 27 day solar rotation period are seen implying long-
lived solar structures well connected to the
magnetosphere during this phase of the solar cycle
(approaching solar minimum). This last year has seen
several long-lived energetic electron enhancements
reported from the NOAA GOES satellite and these shall