
January 9, 2009 10:21 World Scientific Book - 9.75in x 6.5in ws-bo ok975x65˙n˙2nd˙Ed
Displacement Damage and Particle Interactions in Silicon Devices 563
affected by the solar wind and flares. The trapped protons flux varies between 1
to 2×10
6
particles cm
−2
s
−1
with a maximum around 2.0 Re. In the inner zone, the
trapped electrons have energies . 5 MeV. The electron content of the inner zone
may vary considerably in time due to phenomena like solar wind or like nuclear ex-
plosions in upper atmosphere. A low flux of trapped ions of rigidities corresponding
¶
to a few MeV/nucleon and around (3–4) Re, mainly He and O with traces of C and
N, has been observed. These particles are believed to be extracted from the up-
per layers of the atmosphere during solar storms. SAMPEX data [Cummings et al.
(1993)] have also shown the existence of belts included in the inner zone, containing
nuclei such as N, O (of ≈ 10 MeV/nucleon) and Ne [of (10–100) MeV/nucleon]. The
filling mechanism of these SAMPEX belts is likely due to the interaction of the
anomalous cosmic rays with the Earth atmosphere (in anomalous cosmic rays there
are more α-particles than protons and much more oxygen than carbon while in the
galactic cosmic rays there are more protons than α-particles and equal amounts
of oxygen and carbon). Recently, belts below the inner belt zone, at ∼ 1.0 Re,
have been observed by the AMS experiment [AMS Collab. (2000a,b,d, 2002)] with
a relatively large content of electrons, positrons, deuterium and
3
He with rigidi-
ties of 10
2
–10
3
MeV/nucleon. The origin of the AMS belts is believed to result
from the interaction of primary cosmic rays with the atmosphere. The outer b elt
zone is mainly populated with electrons of energies ∼ 7 MeV (up to 10 MeV), with
a flux of an order of magnitude higher than in the inner zone and peaking at
about 5 Re. The trapped electrons flux in the outer zone varies between 10
3
and
2 × 10
6
particles cm
−2
s
−1
. This outer zone is filled by the solar wind.
7.2.3 SEE in Atmospheric Radiation Environment
The atmospheric environment originates from the cosmic ray cascades in the Earth’s
atmosphere and are a concern for avionics. This environment results from the inte-
raction of cosmic rays with atmospheric atoms through ionization or nuclear re-
actions. The isotopic content of the atmosphere is predominantly made of oxygen
(21.8%, Z = 8), nitrogen (76.9%, Z = 7) and argon (1.3%, Z = 18). These nu-
clear reactions are mostly induced by the primary protons which dominate (≈ 87%)
the incident cosmic ray flux and generate secondary particles through elastic and
inelastic scatterings, mainly neutrons (90% and more), pions, kaons, muons (from
charged pion and kaon decays), photons (from neutral pion decays and photopro-
duction reactions), muons from pion decays and electrons from muon decays and
gamma conversion. The neutron component is of interest for avionics although these
neutrons can penetrate the whole atmospheric depth. However, the flux of particles
(neutrons, protons, pions and kaons) is decreasing with altitude and latitude. For
instance, the flux of neutrons is attenuated by their collisions with atmospheric
atoms, thus decreasing the neutron flux at lower altitudes. The Earth’s magnetic
¶
The reader can find the definition of kinetic energies per nucleon in Sect. 1.4.1.