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<supportEmail caption="Support">icrc2007@icrc2007.unam.mx</supportEmail>
<title>30th International Cosmic Ray Conference</title>
<description>The 30th International Cosmic Ray Conference will be held from July 3, 2007 to July 11, 2007 in Merida, Yucatan, Mexico.</description>
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 <name>Merida, Mexico</name>
 <address></address>
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<startDate>2007-07-03T08:00:00</startDate>
<endDate>2007-07-11T19:00:00</endDate>
<creationDate>2005-09-26T05:04:53</creationDate>
<modificationDate>2024-04-12T17:46:55</modificationDate>
<timezone>Mexico/General</timezone>
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  <name first="José" middle="" last="Valdés"></name>
  <organization>IGeof-UNAM</organization>
  <emailHash>40af9343b8bb9d18708b4f0252d5f53c</emailHash>
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 <title>Observations of primary, trapped and quasi trapped particles with PAMELA experiment</title>
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   <title>Dr.</title>
   <name first="Marco" middle="" last="Casolino"></name>
   <organization>INFN ROma2</organization>
   <emailHash>04f6f2576cb478f78f798467b20eee87</emailHash>
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   <title>Dr.</title>
   <name first="Marco" middle="" last="Casolino"></name>
   <organization>INFN ROma2</organization>
   <emailHash>04f6f2576cb478f78f798467b20eee87</emailHash>
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  <name>Merida, Mexico</name>
  <address></address>
  <room>Regency (Hyatt)</room>
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 <startDate>2007-07-06T14:45:00</startDate>
 <endDate>2007-07-06T14:45:00</endDate>
 <abstract>PAMELA  was launched   on June $15^{th}$ 2006 in a pressurized container on board the
Russian Resurs-DK1 satellite.  The satellite is flying  in high inclination ($70^o$),
low Earth Orbit (350-600 km),  performing  measurements in different points and
conditions of the geomagnetosphere.  The device is a multi-purpose apparatus 
composed of a permanent magnet spectrometer to provide particle charge,  rigidity and
incoming angle. A  series of  six 
scintillator  counters arranged at its  extremities provide redundant Time-of-Flight
and  charge data.   Lepton/hadron identification is performed  by a
Silicon-Tungsten calorimeter and a Neutron detector placed at the
bottom of the device. An Anticounter system is used offline to
reject false triggers coming from the satellite. 
PAMELA  is capable of detecting protons (80 MeV- 700 GeV), antiprotons (80 MeV-190
GeV), electrons (50 MeV -  400 GeV), positrons  (50 MeV - 270 Gev) and nuclei
($\simeq 100 MeV/n 200GeV/nuc). In addition a tecnhique employing  scintillator
counting rate and range energy methods allows  to lower the minimum  detectable
energy range of the apparatus to 36 MeV and 3.5 MeV for protons and electrons
respectively.  
The orbit of the satellite and the characteristics of the magnet tracker allows
PAMELA to perform  a very detailed measurement of the nature and spectra of primary
(above cutoff) and secondary particles (sub-cutoff: trapped, reentrant albedo, etc.).
The precise measurements of   particle distribution in different regions of the orbit
  provides information on the processess of  production, propagation and interaction
of particles in Earth’s magnetosphere.  In this work we will also  discuss different
methods of calculation of geomagnetic coordinates and  particle cutoff comparing them
with expected  and measured fluxes.</abstract>
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