The HILT sensor has been designed to measure heavy ion elemental abundances,
energy spectra, and direction of incidence in the mass range from helium to
iron and in the energy range 4 to 250 MeV / nucleon. With its large geometric
factor of 60 cm^2-sr the sensor is optimized to provide compositional and
spectral measurements for low intensity cosmic rays, i.e. for small solar
energetic particle events and for the anomalous component of cosmic rays. The
instrument combines a large area ion drift chamber - proportional counter
system with two arrays of 16 Li-drift solid state detectors and 16 CsI
crystals. The multi dE/dx - E technique provides a low background mass and
energy determination. The sensor also measures particle direction. Combining
these measurements with the information on the spacecraft position and
attitude in the low altitude polar orbit, it will be possible to infer the
ionic charge of the ions from the local cutoff of the Earth's magnetic
field. The ionic charge in this energy range is of particular interest
because it provides unique clues to the origin of these particles and has not
been investigated systematically so far. Together with the other instruments
on board SAMPEX (LICA, MAST, and PET), a comprehensive measurement of the
entire solar and anomalous particle population will be achieved.
I. Introduction
The HILT (Heavy Ion Large Telescope) sensor, together with the LICA sensor,
was originally developed for a Get-Away-Special Payload (G-0335) to measure
solar and anomalous cosmic rays in a high inclination shuttle orbit at solar
minimum conditions [1]. The payload was scheduled for a series of STS flights
starting in 1986. However, because of the Challenger accident, it was delayed
and finally flown only once on the space shuttle mission STS-28 in August
1989. In a collaborative effort of the Max-Planck-Institut fuer
Extraterrestrische Physik and the Aerospace Corporation, the HILT sensor has
been modified to extend the range of elements and energies covered. The
measurements now include heavy ions from helium to iron in the energy range
from 4 to 250 MeV / nucleon. The sensor thus covers the maximum intensity of
the anomalous component of cosmic rays and the medium energy range of solar
energetic ions. The sensor utilizes a large area ion drift chamber, two
position sensitive proportional counters, an array of 16 silicon solid state
detectors and a CsI crystal unit to determine the nuclear charge, the energy,
and the direction of ions entering the telescope. In the low altitude (~600
km) polar orbit of SAMPEX, this information will be used to infer the ions'
ionic charge from the local cutoff of the magnetic field of the Earth.
II. Scientific Objectives
Solar Energetic Particles
During the last few years it has been recognized that solar energetic
particle events (SEP) can be divided into two classes, based on the time
scale of the electromagnetic emissions of their associated flares. SEP events
associated with impulsive flares have mostly low particle intensities, high
3He / 4He flux ratios, enhanced abundances of heavy elements, charge states
indicative of heated flare plasma (~10^7 K), high electron to proton flux
ratios and high ratios of solar (interacting or trapped) to interplanetary
(escaping) protons. The SEP events associated with gradual flares are
characterized by large particle intensities in interplanetary space, low 3He /
4He ratios, low electron to proton flux ratios, low ratios of solar to
interplanetary proton intensities and charge states indicative of typical
(2x10^6 K) coronal temperatures (e.g.[2] and references therein). Due to the
limited collecting power of the instrumentation previously flown, composition
and energy spectra for impulsive events have been studied only over a small
energy range (e.g. [3], [4]). HILT, with its large geometric factor of 60
cm^2-sr, will provide spectral and compositional information in particular for
the low intensity events associated with impulsive flares. At high flux
levels (> 5 protons / cm^2 s sr MeV/n at 5 MeV) pulse pile-up and accidental
coincidences will degrade the performance of the instrument. However, flux
levels exceeding this value are observed in interplanetary space only during
very large, shock associated energetic particle events. However, with the four
instruments of the SAMPEX payload a comprehensive measurement of the entire
SEP population will be achieved (see also [5], [6]).
The large temperature differences as derived from heavy ion charge states
observed in impulsive and gradual flares [7] show that the charge state
measurement provides crucial information. So far charge state measurements
have been obtained only at energies < 3 MeV / nucleon during a limited time
period on ISEE-3 [8]. In the low altitude polar orbit of SAMPEX, it will be
possible to extend these studies using the geomagnetic cutoff as described
below.
Anomalous Component of Cosmic Rays
The anomalous component of cosmic rays (ACR) has been studied extensively
since its discovery in the 1972-1977 solar minimum. In the energy range below
~50 MeV/nucleon, at least 6 elements have been found (He, C, N, O, Ne, Ar)
whose energy spectra show anomalous increases in flux above the quiet time
galactic cosmic ray spectrum and whose composition is different from the solar
or galactic cosmic ray composition [9]. There have been a number of models
proposed to explain the ACR component. The most plausible theory for the
origin of the ACR identifies neutral interstellar gas as the source material
(Fisk et al. [10]). The neutral particles, after penetrating into the inner
heliosphere, are ionized by solar UV radiation or by charge exchange reactions
with solar wind protons. After ionization, the now singly charged ions are
picked up by the interplanetary magnetic field and carried with the solar wind
to the outer heliosphere. There the ions are accelerated to high energies,
possibly at the solar wind termination shock [11]. A unique prediction of
the model of Fisk et al. is that the anomalous cosmic rays should be singly
ionized. Although indirect evidence for low charge states of the ACR has
been found in many investigations (e.g. [12], [13]), results from a more
direct measurement using the transmission of the Earth's magnetic field are
sparse [14], [15]. It was only recently that a more systematic study of ACR
oxygen charge states was started in a collaborative effort of many
institutions [16]. The large collecting power of HILT and MAST [17]
combined with an accurate measurement of time, position, and particle
direction should overcome many of the difficulties encountered previously and
provide definitive measurements of the charge state of oxygen and the less
abundant ions of anomalous cosmic rays.
Recently, the discovery of anomalous cosmic ray oxygen trapped in the Earth's
magnetosphere after charge exchange at low altitudes has been reported [18].
The low altitude polar orbit of SAMPEX will provide an excellent opportunity
to study this newly discovered trapped component in great detail and to extend
the present measurement of trapped oxygen to the less abundant ions.
Determination of Ionic Charge States
The geomagnetic cutoff can be used to infer the ionic charge of heavy ions.
The cutoff rigidity, Rc, depends in general on the location in the magnetic
field of the Earth and on the direction of the particle. The local cutoff Rc
can be computed by using a model of the magnetic field of the Earth and
trajectory tracing techniques. The particle rigidity, R, depends on kinetic
energy per nucleon (T), mass (A), total energy per nucleon (T+E0), and ionic
charge (Q) as
III. Instrument Description
The HILT sensor determines the mass, kinetic energy, and direction of
Principle of Operation
The element or mass analysis is based on the combination of a multi dE/dx
measurement in the position sensitive proportional counter and ionization
chamber system with the measurement of residual energy in the SSD detector
array and the CsI crystal unit.
The direction of incidence is derived from two
position measurements as described below. With the information of particle
energy, mass, and direction, in combination with the spacecraft position and
attitude in the low altitude polar orbit, it will be possible to infer the
ionic charge of the ions from the local cutoff of the Earth's magnetic field.
The Ion Drift Chamber - Proportional Counter System
The drift chamber-proportional counter system consists of three sections
(Fig. 2). Electrons generated along the path of incoming ions drift in the
electric field (85 V/cm) of the chamber to the front proportional counter
(section I, PCF), to a charge collecting plate (section II, IC), and to the
rear proportional counter (section III, PCR). The drift field is generated by
a set of parallel wires (Mo, diameter 100 microns, spacing 5 mm) enclosing the
drift chamber. In order to improve the homogeneity of the drift field near
the wires, the inner layer of wires is enclosed by a second layer at a
distance of 2 cm (see Figure 2, note: only the top and bottom layers of wires
are shown). In the first and third section of the drift chamber energy loss
and position of the ions are determined by 2 position sensitive proportional
counters with triangular shaped cathodes, the centre element is operated as an
ionization chamber and provides a third energy loss measurement. The energy
loss of ions in all 3 sections is pulse height analyzed. The triple dE/dx
measurement, in combination with the determination of the residual energy of
the ions, provides a low background identification of ion type and energy in
the mass range from helium to iron. In addition to the nuclear charge
(element) resolution, the sensor also provides mass identification capability
for helium (see also Table 1).
The signals of the triangular shaped cathodes of the proportional counters are
also pulse height analyzed. The ratios of the position and energy signal are a
direct measure of the position along the proportional counter axis. In section
I also the time elapsed between the response of the SSDs and the anode of PCF,
i.e. the drift time of electrons generated along the track of incoming ions,
is determined. Thus, drift time and position response of PCF provide two
coordinates for the incoming ions at the top plane of the sensor. At the
bottom plane the position response of PCR and the information on the detector
row triggered by the incoming particles provide the other two coordinates. The
trajectory of the incoming ions can be determined from these four coordinates.
The accuracy of the determination of the incident angle is limited by the
diameter of the detectors and the energy and position response of the
proportional counters and is typically 5 degrees for Z >= 6 ions at =< 40 MeV
/ nucleon. The trajectory information will be used for a path length
correction of the energy loss measurement in the proportional counter -
ionization chamber system to improve the elemental resolution of the sensor.
The Isobutane Regulation System
The drift chamber-proportional counter system operates with Isobutane at a
pressure of 100 mbar ( at 20 C). The density of the Isobutane is actively
controlled by a gas regulation system consisting of a thermally controlled
valve, a small ionization chamber with built-in 241Am radioactive source
(Alphatron), and regulation electronics. The volume of the Alphatron is
directly connected to the sensor volume and the current from the 241Am source
is used in the regulation electronics for the control of the Isobutane inflow
by opening or closing the thermal valve. The Isobutane outflow can be
controlled by a motor driven vent valve and flow regulation valve. The gas
supply consists of 7.2 kg of liquid Isobutane, stored in one cylindrical
aluminium - kevlar composite tank in the centre of the spacecraft, and is
sufficient for a continuous operation of 3 years. Similar regulation systems
have been successfully flown on several MPE experiments for the IMP-7/8, S3-2,
and ISSE-1/3 missions.
The Solid State Detector Array
Low energy ions are stopped in one of 16 circular Li-drifted silicon solid
state detectors. The thickness of the detectors is 2 mm and the sensitive area
is 995 mm^2. The detectors are arranged in an 4 x 4 array with one row of 4
detectors connected to one amplifier chain. In addition to the pulse height
analyzed energy signal the information on the particular row triggered by an
ion is transmitted with the pulse height information. The total sensitive
area and the sensor geometry result in a geometric factor of 60 cm^2-sr for
the coincidence measurement (see also Table II).
The CsI Crystal Array
High energy ions penetrating the solid state detectors are stopped in a set of
16 circular CsI crystals of 5 mm thickness and 46 mm diameter which are
arranged behind the SSD array. The CsI signal is used to define low energy
rates (CsI in anticoincidence) and high energy rates (PC-SSD-CsI
coincidences, see also Tables I and II ) for helium and Z>=6 ions. The CsI
coincidence measurement extends the energy range of the sensor to 250 MeV /
nucleon (for neon), however, without an anticoincidence measurement in the
high energy section. The crystals are embedded in a rectangular plate
(PERSPEX) of 2 cm thickness and are viewed by 4 light sensitive silicon
detectors. Due to limitations in the energy resolution of the CsI unit and the
smaller signals in the IC-PC system for high energy ions the directional and
elemental resolution is reduced, compared to low energies, and not sufficient
to provide isotopic resolution for helium. However, elemental resolution for
the more abundant elements can still be achieved (see Table I).
Electronics and Data Handling
Fast analog electronics provide the basic counting rate information needed for
the computation of absolute fluxes, while pulse height analysis contains the
detailed energy, mass, position and time information. All the information is
read out and accumulated in the SAMPEX digital processing unit (DPU) and
transmitted from there to the mass memory of the spacecraft data system [19].
The instrument analog electronics are designed to cover the energy range from
a few MeV / nucleon to 5000 MeV total energy loss in the detector arrays for
the elements in the mass range from helium to iron. A simplified block diagram
is shown in
Rate Data
The rate data are derived from fast thresholds at the output of ten charge
sensitive amplifier chains. These thresholds are used in the Event
Classification Unit (ECU) to define four rate channels, two for helium and
two for Z >= 6 ions (Basic Rates). These rates are accumulated and readout by
the Digital Processing Unit (DPU) every 6 seconds. In addition to the Basic
Rates, the lowest thresholds of all detector elements used in the ECU, three
diagnostic rates on coincidence conditions, and the idle time of the system
(to be used for dead time corrections), are monitored with reduced time
resolution. These monitor rates provide integral measurements of the
particle distribution and information on the health and safety of the
experiment. Furthermore, low thresholds on the IC, PCR, and SSD1-4 channels
are directly fed into the DPU and read out every 0.1 s providing information
on particle intensity variations on a much shorter time scale. The monitor
and high time resolution rates from the front and rear proportional counter
are also sensitive to electrons which are scattered in the front foil or in
the solid state detector array and then penetrate the ionization chamber at
oblique angles. However, because of the low efficiency of the electron
response (2 * 10^-4, see also Table II ), these rates will be dominated by
electrons only during passes of the electron radiation belts of the Earth.
The coincidence logic in the ECU can be switched by command into a mode where
signals from the PC-IC system are not included in the coincidence conditions
(High Energy Mode). This mode will be used after the Isobutane counter gas is
all used up and thus will recover the SSD-CsI coincidence measurement.
However, because no path-length correction is possible without the
proportional counter systems, the elemental resolution will be degraded and
only allow the resolution of element groups (e.g. He, CNO, see also Table I).
With the Isobutane system in operation, this mode can also be used to obtain
measurements of proton spectra. A summary of the response of all the rate
channels is provided in
Pulse Height Event Data
The signals of all channels are pulse height analyzed. The information on the
signal amplitudes, the event type, the SSD row triggered and the time of
observation is transmitted as one pulse height event. The DPU has complete
control of the HILT event readout and a priority algorithm ensures that for
high rates all four event types, corresponding to the four Basic Rates, would
be analyzed at about the same rate. The total number of PHA events read out
per sensor is limited by the memory allocation in the solid state recorder of
the spacecraft (see also [19]), the maximum event rate can be selected by
ground command and will be ~10 events per second for each event type.
Instrument Performance
The position (and directional) resolution depends on the resolution of the
drift time measurement and on the energy loss in the front and rear
proportional counters. The resolution therefore depends on particle type and
energy and is increasing with particle mass and decreasing with particle
energy.
The elemental resolution of the sensor depends on the resolution of the energy loss
measurement in the proportional counter - ionization chamber system and on the accuracy
of the trajectory determination for path length correction. Thus, the elemental
resolution depends on particle type and energy (see also Table I). In Fig. 4. the
energy loss in the front proportional counter (PCF) and the residual energy in the
solid state detector array for carbon and oxygen in a calibration measurement have been
converted into a nuclear charge scale. The data show that the nuclear charge
resolution in the energy range 10 to 32 MeV / nucleon is ~0.3 (FWHM), i.e. all elements
between helium and oxygen can easily be resolved. The elemental resolution of the rear
proportional counter and of the ionization chamber is similar to the one shown. This
provides some redundancy because all three sections of the proportional counter -
ionization chamber system can be used independently for the identification of elements.
Data Products
Routine data products from HILT will include time versus counting rate plots
of the four Basic Rates and of selected monitor rates. These rate plots will
be the basis for the selection of time periods for further detailed analysis
of HILT data and for the collaborative investigation of particular events with
all sensors on board SAMPEX and other spacecraft. Basic rate data and pulse
height data obtained at high geomagnetic latitudes, where cutoff effects are
negligible, will be used to compute absolute fluxes and energy spectra for
different ions during solar particle events. Pulse height data at lower
latitudes will be used to compute the trajectories of the ions in the magnetic
field of the Earth to infer the ionic charge of the ions.
Acknowledgements
The authors would like to thank the many individuals and institutions who
contributed to the design, fabrication and test of the instrument. We are also
grateful for the devoted work of the technical staff and the workshops at the
Max-Planck-Institut fuer Extraterrestrische Physik and at The Aerospace
Corporation. The project is supported in part by DARA with contract 50 OC
90021 and at The Aerospace Corporation by the NASA Cooperative Agreement
26979B.
References
HILT: A Heavy Ion Large Area Proportional Counter Telescope for Solar and
Anomalous Cosmic Rays
B. Klecker, D. Hovestadt, M. Scholer, H. Arbinger, M. Ertl, H. Kaestle, E.
Kuenneth, P. Laeverenz, E. Seidenschwang
Max-Planck-Institut fuer Extraterrestrische Physik
J.B. Blake, N. Katz, D. Mabry
Aerospace Corporation
Abstract
R = T^0.5 * (T + 2*E0)^0.5 * A/Q
Thus, after determining T and A from the measurement, an upper limit for the
ionic charge Q can be obtained from the requirement R > Rc:
Q < T^0.5 (T+2*E0)^0.5 * A / Rc
For solar energetic particle events, the particle tracing technique can be
complimented by the direct determination of the local cutoff rigidity from
the cutoff in the proton spectrum, since the ionic charge is known in this
case.
Fig.1.
particles entering the aperture by measuring the energy loss in a proportional
counter - ionization chamber system and the residual energy in an array of 16
solid state detectors and a CsI crystal unit. A view of the sensor and analog
and digital electronic in flight configuration is shown in Fig.1. The instrument
characteristics are summarized in Table I.
The schematic diagram of HILT in Fig. 2
shows the main sensor components: a three element ion drift
chamber with thin aluminium entrance window (40 mg/cm^2), followed by an array
of 16 solid state detectors (SSD) and 16 CsI scintillation counters which are
embedded in a plate of PERSPEX material and viewed by 4 light sensitive
silicon diodes. The entrance foil serves as part of the gas enclosure and, in
combination with two additional aluminium foils (2 x 20 micro-g / cm^2), as a
shield against micrometeoroid impacts. The entrance foils are protected by an
acoustic cover (see Fig. 1) that can be opened and closed after launch.
Fig. 2
Fig. 3.
The signals from the analog electronic are processed in
the Event Classification Unit (ECU) and Pulse Height Analysis Unit (PHAU).
Both units are implemented in two XILINX 3090 programmable gate arrays. The
configuration program for these units is stored in an EEPROM and loaded after
every startup by the third XILINX, the Command and Control Unit (CCU). The CCU
provides also the interface to the digital processing unit (see also [19]).
Table II.
Table III
provides typical values of the position resolution as
derived from calibration measurements. Table III shows that for helium and Z
>= 6 ions the position resolution is limited by the resolution of the
proportional counter and the size of the solid state detectors, respectively.
The resulting resolution of the zenith angle for Z >= 6 ions at energies < 40
MeV/nucleon is typically < 5 degrees FWHM.
Fig. 4.
Figure Captions: