This elemental analysis instrument consists of nine curium-244 alpha-particle sources and three detectors for each of three types of particles: backscattered alpha particles, protons, and X-rays. The APX spectrometer was placed against rocks and soils on Mars to determine the abundances of all elements except hydrogen, with a lower detection limit of about 0.1 weight percent. The analytical process is based on three interactions of alpha particles with matter: elastic scattering of alpha particles by nuclei, alpha-proton nuclear reactions with certain light elements, and excitation of the atomic structure of atoms by alpha particles leading to the emission of characteristic X-rays. The approach used is to expose material to a radioactive source that produces alpha particles with a known energy, and to acquire energy spectra of the alpha particles, protons and X-rays returned from the sample.
The basis of the alpha mode of the instrument is the dependence of the
energy spectrum of alpha particles scattered from a surface on the
composition of the surface material. The method has the best
resolving power for the lighter elements (carbon and oxygen). A
least-squares analysis of a complex spectrum from an unknown sample in
terms of a library of known, pure element spectra determines the
elements and their abundance in the sample. A characteristic of the
alpha technique is that, due to variations in scattering intensity
with atomic number, there is a minimum in the scattering probability
for elements with atomic numbers between 9 and 14. This includes the
important elements Na, Mg, and Al, so the alpha mode alone is
insufficient for these elements. On the other hand, these elements
produce protons when bombarded with alpha particles. The proton
spectra for alpha particles interacting with elements with atomic
numbers from 9 to 14 are very characteristic of the individual
elements, reflecting the resonance nature of the nuclear interactions
involved. The proton mode allows their detection and measurement. The
alpha particles from the radiation sources are also an efficient
source for production of characteristic X-rays. The addition of a
third detector for X-rays therefore results in a significant extension
of the accuracy and sensitivity of the instrument, particularly for
the heavier, less abundant elements. In the X-ray technique,
characteristic X-rays are emitted when the low electron orbit
vacancies (in the K- and L-shells) produced by bombardment of atoms by
alpha particles are filled by electrons from higher orbits.
The APXS electronics are mounted in the rover warm electronics box in
a temperature-controlled environment. Cables leaving the electronics
box connect the APXS electronics to the APXS sensor head, which
contains the radioactive sources and particle detectors. The
instrument sensor head is held by a robotic arm (deployment mechanism)
attached to the back of the rover. The deployment mechanism, which
places the APXS in contact with rock and soil surfaces, interfaces the
APXS with the microrover. For the APXS to conduct a high quality
measurement of a rock or soil sample, it must be placed with its front
aperture ring in contact with the sample surface and the axis of the
sensor head must be within 20 degrees of normal to the surface. The
linkage is designed to allow the APXS to be placed at a variety of
elevations above nominal ground level and at a variety of rotational
orientations. The mounting of the APXS to the deployment mechanism
permits about 20 degrees of compliance motion as the APXS is placed in
contact with the sample. Three contact sensors on the deployment
mechanism bumper ring indicate to the rover that the positioning is
complete, thereby terminating the positioning motions. The sources
and detectors are recessed in a cylinder 4 cm behind the bumper and
the area of rock or soil that is analyzed with the instrument is a
circle 5 cm across.
Instrument Id | : APXS |
Instrument Host Id | : MPFR |
PI PDS User Id | : R. Rieder |
Instrument Name | : ALPHA PROTON X-RAY SPECTROMETER |
Instrument Type | : SPECTROMETER |
Build Date | : August 28, 1995 |
Instrument Mass | : 570 grams |
Instrument Length | : 10.5 cm |
Instrument Width | : 8.0 cm |
Instrument Height | : 6.5 cm |
Instrument Manufacturer Name | : Max Planck and Univ. Chicago |
Preliminary composition results were obtained [RIEDERETAL1997B] using just X-ray energy spectra and calibration curves of peak areas versus concentration for several standards measured for each element. Conversion of combined alpha, proton, and X-ray energy spectra to elemental abundances requires further instrument calibration, which is still underway. Alpha and proton modes will be recalibrated at Martian pressures.
Refinements of the calibration have been reported in meetings [BRUECKNERETAL1998], [BRUECKNERETAL1999], [DREIBUSETAL1999], and [WAENKE1999].
Alpha and proton modes provided excellent data on the Martian rocks and soils throughout the mission.
On the order of 10 hours integrated measurement time produces high-quality alpha and proton spectra, and about 3 hours are required for high-quality X-ray spectra. All modes (alpha, proton, X-ray) are measured simultaneously when the APXS is powered on and measuring.
Other parameters measured are the temperature of the X-ray preamplifier in the sensor head, temperature of the alpha detector preamplifier in the rover's warm electronics box (°C), and the sampling duration of the alpha, proton, and X-ray measurements (hh:mm:ss).
MissionMars Pathfinder
TargetsPDS Welcome to the Planets: MarsPDS High Level Catalog: Mars
Instrument HostMars Pathfinder Rover
InstrumentMars Pathfinder Rover Cameras
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Data Set DescriptionsAPXS Raw DataAPXS Oxide Abundances Rover Camera Raw Data Rover Camera Calibrated Images and Mosaics Rover Engineering Data ReferencesBRUECKNERETAL1998BRUECKNERETAL1999 DREIBUSETAL1999 RIEDERETAL1997A RIEDERETAL1997B WAENKE1999
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