DATASET_DESCRIPTION |
Data Set Overview
=================
The APXS_oxides is a listing of weight percent oxide abundances
derived from the X-ray portion of the APXS_EDR data from the
Alpha Proton X-ray Spectrometer (APXS). This data is preliminary
and will be later refined as new calibration data become
available. Currently, there are oxide results for five rocks and
six soils.
Geochemists usually express the abudance of elements in rocks and
minerals as weight percents of the oxides. It is a convenience
that is followed because most rock forming minerals are
stoichiometric compounds and it makes comparison and calculations
easier. It does not mean that those specific oxides are
necessarily found as minerals or compounds in the sample
analyzed; it is only a way to recast the element abundances. Nor
does it mean that Fe in the sample is 2+ rather than 3+. It is
simply a way of expressing the chemical abundances by
stoichiometric assignment to oxides. For geochemical
convenience, we have recast the Pathfinder APXS elemental
abundances of Na, Mg, Al, Si, S, K, Ca, Ti, Fe, and Cl to weight
percent Na2O, MgO, Al2O3, SiO2, SO3, K2O, CaO, TiO2, FeO and Cl.
Futher calibration is necessary to determine oxide abundances for
the one other soil and four other rock measurements obtained at
the Pathfinder landing site. The APXS bumper ring did not make
good contact with the soil during A-9 measurements, so more
testing is needed to determine the uncertainties on the oxides
for this. The X-ray spectra for A-19, A-20, A-23, and A-27 rock
measurements were degraded due to the rover battery death on Sol
56. The APXS_EDR data for these are available now, and oxide
abundances will be determined at a later date.
Parameters
==========
The parameters are (1) weight percent abundances of chlorine and
the oxides: Na2O, MgO, Al2O3, SiO2, SO3, K2O, CaO, TiO2, and FeO;
(2) uncertainties on those abundances; and (3) the original sum
of the oxides before normalization. The original sum varies in
response to the measurement geometry and is closer to 100% if
good contact is made between the sample and the APXS bumper ring.
Processing
==========
The only input necessary for processing was APXS EDR data. These
data files were the cumulative sums of data acquired from the
beginning of the measurement cycle until the final reading.
Readings occurred several times for each rock and soil that was
analyzed. The first step in processing the data is to subtract
subsequent spectra from one another and examine the deconvolved
spectra to check for the possibility of any damaged data or
instrument drift (e.g. by changing environmental temperature).
The next step is to establish any changes in energy calibration,
mainly due to changes in environmental temperature and shift the
data to correct gain and zero-offset drift. Then the individual
shifted spectra are summed together. The summed composite go
into a least-squares fitting program that subtracts the
background, finds all the peaks in the spectra, and calculates
the peak areas and their uncertainties. Calibration curves (peak
area versus concentration) for each element are used to derive
abudances of each element. These calibration curves were
obtained by analyzing terrestrial samples of known composition
during the APXS calibration in the laboratory. Some corrections
for matrix effects for a few of the elements are made after this.
Then, to express the element abundances as oxide abundances,
oxygen is assigned stoichiometrically (Fe as FeO, S as SO3, etc.)
and the analyses are renormalized to an arbitrary value, in this
case 98.0%. P2O5, Cr2O3, and MnO are not included in these
preliminary results because they have large errors and the final
calibration for these has not been completed.
Data
====
All of the data in this dataset are contained in an ASCII tabular
file, ('OX_PERC.TAB') with a detached PDS label ('OX_PERC.LBL').
The tabular file is formatted so that it may be read directly
into many database management systems (DBMS) or spreadsheet
programs on various computers. All fields in the table are
separated by commas; text fields are left justified and numeric
fields are right justified. The 'start byte' and 'bytes' values
listed in the PDS label do not include the commas between fields.
The records are of fixed length, and the last two bytes of each
record contain the ASCII carriage return and line feed
characters. This allows the table to be treated as a fixed
length record file on computers that support this file type and
as a normal text file on other computers.
The PDS label is object-oriented. The object to which the label
refers (the TABLE) is denoted by a statement of the form:
^object = location
in which the carat character ('^', also called a pointer in this
context) indicates that the object starts at the given location.
For an object located outside the label file (as in this case),
the location denotes the name of the file containing the object.
For example:
^TABLE = 'OX_PERC.TAB'
indicates that the TABLE object is in the file OX_PERC.TAB, in
the same directory as the detached label file.
The detached label file is a stream format file, with a carriage
return (ASCII 13) and a line feed character (ASCII 10) at the end
of each record. This allows the file to be read by the MacOS,
DOS, Unix, and VMS operating systems.
Ancillary Data
==============
Calibration APXS measurements obtained in the laboratory.
Coordinate Systems
==================
Estimates of the locations of the 5-cm diameter spots measured on
rocks and soils on Mars are reported as XYZ coordinates in the
Martian Local Level Coordinate Frame. Only those for which the
oxide abudances have been determined are listed:
APXS
meas. X Y Z Rock/Soil APXS Target
----- ---- ----- ----- ----------------------------
A-2 1.89 -1.95 0.31 soil off the end of the ramp
A-3 1.30 -2.45 0.18 Barnacle Bill rock
A-4 2.79 -2.64 0.28 soil near Yogi
A-5 3.29 -2.48 0.28 soil near Yogi
A-7 4.58 -2.91 -0.18 Yogi rock
A-8 2.85 1.13 0.32 Scooby Doo indurated soil or rock
A-10 3.74 -0.43 0.28 dark soil next to Lamb
A-15 -5.87 2.80 0.52 Mermaid dune
A-16 -3.79 -1.31 0.12 Wedge rock
A-17 -5.56 -3.25 -0.35 Shark rock
A-18 -4.81 -3.81 -0.54 Half Dome rock, first location
The Mars Pathfinder Lander (L) Coordinate Frame
The Mars Pathfinder Lander is a tetrahedral structure. One of
its faces, the one upon which it sits, is called the base petal
and houses most of the lander equipment. The other three faces,
or petals, open after surface impact to expose these systems.
The rover is mounted on one of these petals. The Mars Pathfinder
Lander Coordinate Frame, or 'L' Frame, has the lander base petal
as its reference plane and its center coincident with the
geometric center of the base petal. The YL-axis of this
coordinate system passes through the geometric center of the
rover petal, and defines the reference direction. The ZL-axis is
normal to the reference plane and coincident with the nominal
spacecraft spin vector. When the lander is upright on the
surface, the ZL-axis is directed positively downward into the
ground.
The Martian Local Level (M) Coordinate Frame
The Martian Local Level Coordinate Frame is a right handed,
orthogonal, frame whose origin is co-incident with the origin of
the Lander Coordinate Frame. The XM axis points north, the YM
axis points east, and the ZM axis points down.
For more information on Mars Pathfinder coordinate systems, see
the [MELLSTROM&LAU1996], [WELLMAN1996B], and [VAUGHAN1995]
references. However, please note that as of the time this
APXDDRDS.CAT file was written, [WELLMAN1996B] had not yet updated
his discussion of elevation measurements to match that agreed
upon by the Project. Where he used elevation ranges of 0 to 180
degrees, the MPF Project used -90 to +90 degrees.
Software
========
The APXS oxides data can be displayed on UNIX, Macintosh, and PC
platforms using any ASCII editor.
Media / Format
==============
The APXS oxides data will be stored on compact disc-read only
memory (CD-ROM) media. The CDs will be formatted according to
ISO-9660 and PDS standards. The data files will not include
extended attribute records (XARs), and will therefore not be
readable on some older VMS operating systems.
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CONFIDENCE_LEVEL_NOTE |
Confidence Level Overview
=========================
These oxide abundances are preliminary results for the X-ray
portion of the APXS_EDR data. The confidence is indicated by the
uncertainties that are assigned to each of the oxides in the
APXS_oxides ASCII table. These uncertainties were derived from
the range in differences found between recommended and measured
values for eight reference standards.
Review
======
Prior to release, the data will be reviewed by the APXS
instrument team and the Planetary Data System.
Data Coverage and Quality
=========================
The quality of the preliminary X-ray oxide abundances is
indicated by the results for Murchison C2 meteorite and the
martian meteorite Zagami [RIEDERETAL1997B]:
(1) (2) (3) (4) (5)
Na2O 2.3 0.7 to 1.2 1.5 0.7 0.2
MgO 8.8 8.6 to 11.6 18.2 18.2 19.9
Al2O3 7.1 4.8 to 6.2 2.4 2.3 2.3
SiO2 49.6 48.4 to 50.9 31.0 31.0 28.5
SO3 0.3 0.15 to 0.29 7.8 7.8 7.9
K2O 0.25 0.13 to 0.24 0.06 0.04 0.04
CaO 10.9 9.7 to 11.1 2.0 1.8 1.9
TiO2 1.0 0.74 to 1.4 0.04 ---- 0.06
FeO 17.4 18.0 to 24.5 30.2 30.2 27.1
(1) Zagami martian meteorite rock slice, APXS analysis for a
counting time of 127,470 seconds. (2) Zagami martian meteorite,
five individual chips of about 0.5 g each, measured using
instrumental neutron activation analysis (INAA), X-ray
fluorescence (XRF) and carbon-sulfur analyzer (GSA) at Max-Planck
Institut fur Chemie. (3) powdered Murchison C2 meteorite,
measured using an APXS for a counting time of 242,030 seconds.
(4) powdered Murchison C2 meteorite, measured using an APXS for a
counting time of 20,360 seconds. (5) powdered Murchison C2
meteorite, measured using INAA, XRF and GSA at Max-Planck
Institut fur Chemie.
Results for the soil A-2 are not as good as the others, due to
poor contact with the sample by the APXS deployment mechanism and
lower counting rates for alpha particles, protons, and X-rays.
This is reflected in the lower original sum of the oxides for
A-2.
When measuring rock and soil samples, the desire was to obtain at
least 10 integrated hours. Only 3 hours of nighttime measurement
were needed for a good X-ray analysis. X-ray spectra obtained
during the night, when ambient surface temperatures were low,
were unaffected by electronics noise. Ten hours of measurement
during the day or night provide good alpha and proton analyses.
Shorter times still provide useful results. The measurement
times for the 11 APXS measurements that have been converted to
oxide abundances are shown below:
APXS Measurement initial start Integrated APXS spectra
meas. time and final stop time meas. time accumulation
number (Local True Solar Time) (hrs) time (hrs) Target
----- ------------------------- ---------- ------------ ------
A-2 Sol 2 14:53 - Sol 3 10:00 19.6 15.9 soil
A-3 Sol 3 15:00 - Sol 4 07:01 16.5 13.6 rock
A-4 Sol 4 16:59 - Sol 5 01:32 8.8 8.1 soil
A-5 Sol 5 16:01 - Sol 6 06:55 15.3 9.2 soil
A-7 Sol 10 14:17 - Sol 11 02:37 12.7 5.7 rock
A-8 Sol 14 14:03 - Sol 15 02:55 13.2 5.7 soil
A-10 Sol 20 14:03 - Sol 21 02:59 8.3 7.0 soil
A-15 Sol 28 14:05 - Sol 29 02:44 8.0 5.3 soil
A-16 Sol 37 14:07 - Sol 38 03:05 8.2 6.5 rock
A-17 Sol 52 14:18 - Sol 53 03:05 8.0 7.0 rock
A-18 Sol 55 14:06 - Sol 56 00:05 7.2 5.9 rock
Measurement initial start and stop times were obtained from the
SCLK times in the downlink telemetry for the acknowledgement of
the exact commands that were issued to trigger the start and stop
of each APXS measurement (usually Meas_Start, Meas_Stop, Reset,
or Shutdown). SCLK times were converted to Local True Solar Time
using the script sclk2ltmst (see Ancillary Data discussion).
This time is only as accurate as the rover's clock, and is a
close approximation to the exact intial start and stop time of
each APXS measurement. In a few cases, the downlink was lost,
and uplink predictions were used instead. Some of the cumulative
APXS measurements were interrupted by other rover activities, in
which case, the first accumulation start time and last stop time
are indicated. Integrated measurement time, as indicated by
ALPHA_SAMPLING_DURATION, PROTON_SAMPLING_DURATION, and
XRAY_SAMPLING_DURATION in the data file headers, is always less
than the accumulation final stop time minus the initial start
time, because the sampling durations do not include quiet periods
when the APXS was powered off and detector 'dead time'.
Limitations
===========
Further calibration and special processing is underway to improve
the conversion of X-ray data to elemental and oxide abundances,
and to calibrate the alpha and proton portions of the data and
combine them with the X-ray data.
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