The data in the archive can be used to classify impactor residues into three general categories:
Category (2) can be divided into subcategories of different types of Interplanetary Dust Particles (IDP's) to the extent that knowledge of the relative abundances of 12C, 24Mg, 40 Ca, and 56Fe allow. Mass fractionation effects must be considered when assigning these subcategories.
Most impact sites examined in this study were on Al/Si based MOS substrates, therefore Al and Si were not quantifiable. Because of the limitations and contamination issues (Refs 1-3), the final SIMS analytical data is limited. There are little or no data for Mn, Cr, and S. There is relatively complete data with high confidence for 23Na, 24Mg, 39K, 40Ca, 48Ti, and 56Fe. Ca was a contaminant at the 100 ppm level in the substrate, so only very high signals (relative to the blank levels) can be interpreted. The mass 48 signal in the SIMS images includes contributions from both 48Ti and 48Ca. The signal can easily be corrected for interference from 48Ca (natural abundance = 0.185%) before quantifying the data using relative sensitivity factors (RSF). This correction is already applied to the abundance data files in this archive.
Two kinds of analytical "blanks" on MOS substrates have useful information:
Two sets of RSF's were used for quantitative reduction in this study.
These values are listed here for use by interested
parties. The first set was developed by investigators
at Washington University McDonnell Center for the Space Sciences
using a Cameca 3f with an oxygen beam similar to the instrument
used in this study. These values are based on average ion yields for
the listed species from several Lunar analogue glasses (LAG).
These RSF's were intended for application to meteorite residues
deposited in molten or vapor condensate form on pure Ge and Ta substrates.
In these forms, the "nearest neighbor" of the resident atoms in the
residue would be other atoms in the residue , i.e. very similar to
the LAG. The second set of RSF's is for species implanted in Si at
concentrations <1% (Ref. 4) and was used for residues on the MOS
substrates where the impactor materials frequently were intermixed
with the Si and SiO2 substrate materials. Both sets of values were
used in practice in order to define the limits of the observed
compositions.
Always remember that the ion images are for RAW PIXEL INTENSITY files.
The IDE data file editor, developed
during the archival process, can be used to define an area of the image
to be quantified. The boxes on each image in this file were the ones
we selected for further reduction after careful consideration.
You may select other areas, but we caution you against contamination
spots around, and sometimes (rarely) within impact feature sites.
These spots may be of interest to some investigators. There are also
debris sprays around some sites, particularly on Al samples.
The levels of ion species present in these features was, in general,
extremely low. These values were used to determine when a signal was
great enough to warrant further quantitative reduction.References
Charles G. Simon and
Klaus G. Paul, 7-8-1994