Also, you mentioned the difference in the sources people are using.
Someone mentioned the backscatter issue when making measurements, and of
course it applies to calibration. I've got some cal sources of the
same nuclide, but they're on different substrates, and I get different
numbers. When you cal the probe are you holding it a specified distance
from the source? I think the end use of the instrument has to drive
your calibration methodology. Might be interesting to take ONE pancake
probe, send it around to 20 different labs and ask for an efficiency determination
on it based on say, Cs137, or whatever nuclide. I bet the differences
might scare us.
************************************************************************ The RADSAFE Frequently Asked Questions list, archives and subscription information can be accessed at http://www.ehs.uiuc.edu/~rad/radsafe.htmlGM probe efficiencies If the commonly used isotopes are: C-14, S-35, P-32, P33 and Ca-45 which are all beta emitters and if a survey meter like the Ludlum Model 3 with a Model 44-9 pancake probe are being used for surveys, what are the counting efficiencies that you use to determine the activity present and at what distance from the source are you determining your efficiency? I raise this question because I hear different efficiencies when I ask other people this question. One reason could be the type of screen covering the window face. I understand that Ludlum might have used 4 different screens over the years. Of course, there are other reasons like the calibration source used, its geometry, and its distance from the meter. Any way, if you feel this comparison between meter users is worth while, respond to me, I will summarize the data and post it. What prompted me to ask is the comment about the S-35 in the post Lambert responded to and also the post that just arrived in which Joel stated what he found as the efficiency for C-14.