Gb. Morgan et D. London, OPTIMIZING THE ELECTRON-MICROPROBE ANALYSIS OF HYDROUS ALKALI ALUMINOSILICATE GLASSES, The American mineralogist, 81(9-10), 1996, pp. 1176-1185
The time-dependent loss of NaK alpha X-ray intensity during electron-b
eam irradiation of hydrous alkali aluminosilicate glasses is apparentl
y more significant during the initial few seconds of beam exposure tha
n it is for anhydrous glasses, and it is pronounced for incident beam
currents >2-5 nA (using 15-20 mu m beam diameters). Exponential fits o
f NaK alpha intensity vs. lime show a progressive decrease in the appa
rent zero-time intercepts for incident beams from 2 to 20 nA, and thus
methods for correcting Na concentrations solely on the basis of curve
fitting and extrapolation to zero-time values may underestimate Na co
ntents by almost 10% (relative) for higher beam currents. Similar expo
nential fits to the intensity-time data for AlK alpha and SiK alpha sh
ow that ''grow-in'' is greater for Al than for Si. For incident curren
ts greater than or equal to 5 nA, the magnitudes of all intensity chan
ges also increase with total H2O content of glass. On the basis of the
se observations, the optimal conditions for analysis of hydrous alkali
aluminosilicate glasses include a 2 nA beam with 20 pm diameter and c
ounting times of 20-40 s for the analysis of alkali aluminosilicate co
mponents, with Na and Al analyzed first (simultaneously, if possible).
These methods minimize Na loss and grow-in for Al and Si to the point
that little or no correction is needed, provide good statistical accu
racy, and work with a wide variety of standard materials (i.e., glass
standards with compositions and H2O contents comparable to the unknown
s are not needed). For complete analysis of more complex multicomponen
t systems, two beam conditions are recommended: an initial 2 nA, 20 mu
m diameter beam for analysis of alkali aluminosilicate components, fo
llowed by a 20 nA, 20 mu m diameter beam for analysis of. all other co
mponents. With the use of these methods, the H2O contents of hydrous g
lasses (H2O as the only unknown) can be determined by difference with
uncertainties mostly <5% (relative to FTIR values) for glasses contain
ing up to 10 wt% H2O. At beam currents >5 nA, corrections for Na loss
ignoring Al (and Si) grow-in underestimate H2O contents by about 10-50
% of concentration.