C. Ma et al., ANALYTICAL ELECTRON-MICROSCOPY IN CLAYS AND OTHER PHYLLOSILICATES - LOSS OF ELEMENTS FROM A 90-NM STATIONARY BEAM OF 300-KEV ELECTRONS, Clays and clay minerals, 46(3), 1998, pp. 301-316
Diffusion of alkali and low-atomic-number elements during the microbea
m analysis of some silicates by analytical electron microscopy (AEM) h
as been known for some time. Our repeated analyses at 300 kV of kaolin
ite, halloysite, smectite, biotite, muscovite and pyrophyllite, howeve
r, showed differential loss (relative to Si) of not only alkali elemen
ts (such as K, Na, Mg) and low-atomic-number elements (such as Al) but
also higher-atomic-number elements (such as Fe, Ti). For AEM of these
phyllosilicates, a Philips EM430/EDAX facility with a tungsten filame
nt was used to provide a current of 0.3 nA in a stationary beam of nom
inal diameter 90 nm. The loss of Al in kaolin minerals during analysis
is particularly severe. Kaolin crystals can be damaged by the electro
n irradiation over several seconds, making it the most sensitive clay
to the electron beam; in general, relative phyllosilicate stabilities
are kaolin < smectite < pyrophyllite < mica. A clear dependence of ele
ment loss on crystallographic orientation has been observed for layer
silicates in our study; a greater element loss occurred when the plane
of the specimen foil was perpendicular to the basal planes of the phy
llosilicate crystals than when the foil was parallel to the basal plan
es. Lower beam current, larger beam diameter and thicker specimens all
reduce the loss of elements. The initial stage of irradiation produce
s highest rates of element loss and the rate of loss can be fitted by
an exponential decay law. The analyses at low temperature of phyllosil
icates showed that element loss remains serious in our analytical cond
itions. Since the element loss appears to be instrument- and method-de
pendent, one should use closely related, well-characterized phyllosili
cates as compositional standards to calibrate any AEM instrument that
is to be used to analyze unknown phyllosilicates, and the standards an
d unknowns should be analyzed under identical conditions.