2

240,
2?
240, 415

the chemical yields for iron

atom concentrations of

originally present in the samples.

in each sample, 242 mass tracer

39,

was added during the chemical dissolu-

Standard chemical procedures were
used for the isolation and purifica-

tion.

Specific activities were

tion of O34, Jolen, and 24]a,

calculated from the measured atom

Gravimetric measurement of the

concentrations and appropriate decay

recovered nickel and samarium -

constants.

carriers provided yields for the 6 Ni
:
1
and
Sm samples.
The addition of

determined mass spectrometrically,

283 am tracer was required to determine

traced plutonium samples was required.

the yield of the 24d samples.

Alpha pulse-height analysis was also

Nickel was purified by numerous pre-

essential for the quantification of

cipitations as nickel dimethylglyoxime.

241an.

The rare earth, samarium, was separated

americium samples were determined

from americium on a Dowex 50 cation-

from the

exchange column by gradient elution

of 238 oy and 2A was accomplished

with a-hydroxyisobutyric acid.

by the ratio of the characteristic

Since

385, could not be

alpha pulse height analyses of

42ou

Chemical yields for the
3am tracer.

Quantification

alpha peak areas to those of the
appropriate tracers.

MEASUREMENT TECHNIQUES

Thin NaI(f1) and planar Ge(Li)

Strontium-90 was determined by beta

diode pulse-height~analysis detection

measurement of the chemically separated

systems were used to measure the

64-h 20, daughter.

characteristic 6-keV Mn x ray of ° Fe.

Interferences

from radiochemical contaminants were

All samples were measured by Nal(T1).

identified and eliminated through

Ge(Li) detection systems served to

least-squares analysis of the data.

confirm results and extend the sen-

These procedures are rather common

sitivity for

for determination of the long-lived
90
Sr parent.

lower levels.

Plutonium—239,

ire detection to
Sixteen samples were

analyzed for their

240, and 241 were

Fe content.

Nickel-63 and samarium-15l were

separately quantified via mass

determined by liquid scintillation

Spectrometric measurement techniques.

counting at LLL with a Packard

Observation of the characteristic

Tri-Carb spectrometer.

mass-to-charge ratio for each isotope

Errors reported with each result

provided the means of separation

represent the measurement uncertainty

and measurement.

and are based primarily on counting

To determine the
=~ 1?~

«agg?

3010054
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