In the case of soils, Sill recommends further

Wessman et al. (1971) reported on a method for trace plutonium analysis in a
large variety of sample matrices and this system formed the basis for the
determination of the other transuraniums, as later reported (Wessman et al.,
1977). A schematic diagram of the procedure is given in Figure 5.
The first
steps of the procedure, which are adequate to solubulize and equilibrate Pu,
are also adequate for any other transuraniums present. Yield tracers are
233pq (234Np) for eaNe 236py for 238py,
239°240py and 24%3am for the combined
|

group consisting of 7"lam, 22cm, and 243*244em, An anion exchange column
(Dowex 1-X4) is used to absorb Np (IV) and Pu (IV) from 8 N HNO3 while Am

(111) and Cm (III) pass through the column, Plutonium ie separated from Np on
a subsequent Dowex 1-X4 ion exchange column. The column is washed with 8

Plutonium is eluted with NH,I-HCl and Np with 2 N HCl.

NEPTUNIUM PURIFICATION

Magnusson and LaChapelle (1949) discussed the procedure devised by Seaborg and
Wahi (1948) to isolate weighable quantities of 23’Np for further study. The
classical reactions were used, mostly lanthanum fluoride precipitations to
carry Np (IV) or Np (III).
Impurities, such as Pu and fission products, were
precipitated with LaF; in the presence of Np (VI).
Burney and Harbour'’s 1974-monograph on the Radiochemistry of Neptunium has a
very complete discussion on the more recent aspects of Np chemistry including
solvent extraction and ion exchange,
They point out that Np is easily converted
in aqueous solution to oxidation states that exhibit markedly different behavior
in coprecipitation, and therefore separation from other elements can be obtained.
They further note that the fon exchange, extraction chromatography, and solvent
extraction separation are used almost exclusively because more complete separation is attained more rapidly. Burney and Harbour presented a collection of
25 procedures, Fifteen are for a combination of the different separation
steps on highly radioactive samples, three are for environmental and biological
samples, and seven are for quantitative elemental determinations. Two of the
procedures for highly radioactive solutions use either 73’Np or 73°9Np as
tracers. None of the 237Np environmental or biological procedures given use

556
557

x

4

The

Am, Cm-containing eluant is further purified using steps which have been
pretested to assure that Am is not fractionated from Cm. Figure 6 shows an
elution curve obtained in testing the final cation exchange column step in the
procedure. In actual analyses, the fractionation of Am and Cm is usually
within 2 to 3% of each other.

*Private communication with K. M. Wong.

R.E. oxalate, Am

Fp C2 O4
PH 1-2

N HNO3 and HCL.

dissolve in 2N HCl
IS

NH,OH

(hydroxides)

Conc.
HCl

! 8N HNO;

Fe, Sb, RE, Am (partial)

elute through Dowex

dissolve in HNO,
adjust to 8N in HNQ

Fe, RE, Sb, Pu

3-5 dpm standardized 2 *pu tracer

| NHLOH
’
(hydroxides)

|

Combine R. E. fractions

NH, -HC!

superhate)
Cs, Sr

Process a reagent
blank after every
eight samples.

separation of the tervalent actinide group from the lanthanides according to
the method of Filer (1974). The Latter procedure combines extraction chromatography with bis(2-ethylhexyl)-phosphoric acid (HDEHP) in the presence of
diethylenetriaminetetraaccetic acid and the use of a column of Teflon-6
powder. Siil further recommends, when necessary, Moore and Jurriaanse's
(1967) method to separate *"2cm from 252C£ whose alpha energies are so identical,
alpha spectrometry cannot resolve them.

500 mg Fe (unstandardized)
10 mg each of standardized Sh, Ce, Nd, Sm, Eu, Y and Cs
2 g standardized Sr

FIGURE 4

WONG, NOSHKIN AND BOWEN'S PROCEDURE AS APPLICABLE TO THE

ANALYSIS OF Pu AND Am* IN SEAWATER SAMPLES
Ref: Methods for Marine Radioactivity Studies, IAEA, Vienna (1970), p 119.

back-extracted with 8 M HNO3.

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