Solubilities of neptunium and plutonium were studied inJ-13 groundwater (ioni
c strength of about 3.7 mmol; totaldissolved
carbonate of 2.8 mmol) from the proposed Yu
ccaMountain Nu
clear Waste Repository site, Nevada, atthree different temperatures (25, 60, and 90
![](/images/entities/deg.gif)
C) and pHvalues (6.0, 7.0, and 8.5). Experiments were performed fromboth over- and undersaturation at defined CO
2 partialpressures. The solubility of
237Np from oversaturationranged from a high of (9.40 ± 1.22) × 10
-4 M at pH 6.0and 60
![](/images/entities/deg.gif)
C to a low of (5.50 ± 1.97) × 10
-6 M at pH 8.5 and90
![](/images/entities/deg.gif)
C. The analyti
cal results of solubility experimentsfrom undersaturation (temperatures of 25 and 90
![](/images/entities/deg.gif)
C andpH values 6, 7, and 8.5)
converged on these values. The
239/240Pu solubilities ranged from (4.70 ± 1.13) × 10
-8 M at pH6.0 and 25
![](/images/entities/deg.gif)
C to (3.62 ± 1.14) × 10
-9 M at pH 8.5 and 90
![](/images/entities/deg.gif)
C. In general, both neptunium and plutonium solubilitiesde
creased with in
creasing pH and temperature. Greenish-brown
crystalline Np
2O
5·
xH
2O was identified as thesolubility-limiting solid using X-ray diffra
ction. A meanthermodynami
c solubility produ
ct for Np
2O
5·
xH
2O of log
K
sp= 5.2 ± 0.8 for the rea
ction Np
2O
5·
xH
2O + 2 H
+ ![](/images/entities/rlhar2.gif)
2NpO
2+ + (
x+1)H
2O at 25
![](/images/entities/deg.gif)
C was
cal
culated. Sparinglysoluble Pu(IV) solids, PuO
2·
xH
2O and/or amorphousplutonium(IV) hydroxide/
colloids,
control the solubility ofplutonium in J-13 water.