To better understand the effects
of solution chemistry on particle
aggregation in the complex legacy tank wastes at the Hanford (WA)
and Savannah River (SC) sites, we have performed a series of tumbler
small- and ultra-small-angle neutron scattering experiments on 20
wt % solid slurries of nanoparticulate aluminum oxyhydroxide (boehmite)
with M1+ nitrates of various concentrations and radii.
The solutes consisted of H, Li, Na, K, and Rb nitrates at 10–5, 10–3, 10–1, 2, and 4 molal
(m) concentrations, as well as in pure H2O. Synthetic boehmite nanoparticles were used with a size range from
∼20 to 30 nm. Tumbler cells were used to keep the solids from
settling. Although particles initially form individual rhombohedral
platelets, once placed in solution, they quickly form well-bonded
stacks, primary aggregates, up to ∼1500 Å long, and a
second level of aggregates whose concentration and structure vary
as a function of cation type and concentration. Aggregation generally
increases with increased solute concentration and with cation radius
up to a concentration somewhat above 10–1
m, at which point the trend reverses. Primary aggregates
become more rodlike and larger. The Kirkwood-like reversal probably
reflects a change from Derjaguin–Landau–Verwey–Overbeek
(DLVO)/Debye behavior controlled by surface chemistry to a frustrated
Coulombic system controlled by the solution structure. These data
suggest that an understanding of the effects of salt concentration
and chemistry on nanoparticle aggregate structures provides useful
physical insights into the microscopic origin of slurry rheology in
the Hanford and Savannah River legacy wastes.