Several exfoliated nylon-6/clay nanocomposites (NnC's) were investigated and compared
with pure nylon-6 using solid-state NMR, both proton and 13C. NnC's had nominally 5 mass
% clay and were generated both by blending and by in situ polymerization (IsP). Most of the
studied NnC's contained layered, naturally occurring montmorillonite clays having nonstoichiometric amounts of nonexchangeable Mg2+ and Fe3+ ions that substitute into
octahedral Al3+ sites along the midplane of the 1-nm-thick clay layers. The Fe3+ ions impart
a useful paramagnetism to the clay. Each Mg2+ ion leaves an embedded negative charge
that must be neutralized with some cation at the surface of the clay. All clays were initially
treated with a cationic so-called organic modifier (OM), often a substituted ammonium ion,
which increases the clay layer spacing, attaching ionically to the surface of the clay layers.
Clay is found to promote growth of the γ-crystalline phase of nylon-6 for both blended and
IsP NnC's; α-crystallites are characteristic of the pure nylon-6. Stability of the γ-phase to
annealing at 214 °C was investigated. Conversion of γ- to α-crystallinity during annealing
was minimal, except for an injection-molded IsP NnC, which had been exposed to a
temperature of 295 °C during molding. This high processing temperature produced an
irreversible change. An attempt was made to understand, at least qualitatively, the nature
of the spectral density of magnetic fluctuations associated with the paramagnetic Fe3+ sites
in the clay. For this purpose, we looked directly at the influence of Fe3+ on the 13C and
proton observables in organically modified clays (OMC). We agree with other investigators
that the spectral density of paramagnetic fluctuations at the surface of the clay is determined
mainly by spin-exchange interactions between Fe3+ sites; thus, the spectral density can be
altered by changing the Fe3+ concentration. Moreover, we find that the spectral density is
very wide, having strong contributions all the way from mid-kHz fluctuations to MHz
fluctuations near the proton Larmor frequencies. Significant variations in the α/γ ratio were
also observed in the injection-molded disk, which reflect either a processing-induced
heterogeneity in clay dispersion or a significant variation in cooling history from region to
region. Proton spin diffusion and multiple-pulse methods were utilized to compare morphologies for a diamagnetic NnC and nylon-6 with the same thermal histories. Long spacing,
crystallinity, and the mobility of the noncrystalline nylon-6 segments are very similar for
NnC's and nylon-6.