Abstract
We have investigated the effect of an inorganic electrolyte (sodium
chloride) on the aggregation behaviour and liquid crystals of Edicol
Sunset Yellow. Edicol self-aggregates in aqueous solution to form
single molecule stacks, which then become ordered to form nematic and
hexagonal (columnar) mesophases at high concentrations. We have
employed changes in the 1H nuclear magnetic resonance (NMR) chemical
shifts to monitor the aggregate formation in solution. A single
spectrum is observed at all concentrations because the exchange between
Edicol monomers in solution and those in stacks is fast on the NMR time
scale. The results show that at low Edicol concentrations (1 wt%) the
concentration of aggregates is small, but at high concentrations (20
wt%) the fraction of monomers is tiny. At low Edicol concentrations,
low levels of salinity appear to alter aggregate shape and size,
resulting in a disaggregation/aggregation effect occurring over four
orders of magnitude of added electrolyte. However, little alteration is
seen in the fraction of aggregates. At high electrolyte levels, when
the Debye length is comparable to the stack lengths (a few nanometres),
the fraction of aggregates increases, presumably because of the reduced
intra-stack electrostatic repulsion. Importantly, we have also shown
that the isodesmic theory of aggregation (equal K) is too simple to
describe accurately the aggregation process from the monomer to the
pre-nematic phase concentrations. NMR quadrupole splittings indicate
that there is no specific Na+ ion binding to the stacks. At the very
highest concentrations of Edicol and sodium chloride the aggregates and
mesophases are destabilised. The reason for this has yet to be
elucidated.
Original language | English |
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Pages (from-to) | 711-722 |
Number of pages | 12 |
Journal | Liquid Crystals |
Volume | 37 |
Issue number | 6-7 |
DOIs | |
Publication status | Published - 2010 |
Keywords
- chromonic
- chemical shift
- NMR
- sodium chloride
- salt
- Edicol Sunset Yellow
- isodesmic
- aggregation
- quadrupole