Gm. Mao et al., FORMATION OF LAYER STRUCTURES IN H2SO4 INTERCALATED POLY(P-PHENYLENE VINYLENE), Physical review. B, Condensed matter, 58(7), 1998, pp. 4089-4094
X-ray-diffraction studies of highly oriented poly(p-phenylene vinylene
) (PPV) films before and after vapor phase or liquid-phase intercalati
on by H2SO4 have been performed. In both cases the data support a stru
ctural evolution dominated by a direct transformation of the original
PPV polymer to a single, heavily doped phase. The best-fit model obtai
ned from structure-factor refinements to the H2SO4-PPV equatorial data
is fully consistent with the previously proposed ''stage-1'' layered
structure in which the PPV chains and the sulfate ions form an alterna
ting sequence of cation- and anion-radical layers with a monoclinic un
it cell dominated by the PPV placement and lattice parameters of a=9.9
8 Angstrom, b=6.80 Angstrom, c=6.6 Angstrom, and gamma=94.5 degrees. N
onequatorial scattering data suggest that at room temperature the H2SO
4 layer is not well ordered. Additional data sets probing the anisotro
py within the equatorial plane (perpendicular to the PPV chain axis) c
learly indicate that the insertion of H2SO4 layers occurs by creating
galleries that are parallel to a-e plane of the PPV host polymer. This
direction is effectively perpendicular to the commonly accepted inter
calation scheme, which has these layers parallel to the pristine PPV [
100] planes.