Calculation of the C-13 NMR chemical shift of ether linkages in lignin derived geopolymers: Constraints on the preservation of lignin primary structure with diagenesis
Gd. Cody et G. Saghi-szabo, Calculation of the C-13 NMR chemical shift of ether linkages in lignin derived geopolymers: Constraints on the preservation of lignin primary structure with diagenesis, GEOCH COS A, 63(2), 1999, pp. 193-205
Methodology for the calculation of C-13 NMR shieldings on molecular organic
fragments, representative of monomers in a type III kerogen, is presented.
Geometry optimization of each molecular fragment was carried out using Den
sity Functional Theory employing the generalized gradient approximation. NM
R shieldings were calculated using the Individual Gauge for Localized Orbit
al Method. Convincing agreement was obtained between calculated and experim
entally derived isotropic chemical shielding values over a broad frequency
range. Shielding calculations employing the localized orbitals/local origin
method resulted in nearly identical results. NMR chemical shift static pow
der patterns also exhibit excellent agreement with experimental values. The
se quantum mechanical calculations were applied to determine the extent of
lignin primary structure preservation with diagenesis. Specifically, the ca
lculations were used to assess whether inhomogeneous spectral broadening du
e to both functional group variation and local configurational variability
may inhibit the detection of otherwise significant quantities of alkyl-aryl
ethers in lignin derived geopolymers. Determination of the chemical-shield
ing tensor principle axis values reveals a strong correlation between aniso
tropy and asymmetry with local configuration effects such as dihedral rotat
ion, phenyl group rotation, and bond angle variation. These results indicat
e that a range of 9 ppm in the isotropic chemical shift can be ascribed to
local configuration. Consequently, an upper limit of 5% alkyl-aryl-linkages
may go undetected using NMR spectroscopy on Lignin-derived geopolymers at
the liginite-sub-bituminous transition. It is concluded that the primary st
ructure of lignin does not persist in kerogens even at relatively low therm
al maturities. Copyright (C) 1999 Elsevier Science Ltd.