A method was developed to demineralize sediment trap material and marine se
diments containing labile organic matter (OM), in preparation for cross pol
arization and magic angle spinning (CP/MAS) solid-state C-13 NMR analysis.
Carbonate and silicate minerals were dissolved with HCl and a mixture of di
lute HCl/HF, respectively. Demineralization kinetics were assessed for a ra
nge of freshwater and marine sediments, as well as pure mineral and organic
samples. For samples with a very low organic carbon (OC) concentration (<
1 wt.%) and samples containing a large fraction of acid-soluble OC, the org
anic molecules solubilized during the dissolution of the mineral fraction w
ere recovered by freeze-drying the supernatants following (i) removal of di
ssolved calcium and residual HF by CaF2 precipitation, (ii) removal of the
dissolved paramagnetic metals by sulfide precipitation, and (iii) desalting
using ion-retardation chromatography. When applied to a wide range of fres
hwater and marine particles, demineralization resulted in OC enrichment fac
tors that varied between 2.2 and 20.8, with losses representing less than 2
0.5% of the initial OC content. X-ray diffraction and fluorescence analysis
of the natural and demineralized samples showed that minerals and paramagn
etic metals were effectively removed. While molecular fractionation might b
e substantial when the mineral constituents were dissolved with HCl and HF,
the small changes (< 11%) in the (C/N)(a) and (H/C)(a) ratios when the aci
d-soluble organic matter was recovered suggest that the molecular compositi
on of the organic fraction was not appreciably altered. In combination with
CP/MAS C-13 NMR spectroscopy, this demineralization method allows comprehe
nsive elucidation of the chemical structure of total OC, especially in samp
les with very low OC concentrations and/or with a significant fraction of c
hemically labile organic compounds. (C) 2001 Elsevier Science Ltd. All righ
ts reserved.