Crystalline domains composed of poly(methylene) chains have been detected b
y solid-state NMR and wide-angle X-ray scattering (WAXS) in several samples
of soil organic matter, including humins, surface soil (peat), and humic a
cids extracted from surface soil and young coal. From the melting range of
60- >80 degrees C and H-1 spin diffusion experiments, a crystallite thickne
ss of ca. 3 nm or 25 CH2 units is deduced. The overall fraction of (CH2)(n)
carbons in these materials is up to 9%. Nearly half of this poly(methylene
) is crystalline, while the rest is noncrystalline and more isotropically m
obile. In humin, several crystalline and noncrystalline poly(methylene) dom
ains form larger aggregates. The crystallites are expected to be resistant
to environmental attack and thus inert in the soil and have long residence
times, while the mobile amorphous regions may play a role in the sorption o
f nonpolar molecules in soil.