Potentially paramagnetic elements such as Fe, Cu, and Mn, did not affect NM
R sensitivity and T-1 rho(H) values of humic, materials from volcanic soils
, despite a large ash content in the extracts. T-1 rho(H) values increased
with increasing C/H ratios, thereby confirming a relationship between the n
umber of protons bound to carbons and process of relaxation in solid humic
materials. Differences in T-1 rho(H) values were explained by molecular com
position of the samples, Few carbon-bound protons and high molecular rigid
ity in highly aromatic humic matter reduced the efficiency of the relaxatio
n. Humic samples richer in polar carbons showed variable T-1 rho(H) values
due to different molecular rigidity conferred by intermolecular hydrogen bo
nds. Not only the number, but also the distribution of protons in humic mol
ecules appeared to affect T-1 rho,(H) values.