G. Davies et al., TIGHT METAL-BINDING BY HUMIC ACIDS AND ITS ROLE IN BIOMINERALIZATION, Journal of the Chemical Society. Dalton transactions, (21), 1997, pp. 4047-4060
Analytical and thermodynamic data, EPR, FTIR, solution H-1 and solid-s
tate C-13 cross polarization magic angle spinning NMR and solid-state
extended X-ray absorption fine structure (EXAFS) and X-ray absorption
near-edge structure (XANES) spectra have been recorded for purified hu
mic acids (HAs) isolated from a German peat (GHA), an Irish peat (IHA)
, an unpolluted New Hampshire bog soil (NHA) and their tightly bound c
opper(II), iron(III) and manganese(II) forms. Brief water washing of p
artly or fully metal-loaded HAs leaves 'tightly' bound metal in the is
olated freeze-dried solids. Mo:rt of this metal is removed by washing
with 0.1 M HCl, indicating acidic HA functional groups as principal me
tal binding sites. The number of nearest-neighbour atoms coordinated t
o tightly bound Cu-II (four), Fe-III (six, probably with distorted geo
metry) and Mn-II (six, undistorted) in solid GHA, IHA and NHA were det
ermined by XANES and EXAFS spectroscopy with reference standards. Isot
herms measured at 20.0 degrees C and pH 2.4-3.2 with [M](total) = 0.18
-25.8 mM for tight, reversible Cu2+(aq), Fe3+(aq), and Mn2+(aq) bindin
g by solid IHA and NHA fit the Langmuir model and give the pH-independ
ent stoichiometric site capacities nu(1) and equilibrium constants K-i
for metal binding at specific HA sites i = A, B and C. Tight binding
sites A, B and C of IHA are occupied by Cu-II, sites A and B by Fe-III
and site A by Mn-II, while only identical metal binding site A in NHA
is tight enough to resist metal removal by brief water washing. A new
helical HA molecular model based on the empirical formula C36H30N2O15
. xH(2)O visualizes metal binding and the likely roles of HAs in biomi
neralization. Site A is suggested to be carboxylate, mixed ligands pro
bably constitute site B, and site C is tentatively assigned as the int
erior of the HA helix. Binding free energies and EPR evidence suggest
that Cu2+(aq), Fe3+(aq) and Mn2+(aq) rapidly transfer between specific
HA binding sites. This affects rates of metal release and transfer to
minerals.