Surface reactivity of minerals is
impacted by structural impurities
in minerals that are prevalent in nature. In this study, we investigate
the impact of Al substitution on ferrihydrite’s surface reactivity
through surface complexation modeling. Al-bearing ferrihydrites were
prepared with various amounts of Al, including 6, 12, and 18 mol %
Al. Potentiometric titrations were simulated with a 1-pK charge distribution
multisite complexation (CD-MUSIC) model and the MUlti-start optimization
algorithm for surface complexation equilibrium parameters (MUSE).
The surface structure model for Al-ferrihydrite was based on the assumptions
that the total surface site density of Al-ferrihydrite is similar
to pure ferrihydrite, the mol % Al corresponds to the respective percentage
of the total site density of the mineral surface, and Al is substituting
singly coordinated surface hydroxyls in Fe1 octahedral sites. Sensitivity
analysis on the protonation constant and site density of Al sites
revealed a nonuniform distribution of Al compared to the bulk composition.
The results indicate a relative increase of AlOH sites on the Al-Ferrihydrite
surface by 21% for 6 Al-Fh, 25% for 12 Al-Fh, and 30% for 18 Al-Fh,
which suggests that the entire surface will contain only singly coordinated
AlOH groups at 22 mol % Al, instead of the maximum of 29% based on
a uniform distribution between bulk and surface. Overall, the findings
of this study indicate that the influence of Al is higher than anticipated
based on the molar ratio and provide insight into the distribution
of impurities within the structure of ferrihydrite.