Surface complexation models (SCMs)
have been successfully used
to describe and predict adsorption phenomena for a large number of
surfaces. SCMs have benefited from advancements in the microscopic
characterization of interfacial structure which has aided in constraining
their parametrization. Yet, SCMs have not adequately addressed the
role of defects and substitutions in surface reactivity despite the
fact that such surfaces are more environmentally prevalent than their
ideal counterparts. In this study, we address this challenge by investigating
the aluminum-doped variant of ferrihydrite (Fh). We consider the placement
of Al within the Fh structure and develop a basic Stern SCM accommodating
that placement which we apply to a set of previously published ζ
potential data. Our hypothesis is that Al primarily replaces Fe1 surface
sites within the Fh structure forming singly coordinated AlOH surface
groups possessing higher protonation constants than their FeOH counterparts.
The SCM fits the ζ potential data adequately, including a close
match to the isoelectric pH values (pHiep, ζ potential
= 0) of 8.0, 8.5, and 8.9 for pure, 12% Al-substituted, and 24% Al-substituted
Fh, respectively. Moreover, the fit slipping plane distance, where
the ζ potential is assumed to be expressed, is consistent with
previous modeling efforts. Although a wider variety of experimental
data will be necessary to determine the true extent and location of
Al substitution within the Fh structure, and to thoroughly characterize
the charging and adsorptive properties of variously substituted Al-Fhs,
our SCM represents a vital stepping stone toward developing more environmentally
relevant SCMs.