Bismuth(III)-based materials are
uniquely suited for in situ subsurface
remedy applications, as they offer many beneficial properties, including
high affinity for multiple contaminants, low human and environmental
toxicity, low cost, and synthetic availability. This review summarizes
the current research trends in targeted development of bismuth materials
potentially useful for subsurface remedy applications, with an emphasis
on recent advances in understanding of relevant structure–property
relationships. While various bismuth mineral phases can provide frameworks
for contaminant sequestration, layered crystalline arrangements are
particularly promising because of their electronic and spatial flexibility
and their ability to accommodate a wide range of negatively charged
species. This translates into a high uptake capacity for several recalcitrant
colocated contaminants found at legacy nuclear processing sites, including
technetium-99, iodine-129, hexavalent chromium (chromate), and uranium,
and offers the potential for both in situ and ex situ remediation
applications. Layered bismuth minerals are found in nature, and knowledge
of their structure informs the targeted design and cost-effective
synthesis of the structurally preorganized materials from readily
available bismuth sources for remedial applications in soil and groundwater.
This comprehensive review highlights the structure, synthesis, and
environmental chemistry of Bi-based materials, including the interaction
between Bi-based materials and key environmental contaminants, to
explore their potential use for remediation. Bismuth oxyhydroxides,
containing clusters of [Bi6O4(OH)4]6+ and [Bi6O5(OH)3]5+ surrounded by easily exchangeable anions such as nitrate,
are versatile and show the greatest potential for environmental remediation
applications. Because of their flexible structural arrangement, they
have been shown to sequester electronically and sterically different
anionic species, including chromate, pertechnetate, iodate, and uranyl
carbonate, even when they are present as comingled contaminants in
groundwater and pore water containing other competing anions (e.g.,
nitrate and carbonate) and in contact with subsurface sediments.