Coal combustion residuals (CCRs),
in particular, coal fly ash,
are one of the major industrial solid wastes in the U.S., and due
to their high concentrations of toxic elements, they could pose environmental
and human health risks. Yet detecting coal fly ash in the environment
is challenging given its small particle size. Here, we explore the
utility and sensitivity of using geochemical indicators (trace elements,
Ra nuclides, and Pb stable isotopes), combined with physical observation
by optical point counting, for detecting the presence of trace levels
of coal fly ash particles in surface soils near two coal-fired power
plants in North Carolina and Tennessee. Through experimental work,
mixing models, and field data, we show that trace elements can serve
as a first-order detection tool for fly ash presence in surface soils;
however, the accuracy and sensitivity of detection is limited for
cases with low fly ash proportion (i.e., <10%) in the soil, which
requires the integration of more robust Ra and Pb isotopic tracers.
This study revealed the presence of fly ash particles in surface soils
from both the recreational and residential areas, which suggests the
fugitive emission of fly ash from the nearby coal-fired power plants.