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Rare Earth Elements (REEs) as Natural
Tracers for Evaluating In-situ
Groundwater Remedies
Innovative Science for a Sustainable Future
EPA developed and tested a methodology for using Rare Earth Element (REE) patterns as tracers to
understand whether groundwater has interacted with reactive materials in the subsurface used for site
remediation. EPA evaluated this approach at several real-world sites where the Permeable Reactive
Barrier (PRB) technology is being used to treat contaminated groundwater.
EPA's Office of Research and Development (ORD) is now able to provide regional, program, state, and
tribal partners with state-of-the-science support on the application of this REE methodology for ground-
water studies, including its use for tracking the efficiency of groundwater remediation efforts.
What are Rare Earth Elements?
The Rare Earth Elements (REEs) are a group of
metallic elements with unique fluorescent,
conductive, and magnetic properties. REEs include
the elements Lanthanum (La) to Lutetium (Lu), or
atomic numbers ranging from 57 to 71, excluding
Promethium (Pm) which is unstable in nature (see
Figure 1). REE's unique properties and natural
presence in the subsurface make them well-suited as
natural tracers in studies of groundwater movement
and groundwater-surface water interactions. These
elements are commonly present in groundwater at
concentrations in the nanogram per liter to microgram
per liter range.
How Can REEs Act as Tracers?
While REEs are commonly used as natural tracers in
studies of regional groundwater migration and
groundwater-surface water interactions, this research
documents the first use of REEs as tracers for
understanding in-situ groundwater remediation. This
research showed that REEs are sensitive tracers for
evaluating how groundwater interacts with reactive
materials, such as zero-valent iron (ZVI) and organic
carbon, that are placed in the subsurface for
contaminant remediation.
Reactive materials used for remediation lower
contaminant concentrations in groundwater by
changing redox (reduction-oxidation) conditions and
contaminant solubility in water, or by providing
57 58 59 60 61 62 63 64 65 66 67 68 69 70 71
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H
a


He
Li
Be

B
C
N
0
F
Ne
Na
Mg


Al
Si
P
S
CI
Ar
K
Ca
Sc
Ti
V
Cr
Mn
Fe
Co
Ni
Cu
Zn
Ga
Ge
As
Se
Br
Kr
Rb
Sr
Y
Zr
Nb
Mo
Tc
Ru
Rh
Pd
Ag
Cd
In
Sn
Sb
Te
I
Xe
Cs
Ba
Q
Hf
Ta
W
Re
Os
Ir
Pt
Au
Hg
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Pb
Bi
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Rn
Fr
Ra
Ac
Rf
Db
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Mt
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Figure 1. The Rare Earth Elements are part of the
Lanthanide group inthe periodic table of elements.
mineral or organic surfaces that bind contaminants
and remove them from water.
Analysis of geochemical tracers for understanding in-
situ remediation is an important tool in cases where
contaminant concentrations in areas downgradient
from treatment zones fail to decrease within expected
timeframes, i.e., where the in-situ remedy fails to
meet cleanup objectives.
How Can REEs Inform Site Cleanup?
Over the past several decades, in-situ remediation
technologies for cleaning up contaminated
groundwater at hazardous waste sites have emerged
through research and applied testing. Technology
development has typically progressed from
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theoretical conceptualization, to laboratory bench-
and pilot-scale testing to full-scale application for site
cleanup.
However, even the "well established" technologies
sometimes fail to provide expected cleanup results.
Such cases typically result in follow-up analysis in
order to uncover the cause(s) of the remedy failure.
EPA research is developing needed methodologies
to evaluate and prevent remedy failures and to
improve monitoring in the field.
What Research Has EPA Done?
EPA's Office of Research and Development (ORD)
developed a method for measuring REEs in
groundwater using a High Resolution-lnductively
Coupled Plasma-Mass Spectrometer (HR-ICP-MS).
The method uses a standard "metals" sample
(filtered or unfiltered) collected in a plastic bottle and
preserved with nitric acid for sample analysis and
determination of REE concentrations in
groundwater.
ORD, working with scientists from EPA Regions 1
and 6, evaluated groundwater geochemistry and
REE concentrations at several sites where the PRB
(Figure 2) technology is being used to treat
contaminated groundwater. The PRBs utilize zero-
valent iron (ZVI) and organic-carbon plus limestone
mixtures for contaminant (inorganics and chlorinated
solvents) treatment.
The research showed that REE concentrations &
patterns can be used as tracers to probe the key
question of whether groundwater has interacted with
reactive materials emplaced using subsurface
injection ortrench-and-fill methods. In several
examples of well-performing PRBs, REE
concentrations were reduced to levels below
detection (<4 ng/L) as groundwater moved across
the location of the installed PRBs. In one example of
a non-functioning ZVI PRB (i.e., no indicated
contaminant reduction), REE levels and patterns
were unchanged across the flow path presumed to
intercept the treatment medium. The implication at
Figure i. Conceptualization of a groundwater
contaminant plume interaticing with a Permeable
Reactive Barrier, Source: https://www.enviro.wiki/index.php?
title=Zerovalent Iron Permeable Reactive Barriers
this site is that the ZVI was not appropriately placed
in order to intercept and treat the contaminated
groundwater plume. This finding has led to
subsequent site investigations to better understand
subsurface conditions.
More information on this collaborative research can
be found in the paper titled "Rare-Earth Elements as
Natural Tracers for In-situ Remediation of
Groundwater," published in Environmental Science &
Technology (2021, volume 55, pages 1251-1259;
https://pubs.acs.orq/doi/10.1021/acs.est.0c06113).
Contacts
Technical Contact/Principal Investigator:
Richard Wilkin, Ph.D.
EPA Office of Research and Development
580-436-8874
wilkin.rick@epa.gov
Communications/Media Contact:
Charlena Bowling
EPA Office of Research and Development
513-569-7648
bowlinq.charlena@epa.gov
EPA/615/F-22/001
June 2022
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