Introduction
Low-level radioactive waste (LLW) comprises all radioactive waste that is not classified as high-level radioactive waste, transuranic waste, spent nuclear fuel, byproduct material [as defined in Section 11e.(2) of the Atomic Energy Act], or naturally occurring radioactive material (
DOE 1999). This type of waste includes items that have become contaminated with radioactive material or have become radioactive through exposure to neutron radiation (
NRC 2002). The activity of LLW can range from just above natural background levels to high activity in certain cases [e.g., in reactor vessel parts, NRC (
2002)]. LLW waste is characterized by radioactive decay, in which an unstable atomic nucleus loses energy by emitting ionizing radiation (
NRC 2002). Mixed waste (MW) is LLW that is codisposed with other wastes, such as hazardous waste. Radionuclides of concern in LLW or MW include
,
,
,
,
,
,
,
,
,
,
,
, and
. Alpha-emitting transuranic nuclides with a half-life
and all nuclides with a half-life
may also be present in LLW (
CFR 2001).
LLW is disposed in near-surface facilities designed to limit the dose received by receptors in the surrounding environment (
Tian et al. 2016a,
b). Facilities for MW are also designed to limit the dose and must also meet applicable regulatory criteria for the codisposed waste stream. Migration of meteoric water through LLW creates leachate as constituents in the waste dissolve through a combination of physical, chemical, and microbial processes in a manner analogous to leachate generation in municipal solid waste (MSW) landfills (
Christensen and Kjeldsen 1989;
Christensen et al. 1998;
Kjeldsen et al. 2002). Multilayer liner systems with composite barriers, leachate collection systems, and leak detection are used for MW facilities and for some LLW facilities to control the release of constituents in leachate (
Benson et al. 2003;
Powell et al. 2011;
Rustick et al. 2013).
Limited information exists regarding concentrations of radionuclides and other chemical components in LLW leachate. Abdelaal and Rowe (
2015) provide a brief summary of the characteristics of LLW leachate from six sites in North America, reporting
(
) and
(
) as the dominant radionuclides with other radionuclides (e.g.,
,
,
, and
) present at low concentrations. Their LLW leachates were alkaline (pH 8.0–12.3) and oxidizing (
). Heavy metals (e.g., Al, Ba, Fe, Pb, Ni, Ag, and Zn) had concentrations
. The major anions were nitrite/nitrate measured as total nitrogen (
),
(
), and
(
).
Leachate data were evaluated in this study from four composite-lined LLW and MW disposal facilities operated by the U.S. DOE to support environmental restoration activities. Composition of the leachates is divided into four categories: inorganic macrocomponents, metals and metalloids, radionuclides, and organic compounds. Temporal trends, temporal variability, and site-to-site variability are described and a typical LLW-MW leachate is suggested.
Data Sources
Leachate data from four LLW disposal facilities operated by DOE were analyzed: the Environmental Restoration Disposal Facility (ERDF) in Hanford, Washington (operated from 1996, leachate data from 1996 to 2010); the On-Site Disposal Facility (OSDF) at the former Fernald Feed Materials Production Center in Crosby, Ohio (operated from 1989, leachate data from 2005 to 2010); the Idaho Comprehensive Environmental Response, Compensation, and Liability Act (CERCLA) Disposal Facility (ICDF) at the Idaho National Laboratory in Idaho Falls, Idaho (operated from 2003, leachate data from 2003 to 2010); and the Environmental Management Waste Management Facility (EMWMF) at the Oak Ridge National Laboratory in Oak Ridge, Tennessee (operated from 2002, leachate data from 2003 to 2010). These DOE facilities engaged in production of materials for nuclear weapons during World War II and the Cold War, resulting in contamination of infrastructure and the surrounding environment. DOE’s Division of Environmental Management is responsible for decommissioning the contaminated infrastructure and restoring the environment at these sites. On-site disposal facilities for LLW and MW are used to manage waste streams derived from decommissioning and restoration activities. Except for Fernald, which is fully decommissioned, each of these DOE disposal facilities is operating. A final cover with a composite barrier system has been placed at Fernald’s OSDF (
Benson et al. 2003) with an anticipated average percolation rate of
(
Powell et al. 2011). Waste at the other sites is covered with interim soil cover.
ERDF is located in the semiarid shrub-steppe of the Pasco Basin in the Columbia Plateau in southeastern Washington State with average annual precipitation of
. ICDF is located in the high desert of eastern Idaho with average annual precipitation of
. Both ERDF and ICDF are in semiarid and seasonal climates, with intermittent snowfall and freezing conditions (
SRNL 2014). OSDF is in southwestern Ohio in a humid and seasonal climate with annual precipitation of
with intermittent snowfall and freezing conditions (
Powell et al. 2011). EMWMF is in a very humid climate in eastern Tennessee, with infrequent snowfall and freezing conditions and the highest annual precipitation of the four sites (
) (
Williams et al. 2000;
SRNL 2014).
The wastes disposed at ERDF, ICDF, OSDF, and EMWMF consist primarily of contaminated soil and debris generated from building demolition (
Benson et al. 2007a,
b;
Powell et al. 2011;
Rustick et al. 2013,
2015;
DOE 2016a,
b). Sludges, contaminated protective clothing, and contaminated refuse (paper, packing material, glassware, tubing, resins, activated metals, rags) are also disposed in these locations. Portland cement–based grouts are used to fill voids in containers containing miscellaneous wastes and larger items with cavities. Wastes from decontamination and decommissioning that are regulated as hazardous and nonhazardous wastes under the Resource Conservation and Recovery Act (RCRA) and wastes regulated under the Toxic Substances Control Act (TSCA) (e.g., asbestos) are codisposed with LLW (
DOE 2009).
Each of these DOE facilities employs a double liner system along with a leachate collection and leachate detection system, as illustrated by the liner system profiles shown in Fig.
1 (
Benson et al. 2007a,
2008a,
b;
Powell et al. 2011;
Rustick et al. 2013,
2015;
DOE 2016b). The leachate collection system is covered with a 305-mm-thick soil protective layer. Leachate at each site is collected in sumps in the leachate collection system, stored temporarily in tanks, and treated prior to discharge to the environment. The tanks are set to automatically pump when reaching 80% capacity (
DOE 2015). Samples of the leachate are collected from the tanks and analyzed quarterly or semiannually at each site as part of regulatory reporting (
DOE 2008,
2011,
2014,
2015). Data from these regulatory reporting activities (all in the public domain) were used for the analyses in this study. The data were provided by site managers or their designees.
All leachate samples were collected using the procedures described in “Environmental Monitoring and Management,” ENV-1-2.20 (
DOE 2008), following site-specific quality assurance/quality control (QA/QC) procedures (
DOE 2008,
2014,
2015). Sampling QA/QC for ERDF is established in ENV-1-2.36, “River Corridor Quality Assurance Program Plans” (
DOE 2008), and for OSDF in “Fernald Preserve Quality Assurance Project Plan” (
DOE 2015). The QA/QC protocols at ICDF follow “The Quality Assurance Project Plan for Waste Groups 1, 2, 3, 4, 5, 6, 7, 10 and Inactive Sites” (
DOE 2014).
A summary of the analytical methods used to analyze the leachate samples is in Table
1. Total concentrations of major cations and heavy metals are determined by inductively coupled plasma-atomic emission spectrometry (ICP-AES) per U.S. EPA Method 6010B and concentrations of major anions are determined by ion chromatography using EPA Methods 9060, 300, 325.2, 353.1, 353.2, 375.2, 4500D, and 4500E (
DOE 2008,
2014,
2015). Total organic carbon is measured using EPA Methods 9060 and 415.1. Radionuclides are analyzed using alpha spectroscopy, alpha-gas proportional counting, liquid scintillation, beta-gas proportional counting, and gamma spectroscopy (
DOE 2008,
2009,
2011,
2014). Uranium is determined using phosphorescence analysis and by U.S. EPA Method 6010B. Volatile organic compounds (VOCs), semi-VOCs, and pesticides were also analyzed by U.S. EPA methods (Table
1), but were not evaluated systematically in this study (see subsequent discussion).
Results and Discussion
Bulk chemical characteristics of the leachates (pH, Eh, and TOC) are summarized in Table
2. Radionuclides analyzed at each facility are summarized in Table
3. Concentrations of the constituents in the leachates are summarized in Tables
4–6. The constituents are grouped into four categories: inorganic macrocomponents, including major cations (
,
,
, and
) and major anions (
,
,
, and
) (Table
4); metals and metalloids such as Al, As, Ba, Cu, Fe, Li, Mn, Ni, Sr, and Zn (Table
5); and radionuclides (Table
6). The radionuclides that are analyzed vary between sites depending on the waste stream being disposed and regulatory agreements.
Bulk Chemical Parameters
The pH of the leachates typically is circumneutral, varying over a modest range (5.7–9.1) with a majority of the data (66%) having pH 6.5–7.5 [Fig.
2(a) and Table
3]. The site average pH ranges from 6.87 to 7.57. Leachate from ERDF had the highest average pH (7.57), which reflects the extensive use of cement-based grouts at ERDF and the alkaline contaminated soils being disposed. Zachara et al. (
2007) report that pH of sediments in the vadose zone at Hanford ranges between 7.0 and 8.5.
The pH is essentially time invariant at all sites [Fig.
2(b)], exception for a drop of approximately 2 pH units at EMWMF after 2 years of operation. The consistency in pH is probably due to buffering provided by contaminated soils that are disposed in these facilities. This is in contrast to the pH behavior of MSW leachate, which varies systematically from 4.5 to 8.0–9.0 during the lifespan of a MSW landfill as the organic fraction undergoes different states of degradation (
Kjeldsen et al. 2002;
Benson et al. 2008b;
Staley and Barlaz 2009;
Barlaz et al. 2010).
Redox potential (Eh) of the leachates ranges from -193 to 344 mV at OSDF, EMWMF, and ICDF [Figs.
3(a and b)]. Redox potential data were not available for ERDF. The mean Eh of the leachate at the three sites ranges from 72.1 to 144.5 mV (Table
2), indicating an oxidizing environment, on average. Similar to pH, Eh is essentially time invariant at all sites.
Total organic carbon (TOC) data were available for the leachates at OSDF, EMWMF, and ERDF (TOC data were not available for ICDF). The TOC ranges from 0.86 to
, the site average TOC ranges from 4.3 to
, and the overall mean TOC is
(Table
3). The relatively low TOC of the leachates is consistent with the waste stream being composed primarily of demolition debris and contaminated soils. This contrasts the TOC of MSW leachate, which ranges from 30 to
due to the high organic fraction in the MSW waste stream (
Kjeldsen et al. 2002;
Staley and Barlaz 2009). The ionic strength of the leachates ranges from 2.15 to 135.8 mM, which is dilute relative to MSW leachate (
Bradshaw and Benson 2014).
Inorganic Macrocomponents
Concentrations of inorganic macrocomponents, including the major cations and the major anions, are listed in Table
4 with ranges of total concentration and mean concentrations. The major cations have the following ranges:
, 0.77–29.40 mM;
, 0.20–6.33 mM;
, 0.04–1.94 mM; and
, 0.19–38.13 mM. The major anions have the following ranges:
, 0.39–29.60 mM;
, 0.12–19.27 mM; and
and
, 0.00021–38.30 mM.
Box plots of concentrations of the major cations (
,
,
, and
) are shown in Fig.
4. Concentrations of
and
are much higher at OSDF than at the other three LLW sites. The majority of waste at OSDF consists of contaminated glacial tills, which contain 40–70% carbonate on average (
DOE OLM 2008). Crushed limestone was used to construct the leachate collection system (LCS) and leak detection system (LDS) at OSDF, providing a source of
and
for the leachate (
DOE OLM 2008). The moderate to high
and
concentrations at ERDF and ICDF may also reflect the extensive use of cement-based grouts for disposal at these sites.
Concentration records for the major cations at the four sites are shown in Fig.
5. Concentrations of all major cations are relatively constant at OSDF, ERDF, and ICDF, reflecting a relatively constant waste stream and well-mixed leachate. At EMWMF, Ca and K were relatively constant for almost 6 years, and then began increasing significantly. In contrast, Na and Mg increased gradually throughout the first 6 years, and then leveled off (Mg) or increased substantially (Na). EMWMF also had the lowest concentrations for the major cations during the first six years, but the increases beginning at 6 years brought the leachate more in line with major cation concentrations at the other sites. The reason for the abrupt increase in concentration at EMWMF could not be identified; it may reflect a change in the waste stream due to a shift in decommissioning activities requiring greater use of grouts.
Concentrations of the major anions (
,
, and
or
) are shown in Fig.
6. OSDF has higher concentrations of
(
) [Fig.
6(a)] due to large amounts of drywall and concrete debris disposed from decommissioning. The EMWMF site consistently has the lowest anion concentrations of the four sites, which reflects the lower cation concentrations shown in Figs.
4 and
5. The elevated
concentrations at ERDF and ICDF reflect disposal of contaminated soils at these semiarid sites, where
tends to be more abundant in the vadose zone.
Concentration records for the major anions are shown in Fig.
7. Similar to those of the major cations, anion concentrations at OSDF, ERDF, and ICDF are relatively constant throughout the record. At EMWMF, the anion concentrations are relatively constant after the first year, except for an abrupt increase in
around 6 years. Some of this increase in
, and the concomitant increase in
, may be due to disposal of drywall from decommissioning. However, the increases in
and
that occurred at the same time are unlikely to be associated with drywall disposal. The
concentrations also increased in the EMWMF leachate during this period (see next section).
Trace Elements (Metals and Metalloids)
Concentrations of trace elements (metals and metalloids) in the leachates can be found in Table
5. All of the trace elements except Al and Fe had very low concentrations: 0.18–87 μM for Al, 0.033–1.89 μM for As, 0.16–3.3 μM for Ba, 0.0047–5.4 μM for Cu, 0.022–43 μM for Fe, 0.090–139 μM for Li, 0.016–132 μM for Mn, 0.010–1.86 μM for Ni, 0.92–55 μM for Sr, and 0.0082–2.6 μM for Zn. While they may be important from the perspective of environmental health risks, they are too low to impact the engineering behavior of the barrier systems used in LLW disposal facilities (
Tian et al. 2016a,
b). Additional trace elements, such Co, Cd, and Cr, are also found in LLW leachates, but the concentrations tend to be below minimum detection levels.
Concentrations of four trace metals (Fe, Mn, Cu, and Ba) in leachate at each site are shown as box plots in Fig.
8 and in a temporal record in Fig.
9. Like those of the major cations and anions, concentrations of the trace elements are relatively constant over time except at EMWMF, although the variability in the trace metal concentrations is much higher than in the concentrations of the major cations and anions. For example, the coefficient of variation (COV) of the trace metal concentrations ranges from 0.17 to 2.70 and has an average of 0.95, whereas the COV for the major cations ranges from 0.12 to 0.63 with an average of 0.36; for major anions the range is 0.05 to 1.75 with an average of 0.53. At EMWMF, the concentration of Mn increased sharply from 0.1 to 30 μM at 6 years, and the concentration of Ba decreased systematically from 6 to 1 μM over the same period. These systematic changes occurred at the same time as the systematic changes in
,
,
, and
, and likely reflect a change in the waste stream at EMWMF.
Attenuation processes may be responsible for the low concentrations of metals in the leachates. Kjeldsen et al. (
2002) indicate that sorption and precipitation immobilize metals in MSW leachate, resulting in fairly low heavy metal concentrations. Similar mechanisms may be occurring in these LLW and MW leachates. Waste soils at neutral pH also can have significant sorptive capacity for heavy metals (
Bozkurt et al. 1999).
Radionuclides
A summary of radionuclide concentrations in the leachates is in Table
6. At the EMWMF site, a much broader suite of radionuclides in leachate is monitored relative to monitoring at ERDF, ICDF, and OSDF. The U and
levels are monitored at all four sites, and
is measured at three of the four sites. Of the four sites, ERDF leachate has consistently higher radionuclide concentrations than leachates from the other sites.
Except for U,
,
,
,
,
, and
, many of the radionuclides are present at concentrations below detection limits. Several of these radionuclides were reported only at a single site (e.g.,
ranging from 1.23 to
and
ranging from 0.14 to
at EMWMF) or had very low activity (e.g.,
at ICDF and EMWMF). Consequently, the focus hereafter is on the four radionuclides that are the most prevalent: total U,
,
, and
. Box plots of concentrations for these radionuclides are shown in Fig.
10. Concentration records are shown in Fig.
11.
Total Uranium
Concentrations of total uranium are shown in Fig.
10(a) (box plots) and Fig.
11(a) (temporal record). Uranium is reported in micrograms per liter for leachate at the OSDF, ERDF, and EMWMF sites, and in terms of activity at ICDF. To provide for a uniform comparison, the total U concentration in micrograms per liter at ICDF was calculated based on the activity of each of the uranium isotopes (
,
, and
). The average uranium concentration across all sites and over time is
, more than 25 times the U.S. maximum contaminant level (MCL) for U in drinking water (
).
The ERDF site leachate has the highest U concentrations of the four sites, being at least an order of magnitude higher on average [Fig.
10(a)]. In addition, the U concentration in ERDF leachate increased from 212 to
during the first decade of data, and then leveled off at approximately
. In contrast, at the other sites, the U concentration remained relatively constant (OSDF, ICDF) or dropped over time (EMWMF).
The high concentration of uranium in LLW leachate reflects the significant amount of uranium-contaminated soil, waste, and debris disposed at OSDF, ERDF, and EMWMF during environmental restoration activities. In addition, attenuation of U in ERDF wastes may be limited due to their near neutral pH (Table
2 and Fig.
1) and the prevalence of
in the leachate [Fig.
5(a)]. Dong et al. (
2005) indicate sorption of uranium is limited in circumneutral environments, particularly with
. Um et al. (
2007) indicate that calcite coatings can block sorption sites, and that
forms a strong uncharged aqueous complex (
Um et al. 2007).
Technetium-99
The
levels range from
to more than
at the four LLW sites [Fig.
10(b)]. The radionuclide
is challenging, with a long half-life (
) and high mobility as the oxyanion pertechnetate
(
Um and Serne 2005). The EPA drinking water standard has a combined standard of
for beta emitters, which converts to a MCL of
(
EPA 2002). The maximum concentrations of
in LLW leachate at ERDF (up to 37.0 Bq) and EMWMF (up to 47.9 Bq) modestly exceed the EPA drinking water standard MCL.
The highest concentrations of
are at ERDF (
) and the lowest are at ICDF (
). The
concentrations are relatively constant at OSDF, ERDF, and ICDF [Fig.
11(b)]. At EMWMF,
concentrations dropped more than two orders of magnitude over 4 years, starting with some of the highest concentrations observed at all four sites and diminishing to the lowest, being comparable to concentrations in leachate at ICDF at the end of the record. The
record at EMWMF exhibits
first flush behavior, which is characteristic of the release of surficial soluble compounds as water percolates through a waste form (
Bin-Shafique et al. 2006). The elevated precipitation at EMWMF, which is located in humid Tennessee and is much wetter than any of the other three sites, may have exacerbated the rapid drop in
concentrations at EMWMF.
Strontium-90
Strontium-90, a byproduct of nuclear fission that is found in spent nuclear fuel and waste from nuclear reactors, is monitored in leachate at EMWMF and ICDF (Table
6). At both sites,
increases during the first 3–4 years and then levels off in the range approximately
[Fig.
11(c)]. The MCL of
, derived from the U.S. EPA drinking water standard (
EPA 2007), is
, or approximately 60 times lower than the highest concentration observed at EMWMF (
).
Even with the initial increase in concentration,
concentrations in the leachate at EMWMF and ICDF are relatively low, which is probably due to sorption though ion exchange mechanisms (
Zachara et al. 2007) and formation of less soluble carbonates. Um and Serne (
2005) report strong sorption of
on Hanford sediments. Rimstidt et al. (
1998) indicate that Sr behaves similarly to Ca, dissociating to a divalent cation in solution with similar atomic radius (1.00 nm for Ca versus 1.12 nm for Sr). Consequently, Sr can substitute for Ca in calcite and aragonite, forming strontianite (
) (
Rimstidt et al. 1998;
Faure 2001).
Tritium
Tritium (
) concentrations are shown in box plots in Fig.
10(d) and in terms of a temporal record in Fig.
11(d) for EMWMF, ERDF, and ICDF. Tritium concentrations are not monitored at OSDF. Tritium concentrations at ERDF (
), although limited, are nearly two orders of magnitude higher than at EMWMF or ICDF (
). No temporal trends are evident in the tritium data [Fig.
11(d)]. The MCL of
derived from the U.S. EPA drinking water standard is
. The
concentrations at EMWMF and ICDF are below the MCL, whereas the
concentration at ERDF is approximately 5 times higher than the MCL.
Gross Alpha and Beta Activity
Gross alpha and beta activity in the leachates at ERDF and EMWMF are shown in Fig.
12. Uranium is the predominant source of alpha activity, whereas
,
, and
are the predominant sources of beta activity.
Gross beta activity increased systematically at both sites, and was approximately the same at both sites, leveling off after 10 years for ERDF. Similar leveling off may occur at EMWMF in subsequent years. The is a likely source of the increase in beta activity, as concentrations increased consistently at both sites, although the concentration at EMWMF leveled off after 4 years, and the concentrations of the radionuclides that are sources of beta activity remained relatively constant () or decreased (). In contrast, gross alpha activity increased systematically at ERDF, but is highly variable at EMWMF. The trends in alpha activity are consistent with the U concentration records, which show consistently increasing total U in leachate at ERDF and variable and decreasing total U for EMWMF.
Organic Compounds
Volatile organic compounds, semivolatile organic compounds, and pesticides are monitored in the leachate at each site. Concentrations of these compounds are consistently below detection limits (
DOE 2008,
2011,
2014,
2016a). This is consistent with the waste stream in these facilities, which has very little organic matter and consists primarily of inorganic contaminated soil, building debris, and cement-based grouts.
Typical Leachate
A typical synthetic LLW leachate (Table
7) was created to represent LLW leachates observed at the DOE LLW facilities. The leachate contains major cations (
,
,
, and
), major anions (e.g.,
and
), trace metals (e.g., Fe, Al, Cu, and Ni), and radionuclides (e.g., uranium and
). Average concentrations were assigned to each component, except for the radionuclides, which were set at upper bound concentrations to represent worst-case conditions (
Tian 2012,
2015). The pH (
) and Eh (
) of the LLW leachate were also set at the averages in the LLW leachate database. This typical leachate can be used to investigate and predict the long-term performance of components in composite liners, similar to those shown in Fig.
1. For example, Tian et al. (
2016a) used this leachate recipe to evaluate the hydraulic conductivity of geosynthetic clay liners to LLW and MW leachate. Similarly, Tian et al. (
2016b) used the leachate recipe to evaluate the service life of geomembranes in DOE facilities.