Groundwater quality eﬀ ects from septic tanks were investigated
in the Woodville Karst Plain, an area that contains numerous
sinkholes and a thin veneer of sands and clays overlying the
Upper Floridan aquifer (UFA). Concerns have emerged
about elevated nitrate concentrations in the UFA, which is
the source of water supply in this area of northern Florida. At
three sites during dry and wet periods in 2007–2008, water
samples were collected from the septic tank, shallow and deep
lysimeters, and drainﬁ eld and background wells in the UFA and
analyzed for multiple chemical indicators including nutrients,
nitrate isotopes, organic wastewater compounds (OWCs),
pharmaceutical compounds, and microbiological indicators
(bacteria and viruses). Median NO3–N concentration in
groundwater beneath the septic tank drainﬁ elds was 20 mg
L−1 (8.0–26 mg L−1). After adjusting for dilution, about 25 to
40% N loss (from denitriﬁ cation, ammonium sorption, and
ammonia volatilization) occurs as septic tank eﬄ uent moves
through the unsaturated zone to the water table. Nitrogen
loading rates to groundwater were highly variable at each site
(3.9–12 kg N yr−1), as were N and chloride depth proﬁ les in the
unsaturated zone. Most OWCs and pharmaceutical compounds
were highly attenuated beneath the drainﬁ elds; however, ﬁ ve
OWCs (caﬀ eine, 1,7-dimethylxanthine, phenol, galaxolide, and
tris(dichloroisotopropyl)phosphate) and two pharmaceutical
compounds (acetaminophen and sulfamethoxazole) were
detected in groundwater samples. Indicator bacteria and
human enteric viruses were detected in septic tank eﬄ uent
samples but only intermittently in soil water and groundwater.
Contaminant movement to groundwater beneath each septic
tank system also was related to water use and diﬀ erences in
lithology at each site.
Fate of E uent-Borne Contaminants beneath Septic Tank Drain elds
Overlying a Karst Aquifer
Brian G. Katz,* Dale W. Gri n, and Peter B. McMahon U.S. Geological Survey
Harmon S. Harden Florida State University
Edgar Wade and Richard W. Hicks Florida Department of Environmental Protection
Je rey P. Chanton Florida State University
A households in the United States uses
a septic tank for wastewater disposal (USEPA, 2003).
Conventional septic tanks are the most commonly used sys-
tems and consist of a tank that allows solids to settle out and
septic tank eﬄ uent (STE) to ﬂ ow to a drainﬁ eld where it per-
colates downward through soil and the unsaturated zone toward
the water table. Various biogeochemical processes occur beneath
the drainﬁ eld that can modify and attenuate certain chemical
and microbiological constituents in the STE. Numerous studies
have assessed the impacts of STE on groundwater quality, with
particular emphasis on the transformation and fate of nutrients
(Wilhelm et al., 1994; Aravena and Robertson, 1998; Hinkle et
al., 2008), bacteria and viruses (DeBorde et al., 1998; Rose et al.,
2000; Darby and Leverenz, 2004), organic wastewater contami-
nants (e.g., Hinkle et al., 2005; Swartz et al., 2006; Conn et al.,
2006), and pharmaceuticals (Seiler et al., 1999; Godfrey et al.,
2007; Carrara et al., 2008). Subsurface pathways of nutrients and
wastewater organic compounds (including pharmaceuticals and
personal care products) are increasingly recognized as a problem
for aquifers (e.g., Barnes et al., 2008; Focazio et al., 2008).
Reasonable estimates of the nitrogen (N) ﬂ ux from septic tanks
to groundwater exist, but this ﬂ ux is mitigated to an unknown
degree by physical, chemical, and microbiological processes
occurring in the shallow subsurface and in the unsaturated zone
above the water table. Apparent loss or attenuation of N beneath
septic tank drainﬁ elds has been observed in varied hydrogeo-
logic settings (e.g., Robertson et al., 1991; Ptacek, 1998; Seiler,
2005; Hinkle et al., 2008). Apparent N loss has been attributed
to several processes, including ammonia volatilization, sorption
of ammonium (NH4+) and organic N on soil particles, denitri-
ﬁ cation, and dilution from inﬁ ltrating rainfall and mixing with
ambient groundwater. Without knowing the amount of N, phos-
phorus, and organic wastewater compounds stored in the unsatu-
rated zone beneath on-site waste disposal sites, it is not possible to
Abbreviations: bls, below land surface; cfu, colony-forming units; DOC, dissolved
organic carbon; KN, Kjeldahl nitrogen; OWCs, organic wastewater compounds; RT-PCR,
reverse transcriptase–polymerase chain reaction; STE, septic tank e uent; UFA, Upper
Floridan aquifer; WKP, Woodville Karst Plain.
B.G. Katz and D.W. Gri n, U.S. Geological Survey, Florida Water Science Center, 2639
N. Monroe St., Tallahassee, FL 32303; P.B. McMahon, U.S. Geological Survey, Colorado
Science Center, Lakewood, CO 80225; H.S. Harden and J. P. Chanton, Florida State Univ.,
Dep. of Oceanography, Tallahassee, FL 32306; E. Wade and R.W. Hicks, Florida Dep.
of Environmental Protection, Tallahassee, FL 32399. Supplemental material available
online for this article. Assigned to Associate Editor Lakwhinder Hundal.
Copyright © 2010 by the American Society of Agronomy, Crop Science
Society of America, and Soil Science Society of America. All rights
reserved. No part of this periodical may be reproduced or transmitted
in any form or by any means, electronic or mechanical, including pho-
tocopying, recording, or any information storage and retrieval system,
without permission in writing from the publisher.
J. Environ. Qual. 39:1181–1195 (2010)
Published online 18 Mar. 2010.
Supplemental les available online for this article.
Received 30 June 2009.
*Corresponding author (email@example.com).
© ASA, CSSA, SSSA
5585 Guilford Rd., Madison, WI 53711 USA
1182 Journal of Environmental Quality • Volume 39 • July–August 2010
accurately model the movement of contaminants to groundwa-
ter and springs from these systems.
A steady increase in nitrate-nitrogen (NO3–N) concen-
trations (0.25–0.9 mg L−1) during the past 30 yr in Wakulla
Springs, a large regional discharge point for water from the
Upper Floridan aquifer (UFA), has increased concerns about
groundwater contamination in the Woodville Karst Plain
(WKP) in northern Florida (Katz et al., 2004). ere are an
estimated 20,000 septic tanks in the WKP (Fig. 1), an area
highly susceptible to groundwater contamination due to
numerous sinkholes and a relatively thin layer of highly perme-
able sands and clays overlying the karstic UFA. Although septic
tanks have been presumed to be a signiﬁ cant source of N to the
unconﬁ ned groundwater system (Chelette et al., 2002), little
direct information exists on the impact of STE on groundwa-
ter quality. Studies in other mantled karst systems have shown
that septic tank systems contributed to elevated NO3 concen-
trations in groundwater (e.g., Panno et al., 2006; Harden et al.,
2003, 2008). Chemicals in many household products can enter
the subsurface from STE in more concentrated amounts, such
as optical brighteners (Murray et al., 2007). Pharmaceutical
compounds have been found in shallow zones of the UFA in
areas where septic tanks are presumably aﬀ ecting groundwater
quality (Katz and Griﬃ n, 2008; Katz et al., 2009).
Our study had two main objectives: (i) to estimate N load-
ing to groundwater from septic tanks in the WKP and (ii) to
determine the attenuation of microorganisms, organic waste-
water compounds (OWCs), and pharmaceutical compounds
in the subsurface beneath septic tank drainﬁ eld sites in the
WKP. Multiple chemical indicators are used to elucidate pro-
cesses controlling the transport and fate of nutrients, OWCs,
and pharmaceutical compounds as eﬄ uent moves downward
from septic tank drainﬁ elds to the groundwater system. In
addition, fecal indicators and enteroviruses are used to examine
the movement of microorganisms beneath the drainﬁ eld sites.
e multitracer approach used in this study can be applied to
a variety of locations in diﬀ erent soil types to improve model
predictions of impacts from NO3 and other contaminants
from septic tanks on groundwater quality.
Description of Study Area and Sites
e study area (approximately 1100 km2) lies within the WKP
and is located in southern Leon and Wakulla Counties (Fig.
1). e WKP is characterized by numerous wet and dry sink-
holes, conduit networks, and disappearing streams (Rupert and
Spencer, 1988). e study area is mostly rural, with low-den-
sity residential areas (most lot sizes >0.4 ha). In the WKP, the
UFA is overlain by a thin veneer of highly porous quartz sand
with highly variable amounts of silt and clay (Fig. 1). Streams
ﬂ owing into this area ﬂ ow into sinkholes and disappear, and
other streams originate in the WKP from spring discharge.
Land-surface altitudes in the WKP are generally less than 15 m
above sea level. e climate is humid subtropical with an aver-
age annual air temperature of 19.5°C and average annual pre-
cipitation of 161 cm (1971–2000), measured at the National
Weather Service station at the Tallahassee Regional Airport
(http://cdo.ncdc.noaa.gov/ancsum/ACS). e largest amount
of monthly rainfall typically occurs in June, July, and August,
and the smallest monthly amount in occurs April, October,
and November. During August 2007 through July 2008, rain-
fall was about 28 cm below average. Recharge to the UFA in
the study area is about 46 cm yr−1 (Davis, 1996), and ground-
water ﬂ ow in the UFA generally is from north to south (Fig. 1)
based on previous potentiometric maps (Chelette et al., 2002).
Fig. 1. Location map showing septic tank sites and generalized lithology at each site.
Katz et al.: Contaminants beneath Septic Tank Drain elds 1183
e three sites selected for this study (Fig. 1) represent a range
of residences and water usage that likely are representative of
septic tank systems in the WKP. Water meters were installed
at each house, and the septic tank at each site was pumped
before the start of the study. Drainﬁ eld pipes are located at
approximately 0.6 m below land surface. e northernmost
site (LT) had two to three adult residents who had lived in the
house since it was built in 1987; the household used the origi-
nal septic tank and drainﬁ eld. Average daily water use at the
LT site was 394 L d−1. No fertilizers had been applied by the
current residents of the house. Depth to groundwater ranged
from 3.0 to 3.6 m during the study.
e HK site had four residents (two adults and two teenage
children), and the septic tank had been in use for approximately
30 yr. Average daily water use during the study period was
1630 L d−1, although water discharge to the septic system was
reduced in early 2008 through the use of water conservation
measures. e septic tank was installed in the mid 1970s, and
the drainﬁ eld was repaired or replaced on three occasions. e
original drainﬁ eld, consisting of terra cotta pipe into a gravel
bed, was extended in 1984. e extension was two gravel-ﬁ lled
trenches with perforated black plastic pipe. at drainﬁ eld
failed in 2005 and was replaced with inﬁ ltrators in February
2005. Due to excessive loading of water, that drainﬁ eld failed
in December 2007 and was replaced in January 2008 by the
current one, which also has inﬁ ltrators. e turf over the new
septic tank drainﬁ eld (approximately 80 m2) was seeded with
rye and given a few handfuls of fertilizer in January 2008. In
May 2008, it was seeded with a summer grass mix, and about
2 kg of fertilizer (10–10–10) was added. In addition, <2 kg of
10–10–10 fertilizer was applied to a garden (about 70 m2) next
to the new drainﬁ eld. Depth to the water table ranged from 2.6
to 2.7 m during the study.
e YG site had two adult residents that have lived in the
household for 4 yr. e house was built around 2003. e
original septic tank system was in use at the time of the study.
Average daily water use was 610 L d−1. No fertilizers had been
applied by the residents of the house. Depth to the water table
ranged from 4.1 to 4.4 m during the study.
All three sites have variable amounts of sands and clays that
overlie limestone of the Upper Floridan aquifer. Soils have low
slopes (0–5%), have low organic matter content (<2%), and
are classiﬁ ed as Alpin sand and Blanton ﬁ ne sands (thermic,
coated Typic Quartzipsamments), Alpin ﬁ ne sands, and Ortega
sands (thermic, uncoated Typic Quartzipsamments) at the LT,
HK, and YG sites, respectively (Allen, 1991). Based on obser-
vations of core material collected during well installation, there
are important diﬀ erences between the lithology of subsurface
material at the three sites (Fig. 1). Sand comprises the upper 2
to 3 m of the subsurface at each site and overlies clayey sand
at the LT and YG sites but overlies weathered limestone at the
HK site. Depth to limestone was variable at each site; the great-
est depth to limestone was at the YG site (Fig. 1). Particle size
analyses of samples from various depth intervals (from land
surface to 123 cm below land surface) at each site indicate vari-
ous mixtures of very ﬁ ne to coarse sand and an increasing per-
centage of silt and clay with depth at each site.
Materials and Methods
e sampling design at each site (Supplemental Fig. S1) con-
sisted of two sets of lysimeters, a background well located
upgradient from the septic tank drainﬁ eld, a well beneath the
drainﬁ eld, and STE. A sampling port was installed by a septic
tank contractor in the pipe that connects the septic tank to the
drainﬁ eld to allow sampling of the STE.
Four suction-cup lysimeters were installed by hand auger
beneath the drainﬁ eld at each of the three sites to collect pore
water samples moving in the unsaturated zone. Details about
lysimeter construction are included in Supplemental Fig. S1.
Each of the shallow lysimeters had a total length of 110 cm and
collected soil water samples from a depth of 92 to 118 cm below
land surface. At this depth the shallow lysimeters were immedi-
ately below the bottom of the drainﬁ eld. Each of the deep lysim-
eters had a total length of 186 cm, sampling from a depth of 168
to 194 cm below land surface. To obtain samples, a suction of
60 kPa was applied to the lysimeters for a period of about 24 h
before sample collection. Nitrogen gas was used to apply a pres-
sure of 5 to 10 kPa to force the water into a collection vessel.
Drainﬁ eld and background wells were installed at each site
using a direct push rig. ese wells consisted of a 1.9-cm-diameter
PVC casing with a 1.5-m-length prepacked screen that was placed
below the water table. A peristaltic pump was used to purge three
well volumes and to collect water samples for analyses.
Water samples were collected at each site on three occasions:
December 2007, March 2008, and July 2008. On each occa-
sion, samples were collected from the STE, the shallow and
deep lysimeters, the drainﬁ eld well, and the background well.
Two lysimeter samples from each depth were combined to
obtain the required volume of sample for laboratory analyses.
Sample collection and preservation methods are described in
the National Field Manual for the Collection of Water-Quality
Data (U.S. Geological Survey, 1999). Speciﬁ c conductance,
pH, dissolved oxygen, and temperature were measured in
water samples in the ﬁ eld. Major ions, nutrients, boron, and
dissolved organic carbon (DOC) were analyzed at the U.S.
Geological Survey National Water Quality Laboratory (USGS
NWQL) in Denver, Colorado (Fishman and Friedman, 1989;
Patton and Truitt, 1992; Brenton and Arnett, 1993; Fishman,
1993; Patton and Truitt, 2000).
Stable isotopes of N, oxygen, and hydrogen were used to
help diﬀ erentiate between sources of N in water samples and to
evaluate N transformation processes. Nitrogen isotope analyses
of dissolved NH4+ (δ15N-NH4) were performed at the USGS
Stable Isotope Laboratory in Reston, Virginia, using continu-
ous-ﬂ ow isotope ratio mass spectrometry (Brenna et al., 1997;
Hannon and Böhlke, 2008) and are reported in parts per thou-
sand (‰) relative to N2 in air. e 2-sigma (σ) uncertainty of
δ15N-NH4 analyses is 0.8‰.
e stable isotope composition of NO3 (δ15N-NO3 and
δ18O-NO3) in water samples was analyzed at the USGS Stable
Isotope Laboratory in Reston, Virginia, by bacterial conversion
1184 Journal of Environmental Quality • Volume 39 • July–August 2010
of NO3 to nitrous oxide and subsequent measurement on a
continuous ﬂ ow isotope ratio mass spectrometer (Sigman et
al., 2001; Casciotti et al., 2002; Coplen et al., 2004). Values
of δ15N-NO3 are reported in ‰ relative to N2 in air (Mariotti,
1983). For samples with NO3–N concentrations ≥0.06 mg L−1,
the 2σ uncertainty of N isotopic results is 0.5‰; for samples
with NO3 concentrations <0.06 mg kg−1 as N, it is 1‰. Values
of δ18O-NO3 are reported in ‰ relative to Vienna Standard
Mean Ocean Water (reference water) and normalized on a
scale such that Standard Light Antarctic Precipitation reference
water is −55.5‰ (Coplen, 1988; Coplen, 1994). For water
samples with NO3–N concentrations ≥0.06 mg L−1, the 2σ
uncertainty of oxygen isotopic data is 1.0‰, and for samples
with NO3–N concentrations <0.06 mg L−1, it is 2‰.
Water samples were analyzed for various groups of OWCs
(Supplemental Table S1) to assess the movement of these com-
pounds into groundwater beneath septic tank drainﬁ elds. e
OWCs included fragrances and ﬂ avorants, ﬂ ame retardants,
antioxidants, fuel-related compounds, detergent metabolites,
plasticizers, disinfectants, solvents and preservatives, poly-
nuclear aromatic hydrocarbons, pesticides, plant and animal
steroids, and caﬀ eine. Samples were collected using protocols
to avoid ﬁ eld contamination of the sample (U.S. Geological
Survey, 1999) because several compounds are present in com-
monly used products, including soaps, fragrances, insect repel-
lants, and beverages. Water samples were ﬁ ltered in the ﬁ eld
through 0.7-μm nominal pore size glass ﬁ ber ﬁ lters, chilled
and maintained at 4°C, and shipped overnight to the labo-
ratory. Samples were analyzed at the USGS NWQL for 63
compounds using capillary-column gas chromatography/mass
spectrometry methods (Zaugg et al., 2002; Burkhardt et al.,
2006; Zaugg and Leiker, 2006). Quality assurance information
for OWCs is included in Supplemental Table S1.
Water samples were collected and analyzed for 16 pharma-
ceutical compounds at the USGS NWQL (Cahill et al., 2004).
Supplemental Table S2 includes a list of these compounds
(selected prescription and over-the-counter drugs and certain
degradates/metabolites) along with laboratory quality assur-
ance information for these compounds.
Subsurface Material Samples
Core samples of unsaturated zone material were collected
beneath the septic tank drainﬁ elds (in between drain lines)
using direct push techniques. is technique resulted in
minimal disturbance to subsurface material due to the small-
diameter holes created by the rig because no cuttings are
produced, and greater sample recovery can be achieved com-
pared with other methods. Subsamples of oven-dried (105°C)
core material from discrete depth intervals were analyzed for
exchangeable NH4+ in a solution extracted with 2 mol L−1 KCl.
Ammonium was analyzed colorimetrically using the salicylate
method (Nelson, 1983; McMahon et al., 2006). Nitrate and
other anions (nitrite, chloride, bromide, and sulfate) were ana-
lyzed in a solution extracted using deionized water (McMahon
et al., 2006). Replicate samples were run after every ﬁ fth envi-
ronmental sample to assess the eﬀ ects of ﬁ eld and laboratory
procedures on measurement variability.
Microbiological samples were collected in sterile 1.0-L bottles
and stored on ice until processed. Samples were analyzed for
the presence of fecal indicator bacteria in duplicate in 5.0 μL
(septic eﬄ uent) to 200-mL volumes. Samples were processed
using membrane ﬁ ltration per Standard Method (SM) 9222D
(American Public Health Association, 1998). Indicator sample
results are expressed in the text and tables as the number of
colony-forming units (cfu) per 100.0 mL of water (average of
Samples also were screened for enteroviruses (polio, cox-
sackie A, coxsackie B, echoviruses, etc.) using 50.0- to 100.0-
mL volumes (volume dependent on particle load) following
a modiﬁ ed reverse transcriptase–polymerase chain reaction
(RT-PCR) and dot blot protocol (Lipp and Griﬃ n, 2004). e
modiﬁ cation was direct concentration of water samples with
Centriprep YM-50 centrifugal ﬁ lter devices (i.e., no acidiﬁ ca-
tion or membrane ﬁ ltration–based preconcentration) follow-
ing the Centriprep protocol in 15-mL increments to a ﬁ nal
volume of ~500.0 µL. RNA was puriﬁ ed from one half of the
Centriprep concentrate using Qiagen’s RNeasy Kit to a ﬁ nal
eluent volume of 30 μL (7 μL was used for RT-PCR). e
combined enterovirus RT-PCR–dot blot results are expressed
as presence (+) or absence (−). Negative and positive controls
were used with all prokaryote and virus assays.
For screening of soil samples for microbial indicators and
viruses, 10 mL of sterile water was added to ~5.0 g of soil and
shaken overnight on a table top rotator at room temperature.
On the following day, samples were centrifuged at 1500 rpm
for 2 min, and 4.5-mL aliquots (×2) were used for membrane
ﬁ ltration following SM 9222D. Indicator sample results are
expressed as the number of cfu per gram of soil (average of
the duplicates). RNA was extracted from ~2.0 g of soil using
the RNA PowerSopil Total RNA Isolation Kit (MO BIO,
Carlsbad, CA). Kit protocol was followed, and 7 μL of eluent
was used for RT-PCR.
Results and Discussion
Distribution of Nitrogen Species in Septic Tank E uent,
Soil Pore Water, and Groundwater
Concentrations of N species varied considerably among
and within sites during the three sampling periods (Fig. 2).
Kjeldahl nitrogen (KN) comprised essentially 100% of the
total N in the STE at each site. About 80 to 94% of the total
N consists of NH4+, which is slightly higher than the range of
75 to 85% in previous studies (McCray et al., 2005). Kjeldahl
nitrogen concentrations in the STE were lowest at the HK site
(17–39 mg L−1) and ranged from 42 to 65 mg L−1 and from
53 to 58 mg L−1 at the YG and LT sites, respectively. High and
low KN concentrations in STE were not consistent temporally
among the three sites (Fig. 2). Nitrate was the dominant form
of N in water samples from the shallow lysimeters, deep lysim-
eters, and the drainﬁ eld well at each site, with median NO3–N
concentrations comprising 94, 95, and 99% of the total N,
respectively. is is consistent with other studies that show
nearly complete and rapid nitriﬁ cation in septic system eﬄ u-
ent within short distances from the distribution lines (Wilhelm
Katz et al.: Contaminants beneath Septic Tank Drain elds 1185
et al., 1994; Ptacek, 1998; Barringer et al., 2006). Ammonium
and organic N comprised almost 44% of the total N in water
from the HK drainﬁ eld well in December 2007, indicating
that the drainﬁ eld was not functioning properly. e hom-
eowner replaced the clogged drainﬁ eld with a new drainﬁ eld
in January 2008, and a new set of lysimeters and a drainﬁ eld
well were installed.
Median NO3–N concentrations were higher in the July
2008 water samples from the shallow and deep lysimeters and
from drainﬁ eld wells at the three sites than in samples from
December 2007 and March 2008. Median chloride concentra-
tions also increased in the July 2008 samples from the deep
lysimeters and drainﬁ eld wells from the three sites but decreased
in the shallow lysimeters. Because the median chloride and KN
concentrations in STE were lower in the July 2008 samples
than in the December 2007 and March 2008 samples, it is
likely that the chloride and NO3–N that were stored beneath
the drainﬁ eld lines moved deeper due to increased rainfall
and recharge during late spring and early summer. e higher
median NO3–N concentration in groundwater samples from
July 2008 also could be biased high due to fertilizer application
at the HK site (see below).
Isotope Ratios of Ammonium, Nitrate, and Water
Values of δ15N-NH4+ in STE samples showed little varia-
tion among sites and temporally, ranging from 4.4 to 4.9‰,
from 4.5 to 5.3‰, and from 5.0 to 5.5‰ at the HK, YG,
and LT sites, respectively. ese values are similar to those
(4.2–5.1‰) for STE from a study of septic tank systems
and packed bed sand ﬁ lters (Hinkle et al., 2008). Values of
− in water samples were more variable and ranged
from <2‰ (YG background well) to 13.4‰ (old drainﬁ eld
well at HK site) (Supplemental Table S3). e low δ15N-
NO3 values (<6.0‰) correspond to values observed else-
where, where NO3 in groundwater is recharged beneath land
receiving inorganic fertilizers (Kendall and Aravena, 2000).
Previous studies have found that NO3–N concentrations and
δ15N-NO3 values were highly variable in groundwater from
sites throughout the WKP and could be attributed to sev-
eral sources, including inorganic fertilizer applied to lawns,
gardens, cropland, and turfgrass, and organic wastes from
domestic wastewater and animal wastes (Katz et al., 2004).
e HK homeowner indicated that fertilizer was applied to
new grass planted on top of the new drainﬁ eld before the col-
lection of the July 2008 samples. Fertilizer applied upgradient
from the YG site may have resulted in the low δ15N-NO3 sig-
nature in the background well, as the homeowner indicated
that no fertilizer had been applied recently.
Additional information about processes aﬀ ecting the trans-
formation of N species can be gleaned from N and oxygen
isotopes of NO3. Values of δ15N-NO3 and δ18O-NO3 increase
systematically in water samples from shallow and deep lysim-
eter samples at the LT and YG sites and plot along trend lines
with a slope of 0.5, which is consistent with denitriﬁ cation
(Fig. 3). is process is related to the ratio of enrichment of
oxygen to N in NO3, which has been shown to be close to 1:2
(Aravena and Robertson, 1998; Kendall and Aravena, 2000).
Additional evidence for this ratio of enrichment of oxygen to
N in NO3 is based on a comparison of plotted values of δ18O-
H2O and δ18O-NO3 (Supplemental Fig. S2 and Table S3). e
higher δ15N-NO3 and δ18O-NO3 values in the LT deep lysim-
eter site could be related to higher clay content in the sub-
surface, which could create conditions (perched-water; slower
water movement, low-dissolved-oxygen microsites) more
favorable to denitriﬁ cation. Problems with ponding and poor
drainage over time at the old HK drainﬁ eld likely resulted in an
enriched δ15N-NO3 and δ18O-NO3 signature in the December
2007 sample from the drainﬁ eld well; however, similarly high
isotopic values were not seen in the shallow lysimeter at this
time. Mixed redox conditions at the water table at the old HK
drainﬁ eld site likely were present in December 2007, as indi-
cated by elevated NH4+, NO3, and dissolved oxygen concentra-
tions (Table 1). e July samples at the new HK drainﬁ eld site
clearly show the inﬂ uence from the application of synthetic
fertilizer, with low δ15N-NO3 values <6‰. Elevated δ15N-NO3
(8–10‰) and δ18O-NO3 (5–6.5‰) values for water from the
HK background well may indicate the inﬂ uence from upgradi-
ent septic tanks in the area.
Fig. 2. Plots showing concentrations of nitrogen species in water
samples from the background well, septic tank, lysimeters, and
drain eld well at each site. Nitrogen species include nitrate (NO3–N),
organic nitrogen (ORG-N), and ammonium (NH4–N).
1186 Journal of Environmental Quality • Volume 39 • July–August 2010
Depth Pro les of Nitrogen Species and Chloride in
Unsaturated Zone Material
Analyses of N species and chloride in soil core material from
various depth intervals provide snapshots of N and Cl ﬂ uxes
to the water table before and after the water samples were col-
lected. Ammonium N concentrations (expressed as mg L−1 by
accounting for moisture content of the oven-dried samples)
were substantially higher in core samples from depths <5 cm
at the YG site compared with the two other sites (Fig. 4). At
depths >50 cm, NO3–N generally was the dominant N spe-
cies at the three sites, which corresponds to the oxic conditions
measured in soil pore water from lysimeters and in groundwa-
ter (top of UFA). Nitrogen concentrations were substantially
higher in the July 2008 samples compared with November
2007 samples at all three sites. At the LT site, the highest N
(NO3) concentration (about 110 mg L−1) at the 180-cm depth
corresponded to the highest chloride concentration. is depth
interval also contains a higher amount of clay (~5%) compared
with other depth intervals analyzed for particle size distribu-
tion. Depth proﬁ les of chloride concentrations were similar at
the YG site between November 2007 and July 2008. In con-
trast, higher chloride concentrations were measured in core
samples beneath the old drainﬁ eld compared with those col-
lected beneath the new drainﬁ eld at the HK site (Fig. 4). At all
three sites, N concentrations in the unsaturated zone generally
were higher than concentrations measured in STE but were
similar to N concentrations measured in water samples from
shallow lysimeters at the YG and HK sites. Concentrations at
the LT site were considerably higher in extracts of unsaturated
zone material than in water from shallow lysimeters. High vari-
ability of N concentrations in soil and unsaturated zone pore
water among sites has been reported in other studies (Rosen et
al., 2006; Hinkle et al., 2008). e high
variability of N concentrations between
the three sites likely is due to a combi-
nation of factors, such as N loading, soil
characteristics and lithology, and dilu-
tion from household activities such as
washing clothes and bathing.
Large diﬀ erences in concentrations
of N species and chloride with depth
between the November 2007 and the
July 2008 samples appear to be related to
diﬀ erences in rainfall and recharge con-
ditions before sampling. In December
2007, the previous 30-, 60-, and 90-d
rainfall amounts (7, 13, and 21 cm)
were substantially lower than before the
March (22, 29, and 36 cm) and July
(15, 25, and 27 cm) sampling events.
Increased recharge in the spring and
early summer of 2008 likely resulted in
downward movement of N (NH4+ and
NO3). With increased rainfall/recharge,
one would expect that concentrations
in the unsaturated zone would be lower
(i.e., more dilution) than during periods
of lower rainfall. However, it is likely that
NH4+ and organic N in water retained beneath the drainﬁ elds
may have been converted to NO3 as it moved toward the water
table. At the LT site, the perched-water conditions created by
the presence of higher amounts of clay at lower depths may
account for the increase in chloride and N at the 170 cm depth
and possibly allowing more water–sediment contact time for
NH4+ desorption reactions.
Attenuation of Nitrogen beneath Septic Tank Drain elds
Median and mean N (dissolved) concentrations in STE
decrease with depth as the STE percolates downward from
the drainﬁ eld to the water table, as indicated by progressively
lower concentrations in shallow lysimeters, deep lysimeters,
and drainﬁ eld wells. Mean N concentrations (± 1σ) for all
samples of STE, shallow lysimeters, deep lysimeters, and drain-
ﬁ eld wells were 45 ± 14, 30 ± 21, 22.6 ± 16.5, and 21 ± 6.8
mg L−1, respectively (Fig. 5). Also, N concentrations decrease
with depth to about 25 to 40 mg L−1 in pore water samples
from the unsaturated zone. Dilution accounts for some of
the decrease in N concentrations (15–25%) based on median
and mean chloride concentrations, respectively, in STE, water
from shallow and deep lysimeters, and drainﬁ eld wells (Fig.
5) (assuming that chloride is conservative and that there are
no naturally occurring sources of chloride in the unsaturated
zone). Nitrogen loss is related to denitriﬁ cation, sorption of
NH4+ (includes adsorption and ion exchange) on soil particles,
and ammonia volatilization.
Denitri cation and Ammonium Volatilization
Decreased N concentrations in soil water and groundwater may
result from denitriﬁ cation or ammonia volatilization. At the
YG and LT sites, there were average increases of 3.3 and 3.6‰
between δ15N-NH4 in water samples from STE and δ15N-NO3
Fig. 3. Plot of nitrate isotope data for water samples from the background well, septic tank, lysim-
eters, and drain eld well at each site. Values of δ15N and δ18O are given with respect to air N2 and
Vienna standard mean ocean water, respectively, in parts per thousand.
Katz et al.: Contaminants beneath Septic Tank Drain elds 1187
Table 1. Physical properties and concentrations† of major dissolved chemical constituents in water samples from septic tanks, background (back.) wells, shallow (shal.) and deep lysimeters (lys.), and drain-
eld (drain.) wells at the three studied sites.
Site Date Smpl.
t‡ Temp. Sp.
as P DOC‡ Ca Mg Na K Cl−Sulfate F−SiO2BAlk., as
°C μS cm−1μg L−1
tank 18 Dec
2007 1430 19.0 725 2.2 6.5 39‡ 47 <0.04 5.8 33 50 1.8 27 9.6 27 E0.12§ 0.14 14 22 293 0.04 680
tank 13 Mar.
2008 1200 23.6 887 1.0 6.6 56 65 <0.04 7.8 46 46 2.2 42 15 41 <0.18 0.12 9.6 253 346 E0.07 591
tank 16 July
2008 1140 20.2 738 6.6 38 42 <0.04 6.2 26 48 1.7 34 9.9 35 4.5 E.09 9.5 191 285 0.05 694
2008 1145 20.2 738 6.6 38 43 <0.04 6.2 26 50 1.7 35 10 35 4.4 0.1 11 207 287 0.05 692
well 18 Dec.
2007 1200 18.4 20 6.2 8.3 <0.10 1.2 <0.04 0.13 7.1 0.15 0.42 1.8 0.17 2.6 1.1 <0.12 8.5 7.9 <5 <0.02 ND
well 13 Mar.
2008 940 17.8 182 5.3 5.3 <0.02 E0.08 0.2 0.12 1.1 33 0.96 1.8 0.40 2.6 1.3 <0.12 5.8 8.7 84 E0.01 263
well 16 July
2008 930 21.7 225 6.5 <0.02 E0.14 0.39 0.13 0.8 39 1.1 2.8 0.37 5.6 2.5 <0.12 5.3 7.9 103 0.03 187
well 18 Dec.
2007 1350 21.0 288 5.6 5.7 0.08 0.29 18.7 0.02 2.2 3.7 7.9 29 11 27 7.6 0.14 6.3 200 <5 0.04 665
well 13 Mar.
2008 1030 20.4 324 4.8 5.0 0.07 0.14 20.5 0.02 1.3 5.4 8.3 29 11 32 7.7 0.17 5.7 164 <5 0.04 805
well 16 July
2008 1000 24.0 294 5.5 0.13 0.21 16.2 0.02 0.7 4.3 6.8 27 8.9 35 7.1 0.14 5.2 142 <5 0.04 865
lys. 18 Dec.
2007 1340 17.0 438 5.9 5.7 0.02 0.49 26.2 <0.006 15 42 3.4 26 4.8 31 17 NS 13 31 27 0.03 1043
lys. 13 Mar.
2008 1130 18.6 439 3.3 5.7 0.11 0.77 18.6 0.02 14 35 1.7 45 5.0 39 22 <0.12 11 186 44 0.04 970
lys. 17 July
2008 1110 29.6 1450 6.2 0.13 4.9 51.9 0.04 24 105 1.6 195 0.96 196 58 <0.12 14 470 153 0.21 933
lys. 18 Dec.
2007 1400 17.2 421 5.3 5.7 0.04 0.58 22.7 <0.006 NS NS NS NS NS 31 20 NS NS NS 34 E0.02 1560
lys. 13 Mar.
2008 1100 17.2 332 4.0 5.5 E0.02 0.45 4.97 E0.003 14 29 1.4 35 1.1 27 19 <0.12 8.6 100 79 E0.02 1370
lys. 16 July
2008 1050 28.4 467 6.0 0.04 0.61 14.4 0.01 16 35 1.1 53 2.3 40 28 <0.12 12 234 78 0.07 571
1188 Journal of Environmental Quality • Volume 39 • July–August 2010
Site Date Smpl.
t‡ Temp. Sp.
as P DOC‡ Ca Mg Na K Cl−Sulfate F−SiO2BAlk., as
tank 19 Dec.
2007 1130 19.0 1050 1.5 6.8 26 30 <0.04 5.4 43 63 15 86 11 136 24 0.21 15 61 257 E0.25 544
tank 12 Mar.
2008 1300 22.2 566 1.7 7.0 14 17 0.2 4.0 22 69 4.6 17 4.3 20 7.1 E0.09 7.6 99 242 0.02 1010
tank 15 July
2008 1200 29.8 725 6.6 35 39 <0.04 7.2 56 56 6.3 26 10.8 30 4.2 0.15 10 115 290 0.05 598
well 19 Dec.
2007 900 21.0 435 1.6 6.2 0.06 0.15 0.37 E0.006 2.1 91 2.3 2.1 0.20 3.1 4.4 0.13 7.6 11 222 <0.04 77
well 12 Mar.
2008 1000 18.9 397 3.5 6.3 <0.02 E0.08 0.53 E0.004 0.9 81 1.9 2.1 0.12 4.3 4.2 <0.12 6.0 8.6 198 E0.02 213
well 15 July
2008 920 25.0 400 6.7 <0.02 <0.14 0.39 0.01 1.2 77 2.1 2.1 0.23 3.4 4.5 E0.07 7.2 12 201 E0.01 339
2007 945 21.0 894 7.3 6.3 6.9 7.6 9.9 0.02 3.1 139 5.7 28 5.1 43 18 E0.09 11 154 338 0.1 427
2008 1110 19.4 560 2.1 6.6 1.00 1.5 8.2 0.11 2.7 93 4.2 11 2.6 18 12 <0.12 6.6 53 211 0.04 453
2008 1115 19.4 560 2.1 6.6 0.81 1.2 8.0 0.06 2.6 93 4.1 11 2.5 18 12 <0.12 6.7 54 211 0.03 603
2008 1020 25.4 763 6.5 <0.02 0.26 30 1.0 2.1 105 6.3 29 5.7 46 19 E0.06 11 51 180 0.11 420
lys. 19 Dec.
2007 1100 15.0 1270 3.0 6.7 0.08 0.81 57 0.87 13 171 20 68 11 103 104 E0.11 13 102 122 0.21 490
lys. 12 Mar.
2008 1230 18.0 673 5.0 6.9 0.62 1.7 23 0.22 11 98 8.4 22 11 27 21 <0.12 24 130 204 0.05 534
lys. 15 July
2008 1120 27.0 1080 6.4 0.06 2 50 0.64 30 156 17 9.7 20 9.1 34 E0.07 13 65 288 <0.02 ND
lys. 12 Mar.
2008 1140 18.5 680 4.2 6.9 0.32 1.2 21 0.16 16 93 8.5 19 7.6 27 23 <0.12 17 105 181 0.06 447
lys. 15 July
2008 1050 26.6 783 6.4 <0.02 1.7 42 0.24 40 118 13 10 14 14 27 <0.12 8.7 52 202 <0.02 ND
tank 19 Dec.
2007 1730 16.0 1030 1.6 7.1 52 58 <0.04 13 50 46 12 57 21 41 2.4 0.24 25 71 391 E0.05 812
tank 11 Mar.
2008 1300 18.4 923 2.8 7.1 48 53 <0.04 11 49 50 9.7 41 20 35 2.0 0.20 23 57 373 E0.03 1150
tank 17 July
2008 1200 25.7 1100 6.9 51 54 E0.02 6.3 31 49 11 85 18 31 9.2 0.18 14 83 491 E0.04 773
well 11 Mar.
2008 1030 18.8 195 4.9 6.8 <0.02 E0.07 0.11 0.01 1.1 34 2.4 1.5 0.22 2.7 3.5 <0.12 5.6 9.0 92 E0.01 270
well 17 July
2008 910 21.3 193 7.0 <0.02 E0.13 0.08 0.01 1.4 34 2.6 2.0 0.23 2.7 3.4 E0.06 7.3 9.1 93 E0.01 271
Table 1. Continued.
Katz et al.: Contaminants beneath Septic Tank Drain elds 1189
in lysimeters and the drainﬁ eld well samples. ese
increases in N-isotopic composition, along with the
decrease in N at these sites, are consistent with iso-
topic fractionation resulting from denitriﬁ cation or
volatilization of ammonia. At the HK site, the lower
average increases of 1.7‰ (0.4‰ median) between
δ15N-NH4 in STE samples and δ15N-NO3 in lysim-
eters and the drainﬁ eld samples likely were aﬀ ected
by fertilizer applications in April and May to turf-
grass above the drainﬁ eld. However, samples showed
an increase of 8.5‰ between δ15N-NH4 and δ15N-
NO3 in water samples collected from the old drain-
ﬁ eld well in December 2007 and an increase of 3.7
to 4.0‰ in the new drainﬁ eld well in March 2008
before fertilizer applications.
Denitriﬁ cation likely occurs directly beneath the
drainﬁ eld lines in all three systems. Other studies
report about 10 to 25% N loss due to denitriﬁ cation
and ammonia volatilization before the leachate leaves
the bottom of the drainﬁ eld, depending on the initial
N concentration in STE (Bauman and Schafer, 1985;
Hantzsche and Finnemore, 1992). Septic tank eﬄ u-
ent from the three sites has elevated concentrations
of DOC, with a median concentration of about 42
mg L−1 (Fig. 5; Table 1). Median concentrations in
soil water from lysimeters decrease to about 15 mg
L−1, indicating that DOC was consumed (or sorbed)
during inﬁ ltration. However, water samples generally
are oxic, but denitriﬁ cation can occur in anaerobic
microsites beneath septic tank systems in otherwise
oxic systems (Koba et al., 1997). Concentrations
of DOC in the drainﬁ eld well decrease to slightly
greater than those in the background wells. Evidence
for some denitriﬁ cation can be seen from enriched
values of δ15N and δ18O of NO3 (Fig. 3). ere is a
shift toward more enriched values for water samples
from shallow and deep lysimeters at the LT and YG
sites and for water from the old drainﬁ eld well at the
HK site. ese slightly enriched values of δ15N and
δ18O of NO3 plot along denitriﬁ cation trend lines
with a slope of 0.5 (Kendall and Aravena, 2000).
Sorption of Ammonium
Ammonium strongly sorbs to mineral surfaces, partic-
ularly clay minerals (Drever, 1988); however, Hinkle
et al. (2008) found essentially complete sorption of
NH4+ on coarse sand with only 0.4% silt and clay in
column experiments. Almost 100% of sorbed NH4+
was recovered using 2 mol L−1 KCl in column desorp-
tion experiments (Hinkle et al., 2008). Even though
soil cores were not collected directly beneath drainﬁ eld
lines (to prevent damage to the existing system), the
cores collected and analyzed for N species between the
drainﬁ eld lines provide information about NH4+ sorp-
tion by soils. Based on 2 mol L−1 KCl extracts of core
samples, NH4+ concentrations ranged from 0.2 to 8.2
−1 (~5–190 μeq NH4+ gsoil
−1) in the November
2007 samples (Fig. 6) below the bottom of the drain-
ﬁ eld (depth of about 80–100 cm). Higher amounts of
Site Date Smpl.
t‡ Temp. Sp.
as P DOC‡ Ca Mg Na K Cl−Sulfate F−SiO2BAlk., as
well 19 Dec.
2007 1430 20.0 733 6.5 6.9 0.14 0.29 23 0.18 3.1 78 19 55 4.2 27 21 0.22 42 304 252 0.08 335
well 11 Mar.
2008 1115 19.3 794 5.8 6.9 0.04 0.19 24 0.17 2.4 85 19 46 4.3 29 21 0.13 30 285 254 0.05 584
well 17 July
2008 1010 21.3 762 6.8 0.03 0.19 26 0.31 1.9 80 20 47 4.4 28 20 0.14 31 210 237 0.05 550
Shal. lys.19 Dec.
2007 1600 12.0 716 5.5 7.3 0.04 1.5 24 3.3 NS NS NS NS NS 30 40 0.20 NS NS 177 <0.02 ND
Shal. lys.11 Mar.
2008 1200 16.9 312 5.6 7.2 E0.02 0.5 0.47 1.1 13 41 12 3.7 1.8 1.6 10 0.14 12 92 146 <0.02 ND
Shal. lys.17 July
2008 1130 27.1 942 6.9 <0.02 1.6 6.5 3.1 40 91 25 60 1.6 18 43 0.30 33 182 359 E0.01 1830
lys. 19 Dec.
2007 1620 16.0 724 4.5 7.2 E0.01 1.6 22 3.2 13 69 20 48 11 27 33 0.24 21 59 204 E0.02 1350
lys. 11 Mar.
2008 1230 16.7 365 5.5 7.3 0.02 0.83 1.9 3.1 9.8 45 13 12 3.4 2.6 8.9 0.19 18 39 172 <0.02 ND
lys. 17 July
2008 1100 27.4 1120 6.6 0.03 1.4 33 5.6 20 90 25 79 17 54 53 0.21 25 70 267 0.05 1086
† Concentrations are in mg L−1 unless otherwise noted.
‡ Smpl. t., sample time; Sp. cond., speci c conductance; Diss., dissolved; Amm., ammonia; ON, organic nitrogen; DOC, dissolved organic carbon; Alk., alkalinity.
§ E, estimated value between method reporting level and detection limit; NS, no sample collected due to insu cient volume of water; ND, not determined as bromide concentration is below method reporting level.
¶ Duplicate sample.
Table 1. Continued.
1190 Journal of Environmental Quality • Volume 39 • July–August 2010
NH4+ were found in KCl extracts of soil material in the July 2008
samples (2–10 µg gsoil
−1). ese values fall within the range of
total cation exchange capacities for glacial outwash sands (5–20
μeq g−1; Bohlke et al., 2006) to various types of clays (28–8800
μeq g−1) (Busenberg and Clemency, 1973). us, there would be
suﬃ cient opportunity for additional NH4+ sorption, particularly
with the increasing relative amounts of clay minerals with depth.
Also, NH4+ sorption by soils was likely greater beneath the new
HK drainﬁ eld because this material was not at steady state with
respect to NH4+ sorption. e source of the higher amounts of
NH4+ in samples from the shallow subsurface (<100 cm) at the
YG site is unknown but may result from ammonia volatilization,
nitriﬁ cation of organic N, or fertilizer applications.
Nitrate-Nitrogen Loading to Groundwater from Septic Tanks
Based on average daily water use at each household (metered)
and NO3–N concentrations at the water table (adjusted for
dilution), N loading (kg N yr−1) to groundwater ranged from
4.3 to 5.4 at the YG site, 3.9 to 4.3 at the LT site, and 6.6 to
12 at the HK site. e higher loading at the HK site compared
with the two other sites results from a higher average daily
water use (~1,630 L d−1) and the larger range in NO3–N con-
centrations over the three sampling events. e July 2008 NO3
data from the HK drainﬁ eld well were not used to calculate
septic tank loads because fertilizer applications in May resulted
in a large increase in NO3 in water
from the drainﬁ eld well (39 mg
L−1) (and the lysimeter samples).
Annual per capita N loading rates
to groundwater at the LT and YG
sites are lower than other estimates
of 4.5 kg N yr−1 (Cox and Kahle,
1999), which would yield 9 and
13.5 kg N yr−1 for households
with two and three people, respec-
tively. Based on septic tank stud-
ies in central Florida (Sherman
and Anderson, 1991) and Oregon
(Morgan et al., 2007), about 9.5
to 9.7 kg N yr−1 per home are
released to the drainﬁ eld, and it is
estimated that an additional 25%
reduction in N occurs beneath the
drainﬁ eld (Anderson et al., 1994;
Morgan et al., 2007). e annual
N loading for the HK site (6.6–12
kg N yr−1) also is lower than the
estimated loading to groundwater
of 18 kg N yr−1 based on per capita
N loading (Anderson et al., 1994;
Cox and Kahle, 1999).
Although only three septic tank
systems were studied, measured N
loading rates to groundwater are
consistent with results from other
studies. Furthermore, the number
of people living in each house-
hold, per capita water use, loca-
tion, and age of the studied septic
tank systems are representative of the area. Given that there are
many uncertainties in extrapolating from the studied sites to
the approximately 20,000 septic tanks in the WKP, it is esti-
mated that annual NO3–N loading to groundwater from septic
tanks in the WKP would range from 78,000 to 240,000 kg.
is estimated range of N loading to groundwater can be con-
sidered conservative because NO3–N loads from septic tanks in
this study are lower than those from other studies (due to lower
per capita water use). Even with the conservative estimate of N
loading from septic tanks in the WKP, this source represents a
substantial contribution compared with the estimated N load-
ing to the land surface (about 2 million kg N yr−1) from other
sources (atmospheric deposition, the land application of treated
wastewater eﬄ uent, commercial fertilizers, livestock, and sink-
ing streams) (Chelette et al., 2002). After N losses are considered
for these other sources (e.g., uptake by vegetation, soils, denitri-
ﬁ cation, and volatilization), the relative contribution from septic
tanks would be considerably higher and would represent a sig-
niﬁ cant source of NO3 to the groundwater system.
Attenuation of Organic Wastewater
and Pharmaceutical Compounds
Given the relatively low analytical spike recoveries for several
OWCs (<60%) and for surrogate compounds (Supplemental
Fig. 4. Depth pro les of ammonium-N, nitrogen (sum of nitrate-N, nitrite -N, and ammonium-N), and chloride in
subsurface samples from various depth intervals collected from each site in November 2007 and July 2008.
Katz et al.: Contaminants beneath Septic Tank Drain elds 1191
Table S4), detections for individual compounds only were
considered when the measured concentrations were at least
three times the method reporting level. No OWCs were
detected in blank water samples submitted to the NWQL
during the study or in samples from background wells. In STE
samples, 25 OWCs were detected out of the 63 compounds
analyzed (Supplemental Table S4). e concentrations for
most of these compounds were below 10 μg L−1; however,
50% or more STE samples had ﬁ ve compounds with concen-
trations >10 μg L−1: caﬀ eine, 1.7-dimethylxanthine (caﬀ eine
degradate), menthol, p-cresol, and phenol. Concentrations of
detergent metabolites and disinfectants (e.g., triclosan) were
considerably lower than those found in other studies (e.g.,
Hinkle et al., 2005; Conn et al., 2006) and may result from
uptake by solids and removal by sedimentation in the septic
tank (Conn et al., 2006).
Substantial attenuation or removal of OWCs was observed
in the subsurface beneath the drainﬁ elds. Phenol and cotinine
were the only compounds detected in samples from lysimeters
(Supplemental Table S4). Five OWCs were detected in the
drainﬁ eld well at the HK site (caﬀ eine, 1.7-dimethylxanthine,
phenol, galaxolide, and tris(dichloroisopropyl)phosphate).
Tris(dichloroisopropyl)phosphate was detected twice in sam-
ples from the YG site drainﬁ eld well. Concentrations of these
OWCs in groundwater samples were <1.0 µg L−1. Multiple
detections of tris(dichloroisopropyl)phosphate in groundwa-
ter samples may indicate that this compound would be useful
as an indicator of STE in shallow groundwater. e higher
number of OWCs detected in drainﬁ eld wells compared with
those for shallow and deep lysimeters may be indicative of the
ineﬃ ciency of lysimeters as collectors of these compounds.
Leachate could be moving along preferential pathways that
Fig. 5. Boxplots showing concentration distribution of nitrogen, chloride, and
dissolved organic carbon in water samples from the background well, septic
tank, lysimeters, and drain eld well at each site.
Fig. 6. Depth pro le of ammonium in soil samples based on extracts
of 2 mol L−1 KCl solution.
1192 Journal of Environmental Quality • Volume 39 • July–August 2010
would lower the eﬀ ectiveness of using lysimeters to collect
OWCs in the unsaturated zone. Another possibility is that
some compounds may have been excluded (i.e., removed)
during passage through the ceramic cup.
Two pharmaceutical compounds (acetaminophen and sulfa-
methoxazole) were detected in water samples from septic tanks,
lysimeters, and drainﬁ eld wells. Median recoveries for these
two compounds in spike samples were 78 and 63%, respec-
tively (Supplemental Table S2). Acetaminophen (an over-the-
counter analgesic) was detected in eight of nine STE samples in
concentrations ranging from 0.18 to 78.2 μg L−1 at the HK site
(Supplemental Table S5). Sulfamethoxazole (an antibiotic) was
detected in only one STE sample (HK site; 0.04 μg L−1). is
compound was detected in all three water samples from the LT
site drainﬁ eld well but not in any of the STE samples from this
site. Sulfamethoxazole also was detected once in concentra-
tions below the method reporting level in drainﬁ eld well water
samples from the YG site (0.02 μg L−1) and the HK site (0.04
μg L−1). Low-level concentrations of these compounds in water
samples from lysimeters and shallow groundwater (drainﬁ eld
wells) are consistent with the movement of sulfamethoxazole
from septic systems and its persistence in shallow groundwater
in other studies (Godfrey et al., 2007; Carrara et al., 2008).
Sulfamethoxazole, which has a low sorption aﬃ nity in soils
(Cordy et al., 2004; Drillia et al., 2005), has been found in
shallow zones of the Upper Floridan aquifer in areas where
septic tanks likely have aﬀ ected groundwater quality (Katz and
Griﬃ n, 2008; Katz et al., 2009).
Microbial Indicators and Enteric Viruses
Numbers of fecal coliforms were highly variable temporally in
STE samples from each site and among sites (Table 2). For
example, fecal coliforms in STE samples from the HK site
ranged from 120,000 cfu per 100 mL in July 2008 to 380,000
cfu per 100 mL in March 2008. Fecal coliforms in STE
from the LT site ranged from 1.4 million cfu per 100 mL in
December 2007 to 7.8 million cfu per 100 mL in July 2008
and from 150,000 in July 2008 to 2.7 million cfu 100 per mL
in March 2008 at the YG site. Rapid attenuation of fecal coli-
forms was observed at all sites; however, occasional detections
of fecal coliforms (e.g., high concentrations in the HK drain-
ﬁ eld well in March 2008) appear to be related to high rainfall
amounts during the previous 30 to 60 d.
Enteroviruses were detected in STE samples from all three
sites in December 2007 and in March 2008 but not in any of
the July 2008 samples (Table 2). Enteroviruses were detected in
an unused domestic well (i.e., an irrigation well) at the HK site,
in the LT deep lysimeter in December 2007, in the LT back-
ground well and in both YG lysimeters in March 2008, and
in the LT shallow lysimeter in July 2008. Sporadic detections
and transport of enteroviruses in soil water and groundwater
samples beneath the three septic tank drainﬁ elds are consistent
with other studies (Darby and Leverenz, 2004; DeBorde et al.,
1998; Abbaszadegan et al., 1999). e absence of enteroviruses
in the July 2008 STE samples may indicate seasonality for this
region because previous studies have shown that the entero-
virus season runs from June through October in temperate
Table 2. Microbiological data for samples of septic tank e uent, soil water from lysimeters, and water from drain eld and background wells at each
Site† Fecal coliforms Enteroviruses
Dec. 2007 Mar. 2008 July 2008 Dec. 2007 Mar. 2008 July 2008
——————— c f u 100 mL−1‡ ———————
Background well 0.0 16.8 0.5 –§ – –
Septic tank e uent 220,000 380,000 120,000 + + –
Drain eld well 0.0 tntc¶ 6.0 – – –
Lysimeter, shallow 0.0 0.0 0.0 – – –
Lysimeter, deep nl 0.0 0.0 nl – –
Domestic well used for irrigation 0.5 0.0 3.0 + – –
Background well 0.0 0.0 0.0 – + –
Septic tank e uent 1,450,000 4,660,000 7,800,000 + + –
Drain eld well 0.0 0.0 0.0 – – –
Lysimeter, shallow 0.0 0.0 0.0 – – +
Lysimeter, deep 0.0 0.0 0.0 + – –
Background well 0.0 0.3 0.3 – – –
Septic tank e uent 210,000 2,720,000 150,000 + + –
Drain eld well 5.7 0.0 0.0 – – –
Lysimeter, shallow 0.0 0.0 0.0 – + –
Lysimeter, deep 2.0 0.0 0.0 – + –
† Data are for culturable fecal coliform and reverse transcriptase–polymerase chain reaction dot blot detection of human enteroviruses.
‡ cfu, colony-forming units.
§ +, presence; −, absence.
¶ nl, no lysimeter installed on this date; tntc, too numerous to count.
Katz et al.: Contaminants beneath Septic Tank Drain elds 1193
regions and may be continuous in tropical and semitropical
environments (Moore, 1982; Melnick, 1989).
Generally there was little relation between detections of
fecal coliforms and OWCs and pharmaceutical compounds. In
samples where enteroviruses were detected, there were occa-
sional detections of OWCs and pharmaceuticals; for example,
in soil water from shallow lysimeters, caﬀ eine was detected at
the YG site in March 2008, and phenol was detected at the LT
site in July 2008. In soil water from deep lysimeters, cotinine
was detected at the YG site in March 2008, and phenol and
camphor were detected at the LT site in December 2007. e
slightly higher number of detected compounds in the March
and July samples may in part be related to increased rainfall
and recharge that may enhance the transport of these com-
pounds in the subsurface.
Movement of Chloride and Bromide
Chloride/bromide (Cl/Br) ratios have been used to discriminate
between wastewater and other sources of chloride from anthro-
pogenic and naturally occurring contaminants in groundwater
(Vengosh and Pankratov, 1998; Panno et al., 2006; Brown et
al., 2009). e Cl/Br ratios in samples of STE ranged from
540 to 1150, with a median Cl/Br ratio of 694 (n = 9). is
median value is similar to the median Cl/Br ratio (769; n =
29) reported by Panno et al. (2006) for STE. Groundwater
samples from wells beneath the three drainﬁ elds had a slightly
smaller range of Cl/Br ratios (335–805) and a median of 518
(Supplemental Fig. S3). Based on the small number of samples
from this study, it appears that groundwater samples with a Cl/
Br range of 400 to 1100 may be useful as a screening tool for
evaluating septic tank inﬂ uence on groundwater quality.
Septic tank eﬄ uent represents a substantial source of N load-
ing to groundwater in the WKP, an area in northern Florida
that is highly vulnerable to contamination due a thin veneer
of sands and clays overlying a karstic aquifer. Given that mea-
sured N loading to groundwater from three studied septic tank
systems is consistent with results from other studies and that
the studied septic tank systems are representative of other sys-
tems in the area, it is estimated that N loading to groundwater
from the approximately 20,000 septic tanks in the WKP would
range from 78,000 to 240,000 kg N yr−1.
e use of multiple chemical and isotopic indicators pro-
vided important information about N transport to ground-
water, which was aﬀ ected by three main processes. e 50%
apparent loss of N as drainﬁ eld STE moves to the water table
is related to (i) dilution, which accounted for only about 10 to
25% of the decrease in N concentrations from STE to ground-
water; (ii) denitriﬁ cation, indicated by a systematic increase in
δ15N and δ18O of NO3 in soil water from lysimeters; and (iii)
sorption of ammonia and retention on soil particles, indicated
by the release of NH4+ in 2 mol L−1 KCl extracts of soil core
samples. Fertilizers applied to lawns and gardens also may rep-
resent an important (but unknown) source of N contamina-
tion in this area.
For the most part, microbial indicators, viruses, organic
wastewater compounds, and pharmaceutical compounds are
highly attenuated or removed as the STE percolates through
about 5 to 7 m of unsaturated zone material. Only sporadic
detections of fecal coliforms, enteroviruses, organic wastewater
compounds, and pharmaceutical compounds were found in
soil water from shallow and deep lysimeters and in ground-
water (drainﬁ eld wells). Higher detections of fecal indica-
tors, enteric viruses, OWCs, and pharmaceuticals were found
in groundwater at the site where the depth to the limestone
was the shallowest and average daily water use was highest.
Enterovirus data from this study are consistent with the move-
ment of viruses from septic tanks found in other studies, indi-
cating that there is a potential for contamination of drinking
water supplies from septic tanks and that there is a human
health risk in karstic aquifer systems.
Further work is needed to assess the impacts of septic sys-
tems on groundwater quality in higher density areas in the
karst plain, particularly where limestone is near the land sur-
face, to protect drinking water supplies from on-site waste dis-
posal practices. Current health department regulations require
a 23-m separation between a septic tank drainﬁ eld and a pota-
ble well, which may not be suﬃ cient in areas of higher septic
tank density or where the top of the limestone aquifer is near
is study was funded by the Florida Department of Environmental
Protection and the USGS. e authors thank D. Blum and H. Davis
for assistance with sampling; T. Coplen for stable isotope analyses; the
USGS National Water Quality Laboratory for analyses of wastewater
and pharmaceutical compounds; and S. Hinkle, S. Panno, L. Hundal,
and several anonymous reviewers, whose comments were very helpful
in revising this manuscript.
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