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Water Research 37 (2003) 3145–3154
Environmental fate of Triclosan in the River Aire Basin, UK
Darius Sabaliunasa,*, Simon F. Webbb, Armin Haukc, Martin Jacobc,William S. Eckhoffd
aProcter & Gamble Technical Centers Ltd., Rusham Park, Whitehall Lane, Egham, Surrey, TW20 9NW, UKbProcter & Gamble Eurocor, BelgiumcCiba Specialty Chemicals, SwitzerlanddThe Procter & Gamble Company, USA
Received 24 May 2002; accepted 21 March 2003
Abstract
The concentrations and removal rate of Triclosan, an antibacterial ingredient in consumer products, were measured
at advanced trickling filter (TF) and activated sludge (AS) wastewater treatment plants (WWTPs) in the River Aire
basin in the UK in September 2000. Additionally, the in-stream removal of Triclosan was measured directly in Mag
Brook, the stream receiving the treated effluent from the TF plant, using a fluorescent dye tracer to determine the water
plug travel times. The in-stream removal of the dissolved and un-ionized (i.e. bioavailable) fraction of the compound
was measured using semipermeable membrane devices (SPMDs) deployed at various distances downstream from the
WWTP discharge point. The estimated removal rates were used in the GREAT-ER (Geography-Referenced Regional
Exposure Assessment Tool for European Rivers) model to predict the site-specific distribution of Triclosan
concentrations in the Aire basin as well as to calculate regional concentrations. High WWTP (B95%) and in-stream(0.21–0.33 h�1) removal rates of Triclosan in Mag Brook confirm that this chemical is rapidly eliminated from the
aquatic environment.
r 2003 Elsevier Science Ltd. All rights reserved.
Keywords: Triclosan; Environmental fate; GREAT-ER; SPMD; Exposure modelling
1. Introduction
Triclosan (5-chloro-2-(2,4-dichlorophenoxy)phenol;
CAS# 3380-34-5, Fig. 1) is an antibacterial agent and
a preservative approved by the EU Cosmetics Directive
[1]. Its widespread use in consumer products, including
cosmetics, is determined by its bacteriostatic efficacy
against a broad spectrum of microorganisms [2] and a
favorable human safety profile [3]. In cosmetic products
such as toothpastes, mouth rinses, soaps, shampoos,
deodorants, skin care creams and lotions, its concentra-
tion is typically in the range of 0.1–0.3%.
Triclosan (MW=289.5) is a non-volatile
(VP=4� 10�6mmHg at 20�C) [2] and poorly solublein water (10mgL�1 at 20�C) organic compound with an
estimated logKow of 4.8 [4]. One of the main routes this
compound enters the environment is with personal care
and other consumer products that are washed down-the-
drain during their normal use. The concentrations and
distribution of Triclosan in the aquatic environment are
governed by its consumer use pattern, removal rate
during wastewater treatment, partitioning (sorption and
ionization) and chemical and biological degradation in
surface waters. Triclosan has been shown to undergo
complete biodegradation in a batch activated sludge test
and to be highly removed in a continuous activated
sludge treatment system [2]. Even though hydrolytically
stable, in the aquatic environment, Triclosan is subject
to photolytic transformation with an estimated half-life
of less than an hour in natural sunlight [2,5,6].
Understanding the processes that determine the fate
of Triclosan in the aquatic environment is important for
the estimation of its environmental exposure and*Corresponding author. Tel.: +44-1784-498615.
E-mail address: [email protected] (D. Sabaliunas).
0043-1354/03/$ - see front matter r 2003 Elsevier Science Ltd. All rights reserved.
doi:10.1016/S0043-1354(03)00164-7
assessment of the associated environmental risk. The
wastewater treatment and in-stream removal rates of
Triclosan may be used in generic mathematical distribu-
tion and exposure models to estimate its predicted
environmental concentration (PEC) in various environ-
mental compartments. Such an approach is used, for
example, in the Technical Guidance Documents (TGDs)
supporting the European Union’s current chemical
legislation [7] to predict ‘‘regional’’ and ‘‘local’’ con-
centrations of a substance undergoing environmental
risk assessment. Even though a ‘‘generic scenario’’
provides a reasonable approximation of substance’s
environmental fate and exposure, it does not account for
spatial and temporal variability in emissions, regional
infrastructure, river flow rates, dilution factors, physical
chemical conditions and other important parameters.
This often invokes the use of conservative assumptions
and application factors to account for worst-case
situations. A ‘‘reality-check’’ of such generic models
may be accomplished via the use of environmental
monitoring data in advanced GIS-based models capable
of predicting site-specific chemical concentrations using
the available underlying environmental databases [8].
The current study was undertaken in order to better
understand the fate of Triclosan in the aquatic environ-
ment and to generate the necessary data for its site-
specific and regional exposure assessments. The primary
objective of the study was to measure the environmental
loadings, concentrations and removal of Triclosan
during wastewater treatment and in river water under
the North European conditions. The second objective
was to use the estimated parameters to model the
concentration distribution of Triclosan in a real river
catchment using GREAT-ER, a GIS-based regional
exposure assessment model.
2. Methods
2.1. Study area and study sites
The River Aire basin is situated in Yorkshire, north of
England. It comprises four catchments, Aire, Calder,
Went and Rother. The River Aire drains the central
Pennines and flows south-eastward through the West
Yorkshire metropolitan area and the Yorkshire coal-
field, where it is joined by the Calder, its major tributary.
This area is characterized by a high population density,
large number of small tributaries and medium to small
size wastewater treatment plants with wastewater dilu-
tions factors as low as 2 (Table 1, [9]).
Based on the default environmental infrastructure
data from GREAT-ER (see below), two wastewater
treatment plants (WWTPs) were selected for the study
carried out in September, 2000. The Crofton activated
sludge (AS) plant southeast of Wakefield serves a
population of about 9000 people with the average
wastewater flow of 1800m3 day�1
(200L � capita�1 � day�1), and the Meltham trickling
filter (TF) plant south of Huddersfield serves a popula-
tion of 7900 people with the average wastewater flow of
4100m3 � day�1 (520L � capita�1 � day�1). The latter
plant operates two consecutive series of trickling filters
and should effectively be regarded as an advanced
secondary treatment plant. In both plants, nearly all of
the influent (>98%) is composed of domestic waste-
water. The historic WWTP performance data (York-
shire Water) showed that both plants operated well, with
the effluent biological oxygen demand (BOD) values
typically in the range of 3–10mgL�1. This was
confirmed during the reconnaissance trip to the plants
in July, 2000, in which the measured BOD, total
suspended solids (TSS) and linear alkylbenzene sulfo-
nate (LAS) removal rates based on grab influent and
effluent samples were 95%, 92% and 99.6%, respec-
tively, at the Meltham WWTP, and 97%, 93% and 98%
at the Crofton WWTP. LAS was used in the study as a
benchmark chemical for WWTP removal rates, as it is a
common surfactant used in detergents and has a well
established environmental fate profile.
The Crofton WWTP discharges the treated effluent
directly into the River Calder, whereas the Meltham
WWTP discharges into Mag Brook, which is part of the
Calder catchment. The in-stream removal of Triclosan
was studied in the 3.5-km section of Mag Brook directly
Cl
OH
O
Cl
Cl
Fig. 1. Chemical structure of Triclosan.
Table 1
Main characteristics of the Aire and Calder catchments (from
Fox et al. [9])
Catchment Aire (above
confluence with
Calder)
Calder
Area, km2 1100 957
Population 1,100,000 790,000
Number of WWTPs 40 23
Dry weather flow, m3 s�1 9 10
Mean flow, m3 s�1 16.5 17.8
5th-percentile flow, m3 s�1 5.4 6.9
D. Sabaliunas et al. / Water Research 37 (2003) 3145–31543146
below the WWTP discharge point. Mag Brook (Table 2)
is a small and shallow natural stream with a relatively
constant water flow rate, velocity, width and depth over
the entire stretch used for the study, except for the
farthest downstream site where the flow velocity drops
as the river becomes wider and deeper. The river bottom
is mainly covered by rocks, and sediments are only
found at the downstream end of the stretch, where the
lower flow velocity and deeper waters favor the settling
down of suspended matter.
2.2. Wastewater sampling
Hourly time-proportional composite influent, primary
effluent and final effluent samples were collected at both
selected WWTPs over the time period of 24 h using
ISCO (Model 3600) automatic samplers. Immediately
upon collection, before compositing, the individual
samples collected at odd hours were acidified with
concentrated phosphoric acid to pHo2. The samplescollected at even hours were preserved with 3% formalin
(v/v). The individual samples preserved with phosphoric
acid and formalin were composited separately. The
composite samples preserved with phosphoric acid were
spiked with 13C-labeled Triclosan standard and shipped
on ice to the Ciba SC analytical laboratory (Basel,
Switzerland) for determination of Triclosan. The for-
malin-preserved composite samples were submitted to
the local laboratory of the Environment Agency (Leeds,
UK) for the analysis of LAS. Additionally, unpreserved
grab samples of influent, primary effluent and final
effluent were taken at each site in the early afternoon
hours on the same day when composite samples were
collected. These samples were also analyzed at the
Environment Agency’s laboratory for conventional
water quality parameters such as biological oxygen
demand (BOD), conductivity, pH, total suspended
solids (TSS), total organic carbon, ammonia, total
nitrogen, phosphorus, calcium, magnesium, etc.
The weather conditions were generally dry through-
out the entire sampling period, except for a short rainfall
event during sampling at Meltham. Based on the
measurements by flow gauges installed at both plants,
the daily integrated flow rates during the sampling
period were 4140m3 day�1 (524L � capita�1 � day�1) atthe Meltham WWTP and 1385m3 day�1
(156L � capita�1 � day�1) at the Crofton WWTP. At thelatter plant, the flow rate was lower than the yearly
average value from GREAT-ER (1800m3 day�1), con-
sistent with the dry weather conditions at the time of the
study, whereas at the Meltham WWTP, it was similar to
the yearly average, possibly reflecting on the rainfall
event and/or groundwater infiltration during the sam-
pling.
2.3. In-stream removal
The study was carried out following the guidelines by
the US Geological Survey [10,11]. An approximate
water travel time was estimated in a pilot study carried
out during the reconnaissance trip to the study area in
July 2000. In the pilot study, Fluorescein dye (Sigma-
Aldrich) was released at the WWTP discharge point,
and the colored water plug was visually followed
downstream. At the same time, water flow velocity,
depth, width, water temperature, conductivity, dissolved
oxygen (DO) measurements were taken. River flow rates
at several sites were calculated based on the river width
at these sites and cross-sectional flow velocity and depth
measurements. Importantly, the river perimeter was
carefully inspected for any additional water inflows. It
was determined that there were no additional water
inflows along the entire 3.5 km river stretch selected for
the study, which was also confirmed by rather uniform
water conductivity values measured at various points
Table 2
Characteristics of the Mag Brook stretch used in the in-stream removal study, default GREAT-ER and measured values
Default GREAT-ER values
Mean 5th percentile Measureda
Flow rate, m3 s�1 0.526 0.149 0.13–0.18
Flow velocity, m s�1 0.218 0.117 0.015–0.57
Length, m 3464 N/A 3464
Depth, m 0.547 0.348 0.05–0.47
Width, m N/A N/A 2–6.1
Meltham WWTP discharge, m3 s�1 0.049 N/A 0.048b
Flow-based dilution factor 10.7 3.0c 2.65
Conductivity-based dilution factor N/A N/A 2.94
aAt the time of study.bDaily average during study period (5 days).cBased on the daily average WWTP flow rate (default GREAT-ER values).
D. Sabaliunas et al. / Water Research 37 (2003) 3145–3154 3147
downstream the stretch. Five sampling sites were
selected for the study, mainly based on the ease of
access to the river. One of these sites was located about
50m upstream from the WWTP effluent discharge
point, the other four were 20, 750, 1500 and 3500m
downstream from the discharge point. The stream
section between the WWTP discharge point and the
first downstream site was narrow (2m wide) and highly
turbulent, ensuring full water mixing at this site as was
also confirmed in the pilot study using the Fluorescein
dye. At all of these sites, sets of 4 semipermeable
membrane devices (SPMDs) were deployed in the river.
Additional 4 SPMDs were retained as field blanks.
SPMDs are membrane-based time-integrated passive
samplers capable of bio-mimetic preconcentration of
moderate to highly hydrophobic chemicals from water,
sediments, soil or air [12]. The SPMDs used in the
current study were of standard configuration (96 cm
long, 1 g triolein; from Environmental Sampling Tech-
nologies, St. Joseph, MO), placed in protective steel
mesh containers. At all sites, the SPMDs were exposed
to the running river water, except for the farthest
downstream site, where river sedimentation occurred,
and the SPMDs were found to have been buried in the
sediment. The SPMDs were collected at the time of the
main study, with the resultant exposure period of 5
weeks. After the exposure, the SPMDs were sealed in
stainless steel cans and shipped on ice to the analytical
laboratory for Triclosan analysis.
On the day of the main study, September 8, 2000, the
hydraulic residence times at the sampling sites were
determined using the Rhodamine WT (Crompton
Colors, Gibraltar, PA) dye tracer with fluorescent
detection. Briefly, 180mL of the dye (20% aqueous
solution) was released into the river water directly below
the WWTP discharge point. The amount of the dye
released was calculated using an empirical equation [11]
to give the peak dye concentration of about 10 mgL�1 atthe farthest downstream site. The dye concentration at
each site was monitored using continuous flow fluorom-
eters with automatic data logging capability (Turner
Designs, Model 10-AU-005-CE). At the time when the
dye reached peak concentration, four 1L river water
samples were taken at each site across the river section.
Three water samples were preserved with phosphoric
acid as described above for wastewater samples, and the
remaining sample was submitted immediately to the
local laboratory of the Environment Agency for the
analysis of conventional water quality parameters (same
as for wastewater samples). The preserved samples were
spiked with 13C-labeled Triclosan standard and shipped
on ice to the analytical laboratory for Triclosan analysis.
On the day of the study, additional river flow velocity
and flow rate measurements were also carried out as
described above (Table 2). The measured flow rate was
close to the 5th percentile of the yearly distribution of
flow rates (default GREAT-ER data) in the studied
section of Mag Brook. This low flow rate observed in the
study was probably due to a long period (>2 months) of
dry weather conditions preceding the study.
2.4. Sample processing and analytical
Details of the analytical method used in the current
study are described elsewhere [13]. Briefly, an aliquot of
each WWTP sample was mixed with concentrated
sulfuric acid and extracted with hexane/dichloro-
methane mixture. An appropriate aliquot of each extract
was derivatized with a silylating agent and measured by
GC/MSD in a single ion monitoring (SIM) mode.
Quantification was carried out using the isotope dilution
method, based on the 13C-labeled Triclosan on-site
spike.
River water samples were applied to solid phase
extraction cartridges, which were subsequently extracted
using supercritical fluid extraction (SFE) with pure CO2.
The SFE extracts were derivatized with a silylating agent
and analyzed with GC/MS as described above.
The SPMDs were rinsed with running distilled water
and air-dried. Three SPMDs from each site were
combined together and dialyzed at 20�C in 500mL of
hexane for 48 h, with the solvent replacement after 24 h,
resulting in the total of 1000mL of dialyzate. The
dialyzates were reduced to a known volume, filtrated
through anhydrous Na2SO4 and spiked with13C-labeled
Triclosan. An aliquot of each extract was derivatized
with a silylating agent and analyzed by GC/MSD in the
same way as the extracts from water.
2.5. GREAT-ER model
The River Aire and three related river catchments
(Calder, Went and Rother) have been modeled in
GREAT-ER, the Geography-Referenced Regional Ex-
posure Assessment Tool for European Rivers (version
1.02). GREAT-ER combines environmental models and
GIS techniques to predict and visualize the concentra-
tion of down-the-drain chemicals in several European
river catchments [14]. The output of the GREAT-ER
software is chemical’s site-specific Predicted Environ-
mental Concentrations (PECs), which can also be
integrated for the whole catchment using various
weighting methods [15]. The chemical-specific input
data are physical, chemical and biochemical parameters,
together with geographical production and consumption
patterns. The GREAT-ER project is managed by a task
force of ECETOC (European Centre for Ecotoxicology
and Toxicology of Chemicals). More information on
this model and its application areas can be found on the
GREAT-ER website (www.great-er.org).
D. Sabaliunas et al. / Water Research 37 (2003) 3145–31543148
3. Results and discussion
3.1. Wastewater treatment removal
Concentrations of Triclosan in the influent, primary
effluent and final effluent at both wastewater treatment
plants and the calculated removal rates are presented in
Table 3, along with the measured concentrations of LAS
and water quality parameters, including BOD. Concen-
trations of Triclosan and LAS in the influent of the
Meltham plant were considerably (2–3 fold) lower
compared to the Crofton plant, probably due to the
significantly higher per-capita water flow at the former
plant pointing to likely dilution of influent with
Triclosan- and LAS-free water from other, unidentified
sources such as groundwater infiltration. However, the
calculated (based on the population served by the plants,
wastewater flow rates and influent concentrations) per-
capita use of Triclosan was similar for both plants
(1400mg � capita�1 � year�1 for Meltham WWTP and
1240mg � capita�1 � year�1 for Crofton WWTP) indicat-ing that the distribution and use of Triclosan-containing
consumer products is rather uniform in this region.
The results of the current study demonstrated that
Triclosan was extensively removed (B95%) during bothactivated sludge and advanced trickling filter wastewater
treatment. Triclosan removal rates were somewhat lower
than those of LAS, BOD and comparable to those of
organic carbon. The WWTP influent concentrations and
removal rates at Meltham and Crofton plants are
comparable with other recent Triclosan measurements
in the US and the UK. At several wastewater treatment
plants in Ohio, US, the measured Triclosan concentra-
tions in influent were in the range of 3.8–16.6 mgL�1,whereas the wastewater treatment removal rates ranged
from 58% to 86% at three trickling filter plants and
were approximately 96% at two activated sludge plants
[13]. Triclosan removal at Stretford (Greater Manche-
ster, UK) trickling filter plant has been measured at
79%, and its removal at Crewe (Cheshire, UK) activated
sludge plant was 83% (unpublished data from a Procter
& Gamble study, 1997). In the latter study, influent
concentrations were 2.8 and 5.4 mgL�1, respectively.
3.2. In-stream removal
Concentrations of Triclosan in river water and the
calculated in-stream removal rates are presented in
Table 4. It is important to note that Site E, the farthest
downstream site, was excluded from the rate calcula-
tions due to its significantly higher suspended solids
concentration compared to the upstream sites. As noted
above, the visual inspection of the river bottom
indicated that river sedimentation occurred at this site.
The SPMDs at this site were also found to be fully
submerged in sediment at the time of recovery. The
elevated suspended solids at site E may reflect dis-
turbance of sediments at the time of sampling and thus,
the measured total concentration of Triclosan in water
at this site included a contribution from its solids-
associated fraction distorting the concentration die-
away data in the aquatic compartment. Similarly, the
SPMDs at site E were exposed to the sediment
interstitial water with Triclosan concentrations different
from those in the running water column. Meanwhile,
there were no substantial sediments in the river stretch
from site B to site D with the river bottom being covered
with rocks. In this stretch, going downstream, the
suspended solids concentration decreased from 9 to
6mgL�1, while the river water pH values increased from
Table 3
Wastewater treatment removal of BOD, organic carbon, suspended solids, LAS and Triclosan at Meltham and Crofton wastewater
treatment plants
BODa
(mgL�1)
Organic carbona
(mgL�1)
Suspended solidsa,
(mgL�1)
LAS
(mgL�1)
Triclosan
(mgL�1)
Meltham WWTP (trickling filter)
Influent 204 151 228 1.71 7.5
Primary effluent 55.3 33.2 56 2.4 5.9
Final effluent 2.7 5.88 14 0.029 0.34
Primary removal, % 72.9 78 75.4 0 21.3
Total removal, % 98.7 96.1 93.9 98.3 95.5
Crofton WWTP (activated sludge)
Influent 262 126 166 3.18 21.9
Primary effluent 230 142 120 2.88 13.35
Final effluent 4.1 21.4 14 0.016 1.1
Primary removal, % 12.2 0 27.7 9.4 39
Total removal, % 98.4 83 91.6 99.5 95
aBased on grab unpreserved samples.
D. Sabaliunas et al. / Water Research 37 (2003) 3145–3154 3149
6.94 to 7.18. Even though these changes may seem
insignificant, Triclosan is a sorptive and ionizable
compound, and any changes in the suspended solids
concentration and water pH values could have caused its
repartitioning between the sorbed and freely dissolved as
well as protonated and ionized forms, which in turn
could have influenced the overall removal rate. To
estimate the proportion of various forms of Triclosan
from its total concentration, one can use the following
partitioning equations [16]:
Csole-union ¼CT
½1þ 10ðpH�pKaÞ þ KOCfOCM;
Csol-ion ¼ Csol-union10ðpH�pKaÞ;
Csor-union ¼ ðKOCfOCMÞCsol-union;
where Csol-union; Csol-ion and Csor-union are the concentra-
tions of dissolved unionized, dissolved ionized and
sorbed compound, respectively (mgL�1), CT is its total
concentration, pKa is the acid dissociation constant
(8.14 for Triclosan [17]), KOC is the water/organic
carbon partition coefficient (46,800Lkg�1 for Triclosan
[2], fOC is the fraction of organic carbon of suspended
solids (assumed to be 0.13), and M is the suspended
solids concentration (kgL�1). Using the above equa-
tions, it can be calculated that from site B to site D, the
proportion of sorbed Triclosan decreased from 4.9% to
3.2% of the total measured water concentration,
whereas the proportion of ionized Triclosan increased
from 5.6% to 10.2% of the total concentration. These
changes were considered insignificant in the view of
natural variability associated with this type of measure-
ments, and thus, the calculated Triclosan in-stream
removal rates in that river section were not corrected for
its repartitioning due to sorption and ionization.
In river water, the Triclosan removal rate was
comparable to or even higher than the rate of BOD
decay (Table 4, Fig. 2). The estimated SPMD-based in-
stream removal rate (0.33 h�1, t1=2 ¼ 2:1 h) was some-what higher than the rate based on the grab water
samples (0.21 h�1, t1=2 ¼ 3:3 h). The rate based on thewater samples reflects the total loss rate of all forms of
Triclosan due to chemical (photolysis) and biological
degradation and, to a smaller extent, settling of
suspended solids with sorbed Triclosan. SPMDs, on
the other hand, sample only truly dissolved and union-
ized (i.e. bioavailable) compound. The SPMD data
therefore reflect the time-integrated loss rate of the
dissolved and protonated form of Triclosan over the
exposure period of 5 weeks. Thus, the factors that may
have determined the higher SPMD-based removal rate
compared to the rate based on the grab water samples
include different exposure conditions and duration,
increase in pH downstream (resulting in increased
ionization of Triclosan diminishing its availability to
SPMDs) and a higher loss rate due to degradation
versus the total loss rate that includes settling.
Interestingly, the in-stream removal rate of Triclosan
in Mag Brook was significantly higher than its removal
Table 4
Measured conductivity, suspended solids, BOD and Triclosan concentrations in Mag Brook upstream (Site A) and downstream (Sites
B–E) from the Meltham WWTP effluent discharge point and calculated in-stream removal rates
Conductivity Suspended
solids
(mgL�1)
pH BOD
(mgL�1)
Organic
carbon
(mgL�1)
Triclosan
mS cm�1 Dilution Water (ngL�1)
(mean7SE,n ¼ 3)
SPMD
(ng/3
units)
Site A (50m upstream) 175 — 10 7.18 3.9 6.36 1971.4 93
Site B (20m downstream,
travel time 1min)
352 2.94a 9 6.94 3.6 9.28 80715 489
Site C (750m downstream,
travel time 55min)
282 1.25b 7 7.12 2.4 7.53 5373.2 423
Site D (1500m downstream,
travel time 165min)
293 1b 6 7.21 2.2 7.07 4375.6 205
Site E (3500m downstream,
travel time 310min)
316 1b 51 7.18 3.1 5.95 4474.2 399
Die away rate B–Dc, h�1
(slope7SE)N/A 0.1470.05 N/A 0.1670.08 0.0970.04 0.2170.08 0.3370.06
aDilution of effluent by river water at the point of discharge, based on conductivity.bDilution of river water flow between this site and the preceding site, based on conductivity.cSite E was excluded from the rate calculations as the SPMDs at this site were found to be submerged in sediment at the time of
recovery. Elevated suspended solids at Site E may reflect disturbance of sediments at the time of sampling.
D. Sabaliunas et al. / Water Research 37 (2003) 3145–31543150
rate measured in a similar study in Cibolo Creek in
Texas, US [16]. In Cibolo Creek, the removal of
Triclosan was studied over an 8 km-long section of the
river downstream from a trickling filter WWTP effluent
discharge point using bromide as a conservative tracer
to estimate the water plug travel time. The total loss rate
of Triclosan from the water column was 0.06 h�1, i.e.
3.5–5.5 fold less than the rate observed in Mag Brook.
This observed difference may be due to several reasons.
One of them is a different degree of photolysis
contribution to the overall rate of Triclosan removal in
these streams. It has been shown that Triclosan under-
goes rapid photolytic transformation in surface waters
under a natural sunlight with the estimated half-life less
than an hour and as short as 15min [2,5,6]. The direct
photolysis of the anionic form appeared to be the major
elimination process for Triclosan in Swiss lake water
[5,6]. It was shown in the latter study that the rate of
photolytic transformation of Triclosan was dependent
on a number of natural factors, with water pH, solar
light intensity and surface water depth being amongst
the most important of them. Specifically, the rate of
direct phototransformation of Triclosan increased 30-
fold with an increase in pH from 5.9 to 11.0. Further, at
the lake water depth of 50 cm, the rate was only 5% of
the rate at the water surface indicating that 95% of the
photochemically active sunlight was absorbed in the
upmost 50 cm of the lake water. Even though the
measured water pH values were rather similar in Mag
Brook and Cibolo Creek, the latter stream was
reportedly turbid, significantly deeper (0.4–1.5m com-
pared to 0.005–0.47m in Mag Brook, Table 2), and less
turbulent than Mag Brook. It seems likely, therefore,
that conditions for photolysis in Cibolo Creek were not
as favorable as in Mag Brook due to a lesser availability
of photochemically active sunlight in the overall water
column.
Naturally, there may have been other environmental
factors that contributed to the observed rate differences
between Mag Brook and Cibolo Creek, including
different Triclosan sorption and solids settling rates as
well as differences in biodegradation rates due to
different amount of surface biofilm present in these
two streams.
3.3. GREAT-ER simulation
High dependency of substance-specific aquatic fate
processes on a broad spectrum of environmental factors
has significant implications for regional fate models such
as GREAT-ER, which use experimental parameters
(WWTP, in-stream removal rates) determined at one or
several sites to model the fate and distribution of
substance’s concentrations on a larger scale or even in a
different region. Even though a large number of river
stretches in the Aire basin are similar in properties to
Mag Brook, the downstream sections of the basin may
become more turbid and deep (up to 2m in depth), with
less favorable conditions for photolysis and other
removal processes. Thus, the in-stream removal rate
determined in Mag Brook cannot be directly applied in
the model for the whole river basin. To be able to more
accurately predict site-specific concentrations of Triclo-
san in the Aire basin as well as to use the Mag Brook
rate in other river basins, it would be important to
quantify all the processes that may affect the overall
removal rate of Triclosan in a river system, including
photolysis, biodegradation, sorption and solids settling
rates. The rate of photolysis, for example, will depend
on water pH, solar light intensity, which is a function of
latitude and year seasonality, river depth, suspended
solids concentration, and water convection (turbulence)
rate. Biodegradation will depend on water temperature,
which varies considerably throughout the year and at
different water depths and the amount of surface
biofilm, which is proportional to the water surface area
to volume ratio. Sorption will depend on water pH and
the amount of suspended solids present in the water
column as well as their characteristics such as organic
carbon content and the particle size distribution. With-
out such adjustments, the in-stream removal rate
measured in the current study could be directly used to
describe the removal of Triclosan in small and shallow
streams of Northern Europe similar in their properties
to Mag Brook.
Further, the wastewater treatment removal rate of
Triclosan measured at the Meltham trickling filter plant
may not be representative of other trickling filter plants
in the region and elsewhere, which do not have advanced
secondary treatment system as at the Meltham plant
(two consecutive series of trickling filters).
To avoid bias in a regional model due to the use of
site-specific data that may not necessarily be representa-
tive of the whole region, one can carry out an
uncertainty analysis of the distribution of experimental
0
20
40
60
80
100
120
0 20 40 60 80 100 120 140 160 180
Time, min
Con
cent
ratio
n lo
ss, %
BOD
TCS - water
TCS - SPMDs
Fig. 2. Loss of BOD and Triclosan (TCS) in Mag Brook
downstream from the Meltham WWTP effluent discharge
point.
D. Sabaliunas et al. / Water Research 37 (2003) 3145–3154 3151
substance-specific fate parameters. Such an approach
was used in the GREAT-ER model. The input
parameters (Table 5) were variables represented by
normal (WWTP removal) or uniform (in-stream re-
moval) distributions of rates based on the experimental
values from the current study and other studies referred
to in this paper. In the model simulation, the Monte-
Carlo sampling (5000 iterations) of these distributions
and the yearly distribution of Mag Brook flow rates
(default GREAT-ER values) was used to simulate the
site-specific concentrations of Triclosan in the basin
(Figs. 3 and 4). Using various methods, these concen-
trations can be spatially aggregated to a single value of
PEC representing exposure in the basin (Table 6).
PECinitial represents an unweighted average of initial
river concentrations directly below each wastewater
effluent discharge in the basin, and as such, it is
equivalent (but not identical) to PEClocal used in the
Technical Guidance Document (TGD) for environmen-
tal risk assessment in the EU [7]. PECcatchment represents
a weighted aggregated exposure value for the entire
basin, and it is similar to the concept of PECregional used
in the EU TGD. By means of various weighting
methods, PECcatchment can be calculated including all
stretches (i.e. both receiving and not receiving waste-
water effluent discharge) or exposed stretches only (i.e.
receiving wastewater effluent discharge). Volume-
weighted PECcatchment based on all stretches and flow
increment-weighted PECcatchment based on impacted
stretches only have been shown to be the most
representative aggregated PEC values as they can best
resolve scale-dependencies [15].
Table 5
GREAT-ER input parameters
Parameter Value Comments
Per-capita use of Triclosan 1340mg � capita�1 � year�1 Based on measured wastewater flow rate (520L � capita�1 � day�1 atMeltham WWTP and 156L � capita�1 �day�1 at Crotfon WWTP),influent concentration (Table 3) and known population size served
by the Meltham (7900) and Crofton (8900) WWTPs, average for
both plants (no distribution assumed in the model)
Wastewater treatment
primary removal rate
31.0712.8% (normal
distribution)
Based on reported measured values, including the current study (8
values in total)
Trickling filter WWTP
overall removal rate
80.2713.9% (normal
distribution)
Based on reported measured values, including the current study (5
values in total)
Activated sludge WWTP
overall removal rate
92.276.5% (normal
distribution)
Based on reported measured values, including the current study (4
values in total)
In-stream removal rate 0.06–0.33 h�1 (uniform
distribution)
Based on measured values in Cibolo Creek and Mag Brook
Monte Carlo iterations 5000
Fig. 3. Graphic representation of mean Triclosan concentrations in the Aire and Calder Basin predicted by GREAT-ER simulation.
D. Sabaliunas et al. / Water Research 37 (2003) 3145–31543152
Several important factors should be considered when
interpreting the modeled concentrations and especially
when using them for environmental risk assessment
purposes. The simulated PECs at any point in the basin
represent very approximate estimates only due to wide
ranges of input parameters (especially the in-stream
removal rate) used in the model calculations. For the
reasons discussed above, it is likely that the predicted
concentrations in the upstream sections of the basin
(shallow and clear streams, higher removal rate ex-
pected) overestimate the actual concentrations, whereas
in the downstream sections (deep and turbid, slower
removal), they underestimate the actual levels. It is also
worth noting that trickling filter wastewater treatment
plants in the US are operated in a slightly different way
than TF plants in the UK. Plants in the UK generally
achieve higher removal rates for consumer chemicals,
and thus, the use of the US removal data in the model
calculations may have caused a bias toward over-
estimating PECinitial, and, consequently, the downstream
concentrations. The simulated concentrations of Triclo-
san in Mag Brook illustrate the importance of these
factors (Table 7). The calculated mean concentrations
were higher than the measured concentrations, even
though the measurements were made under low flow
conditions (close to the 5th percentile, Table 2), when
higher than the yearly average levels of Triclosan could
be expected in the river water due to lower dilution
factors.
The large standard deviations associated with the
model estimates reflect the wide spread of input
parameters used in the model calculations. Thus, the
calculated standard deviations and, importantly, the
90th percentile values of the regional estimates do not
merely reflect the variability of PEC that can be expected
in the river basin. They are rather a combination of the
variability and mathematical uncertainty of the mean,
and as such, they can hardly be applied directly in
environmental risk assessment as probabilistic PECs.
For risk assessment purposes, therefore, the calculated
mean PEC values should be used.
4. Conclusions
The results of the current study confirm that Triclosan
is not a persistent chemical. It was extensively removed
during wastewater treatment, with the measured re-
moval rate at both advanced trickling filter and
activated sludge wastewater treatment plants of about
95%. In river water of Mag Brook, concentrations of
Triclosan further declined rapidly, with the measured in-
stream removal rate in the range of 0.21–0.33 h�1,
(t1=2 ¼ 2:123:3 h). This rate was comparable to or evenhigher than the BOD removal rate. The in-stream
removal rate measured in the current study is character-
istic of and may be directly applied to small and shallow
streams of Northern Europe. In other rivers, this rate
should be adjusted to account for factors that influence
the fate of Triclosan in the aquatic environment,
Table 6
Concentrations of Triclosan in the Aire and Calder Basin
simulated by GREAT-ER
Calculated
concentrations
(ngL�1)
Weighting
method
PECcatchment (all stretches)
Mean 45.1 Volume
90th percentile 94.2
PECcatchment (exposed stretches)
Mean 52.0 Flow
increment
90th percentile 109.3
PECinitial (mean) 334.9 Not
weighted
Table 7
Measured and simulated by GREAT-ER concentrations of
Triclosan in Mag Brook
Calculated by
GREAT-ER,
Mean7SD(ngL�1)
Measured
(ngL�1)
Csim (start of the stretch) 1277146 80
Csim (end of the stretch) 46.2749.2 44
Csim (90%)a 161
a90th percentile of the concentration distribution for the
whole river stretch.
Horbury
DewsburyHuddersfield
Deighton
Brighouse
Meltham
Caldervale
Stanley Pinder Green
Mill LaneWheldale
Sutton
0
20
40
60
80
100
120
140
River length, km
Con
cent
ratio
n, n
g/L
Fig. 4. An example profile of mean Triclosan concentrations
simulated by GREAT-ER downstream from Mag Brook (Mag
Brook–Holme–Calder–Aire). The concentrations represent
internal means for each stretch.
D. Sabaliunas et al. / Water Research 37 (2003) 3145–3154 3153
specifically, the rate of photolysis, biodegradation and
settling.
The GREAT-ER model is a useful tool for predicting
and visualizing site-specific concentrations of down-the-
drain chemicals, however, a good knowledge of factors
influencing the fate of the compound of interest in a
varied environment is necessary for the correct inter-
pretation and use of the model data. Ideally, such key
parameters as the in-stream removal rate should also be
geo-referenced, or more robust probabilistic approaches
should be employed to account for the fate parameter-
related spatial variability.
Acknowledgements
The authors would like to thank Drew McAvoy,
Geert Boeije, Nick Fendinger, Scott Dyer, Donna
Morrall and Diederik Schowanek for the critical review
of the manuscript and their valuable comments. We also
would like to thank the heeds office of the UK
Environment Agency for their practical help in con-
ducting this study.
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