the level and distribution of selected...
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ORIGINAL PAPER
The level and distribution of selected organochlorinepesticides in sediments from River Chenab, Pakistan
Syed Ali-Musstjab-Akber-Shah Eqani •
Riffat Naseem Malik • Ashiq Mohammad
Received: 6 July 2009 / Accepted: 15 April 2010
� Springer Science+Business Media B.V. 2010
Abstract Organochlorine pesticides (OCPs), viz.
b-hexachlorocyclohexane (b-HCH), c-HCH, aldrin,
dieldrin, endrin, heptachlor, endosulfan-I, endosulfan-
II, heptachlor endoepoxide, heptachlor exoepoxide,
mirex, dicofol, o,p0-dichlorodiphenyltrichloroethane
(o,p0-DDT), p,p0-dichlorodiphenyltrichloroethane (p,p0-DDT), dichlorodiphenyldichloroethane (DDD), and
dichlorodiphenyltrichloroethylene (DDE) and 12 other
physicochemical parameters were measured in surface
sediments from River Chenab during two sampling
seasons (summer and winter, 2007) to evaluate spatial
and temporal trends of sediment pollution. Hierarchical
agglomerative cluster analysis identified three groups of
sites based on spatial similarities in physicochemical
parameters and OCP residual concentrations. Spatial
discriminant function analysis (DFA) segregated 14
parameters, viz. dicofol, endosulfan-I, heptachlor
endoepoxide, dieldrin, DDD, DDE, endosulfan-II,
o,p0-DDT, p,p0-DDT, pH, electrical conductivity (EC),
Cl-1, total P (%), and silt, which explained 96% of total
variance between spatial groups. c-HCH was the most
frequently detected (63%) pesticide, followed by DDD
(56%). The ratio of DDTs to their metabolites
indicated current input and anaerobic biodegradation.
Temporal DFA highlighted aldrin, heptachlor endo-
epoxide, Cl-1, total P, and EC as important variables
which caused variations between summer and winter.
DDTs were relatively more prevalent as compared to
other OCPs in the sediments samples during both
seasons. DDT metabolites were detected at greater
frequencies and concentrations in winter, whereas DDT
isomers were more prevalent in summer sediment
samples. Factor analysis identified agricultural and
industrial activities as major sources of sediment OCP
contamination. Concentrations of c-HCH, heptachlor
endoepoxide, dieldrin, and DDTs (isomers and metab-
olites) in all sediment samples were well above interim
sediment quality guidelines (ISQGs) and probable
effect limits (PEL) given by Canadian Sediment Quality
Guidelines (CSQGs).
Keywords Organochlorine pesticides �DDT � HCH � Dicofol � Multivariate analysis �Probable effect limit � River Chenab �Pakistan
Introduction
Pesticides such as organochlorines (OCPs) along with
industrial-based chemicals have been discharged
in large quantities into the environment for the
last 50 years, mainly to control agricultural pests,
S. Ali-Musstjab-Akber-ShahEqani � R. N. Malik (&)
Environmental Biology Laboratory, Department of Plant
Sciences, Quaid-i-Azam University, Islamabad 46000,
Pakistan
e-mail: [email protected]
A. Mohammad
Ecotoxicology Research Program, National Agricultural
Research Center, Park Road, Islamabad 45500, Pakistan
123
Environ Geochem Health
DOI 10.1007/s10653-010-9312-z
insect-borne diseases, and termites (Malik et al.
2010). Widespread use of these chemicals for agri-
cultural and nonagricultural purposes in past years
has resulted in contamination of water, sediment, and
biological organisms, and is of major concern at
local, regional, and global level (Doong et al. 2002a,
b; Kishimba et al. 2004; Ioannis et al. 2006; Sarkar
et al. 2008). OCPs are toxic to biological organisms,
threaten ecosystem integrity due to their high lipo-
philic properties (Vashchenko et al. 2005), tend to
adsorb on particulate matter due to low water
solubility (Nowell et al. 1999; Yang et al. 2005),
and are transferred to higher trophic levels through
food chains (Lopez et al. 2005; Zhou et al. 2006;
Malik and Zeb 2009). OCPs, like other contaminants
such as inorganic chemicals, make their way into
natural aquatic ecosystems via industrial and muni-
cipal effluents, agricultural and urban nonpoint run-
off, and atmospheric deposition (Qadir et al. 2008),
ultimately accumulating and settling in bottom sed-
iments, which act as a sink (Sarkar et al. 2008).
Residue levels of chlorinated pesticides have
declined significantly in the last two decades (Zhang
et al. 2003), but some OCPs such as DDTs, HCHs,
cyclodiene, etc. are still used in developing countries,
including Pakistan (Malik et al. 2010); although most
of them are banned, their low cost and illegal use
cannot be ignored (Tariq et al. 2007). DDT was banned
in 1994 in Pakistan; however, thousands of kilograms
of DDTs along with other obsolete persistent organic
pollutants are still found in chemical warehouses (Jan
et al. 2008). According to Malik et al. (2010) and Tariq
et al. (2007), large stockpiles of outdated pesticides
exist, estimated at 3,805 tonnes in Punjab, 2,016 ton-
nes in Sindh, 179 tonnes in Khyber Pukhtoon Khawa
Province, 128 tonnes in Baluchistan, and an obsolete
stock of 178 tonnes in the Federal Department of Plant
Protection, from where these toxic chemicals find their
way into various environmental compartments via
surface runoff and possibly contamination of ground-
water. On the other hand, illegal use of these polluting
chemicals cannot be neglected due to poor enforce-
ment of environmental laws. Of the pesticides, 74% are
used as insecticides, 14% as herbicides, 9% as
fungicides, 2% as acaricides, and 1% as fumigants.
Of all pesticides used in Pakistan,[65% are applied on
cotton, while others are used on crops such as rice,
sugarcane, maize, fruits, vegetable, and tobacco (Eco-
nomic Survey of Pakistan 2005–2006).
To our knowledge, few studies have assessed OCP
residues in various environmental compartments
from Pakistan (Jabbar et al. 1993; Tehseen et al.
1994; Munshi et al. 2004; Saqib et al. 2005; Tariq
et al. 2007; Malik et al. 2010). However, there is no
information available regarding OCP concentrations
in sediments of River Chenab, which is one of the
largest rivers of the Indus Basin. The present study
aimed to determine the contamination level of OCPs
and to assess their spatial and temporal variation in
sediments of River Chenab, Pakistan.
Materials and methods
Sediment sample collection
A total of 16 sites were marked for sampling in
selected river stretches (Fig. 1), and surface sedi-
ments were collected in summer (May 24–30) and
winter (November 3–10) during 2007. Site S1 was
selected on River Jhelum before it meets River
Chenab, and one site (S2) was selected on
River Chenab before River Jhelum meets with River
Chenab. Site S3 was located on Trimun Headworks,
which provides water for irrigation of Punjab Prov-
ince. Sites S4, S5, S6, and S7 were located before the
River Ravi discharge into River Chenab. Site S8 was
located on River Ravi, 10 km upstream of the joining
point with River Chenab. Five sites (S9, S10, S11,
S12, and S13) were located in the cotton belt of
Khanewal District, where pesticides are used in large
quantities for agricultural purposes. Site S14 was
located after the joining of Suraj Maini drain line,
which brings municipal and industrial wastewater
from Multan City. Site S15 was located after the
joining of Indus link canal with River Chenab, near
Muzaffarghar, and site S16 was located at Shershah
Bridge. Each site was marked and located with the
help of global position system (GPS). Composite
surface sediment sample (0–5 cm) consisting of five
subsamples was collected from each site within the
vicinity of 100 m using a stainless-steel ladle, mixed
well, and kept in a glass bowl for immediate transfer
to the laboratory for storage at -20�C in refrigerator.
Samples were air-dried, sieved, and placed in airtight
glass bottles until extraction. All equipment used for
sampling, transportation, and preparation was free
from OCP contamination.
Environ Geochem Health
123
Laboratory analyses of physicochemical
properties of sediments
Parameters such as pH, EC, and total dissolved solids
(TDS) of each sediment sample were determined by
using portable combined meter (Milwaukee, model
SM802). Organic matter (OM) was determined by
Tyurin’s method (wet oxidation method) as described
by Nikolskii (1963). The proportions of sand, silt, and
clay were calculated using Bouycous hydrometer,
and sediment textural classes were determined on the
basis of relative proportion of soil particles using
textural triangle (Robert and Frederick 1995). Total
phosphorus (P) and total sulfur (S) percentages were
determined by the method described by Allen et al.
(1974), and nitrates (NO3–N) were determined by the
procedure described by Metson (1956). Total P, total S,
and NO3–N were finally estimated using spectropho-
tometer (Agilent 8453). Alkalinity and chloride (Cl-1)
were determined by titration method (AOAC 1995).
Extraction and clean-up of OCPs
Selected OCPs, viz. b-HCH, c-HCH (lindane), hepta-
chlor, heptachlor exoepoxide, heptachlor endoepoxide,
aldrin, dicofol, endosulfan-II, endrin, endosulfan-II,
dieldrin, DDD, DDE, o,p0-DDT, p,p0-DDT, and mirex,
were extracted from each sediment sample using
Automated Soxtec System (HT2 Tecator with 1,045
extraction unit and 1,046 service unit) using EPA
method no. 3541. Each sediment sample (5 g) was
premixed with an equal amount of anhydrous sodium
sulfate to form a free-flowing mixture, placed in a pre-
extracted cellulose extraction thimble, and extracted
with 60 ml n-hexane:dichloromethane 1:1 (v/v).
Extracts were concentrated, solvent-exchanged to
hexane, and purified on an 8-mm-i.d. alumina/silica
column packed, from bottom to top, with neutral
alumina (6 cm, 3% deactivated), neutral silica gel
(10 cm, 3% deactivated), 50% (w/w) sulfuric acid
silica (10 cm), and anhydrous sodium sulfate. Alu-
mina, silica gel, and anhydrous sodium sulfate were
pre-extracted for 48 h with dichloromethane (DCM).
Extraction thimbles were also pre-extracted with DCM
for 4 hours. The column was prewashed with
50 ml dichloromethane/hexane (1:1) and eluted with
50 ml dichloromethane/hexane (1:1) to yield OCPs
fraction. Organic fraction was solvent-exchanged to
ethyl acetate and concentrated to 0.5-ml gas chroma-
tography (GC) vials under a gentle nitrogen stream.
Fig. 1 Map of study area
showing the location of
sampling sites
Environ Geochem Health
123
Gas chromatographic analysis of OCP
Residual concentration of selected OCPs in extracted
samples was determined using gas chromatograph
(Perkin Elmer autosystem) equipped with an electron
capture detector (ECD-Ni63), fused silica capillary
column (P.E.No. N931-2414, 25 m length 9 0.32
inner diameter 9 0.5 lm film thickness, Perkin
Elmer, USA), and Turbochrom data analysis software.
During analysis, the injector (splitless mode) and
detector temperature were kept at 225�C and 300�C,
respectively. Initial oven temperature was set at
100�C, which was held for 5 min and then ramped
to 160�C at a rate of 15�C/min and to 190�C at a rate of
2�C/min. The backup pressure of carrier gas (N2) was
kept at 12 ml/min. The carrier flow rate was kept at
10 ml/min, whereas the pressure of the make-up gas
(N2) was 32 ml/min. Standard/sample measuring 1 ll
was injected using 10-ll Hamilton syringe by solvent
flush injection technique (Malik et al. 2010). The
results were confirmed by GC-ECD with Elite-CLP
fused-silica capillary column (P.E. no. N931-6664,
30 m length 9 0.32 mm inner diameter 9 0.5 lm
film thicknesses; Perkin Elmer, USA). The Elite-
CLP column was maintained at 110�C, which ramped
to 160�C at a rate of 30�C, programmed to 210�C at a
rate of 2�C, eventually temperature increased to 230�C
at a rate of 10�C and held for 10 min.
Quality control and assurance
All analytical methods were under accreditation, and
strict quality-control criteria were applied. Mixture of
standard solutions was injected into GC followed by
sample injection. Analytes of interest were identify on
the basis of their respective retention times matched to
the standards and quantified on the basis of peak areas,
which were used to calculate the concentration of
pesticide residues. For every set of ten samples a
procedural/laboratory blank and spiked sample
consisting of all reagents were run to check for
interference and cross-contamination. Instrument
performance was monitored using quality control
standards after every six samples analyzed on the
instrument. Method performance was assessed by
evaluating quality parameters such as recovery,
repeatability, correlation coefficients, and limits of
detections (LODs) and quantification (LOQs). Repeat-
ability and recovery were assessed by analyzing
uncontaminated sediment samples (n = 6) spiked at
50, 100, and 200 ng g-1 for each of the studied OCPs.
Mean recovery of OCPs ranged from 64% to 112%
with repeatability (relative standard deviation, RSD)
from 2% to 13%, while the correlation coefficient (r)
ranged from 0.993 to 0.999 (Table 1). LODs and
LOQs were calculated on the basis of signal-to-noise
ratio (S/N) of 3 and 10, respectively.
Chemical sources
Standard solutions of selected OCPs were purchased
from Dr. Ehrenstorfer GmbH (Ausburg, Germany).
Stock solution of pesticides were prepared by dissolving
precisely weighed amount of pesticides in n-hexane
containing 10–15% acetone, while working standard
solutions were made by diluting the stock standards. All
solvents and chemicals were of high-performance liquid
chromatography (HPLC) grade (Merck, Germany).
Extraction thimbles (31 9 91 mm) were purchased
from Macherey–Nagel (GmbH, Germany) and anhy-
drous sodium sulfate from Merck (Germany). All
sorbents, glassware, and GC vials were backed at
450�C before use. All sorbents and GC vials were stored
in sealed containers to avoid any possible contami-
nation.
Statistical analyses
Analytical results were compiled to form a multi-
elemental database using Excel software. Hierarchical
cluster analyses (HACA) was performed using Euclid-
ean distance as a distance matrix and unweighted pair
group method using arithmetic averages (UPGMA) as
a linkage method, to extract information regarding
spatial similarities/dissimilarities between sampling
sites based on 12 physicochemical parameters and
selected OCPs residual level.
Factor analysis based on principal component
analysis (FA/PCA) was employed for source identi-
fication of OCPs. Temporal FA/PCA was applied for
two sampling seasons, i.e., summer and winter,
whereas spatial FA/PCA was applied on the normal-
ized data set (25 variables) separately for three
groups of sites (region 1, region 2, and region 3) as
identified by HACA.
Discriminant function analysis (DFA) was applied
to study spatial and temporal trends of OCPs and
physicochemical parameters. Temporal DFA was
Environ Geochem Health
123
carried out on raw data, which was divided into two
seasons, i.e., summer and winter, while spatial DFA
was performed with the same 25 variables and three
groups of sites (region-1, region-2 and region-3). The
statistical software package Statistica (version 5.5)
for Windows was used for all statistical analyses.
Results and discussion
Physicochemical properties and OCPs
concentrations of surface sediments
Physicochemical parameters and OCPs concentrations
of sediments collected from River Chenab during
summer and winter seasons are presented in Table 2.
Sediments were slightly acidic to moderately alkaline
in winter, with pH varying from 6.6 to 8.9, while in
summer most sediments were moderately alkaline.
Sandy, loamy sand, and sandy loam were the dominant
textural classes. Higher values of EC, TDS, and
organic matter were recorded in winter, in contrast to
total P (%) and total S (%), which were measured
highest in summer. Greater alkalinity and concentra-
tion of Cl-1 and NO3–N were measured in winter. This
may be due to deposition of sediments, as water flow
was relatively low during winter. Clay content and OM
showed correlation with c-HCH (r = 0.65), dicofol
(r = 0.58), DDD (r = 0.72), and DDE (r = 0.61),
indicating strong adsorption with sediment particles.
DDTs and HCHs were frequently detected OCPs,
followed by dicofol and heptachlor (Table 2). Greater
concentrations of HCHs and DDTs were detected in
summer season; however, heptachlor was more fre-
quent (62%), followed by p,p0-DDT (50%), DDD
(43%), b-HCH (43%), and c-HCH (43%). Dicofol,
endosulfan-II, and o,p0-DDT were detected in few
samples. Aldrin and heptachlor endoepoxide were not
detected in any sediment samples. During winter, c-
HCH was the most frequently detected compound
(81%), followed by DDD (68%), o,p0-DDT (43%),
dicofol (43%), heptachlor (38%), DDE (32%), and b-
HCH (31%). Concentration of total OCPs was greater
in winter season, which may be due to weak desorption
of OCPs with sediment at lower temperature (Zhou
et al. 2006). The residual concentration of OCPs
detected in the current study was considerably high
compared with those measured in sediment from Da-
han and Erh-jen Rivers in Taiwan (Doong et al. 2002a,
b), from Arabian Sea (Sarkar et al. 1997), and from
Bay of Bengal, India (Babu et al. 2005).
Table 1 Percentage mean recovery (n = 6) with RSD (repeatability) of selected organochlorine pesticides at three spiking level
along with correlation coefficient (r), limit of detection (LOD), and limit of quantification (LOQ) of the optimized method
Pesticide Concentration (ng g-1) Correlation
coefficient, rLOD
(ng g-1)
LOQ
(ng g-1)50 100 200
b-HCH 87.20 ± 3.75 87.20 ± 1.88 77.40 ± 4.97 0.999 6 11
c-HCH 102.60 ± 3.34 99.20 ± 3.13 97.20 ± 4.50 0.998 2 3
Heptachlor 100.20 ± 4.90 92.20 ± 3.79 98.80 ± 5.15 0.999 7 14
Aldrin 82.60 ± 9.86 97.70 ± 9.10 100.20 ± 11.4 0.989 6 12
Dicofol 99.60 ± 4.41 104.50 ± 8.99 98.30 ± 11.87 0.998 6 12
Heptachlor exoepoxide 77.10 ± 2.29 110.90 ± 8.11 78.60 ± 13.47 0.998 8 15
Heptachlor endoepoxide 82.60 ± 9.32 88.00 ± 8.23 98.40 ± 11.19 0.998 7 13
Endosulfan-1 64.20 ± 6.17 64.80 ± 3.99 67.60 ± 9.67 0.997 5 9
Dieldrin 106.10 ± 2.55 106.40 ± 9.35 109.90 ± 11.2 0.999 6 12
DDD 106.40 ± 5.50 94.80 ± 8.08 112.60 ± 5.38 0.999 6 12
DDE 101.40 ± 3.62 104.00 ± 7.50 111.90 ± 8.30 0.993 5 10
Endrin 109.80 ± 4.01 105.50 ± 9.01 100.80 ± 9.50 0.998 5 9
Endosulfan-II 67.20 ± 14.51 71.90 ± 7.40 70.80 ± 11.07 0.999 2 3
o,p0-DDT 80.20 ± 5.37 76.50 ± 12.96 84.00 ± 9.70 0.995 3 6
p,p0-DDT 99.40 ± 6.35 102.40 ± 9.01 93.70 ± 10.40 0.997 7 14
Mirex 73.50 ± 9.02 105.00 ± 4.48 97.80 ± 8.37 0.993 5 10
Environ Geochem Health
123
The mean concentrations ofP
HCH measured in
the current study (4.7 and 5.7 ng g-1 in winter and
summer) were within the range detected in sediments
of the Kizilirmak River from Turkey (Bakan and
Ariman 2004) and of the Wu-Shi River from Taiwan
(Doong et al. 2002a). However, measured concentra-
tions were far greater than those reported from Pearl
River Estuary, PRC (Hong et al. 1999) and from
Xiamen Harbor, PRC (Hong et al. 1995), while Zhou
et al. (2006) measured far higher concentration ofP
HCH in river sediments from China as compared
with those recorded in this study. The concentration
of heptachlor detected in the current study suggested
continuing use for insect control and in seed and
wood preservation, and its presence can also be
related to surface runoff from agriculture cropland
and urban areas, municipal and industrial effluents,
and atmospheric deposition (Zhou et al. 2006). The
high detected concentration of dicofol could be due to
its use for protecting sugarcane, cotton, and fruit trees
in areas adjoining River Chenab. Dieldrin, aldrin,
endosulfan-I, and endosulfan-II were found at sam-
pling sites near cotton belt areas, but in small
quantities.
DDTs were more prevalent than HCHs and other
OCPs in sediments in both seasons. During winter,
Table 2 Descriptive statistics of OCP concentrations and physiochemical properties in sediment samples (n = 16) collected from
River Chenab, Pakistan during summer and winter season, 2007
Parameters Summer season Winter season CSQGs
N (detected) Min–Max Mean SD N (detected) Min–Max Mean SD ISQG
(ng g-1)
PEL
(ng g-1)
b-HCH (ng g-1) 7 6.20–11.89 9.13 2.12 5 5.78–8.23 7.01 1.05 – –
c-HCH (ng g-1) 7 1.77–7.59 3.84 2.25 13 1.73–4.69 3.06 0.89 0.94 1.38
Heptachlor (ng g-1) 10 14.11–36.11 21 7.31 6 19.50–33.66 27.6 6.47 – –
Aldrin (ng g-1) ND – – – 4 8.96–14.25 11 2.45 – –
Dicofol (ng g-1) 4 24.26–39.22 30.6 6.53 7 11.23–73.23 31.5 20.7 – –
Endosulfan-I (ng g-1) 2 8.25–11.32 9.79 2.17 ND – – – – –
Heptachlor
endoepoxide
(ng g-1)
ND – – – 3 7.95–13.25 10.9 2.69 0.6 2.74
Dieldrin (ng g-1) 2 14.35–18.26 16.3 2.76 4 19.25–32.59 25.2 5.52 2.58 6.67
DDD (ng g-1) 7 5.98–22.56 13.2 7.28 11 6.06–14.25 8.46 2.58 3.54 8.51
DDE (ng g-1) 3 9.17–16.95 13.2 3.9 5 9.42–22.94 16.3 4.96 1.42 6.75
Endosulfan-II (ng g-1) 6 1.93–3.67 2.87 0.71 4 2.14–7.19 5.14 2.41 – –
o,p0-DDT (ng g-1) 4 4.23–12.25 7.58 3.5 4 6.13–11.34 8.04 2.28 1.19 4.77
p,p0-DDT (ng g-1) 8 7.64–53.60 17.9 14.99 7 7.82–21.56 12.4 4.85
pH 7.7–9 8.65 0.32 6.6–8.9 7.88 0.79 – –
EC (lS cm-1) 0–190 33.1 45.71 0–210 90.62 61.7 – –
TDS (ppm) 0–120 20.6 29.31 0–140 57.5 39.4 – –
Alkalinity (mg g-1) 0.16–0.54 0.34 0.11 0.6–1.33 0.95 0.19 – –
Cl-1 (mg g-1) 0.16–0.55 0.24 0.08 0.58–0.83 0.65 0.06 – –
Total P (%) 0.03–0.07 0.04 0.008 0.02–0.06 0.03 0.01 – –
NO3–N (mg g-1) 0.042–0.49 0.15 0.1 0.118–0.61 0.23 0.12 – –
Total S (%) 0.0003–0.05 0 0.01 0.001–0.004 0.001 0 – –
OM (%) 0.06–1.37 0.49 0.4 0.29–4.43 2.21 1.4 – –
Clay (%) 0.8–20.05 7.63 5.63 0–16.6 6.85 5.43 – –
Silt (%) 0.2–21.3 7.75 8.68 0.1–17.7 5.43 6.14 – –
Sand (%) 67–98.9 85 11.81 71.2–100 88.6 10.1 – –
Environ Geochem Health
123
DDT metabolites were more prevalent, while in
summer DDT isomers were detected more frequently.
Greater concentration of DDTs can be linked to its
chronological use as well as excessive use of dicofol
as a pesticide. DDTs are used in the production of
dicofol as by products (Minh et al. 2007). The high
residual level of dicofol in sediments is related to its
use in agricultural activities as a cheaper pesticide
and it can also be identified as an additional source of
o,p0-DDT (Zhang et al. 2003; Leung et al. 2005; Wei
et al. 2008). Biodegradation of DDTs into its metab-
olites in riverine ecosystem cannot be neglected,
which may be another reason for the high concen-
tration of its metabolites in river sediments (Zhang
et al. 1999; Peris et al. 2005). Mean concentration ofP
DDTs detected in the current study during summer
(19.1 ng g-1) and winter (18.2 ng g-1) were rela-
tively lower than those measured in sediment from
Chinese rivers such as Haihe (15.9 ng g-1), Dagu
drainage (35.9 ng g-1), and Qiatang (21.62 ng g-1)
(Yang et al. 2005; Zhou et al. 2006), and Ebro River
(51.8 ng g-1) from Spain (Fernandez et al. 1998).
However, measured concentrations were greater than
those found in sediment of Minjiang River from
China (Zhang et al. 2003), Pearl River Estuary, PRC
(Hong et al. 1999), and Wu-Shi, Da-han, and Erh-jen
Rivers from Taiwan (Doong et al. 2002a, b).
Technical-grade DDT contains 75% p,p0-DDT,
15% o,p0-DDT, 5% p,p0-DDE, and\5% others (Hites
and Day 1992; Yang et al. 2005). DDT can be
biodegraded into DDD via reductive dechlorination
under anaerobic conditions and to DDE under aerobic
conditions through dehydrochlorination, an oxidative
process (Kalantzi et al. 2001; Luo et al. 2004).
Among metabolites, DDD was detected in greater
concentration, showing degradation of DDT during
both seasons, i.e., summer and winter. Among the
isomers, p,p0-DDT was the most frequently detected
compound in both seasons, indicating new input of
DDTs which have not yet been degraded. New inputs
of DDT can maintained high compositional percent-
age of DDT (Sarkar et al. 2008), while the DDT
proportion gradually reduces when there is no more
new input of DDT, accompanied by a gradual
increase in the concentration of metabolites (Doong
et al. 2002a). Figure 2 shows the compositional
percentage of DDTs in sediments during summer
and winter seasons. In summer season, p,p0-DDT in
sediment samples accounted for 46% of total DDTs,
followed by DDD (30%), DDE (12%), and o,p0-DDT
(9%). During winter season, p,p0-DDT accounted for
about 30% of total DDTs, while DDD, DDE, and o,p0-DDT accounted for 31%, 27%, and 10%, respectively,
indicating recent input of DDTs, aged DDT breakdown
products, as well as anaerobic conditions in River
Chenab.
Various indicative ratios such as (DDE ? DDD)/P
DDT, p,p0-DDT/P
DDT, and DDD/DDE are widely
used to assess decomposition of the parent compound
and recent DDT input (Phuong et al. 1998; Doong
et al. 2002b; Sarkar et al. 2008). In the current study,
(DDE ? DDD)/P
DDT was [0.5 during both sea-
sons, suggesting that sediments undergo a long-term
weathering process (Hong et al. 1999; Yang et al.
2005). In addition, p,p0-DDT/P
DDT ratios exceeded
0.5 at some sampling stations associated with recent
input of p,p0-DDT in both seasons. The DDD/DDE
ratio also exceeded unity for most sediment samples,
highlighting the high proportion of DDD in the
environment and indicating anaerobic environmental
conditions (Bossi et al. 1992) in River Chenab,
Pakistan.
Grouping of sites using hierarchical cluster
analysis (HACA) and identification of significant
parameters using discriminant function analysis
(DFA)
HACA grouped sampling sites into three regions based
on physicochemical properties and OCPs residue level;
however, site S1 located on Jhelum upstream was
identified as an outlier (Fig. 3). Region 1 consisted of
sites S2, S8, and S10, which were characterized by
relatively higher amounts of OCPs; EC, TDS, pH, and
Fig. 2 Composition of DDTs in sediments collected from
River Chenab, Pakistan during two sampling seasons
Environ Geochem Health
123
nutrients also showed higher concentrations. Site S8
was located at River Ravi, about 10 km above the
joining point of Rivers Ravi and Chenab. River Ravi
receives industrial and municipal waste from Lahore
and Qasoor Cities and OCPs from adjoining agricul-
tural fields. Site S2 receives toxic industrial waste from
Faisalabad City and agricultural runoff from adjoining
cotton cropland areas. Relatively high concentration of
heptachlor was found in the sediment of site S2,
indicating high usage of pesticide in upstream of River
Chenab. Cyclodienes, i.e., aldrin, dieldrin, endosulfan-
I, and endosulfan-II, were detected in considerably
higher concentration at sites S8 and S10, located in
cotton belt, indicating their usage in large quantities in
cotton belt as compared with rice- and sugarcane-
growing areas. Region 2 comprised five sites (S3, S4,
S6, S9, and S13) with the least OCPs contamination.
Sites viz., S3, S4, and S6 were located after the joining
of the River Jhelum to the River Chenab, which may
result in dilution of water thus improving the water
quality. The sediments at this site were also were
dominated by sand. Region 3 consisted of seven sites
(S5, S7, S11, S12, S14, S15, and S16). These sites were
located in cotton-growing areas, characterized by
severely eroded banks which incessantly slashed the
surrounded agricultural land into river. HCHs and
DDTs were measured in considerably higher concen-
tration in this region.
Temporal and spatial variation of OCPs in River
Chenab were further evaluated by discriminant func-
tion analysis (DFA). Forward and backward stepwise
spatial DFA modes generated 20 and 14 discriminant
variables with 100% and 96% classification accura-
cies. Backward stepwise DFA highlighted dicofol,
endosulfan-I, heptachlor endoepoxide, dieldrin, DDD,
DDE, endosulfan-II, o,p0-DDT, p,p0-DDT, pH, EC,
Cl-1, total P, and silt as significant parameters that
highlighted variations between the three spatial
regions defined by HACA (Fig. 4). Spatial DFA
discriminated parameters that showed higher concen-
tration in sites classified to region 1. These sites (S2,
S8, and S10) receive contaminant load mainly from
industrial, urban, and agricultural runoff. Sediment
samples collected from sites of region 2 showed high
residual level of endosulfan-I, endosulfan-II, hepta-
chlor endoepoxide, and DDD. Greater concentration of
endosulfan-I, endosulfan-II, and heptachlor endoep-
oxide reflected their widespread use for agricultural
activities. Greater residual level of DDD indicated
anaerobic degradation of DDT. Dicofol, endosulfan-I,
dieldrin, DDE, o,p0-DDT, p,p0-DDT, pH, EC, Cl-1,
total P, and silt showed higher values in sediments
collected from sites which comprised region 3. These
sites were situated in cotton belt, which receives
pesticide load from adjoining cropland land due to
severely eroded banks and agricultural runoff. River
Unweighted pair-group averageEuclidean distances
(Dlin
k/D
max
)*10
0
0
20
40
60
80
100
120
S-2 S-11
S-7 S-12
S-15 S-14
S-16 S-5
S-13 S-6
S-9 S-4
S-3 S-8
S-10 S-1
Fig. 3 Hierarchical dendrogram of sampling sites obtained using UPMGA as linkage method and Euclidean distance matrix
Environ Geochem Health
123
Ravi, which joins River Chenab, brings effluent from
major industrial cities such as Qasoor, Lahore, and
Gujarat and also contributed to deterioration of quality
of sediments of region 3. The results of HACA also
supported the trends identified by spatial DFA.
Standard, forward stepwise, and backward stepwise
temporal analysis generated 25, 16, and 5 discriminant
variables, respectively, giving CMs (Classification
Matrices) with 99.7% correct assignation. Temporal
DFA showed aldrin, heptachlor endoepoxide, Cl-1,
phosphorus, and EC to be the most important variables
discriminating between summer and winter seasons
(Fig. 5). The distribution and variability of OCPs are
largely dependent on the physicochemical properties
of the sediments, environmental behavior of contam-
inant, and geology of the area (Leonard 1990; Glynn
et al. 1995; Brasher and Wolf 2004). DFA proved to be
a valuable tool for determining the patterns of spatial
and temporal trends and highlighted residual concen-
trations of dicofol, endosulfan-I, heptachlor endoep-
oxide, dieldrin, DDD, DDE, endosulfan-II, o,p0-DDT,
and p,p0-DDT as important variables which require
more attention and future monitoring. Furthermore, all
sites of region 1 were more polluted as compared with
other sites and should be monitored regularly.
Source identification using FA/PCA
Temporal FA/PCA extracted seven varimax factors
(VFs) for each season with eigenvalue[1, explaining
84.77% and 87.44% of total variance for both winter
and summer, respectively. For summer season, of
seven VFs, VF1 explained 40.10% of total variance,
showing strong positive correlation with EC, TDS,
Cl-1, and NO3–N and sources mainly related with
agricultural runoff from adjoining fields and from the
natural mineral composition of river sediments. The
mineral composition of River Chenab sediments
mainly comprises thick deposits of calcareous, fine
and wind-laid sands, and silt originating from sand-
stones and shale rocks of the catchment area, espe-
cially Salt Range. This may have resulted in high
content of dissolved salts. Source of NO3–N is mainly
correlated with excessive use of nitrogenous fertiliz-
ers in agricultural fields. Nitrogenous fertilizers such
as urea are used in large quantities in Pakistan and
undergo extracellular enzymatic decomposition to
form ammonium compounds, which are either
absorbed by plant roots or converted to nitrates, get
absorbed or are lost by leaching, or are released to the
atmosphere to become part of the nitrogen cycle
(Singh et al. 1995). VF2 and VF3 explained 12.09%
and 9.22% of total variance, with positive correlation
with heptachlor, endosulfan-I, c-HCH, and DDD,
while total P showed strong negative correlation,
indicating input related to agricultural activities in the
catchment, and industrial and municipal input. VF3
represented the anaerobic degradation of DDT into
DDD while c-HCH residues contamination in river
sediments could have resulted due to partial sedimen-
tation from surrounding soils however, negative
loading of total P showed indicated that it is not
associated with parent rock material. VF4 explained
8.24% of total variation, strongly correlated with
dieldrin and organic matter, while VF5 explained
7.34% of total variance, with positive loading on silt
and negative loading on o,p0-DDT and sand. VF6 and
VF7 explained 5.28% and 4.64% of total variance,
with positive loading on p,p0-DDT and total S and
sources of these two parameters mainly related with
human activities in catchment of study area.
For winter season, of seven VFs, VF1 explained
25.19% of total variance, with significant positive
loading on pH, EC, TDS, clay, and silt and strong
negative loading on sand, indicating their source
related with parent rock material. VF2 explained
16.78% of total variance, with strong positive loading
on aldrin and o,p0-DDT but negative loading on total P
and organic matter. This factor can be interpreted as
indicating that aldrin and o,p0-DDT contamination are
due to excessive use of these pesticides in surrounding
agricultural fields, and detection in most samples
during winter may be due to weak desorption at low
temperature, while phosphorus contents decreased due
to low organic matter contents. VF3 explained 12.26%
of total variance, with positive loading on c-HCH and
negative loading on heptachlor and total S. This factor
indicates that c-HCH residues associated with sedi-
ment due to wet deposition and heptachlor and sulfur
entered the riverine ecosystem through municipal
sewage. VF4 explained 10.52% of total variance, with
positive loading on dicofol, heptachlor endoepoxide,
and NO3–N. VF5, V6 and VF7 explained\10% of total
variance and these factors highlighted the dominance
of b-HCH (VF5), Cl-1 (VF6) and endosulfan-11
(VF7). It suggested that b-HCH, Cl-1 and endosul-
fan-11 were found frequently during winter and mainly
originated from surface runoff from agricultural fields.
Environ Geochem Health
123
Dic
ofol
(ng
g-1)
-5
5
15
25
35
45
Region-1 Region-2 Region-3
Min-Max
25%-75%
Median value
EN
DO
-1 (
ngg-
1)
-2
0
2
4
6
8
10
12
14
Region-1 Region-2 Region-3
Hep
tach
lor
endo
epox
ide
(ngg
-1)
-2
0
2
4
6
8
10
12
14
16
Region-1 Region-2 Region-3
Die
ldrin
(ng
g-1)
-5
0
5
10
15
20
25
30
35
Region-1 Region-2 Region-3
EN
DO
-II (
ngg-
1)
-1
0
1
2
3
4
5
6
7
8
Region-1 Region-2 Region-3
DD
D (
ngg-
1)
-2
2
6
10
14
18
22
26
Region-1 Region-2 Region-3
DD
E (
ngg-
1)
-2
2
6
10
14
18
22
26
Region-1 Region-2 Region-3
a
c
e
g
f
d
b
Fig. 4 a–n Spatial variations identified by discriminant function analysis: dicofol, endosulfan-I, heptachlor endoepoxide, dieldrin,
DDD, DDE, endosulfan-II, o,p0-DDT, p,p0-DDT, pH, EC, chloride, phosphorus, and silt
Environ Geochem Health
123
o,p'
-DD
T (
ngg-
1)
-2
0
2
4
6
8
10
12
14
Region-1 Region-2 Region-3
p,p'
-DD
T (
ngg-
1)
-5
5
15
25
35
45
55
65
Region-1 Region-2
pH
6.4
6.8
7.2
7.6
8.0
8.4
8.8
9.2
Region-1 Region-2 Region-3
EC
(µS
/cm
)
-20
20
60
100
140
180
220
260
Region-1 Region-2 Region-3
Chl
orid
es (
ngg-
1)
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
Region-1 Region-2 Region-3
P (
%)
-5
0
5
10
15
20
25
30
35
Region-1 Region-2 Region-3
Silt
(%
)
-2
2
6
10
14
18
22
26
Region-1 Region-2 Region-3
Region-3
h i
j k
lm
n
Fig. 4 continued
Environ Geochem Health
123
Spatial FA/PCA extracted five VFs for region 1
and six VFs for regions 2 and 3 with eigenvalue [1,
explaining 100%, 90.67%, and 84.80% of total
variance. For region 1, VF1 explained 34.94% of
total variance, in which aldrin, dieldrin, o,p0-DDT,
and alkalinity had strong positive correlation, while
heptachlor and total P showed negative correlation.
This factor indicated that high concentrations of
dieldrin, aldrin, and o,p0-DDT in region 1 were due to
anthropogenic activities (agricultural and industrial),
whereas source of alkalinity can be linked with
natural as well as anthropogenic processes in the
catchment, while the negative correlation of hepta-
chlor and phosphorus suggested the source of these
two parameters from agricultural activities. Hepta-
chlor is used in agricultural fields to protect citrus
trees and crops from insects. Phosphorous contents
may be correlated with use of fertilizers containing
high phosphorus contents. VF2 explained 30.57% of
total variance, and EC, TDS, Cl-1, total S, organic
matter, and clay showed strong positive loading; their
sources were mainly related with natural mineral
Ald
rin (
ngg-
1)
-2
0
2
4
6
8
10
12
14
16
WinterSummer
Min-Max
25%-75%
Median value
Hep
tach
lor
endo
epox
ide
(ngg
-1)
-2
0
2
4
6
8
10
12
14
16
EC
(µS
/cm
)
-20
20
60
100
140
180
220
260
Chl
orid
es (
ngg-
1)
0.1
0.2
0.3
0.4
0.5
0.6
0.7
0.8
0.9
P (
%)
-5
0
5
10
15
20
25
30
35
WinterSummer
WinterSummer
WinterSummer
WinterSummer
a
c
b
e
d
Fig. 5 a–e Temporal variations highlighted by discriminant function analysis: aldrin, heptachlor epoxide, EC, chloride, and P (%)
Environ Geochem Health
123
composition. VF3 explained 18.41% of total vari-
ance, showing strong positive loading on c-HCH,
dicofol, endosulfan-II, and nitrates, while pH showed
negative loading. This factor indicated surface runoff
from agricultural fields as a main contributing factor.
VF4 explained 10.19% of total variance and showed
positive loading on p,p0-DDT and negative loading on
endosulfan-I and silt. This factor represents the high
p,p0-DDT residue level from agricultural source.
For region 2, of six varimax factors (VFs), VF1
explained 27.15% of total variance and showed
positive loading on EC, TDS, alkalinity, Cl-1, and
organic matter. VF2 explained 17.15% of total
variance, positively related to dicofol and heptachlor
endoepoxide, indicating that their source was mainly
due to agricultural activities in sites comprising
region 2, where pesticides are being used to protect
crops from insects and various diseases. VF3
explained 15.67% of total variance and showed
positive correlation with DDE and clay, indicating
adsorption capacity of clay with DDE. VF4 explained
13.88% of total variance, positively loaded on sand
but negatively loaded on endosulfan-I and silt. VF5
explained 10.25% of total variance and showed
negative loading on dieldrin and p,p0-DDT. VF6
explained 6.57% of total variance, showing negative
loading on aldrin. Most of the factors highlighted the
role of agricultural, industrial, and urban activities in
OCP contamination.
For region 3, out of six variables, VF1 explained
26.34% of total variance and showed positive loading
on c-HCH and DDE. This factor represented the high
residue level of c-HCH and DDE from agricultural
fields. VF2 explained 24.59% of total variance,
showing positive loading on alkalinity, organic
matter, and Cl-1 and negative loading on pH. This
factor showed a decline of pH value due to high
organic matter content, which may affect many
reactions in the sediments (Cirmo et al. 2000). Acidic
conditions accelerated the fluxes of acidic anions
(e.g., SO2-4 and NO-3). On the other hand, increased
hydrogen ion concentration also associated with clay
particles, which resulted in chemical solution of
minerals. Hydrogen ions also removed Al3? ions held
within the structure of soil minerals and accelerated
formation of organic complexes (Brady and Weil
1996), while the source of alkalinity and Cl-1 was
from naturally occurring minerals in the river system.
VF3 explained 12.71% of total variance and showed
positive loading on total S, indicating its sources
related to municipal effluents. VF4 explained 8.31%
of total variance and showed positive loading on
dicofol, EC, and TDS. This factor shows that dicofol
concentration increases with EC and TDS. VF5 and
VF6 explained [5% of total variance and extracted
total P and p,p0-DDT as important variables, respec-
tively. VF5 and VF6 can be interpreted as indicating
that the source of phosphorus and p,p0-DDT were
mainly from agricultural activities.
Ecotoxicological concerns
OCP concentrations in assessed sediment samples
were compared with sediment quality guidelines for
the protection of aquatic life (CCME 1999) for
assessment of relative sediment quality and potential
risk to aquatic life in River Chenab. Concentration of
c-HCH in the detected samples ranged from 1.77 to
7.59 ng g-1 during both seasons, which exceeded
both ISQGs (0.94 ng g-1) and probable effect limit
(PEL) values (1.38 ng g-1). Concentrations of diel-
drin (14.35–32.59 ng g-1) and heptachlor epoxide
(7.95–13.25 ng g-1) in winter season were also
found to be well above their ISQGs and PEL values.
Concentrations of DDTs (o,p0-DDT and p,p0-DDT)
ranged from 5.63 to 53.60 ng g-1, which were far
greater than the ISQGs (1.19 ng g-1) and PELs
(4.77 ng g-1). Similarly, residual levels of DDD and
DDE also exceeded the ISQGs and PEL values,
indicating severe contamination of DDTs and their
metabolites. This highlights that River Chenab sed-
iments pose a serious threat to aquatic life, and urgent
restoration and management is warranted to safe-
guard the aquatic system.
Conclusions
The present study provides the first systematic data
on the distribution of OCPs in sediments of River
Chenab, Pakistan. The results highlight that OCPs
contamination should be considered as an important
environmental issue due to their excessive use in
agriculture and industrial sector. DDTs, HCHs,
heptachlor, and dicofol were the dominant OCPs
found in River Chenab sediments. High concentration
of p,p0-DDT in sediments in both seasons reflected
recent use of the parent DDT compound, while
Environ Geochem Health
123
presence of DDD in most sediment samples sug-
gested its contamination mainly from agricultural
soils aged under anaerobic environmental conditions.
HACA grouped sampling sites into three spatial
groups with varying proportion of OCPs contamina-
tion, whereas FA/PCA highlighted sources of OCPs
mainly related to agricultural and industrial activities.
DFA identified 6 variables (aldrin, heptachlor endo-
epoxide, Cl-1, total P, and EC) and 14 parameters
(dicofol, endosulfan-I, heptachlor endoepoxide, diel-
drin, DDD, DDE, endosulfan-II, o,p0-DDT, p,p0-DDT, pH, EC, Cl-1, phosphate, and silt) that
accounted for most of the total spatial and temporal
variations. Parameters identified by temporal and
spatial DFA require more attention for management
and conservation of River Chenab aquatic resources.
The residual level of OCPs measured in the sediments
indicates the need to study the associated risks to the
aquatic ecosystem and in particular to directly
associated communities.
Acknowledgments The first author thanks the Higher
Education Commission (HEC) for providing financial support
under the Indigenous 5,000 fellowship program towards his
PhD. We also acknowledge the Pakistan Wetland Program
(PWP) for providing transportation during fieldwork. Efforts of
research students of EBL, QAU during exhaustive fieldwork
are gratefully acknowledged.
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