automated method for the determination of total arsenic
TRANSCRIPT
ORIGINAL PAPER
Automated method for the determination of total arsenicand selenium in natural and drinking water by HG-AAS
Mariela Piston • Javier Silva •
Ramiro Perez-Zambra •
Isabel Dol • Moises Knochen
Received: 10 February 2010 / Accepted: 11 April 2011
� Springer Science+Business Media B.V. 2011
Abstract A multicommutated flow system was
designed and evaluated for the determination of total
arsenic and selenium by Hydride Generation Atomic
Absorption Spectrometry (HG-AAS). It was applied to
the determination of arsenic and selenium in samples
of natural and drinking water. Detection limits were
0.46 and 0.08 lg l-1 for arsenic and selenium, respec-
tively; sampling frequency was 120 samples h-1 for
arsenic and 160 samples h-1 for selenium. Linear
ranges found were 1.54–10 lg l-1 (R = 0.999) for
arsenic and 0.27–27 lg l-1 (R = 0.999) for selenium.
Accuracy was evaluated by spiking various water
samples and using a reference material. Recoveries
were in the range 95–116%. Analytical precision
(sr (%), n = 10) was 6% for both elements. Compared
with the Standard Methods, APHA, 3114B manual
method, the system consumes at least 10 times less
sample per determination, and the quantities of acid
and reducing agent used are significantly lower with
a reduction in the generation of pollutants and waste.
As an additional advantage, the system is very fast,
efficient and environmentally friendly for monitoring
total arsenic and selenium levels in waters.
Keywords Flow analysis � Selenium � Arsenic �Water � Trace element monitoring
Introduction
Arsenic and selenium are two widely distributed
semimetals which for different reasons have attracted
interest in connection with public health issues.
Arsenic has been known for centuries as a toxic
element: in popular imagination, it has become a
synonymous of poison. Besides the obvious behavior
of some of its compounds in acute exposure, there is an
increasing concern about the risk associated with long-
term exposure. There exists considerable evidence
suggesting that consumption of arsenic-containing
water can cause skin, bladder and lung cancer (Goyer
1996).
One of the main problems in some geographical
areas arises from groundwater contamination of either
mineral or anthropogenic origin. A number of chronic
intoxication episodes have occurred that have drawn
attention to the risk to which the population of certain
areas is exposed due to consumption of water from
contaminated wells. Thus, it has been classified as a
high-priority substance for screening in drinking water
sources. Maximum acceptable levels of total arsenic in
drinking water have been the object of some contro-
versy, although there is a trend toward the establish-
ment of lower values. WHO, in its Guidelines for
M. Piston (&) � J. Silva � R. Perez-Zambra �I. Dol � M. Knochen
Facultad de Quımica, Universidad de la Republica,
Catedra de Quımica Analıtica. Av. Gral. Flores 2124,
P.O. Box 1157, 11800 Montevideo, Uruguay
e-mail: [email protected]
123
Environ Geochem Health
DOI 10.1007/s10653-011-9436-9
Drinking-water Quality (World Health Organization
2004), sets up the recommendation for a provisional
guideline value of 10 lg l-1. This value coincides with
other standards such as that set up by EPA (Environ-
mental Protection Agency 2001) and several regula-
tory bodies throughout the world. However, values as
high as 20 lg l-1 (Instituto Uruguayo de Normas
Tecnicas 2008) can still be found in some countries.
For drinking water sources, such as river or ground-
water, the maximum values set up are often lower
(\10 lg l-1).
Selenium on the other hand is now known as
necessary for life. It occurs in all environments
unevenly distributed throughout the planet; in some
places, selenium concentrations in soil are so low that
consumption of vegetables by animals or humans
cannot guarantee the recommended daily intake of
selenium.
In other areas, it can be found at high levels, for
example, in soils in very dry zones of USA where there
are plants with high concentrations of selenium
(Fordyce 2005).
In the 1950s, the essentiality of selenium in animals
and humans was revealed with the discovery of its
ability to prevent the Keshan disease, first described in
1935 in the Chinese province of that name. This
population showed symptoms attributed to selenium
deficiency: different degrees of heart disease or
cardiac deficiencies; myocardial histology showed
degeneration and necrosis of ultrastructure of muscle
fibers. Selenium is an essential component of enzymes
such as glutathione peroxidase that is found in human
tissues (Flynn and Cashman 1997).
Subsequently, its important role as part of the
body’s antioxidant mechanisms and the role in
protecting the body against heavy metals as well as
its importance in the immune system were discovered
(Tiglea and Mello De Capitani 2003; Fordyce 2005).
Related to the latter, the patients with AIDS show
evidence of selenium deficiency, such as a marked
decrease in the activity of glutathione peroxidase.
RDA (Recommended Dietary Allowance) accepted
value in the USA ranges from 20 lg/day for children
under 3 years of age up to 55 lg/day for adults. These
values can be increased to 60 lg/day for pregnant
women and 70 lg/day during lactation (Flynn and
Cashman 1997). These nutritional requirements should
be satisfied by food and water ingested by the
individual.
Selenium has one of the narrowest ranges between
dietary deficiency and toxic levels, so control in the
intake of selenium by humans and other animals is
imperative (Fordyce 2005). The WHO guideline value
for selenium in drinking water is 10 lg l-1 (World
Health Organization 2004).
In Uruguay, the government promotes the moni-
toring of some trace elements in waters through
different programs involving surface and groundwater
as well as drinking water.
The increasing interest in these trace elements has
expanded the need for reliable data, which puts
considerable pressure on environmental analytical
laboratories. This has triggered research for new and
improved automated analytical methods for the deter-
mination of ultra-trace levels of arsenic and selenium
in water samples. These methods should not only be
reliable but also fast and environmentally friendly.
Total arsenic and selenium at the trace and ultra-
trace levels are determined by atomic absorption
spectrometry (AAS) and atomic fluorescence spec-
trometry (AFS) (Standard Methods, APHA 1998;
Welz and Sperling 1999). For AAS determinations,
electrothermal atomization can be used (Aleixo and
Nobrega 2003; Paiva Oliveira et al. 2005; Hung et al.
2004; Michon et al. 2007). However, the use of
hydride generation (HG) (Dedina and Tsalev 1995) is
preferable since it provides separation of the analyte
from the matrix which in turn reduces the effects of a
number of interferences. Hydride generation can be
coupled to atomic absorption (HG-AAS) or to atomic
fluorescence (HG-AFS) spectrometric detection. The
latter provides lower detection limits at the cost of
more expensive instrumentation.
Hydride generation can be automated employing
different flow techniques such as flow injection
analysis (FIA) (Zhang and Adeloju 2008; Li et al.
2009) or sequential injection analysis (SIA) (Seme-
nova et al. 2000). Multicommutated flow analysis
(MCFA) is an emerging flow technique based on flow
networks built around solenoid valves which can be
commutated independently under computer control
in order to perform specific tasks (Reis et al. 1994;
Rocha et al. 2002; Catala Icardo et al. 2002; Feres et al.
2008). This technique has proven to be very flexible
since several modifications can be carried out simply
by changing parameters in the control software.
For instance, the sample volume can be easily changed
by modifying the time a given solenoid valve is
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123
energized, thus allowing for different concentration
ranges. Since MCFA is a microanalytical technique,
methods based on it usually present low reactive
consumption and generate low volumes of chemical
residues. The literature reflects the usefulness of this
technique that has been applied to the determination of
different analytes in a wide range of matrixes (Kno-
chen et al. 2005; Piston et al. 2006; Sixto and Knochen
2009; Piston et al. 2009).
The goal of this work was to develop a fast, efficient
and environmentally friendly method for the determi-
nation of total arsenic and selenium in water samples.
For this purpose, an MCFA system with HG-AAS
detection was designed. The analytical method was
validated and applied to the determination of arsenic
and selenium in samples of natural and drinking water.
Materials and methods
All reagents used in sample treatment were of
analytical reagent grade or better.
Sodium tetrahydroborate (Hydride-Generation
grade) was obtained from Fluka (Buchs, Switzerland).
0.5% (w/v) and 1.2% (w/v) solutions were prepared
daily by dissolving the solid in 0.05% (w/v) sodium
hydroxide.
Purified water (ASTM Type I) was obtained from a
Millipore (Sao Paulo, Brazil) Simplicity 185 purifier
fed with glass-distilled water.
A selenium standard solution (1,000 mg l-1) was
prepared from selenium metal (Aldrich, St. Louis,
MO, USA, 99.99%) dissolved in nitric acid and made
up to volume with 10% (v/v) hydrochloric acid.
An intermediate standard solution (0.8 mg l-1) was
prepared daily by stepwise dilution with 1.5% (v/v)
hydrochloric acid.
An arsenic standard solution (1,000 mg l-1) was
prepared from arsenic trioxide (Sigma–Aldrich, Pri-
mary standard grade 99.95%) dissolved in 0.4% (w/v)
sodium hydroxide solution. An intermediate standard
solution (0.6 mg l-1) was prepared by dilution with
1.5% (v/v) hydrochloric acid.
All glassware were soaked overnight in 10% (v/v)
nitric acid and then rinsed exhaustively with purified
water.
Samples of surface water, groundwater and drinking
water were obtained from different locations of
Uruguay. For arsenic, the calibration curve in the
range 2.0–15 lg l-1 was prepared by accurately mea-
suring 0.05-, 0.1-, 0.2- and 0.3-ml of the 0.6-mg l-1
intermediate standard solution, followed by the addition
of 10 ml of water, 0.2 ml of 7% (v/v) sulfuric acid and
0.4 ml of 5% (w/v) potassium persulfate. The mixture
was heated on a hot plate for 1 h at gentle boiling and
then cooled down at room temperature. Afterward, 1 ml
of 7% (w/v) sodium iodide and 1 ml of concentrated
hydrochloric acid were added to carry out the pre-
reduction of As(V) to As(III), followed by dilution to
15 ml with water.
For selenium, calibration solutions in the range
1.0–10.0 lg l-1 were prepared by accurately measur-
ing 0.05-, 0.1-, 0.2-, 0.3- and 0.4-ml aliquots of the
0.8 mg l-1 intermediate standard solution, to which
20 ml of water and 10 ml of concentrated hydrochlo-
ric acid were added. The mixture was heated on a hot
plate for 1 h at gentle boiling to carry out the pre-
reduction of Se(VI) to Se(IV) and then cooled down to
room temperature and diluted to 30.0 ml with water.
Water samples (10 ml) were processed similarly to
the standards according to the procedures described
above for the respective elements.
MCFA system
The flow system was described elsewhere (Piston et al.
2009). It was based upon a Gilson (Villiers-le-Bel,
France) Minipuls 2 multichannel peristaltic pump and
two 3-way 12 V solenoid valves (NResearch, West
Caldwell, NJ, USA, model 161T031) which were used
for fluid control. In order to avoid unnecessary
consumption, sample and NaBH4 solution were recy-
cled to the bottle when not used.
Nitrogen (dried and purified by a combined
Drierite/molecular sieve trap) was used as carrier gas.
All measurements were taken on a Perkin-Elmer
(Norwalk, CT, USA) model 5000 atomic absorption
spectrometer, fitted with a 10-cm burner (air-acetylene
flame) and a T-shaped quartz atomization cell (Preci-
sion Glassblowing, Centennial, CO, USA) and oper-
ated at 193.7 nm (As) or 196.0 nm (Se). The slit width
was 0.7 nm for both determinations. Superlamp�
intensified emission hollow cathode lamps (Photron,
Narre Warren, Australia) were used as light sources
and operated as recommended by the manufacturer.
For the operation of the system, a program was
compiled in Visual Basic 6.0 (Microsoft) using the
Environ Geochem Health
123
Software 3.1 (Measurement Computing) graphical
programming environment. The program controlled
the timing and the activation of the solenoid valves
using the parameters set up before the beginning of the
analysis and also handled the data acquisition, visual
display and storage on hard disk.
Results and discussion
The influence of the most significant variables (con-
centration of HCl and NaBH4, carrier gas flow rate,
sample volume and sample and reagents flow rates)
was studied by means of multivariate experiments
based on central composite design. Optimal conditions
found were as follows: for arsenic, 1.2% (w/v) NaBH4
and 1.0 ml sample volume; for selenium, 0.5 (w/v) and
0.6 ml, respectively. For both elements, 5% (v/v) HCl
was used, while optimum flow rates were 0.32 l min-1
(nitrogen), 7.2 ml min-1 (sample), 3.2 ml min-1
(HCl solution) and 1.7 ml min-1 (NaBH4 solution).
Under the final operating conditions, sampling
frequencies were 120 samples h-1 (arsenic) and 160
samples h-1 (selenium).
Precision, accuracy, linear range as well as detec-
tion and quantification limits were determined
(Table 1). Precision (repeatability) was estimated by
the analysis of a given sample (n = 10) and expressed
as relative standard deviation [sr(%)].
Accuracy was evaluated as recovery from analysis
of a reference material provided by Mexico’s Centro
Nacional de Metrologıa (CENAM) for proficiency
testing and coded ‘‘620-Q004-0127-PA MERCOSUR
y Chile/MA2008’’, as well as from analysis of spiked
samples.
Linear range was estimated by the analysis of
regression coefficients and visual inspection of regres-
sion plots. Detection (3 s) and quantification (10 s)
limits were also estimated.
In our laboratory, we have gathered data for arsenic
and selenium content in natural and drinking water
from different areas in Uruguay for a period of 4 years.
Over 340 samples were analyzed for arsenic and 250
for selenium using the APHA 3114B HG-AAS manual
standard method (Standard Methods, APHA 1998).
The values found were always in the range up to
84 lg l-1 (arsenic) and 4 lg l-1 (selenium). A map
representing the different levels of selenium found in
Uruguay is presented in Fig. 1. The proposed system is
suitable for handling these concentration ranges, and
the methods present sampling frequencies of 120 and
160 samples h-1 compared with just 15 samples h-1 of
the APHA standard manual methods. Other analytical
methods widely used for these elements, such as
Table 1 Validation of arsenic and selenium determination by the proposed methods (MCFA) compared with the Standard Method
APHA 3114B
Figures of merit As Se
APHA 3114 B MCFA APHA 3114 B MCFA
LD (lg l-1), n = 5 0.40 0.46 0.3 0.08
LQ (lg l-1), n = 5 1.50 1.54 1.0 0.27
Precision, sr (%), n = 10 \6 \3 \6 \4
Recovery (%) 90–109* 96–99* 98–106** 95–116**
Linear range (lg l-1) 1.50–5
(R = 0.999)
1.54–15 (R = 0.999) 1.0–15 (R = 0.998) 0.27–27 (R = 0.999)
Sample consumption per determination (ml) 10 1.0 10 0.6
HCl consumption per determination (ml) 2.5 0.08 2.5 0.05
NaBH4 consumption per determination (mg) 320 20 320 5
Sampling frequency (samples h-1) 15 120 15 160
LD, LQ detection (3 s) and quantification (10 s) limits, sr (%) precision (relative standard deviation) determined by repeated analysis
of samples
* Accuracy evaluated by recovery on reference material provided by Centro Nacional de Metrologıa, CENAM (Mexico) for
participation in proficiency testing and coded ‘‘620-Q004-0127-PA MERCOSUR y Chile/MA2-2008’’
** Accuracy evaluated by spiking various water samples
Environ Geochem Health
123
electrothermal atomic absorption spectrometry, are
also very slow.
Thus, the proposed methods seem suitable for rapid
monitoring of these elements in an environmentally
friendly way, as less than 2 ml of chemical residues
are generated per determination, while the manual
standard methods generate at least 10 times more.
Conclusion
Multicommutated flow analysis was successfully used
for the generation of arsenic and selenium hydride and
applied to the determination of these trace elements by
HG-AAS in the samples of natural and drinking water.
Methods based on the proposed technique were
validated and resulted sufficiently accurate and precise
for the determination of total arsenic and selenium
contents in that type of samples.
The use of multicommutation provided several
advantages such as low consumption of reagents and
sample with less generation of chemical residues, and
a fast and flexible system which can be easily modified
by software to allow for different operating conditions.
The system was applied to the determination of total
arsenic and selenium in samples of drinking water from
Uruguay and could be used for monitoring total arsenic
and selenium in natural waters in a routine work.
Acknowledgments The authors thank UdelaR-CSIC for a
research grant and PEDECIBA-Quımica for partial support.
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