Water
Quality 1 - Spectrophotometric Determination of Iron in Drinking Water
Introduction
The safety of
drinking water is a very important public health issue. The
A commonly used
method for the determination of trace amounts of iron involves the complexation
of Fe2+ with 1,10-phenanthroline (phen) to produce an intensely
red-orange colored complex:
Fe2+ + 3
phen à Fe(phen)32+
Since the iron present
in the water predominantly exists as Fe3+, it is necessary to first
reduce Fe3+ to Fe2+.
This is accomplished by the addition of the reducing agent
hydroxylamine. An excess of reducing
agent is needed to maintain iron in the +2 state (because dissolved oxygen will
reoxidize Fe2+ to Fe3+). Fe2+ is
quantitatively complexed by 1,10-phenanthroline in the pH range from 3 to 9.
Sodium acetate is used as a buffer to maintain a constant pH at 3.5. If the pH
is too high, the Fe2+ will be oxidized to Fe3+; if the pH
is too low, H+ will compete with Fe2+ for the basic
1,10-phenanthroline (to form phenH+). Either way, you won’t get complete
complexation. You should discuss these
possible problems and their impact in the Introduction section of your report. The determination of the iron-phen complex is
performed with a spectrophotometer at a fixed wavelength of 508 nm using
external calibration based on iron standard solutions.
Apparatus
plastic cuvette (1)
500 mL volumetric flask (1)
50 mL volumetric flasks (10)
500 μL automatic pipettor (1)
1 mL pipet (1)
5 mL pipets (2)
25 mL pipet (1)
Instrumentation
(See Appendices for Operating Instructions)
WPA Biowave II or
other benchtop UV-Vis spectrophotometer
Solutions available
(1) 0.29 M hydroxylamine hydrochloride
(NH2OH•HCI): measure out about 12 mL to a small beaker.
(2) 5.0
x10-3 M 1,10-phenanthroline: measure out about 50 mL to a 100 or 200
mL beaker.
(3) 1.2
M sodium acetate: measure out about 50 mL to a 100 or 200 mL beaker.
(4) 2
M H2SO4 (Caution: strong oxidizing acid.)
Solution
to be prepared
Standard iron solution (5.0 x10-4
M).
Accurately weigh out about 0.100 g Fe(NH4)2(SO4)2-6H20
(FW = 392.14). Transfer quantitatively into a 500-mL volumetric flask. Add about 10 mL of 2 M H2SO4
and 50-mL deionized water to the flask to dissolve the Fe(NH4)2(SO4)2·6H2O
completely. Fill the flask to the mark
with deionized water and mix thoroughly.
Procedure
(1) Preparing
the working standard solutions
Use the 500 μL
automatic pipettor to pipet 0, 0.5, 1.0, 1.5, 2.0, and 2.5 mL of the standard
iron solution into a series of six 50 mL volumetric flasks. Pipet the following solutions into each of the
six volumetric flasks.
a) 1 mL of the hydroxylamine solution
b) 5 mL of the sodium acetate solution
c) 5 mL of the 1,10-phenanthroline
solution
Fill each flask to
the mark with deionized water and mix thoroughly. Allow the solutions to stand for 10 min. Mix the solutions again before measuring the
absorbance. If more than half of the standard iron solution remains when you
complete the experiment, you can retain it for the other experiment in this set.
(2) Measuring
the blank
To determine any
possible absorbance from the matrix (i.e.,
the other reagents), deionized water will be used as the blank. Rinse the cuvette several times with tap
water followed by deionized water, fill it with deionized water, place it the
holder, and blank the spectrometer.
(3) Measuring
the standards
Rinse the cuvette
with each solution (including the zero iron concentration sample) three times,
and then fill it with the solution, place it in the holder, and measure the
absorbance. Repeat the measurement with
a fresh aliquot of the solution (no need to rinse this time.) The two absorbance values should be similar,
otherwise you should measure another one.
If you work from lowest iron concentration to highest, you will minimize
the potential for carryover.
(4) Measuring
the unkown water samples
Prepare two
challenge “unkown” samples, one that will end up near mid-range on the
calibration curve and one near the lower end, to test for method recovery and
accuracy. Pipet 25 mL aliquots of your cold and hot tap water and two unknown
samples into four 50 mL volumetric flasks.
Finish preparing the samples as described in the procedure (1). Measure the absorbance of the solutions. If the absorbance is outside of the range of
the iron standards, you should repeat the measurement after adjusting the
concentration to bring it into the range of the standards. If it is too concentrated, you can simply use
a smaller volume of the sample. If it is
too dilute, you may try evaporative concentration, if time permits. Be sure to document any deviations from the
suggested procedure in the Experimental section of your report.
Report: In preparing the
Partial Report for this part of the experiment, you should
consider/complete/discuss the following:
(1) Calculate
the analytical concentration of iron in the standard iron solutions. Tabulate the observed absorbance and the
derived concentrations (in ppm and molarity) of iron for all the standards, tap
water samples, and unknown samples. (Do
not forget to consider the dilution factors in your calculations.) Comment on the recovery and accuracy of the
determination, based on the challenge unknowns.
Calculate the limits of detection and quantitation of the method based
on the standard error of the intercept.
If any of your unknowns are below these limits, how should their
concentration be reported?
(2) Plot
the absorbance vs. iron concentration for the standards (including the
iron-free solution.) Use the method of
least-squares (i.e., linear
regression) to derive the Beers law equation in the form of A = m[Fe]+b. Be sure to report the calibration equation in
the Results and Abstract sections of your report. If the intercept has a non-zero value,
explain why, and comment on the R2 value.
(3) Calculate
the molar absorptivity of Fe(phen)32+ at 508 nm. Compare your value with the literature value,
11,100 M-1cm-1.
Explain possible causes for the difference, if any is observed.
(4) Comment
on whether or not the water samples meet the Federal standards for drinking
water and any differences observed between the cold and hot water from the same
tap.
Revised