CVEN 3454/5404 Water Chemistry
Lab 2: Carbonate
Alkalinity Determination
Purpose
The purposes of today's laboratory are to (1) understand the
acid-base chemistry behind the carbonate alkalinity measurement and (2) to accurately
measure the alkalinity of three Lefthand Creek watershed water samples.
Materials
- pH meter (Orion, model 250A or 290A)
- pH electrode (Orion Triode® model
9107BN) and electrode stand
- pH buffers (4.01 and 7.00)
- stir plate, stir bars, beakers, 50 mL burette,
stand
- sodium
bicarbonate solution (NaHCO3; about 0.2 mM; exact concentration
will be provided)
- sulfuric acid solution of unknown concentration
(H2SO4; about 0.001 M, or 0.002 N)
- water samples
1. Lefthand Creek (about 40 m upstream of the Big Five Tunnel drainage)
2. Lefthand Creek (about 40 m downstream of the Big Five Tunnel drainage)
3. Big Five Tunnel Drainage (at entrance to Lefthand Creek)
Procedure
- Calibrate your pH meter with pH 4.0 and 7.0 standards.
Remember to
make sure that the auto-shutoff feature has been turned off (press 2nd+setup,
press yes
down to setting 1-4, press down arrow
to change the setting to "no", press yes
to go to setting 2-1, press measure
to return to measurements).
- In the first titration, we'll determine the exact concentration of the
sulfuric acid titrant solution (about 0.001 M) by titrating the sodium
bicarbonate standard.
a. Fill the titration burette with the
sulfuric acid titrant.
b. Add 100 mL (know the exact volume) of the sodium bicarbonate solution
to a beaker and add a stir bar.
c. Arrange the beaker on the stir plate and insert the pH electrode into
the beaker.
d. Titrate the bicarbonate solution with the titrant with additions ranging from 0.5 to 2.0 mL.
e. Monitor pH as a function of volume of titrant added until pH reaches
about 3.
f. Use the Lab 2 spreadsheet to create a graph of pH versus volume of
titrant added to show your progress.
- In the next three titrations, we will use the
sulfuric acid titrant to determine the carbonate alkalinity of three water
samples from Lefthand Creek and the Big Five Tunnel drainage. Follow the
titration directions listed above, but substitute the water samples for the
sodium bicarbonate solution (with the exception that the sample volume should
be 50 mL instead of the 100 mL for the sodium bicarbonate). These titrations will be relatively quick
(i.e., low titrant volumes). Recall that
water samples with pH values below the carbonate alkalinity endpoint (the pH
at which {H+} = {HCO3-}) have negative
alkalinity, and the alkalinity can be determined from using these titrations,
too.
Determining the Endpoint using the Gran Function
The Gran function can be used to determine the end point of the
carbonate alkalinity determination more precisely than other methods (e.g., a fixed pH
value, an color indicator like methyl orange). Here's a quick review of the Gran
function along with an application
of it to a set of data gathered by the TAs.
The Gran function is a measure of the number of moles of H+
added to the solution after the end point has been reached:
excess moles H+ added = F1 = (Vorig
+ Vtitr) {H+} = (Vorig + V) (10-pH)
(1)
where F1 is the Gran function,
Vorig is
the original volume of the sample solution (mL), Vtitr is the volume of acid
titrated into the
solution (mL), and {H+} is the activity of protons.
| Use
the Lab 2 spreadsheet to create a graph of the Gran
function (F1)
versus the titrant volume (Vtitr). At
a certain point along the x-axis, F1 will increase rapidly. These are the data
points measured after the endpoint, where the acid added is no longer titrating carbonate
species. Instead, the added acid is decreasing the pH directly.
Make a linear regression
of these points with F1 > 0 and determine where the linear regression crosses the x-axis (where
y = 0). The point at which the linear regression crosses the x-axis is called
Vend,
the end-point volume that you are seeking.
The following
figure contains an example using some data gathered by the TA for the titration of 2.00 mM
NaHCO3. The top graph shows the titration curve -- you can see that it would
difficult to pick out the end point just from the titration curve because the slope is not that
steep where you would expect the end point (near pH 4 to 5).
The bottom graph shows the
plot of the Gran function vs. the volume of titrant added. The linear regression line passes
through the x-axis at Vend = 9.40 mL, so that is the end point. |
 |
Lab Technique Note
As you may have noticed last week, titrations are not very exciting.
However, a little perseverance and a some patience will produce some good data. If you
have good data, answering the lab report questions will be much easier. Patience is a very
important quality for anyone doing research in the lab. Once recent Nobel Prize winner
in Biology who
worked on the genetic make-up of flies said that 90% of his experiments were failures!
Questions to Address in Lab Report
- (results) Show the titration curve (pH versus
volume) and Gran function curve (F1 versus volume) for the bicarbonate standard.
Show the Gran endpoint on both graphs.
- (results) What was the molar concentration of the H2SO4
titrant solution?
- (results) Show the titration curves and Gran
function curves for the three samples. Show the Gran endpoints on all
graphs.
- (results) What were
the endpoint volumes and alkalinities (in
molar concentration and as mg L-1 CaCO3) of the three Lefthand
Creek water samples? Show the equation used to make these
calculations (use an Equation Editor). Present these data
in a table (with columns of endpoint volume, alkalinity (M), alkalinity (mg L-1
CaCO3)) for each sample.
- (discussion) Based on the pH and alkalinities you measured in the
Lefthand Creek samples (not the Big Five Tunnel sample), estimate the concentrations of the various carbonate species (carbonic
acid, bicarbonate, carbonate). Assume that the Lefthand Creek water is
closed to the atmosphere. Present these calculated concentrations
in a second table.
- (discussion) What other weak acids might contribute to alkalinity in
the watershed samples?
- (discussion) Does the alkalinity measured for
the Lefthand Creek sample taken downstream of Balarat Gulch make sense
(i.e., as a mixture of upstream Lefthand Creek and the Big Five Tunnel
drainage water)? If
so, calculate the relative flows of the Lefthand Creek (upstream) and the
Big Five Tunnel Drainage (i.e., determine the ratio QLefthand/QBig
Five).
Last updated on
July 31, 2007 at
07:18 AM by
Joe Ryan