Introduction

Method overview

Alkalinity is the measure of how much acid it takes to lower the pH of a water sample enough to convert all bicarbonate (HCO₃^–) and carbonate (CO₃^2–) to carbonic acid (H₂CO₃). Although total alkalinity is equal to the stoichiometric sum of all bases in solution, not just carbonates, ~97% of alkalinity in typical seawater is due to carbonates.

Note that this method should only be used on interstitial water (IW) squeezed from the core material by the titanium squeezers. The RHIZON samplers alter the pH and alkalinity of the IW samples and should not be analyzed for alkalinity or pH.

Method theory

To measure alkalinity, a pore water sample is titrated with an acid to an endpoint at which carbonate is converted to bicarbonate and bicarbonate is converted to carbonic acid. In seawater, this endpoint occurs at about pH = 4.2.

H⁺ + CO₃^2– = HCO₃^–

H⁺ + HCO₃^– = H₂CO₃

The alkalinity determination in this method (Gran titration) relies on a mathematical evaluation of the second equivalence point of carbonate titration in seawater using the most stable part of the titration curve (i.e., the part beyond the equivalence point on the low pH side). In essence, the Gran method linearizes the titration curve by means of a simple function:

F = (v + V₀) × 10^E/A,

where:

F = Gran factor,

v = volume of acid added to the solution in the titration vessel,

V₀ = original volume of the sample,

E = EMF (millivolts) at v, and

A = slope of electrode determined on the basis of the electrode calibration.

Generally, the slope is ~59 mV at 25°C. Slope is determined during calibration (see Calibrating the electrode)

The function F, when plotted as a function of the volume of acid added (v), is linear when sufficiently removed from the equivalence point. We measure mV instead of pH to determine the endpoint because this method offers better precision. The optimum range of millivolts for linearity is 220–240 mV. The value of v at F = 0 is the equivalence point from which the alkalinity is evaluated.

The slope of the F vs. v plot changes with variations in the sulfate content of the samples. This is because at lower pH values the following reaction

H⁺ + SO₄^2– = HSO₄^–

plays an important role in establishing the pH of the solution through a buffering effect. This change in slope, however, has no effect on the Gran extrapolation intercept with the y-axis and is not accurate enough to estimate sulfate concentrations.

Reagents

- IAPSO standard seawater (alkalinity ~2.325 mM)

- Potassium chloride (KCl)

- Borax (Na₂B₄O₇·10H₂O)

- Sodium bicarbonate (NaHCO₃)

- Sodium carbonate (Na₂CO₃)

Reagent solutions

- 0.1 M HCl solution (premade from Fisher, AMS# CH5009)

- 0.7 M KCl solution (52 g KCl in 1 L reagent water)

Stock standard solutions (1 L)

- 0.1 M borax solution (38.1 g borax in 1 L reagent water)

- 0.5 M NaHCO₃ (42 g sodium bicarbonate in 1 L reagent water)

- 0.1 M Na₂CO₃ (10.6 g sodium carbonate in 1 L reagent water)

- 0.5 M Na₂CO₃ (53.0 g sodium carbonate in 1 L reagent water)

Standard solutions (100 mL)

- 5 mM alkalinity (pipet 2.5 mL 0.1 M Na₂CO₃ into 97.5 mL 0.7 M KCl)

- 20 mM alkalinity (pipet 10 mL 0.1 M Na₂CO₃ into 90 mL 0.7 M KCl)

- 40 mM alkalinity (pipet 20 mL 0.1 M Na₂CO₃ into 80 mL 0.7 M KCl)

- 50 mM alkalinity (pipet 10 mL 0.5 M NaHCO₃ into 90 mL 0.7 M KCl)

- 100 mM alkalinity (pipet 10 mL 0.5 M Na₂CO₃ into 90 mL 0.7 M KCl)

Main instrument panel

Instrument calibration

To ensure accuracy of sample measurements, the titrator settings must be optimized. Calibration of the system includes calibrating the electrode, selecting a dispensing rate program and calculating a standard ratio.

Calibrating the electrode

Before the titrator can be used to measure samples, the electrode must be calibrated against pH buffers in the range expected in samples. Generally, calibration at pH 4, 7 and 10 covers the necessary range.

Select Calibrate Electrodes from the main Alkalinity interface.
Enter your range of buffers (4, 7, 10).
Select your Drift Span. The default drift span is 30.
Place 3 mL of the first buffer solution in the vessel. Add stir bar and immerse electrode in vessel.
Select Cal 1 and then Start.
When finished, clean vessel and the electrode.
Repeat steps 4–6 with each calibration buffer, selecting Cal2 and Cal3 when appropriate.
When all three buffers have been run, select OK-Save to save the calibration.
Dispensing rate
The rate at which the titrator dispenses the acid into the sample can be adjusted according to the expected alkalinity value. Higher alkalinities may require faster dispensing rates. The dispensing rate can be selected from a list of predetermined programs, or a new dispensing rate program can be created.
Select Edit Rates from the main alkalinity interface.

Standard ratio
Calculating the standard ratio (estimated vs. actual alkalinity, “fudge factor”) for the anticipated range of alkalinity values accounts for measurement error in acid strength. Standard ratio can be calculated using borax solution, sodium bicarbonate solution, or IAPSO standard seawater, as necessary, to most closely match alkalinity values (within 5 mM, to preserve the first-order transfer function) of the unknown samples. Generally, IAPSO standard seawater is used to establish this ratio, and additional calibration standards are used if samples deviate >5 mM from the alkalinity of IAPSO (~2.325 mM). The measurement is repeated until at least 3 consistent measurements are obtained within 5% of actual value for each standard:
-         IAPSO = 2.21–2.44 mM
-         20 mM standard = 19–21 mM
-         40 mM standard = 38–42 mM
To start creating a standard ratio, select STANDARDS from the main alkalinity interface.

Place 3 mL of standard in vessel. Add stir bar and immerse electrode in vessel.
Select Continue.
Click START.
Insert the acid dispensing probe when prompted.
When finished, clean vessel and electrode. Repeat steps 1–4 until you have at least three consistent measurements per standard.

Now go to the STND Manager, selected from the main alkalinity interface.

Select the three measurements (or however many were done in the prior step) and click Average.
The window to the right shows the next step to which you can save the new ratio to a new name or replace a prior name. Usually we save as a new ratio (e.g. 371_13august). The window showing the name creation is not shown.
Click Done.

To select a standard ratio for subsequent measurements go to Setup in the main alkalinity interface.

This window also shows where to set the path to the datalog file, the default setting for the Drift Span, and where to select the standard ratio correction.

To select a saved standard ratio, double-click on a value in the list.

Measuring samples

The system is now calibrated, dispensing rates selected (generally start with the slowest rate, assuming that alkalinity will be around the value of IAPSO) and standard ratio selected (again, generally start with the IAPSO standard ratio and adjust accordingly to what is measured in the samples).

Select SAMPLE from the main alkalinity interface.

Select the sample (IWS) from the LIMS database. Use the tree or type in the Text_ID in the appropriate field.

Place 3 mL of standard in vessel. Add stir bar and immerse electrode in vessel.
Select Continue.
Click START.
The first measurement that the system measures, is sample pH. Record the value in the blue book.
Insert the acid dispensing probe when prompted.
When the titration is complete, a window appears to let you know that the analysis is complete. Click Ok.
A Gran-Method window appears with results of the titration. Write the Alkalinity Cor value in the blue book. This is the result with the standard ratio applied to it. Click Ok/Save. This will upload the result to LIMS assuming the MUT uploader is active.

When finished, clean vessel and the electrode.
Click Ok/Save to save the results to the LIMS database. The value saved to LIMS and the value you need to note in the blue book is the “Alkalinity Cor” value. This is the value with the standard ratio applied to it.

Page tree

Autotitrator pH/Alkalinity: Quick Start Guide