|
Sea Water
This electrolyte has the virtue of high conductivity
making
electrochemical tests a natural choice. In-situ testing has the advantage of allowing the
natural bio-film to form. The Field Machine is used in this case to monitor galvanic
currents
Tafel slopes
LPR and AC Impedance. In the laboratory the same tests are
undertaken with the Gill range
possibly using man-made sea water. Laboratory testing is
usually short term with the advantage that specific environmental conditions can be
controlled. The disadvantage of laboratory testing is that the actual service environment
and conditions are not being evaluated. The special case of coated samples in sea water
relies on testing with AC impedance to overcome the paint resistance and 'look through' to
the metal surface. Galvanic coupling in seawater systems can be a problem
the use of
multiple electrode tests can help diagnose this. As an example consider the test rig below
connected to a GalvoGill 12 for testing torpedo parts in seawater.

The effect of temperature in real seawater is not as straightforward as
with industrial electrolytes. As a general rule the corrosion rate in seawater increases
as the temperature is increased. This rule holds true when only the effect of temperature
on the corrosion rate is considered. However
other variables such as oxygen concentration
and biological activity must be accounted for. The solubility of oxygen decreases as
temperature is increased. Biological activity generally increases with increasing
temperature
and calcareous deposits and other protective scales are also more likely to
form/deposit on metal surfaces at higher temperatures. The preferred environment for
laboratory testing is natural seawater
but synthetic seawater is often used. Natural
seawater is fresh water piped straight to the laboratory
once it is removed from it's
natural environment and stored in bowsers the composition changes and this can have a
large impact on the resultant metal corrosion rate. Synthetic seawater solutions that are
typically used include 3.5 wt.% sodium chloride and ASTM D 1141 substitute ocean water
mix. The results from this synthetic seawater may not be the same as for real fresh
seawater. One advantage of using the easily made up 3.5% NaCl is that calcareous deposits
will not form under cathodic polarisation conditions in the solution. Although seawater
has high electrical conductivity there are cases when the IR drop should be considered. In
systems with large current flow
such as testing sacrificial anode material
the I
component could be of the order of Amps. Even with an R component of say
100 mOhm
this
would lead to a drop of 100s of mV between RE and WE. This may be minimised by good cell
geometry and compensated for by using IR compensation after measuring the drop with AC
Impedance.
|