Conductivity (Total Dissolved Solids)
an excerpt from our April
2004 Newsletter
What is Conductivity?
Conductivity is the ability to conduct electricity. Water conducts electricity
because it contains dissolved solids that carry electrical charges.
For example, chloride, nitrate, and sulfate carry negative charges,
while sodium, magnesium, and calcium carry positive charges. These dissolved
solids affect the waters ability to conduct electricity. Therefore,
measuring the conductivity of the water indirectly indicates the amount
of Total Dissolved Solids (TDS) in the water.
Why is it important?
Most streams have a fairly constant range of conductivity under normal
circumstances. Therefore, significant changes in conductivity can be
an indicator that a discharge or some other source of pollution has
entered the water. The composition of the water can be critical for
aquatic organisms as well, as many critters have very specific ranges
that they can tolerate.
How do we measure Conductivity?
Stream Team uses a conductivity meter that applies voltage between two
electrodes. The drop in voltage between the two electrodes is used to
measure the resistance in the water, which is converted into conductivity.
What factors affect
Conductivity?
Conductivity can be affected by many factors. Examples include:
The addition of fresh water
(rain) lowers conductivity because rainwater has low conductivity
and the increase in water levels dilutes mineral concentrations. Conversely,
during low flow conditions (summer and fall) the dissolved solids
are more concentrated and therefore conductivity levels are higher.
Conductivity is affected by temperature: the warmer the water,
the higher the conductivity.
Soil and rocks release dissolved solids into the waters that
flow through or over them. Therefore, the geology of a certain area
will determine the conductivity.
In coastal streams or estuaries, salt water often mixes with
fresh water. The addition of salt water greatly increases conductivity.
What are expected
Conductivity levels?
According to the California State Water Resources Control Board, typical
conductivity ranges are:
Distilled Water: 0.5 to 3.0 mS
Melted Snow: 2 to 42 mS
Drinking Water: 30 to 1500 mS
Freshwater Streams: 100 to 2000 mS
Stream Team Conductivity results
Here in the Santa Barbara/Ventura area, our coastal mountains are formed
from easily eroded marine sediments. Therefore, conductivity in our
local streams is usually above 1000 mS,
and can be as high as 3000 or even 4000 mS.
The highest result we have ever seen was 8280 mS,
this was at San Jose Creek in Goleta (site
SJ1) in January 2004.
One very interesting thing to note is that heavy rain seems to have
very different effects in Ventura and Goleta. In Goleta, heavy rain
greatly lowers conductivity, whereas in Ventura, heavy rain seems to
increase conductivity levels. This is very interesting, and will require
more investigation!