Salinity - Dissolved Salts, Measuring Salinity

Click for full size

A student from the HIGH TIDE project turns on the CTD instrument. High school students use the CTD recorder to measure salinity, temperature and depth of the water in the Lafayette River which is a part of Chesapeake Bay.
Click on image for full size (54K JPEG)
Image courtesy of the HIGH TIDE project
One way to measure how much dissolved salt is in water is to look at the concentration of salt in the water. Concentration is the amount (by weight) of salt in water and can be expressed in parts per million (ppm). Here are the classes of water:
  • Fresh water - less than 1,000 ppm
  • Slightly saline water - From 1,000 ppm to 3,000 ppm
  • Moderately saline water - From 3,000 ppm to 10,000 ppm
  • Highly saline water - From 10,000 ppm to 35,000 ppm

Ocean water has a salinity that is approximately 35,000 ppm. If you take 35,000/1,000,000 then you end up with 3.5%. So, ocean water is about 3.5% salt. Scientists used to report salinity in ppt (parts per thousand), but reporting salinity in ppt is obsolete now as the method of determining ocean salinity in ppt is not used anymore. Instead psu (practical salinity units) are used. Scientists measure salinity by measuring the conductivity of the water as would be measured by a CTD instrument (CTD = conductivity, temperature, depth). Using this method ocean salinity is approximately 35 psu.

Ocean water is about 3.5% salt. That means that if the oceans dried up completely, enough salt would be left behind to build a 180-mile-tall, one- mile-thick wall around the equator. About 90 percent of that salt would be sodium chloride, or ordinary table salt. What other dissolved salts are found in ocean water? The major dissolved salts of the ocean are listed in the following table:

Dissolved salts in
sea water (atoms):
55.3 % Chlorine
30.8 % Sodium
3.7 % Magnesium
2.6 % Sulfur
1.2 % Calcium
1.1 % Potassium


The HIGH TIDE project involving lower Chesapeake Bay

Salinity Versus Depth Profile for Ocean Water

The Oceans and Seas

Estuaries

A look at Chesapeake Bay

George E. Brown Jr. Salinity Laboratory - exploring soil-plant-water systems

The Salt Institute

Salinity - Dissolved Salts, Measuring Salinity

Click for full size

A student from the HIGH TIDE project turns on the CTD instrument. High school students use the CTD recorder to measure salinity, temperature and depth of the water in the Lafayette River which is a part of Chesapeake Bay.
Click on image for full size (54K JPEG)
Image courtesy of the HIGH TIDE project
When we measure the salinity of water, we look at how much dissolved salt is in the water, or the concentration of salt in the water. Concentration is the amount (by weight) of salt in water and can be expressed in parts per million (ppm). Here are the classes of water:
  • Fresh water - less than 1,000 ppm
  • Slightly saline water - From 1,000 ppm to 3,000 ppm
  • Moderately saline water - From 3,000 ppm to 10,000 ppm
  • Highly saline water - From 10,000 ppm to 35,000 ppm

Ocean water has a salinity that is approximately 35,000 ppm. That's the same as saying ocean water is about 3.5% salt. Sometimes, salinity is measured in different units. Another common unit is the psu (practical salinity units). Ocean water has a salinity of approximately 35 psu. Scientists measure salinity using a CTD instrument (CTD = conductivity, temperature, depth).

Ocean water is about 3.5% salt. That means that if the oceans dried up completely, enough salt would be left behind to build a 180-mile-tall, one- mile-thick wall around the equator. About 90 percent of that salt would be sodium chloride, or ordinary table salt. Chlorine, sodium and the other major dissolved salts of the ocean are listed in this table:

Dissolved salts in
sea water (atoms):
55.3 % Chlorine
30.8 % Sodium
3.7 % Magnesium
2.6 % Sulfur
1.2 % Calcium
1.1 % Potassium


The HIGH TIDE project involving lower Chesapeake Bay

Salinity Versus Depth Profile for Ocean Water

The Oceans and Seas

Estuaries

A look at Chesapeake Bay

George E. Brown Jr. Salinity Laboratory - exploring soil-plant-water systems

The Salt Institute

Salinity - Dissolved Salts, Measuring Salinity

Click for full size

A student from the HIGH TIDE project turns on the CTD instrument. High school students use the CTD recorder to measure salinity, temperature and depth of the water in the Lafayette River which is a part of Chesapeake Bay.
Click on image for full size (54K JPEG)
Image courtesy of the HIGH TIDE project
Salinity is the measure of how much salt is in water. Ocean water has a high salinity and fresh water has a very low salinity.

Sometimes, salinity is measured in parts per million (ppm). Ocean water has a salinity that is about 35,000 ppm. That's the same as saying ocean water is about 3.5% salt. Sometimes, salinity is measured in different units. Ocean salinity is also about 35 psu (practical salinity units).

Ocean water has a lot of salt in it. Most of it is normal table salt (made up of chlorine and sodium). Chlorine, sodium and the other major dissolved salts of the ocean are listed in the following table:

Dissolved salts in
sea water (atoms):
55.3 % Chlorine
30.8 % Sodium
3.7 % Magnesium
2.6 % Sulfur
1.2 % Calcium
1.1 % Potassium


The HIGH TIDE project involving lower Chesapeake Bay

Salinity Versus Depth Profile for Ocean Water

The Oceans and Seas

Estuaries

A look at Chesapeake Bay

George E. Brown Jr. Salinity Laboratory - exploring soil-plant-water systems

The Salt Institute


Last modified June 2, 2002 by the Windows Team

The source of this material is Windows to the Universe, at http://www.windows.ucar.edu/ at the University Corporation for Atmospheric Research (UCAR). © The Regents of the University of Michigan. Windows to the Universe® is a registered trademark of UCAR. All Rights Reserved. Site policies and disclaimer