Vernier Software and Technology
Vernier Software & Technology

Chloride and Salinity



Chloride, in the form of the Cl ion, is one of the major inorganic anions, or negative ions, in saltwater. Chloride ions come from the dissociation of salts, such as sodium chloride or calcium chloride, in water.

Cannot create image: \text{NaCl(s)} \to \text{Na}^{+}\text{(aq)} + \text{Cl}^{-}\text{(aq)} Cannot create image: \text{CaCl}_{2}\text{(s)} \to \text{Ca}^{2+}\text{(aq)} + \text{2 Cl}^{-}\text{(aq)}

These salts, and their resulting chloride ions, can originate from natural sources such as saltwater intrusion, or manmade sources such as road salts and water softeners. Even water considered to be fresh often contains salt ions. Compared to seawater or brackish water however, freshwater has much lower levels of salt ions such as Na+ and Cl; in fact, these ions are often lower in concentration than hard-water ions such as calcium (Ca2+) and bicarbonate (HCO3). Due to this variable ratio of ions, an ion-selective electrode is commonly used to specifically measure chloride ion concentration.


Salinity is a measure of all salts dissolved in water, commonly expressed in parts per thousand, ppt. Unlike chloride concentration, salinity is a measure of the total salt concentration, comprised mostly of Na+ and Cl ions in saltwater and brackish water. Even though there are smaller quantities of other ions in seawater (e.g., K+, Mg2+, or SO42–), sodium and chloride ions represent about 91% of all seawater ions. The salinity of seawater is fairly constant, at about 35 ppt, while brackish estuaries may have salinity levels between 1 ppt and 10 ppt.

Increased salinity has been observed in the lower reaches of the Colorado and Rio Grande rivers due to return of irrigation water. In these arid regions of the United States, water readily evaporates during irrigation, resulting in high concentrations of salt ions in the water that returns to the rivers.

Salinity is also of interest in bodies of water where seawater mixes with freshwater, since aquatic organisms have varying abilities to survive at different salinity levels. Many saltwater organisms survive in a salinity of up to 40 ppt, yet many freshwater organisms cannot live above 1 ppt.

Salinity is commonly determined by measuring the electrical conductance of the water. Since most anions in seawater or brackish water are chloride ions, salinity of those types of water can also be determined from chloride concentration using the following formula:

salinity (ppt) = 0.0018066 × Cl (mg/L)

This conversion is not valid for freshwater or low-saline brackish water due to the varying concentrations of chloride ions compared to other types of ions in the water.


  • Measure the chloride ion concentration in a stream or lake using a Chloride Ion-Selective Electrode.
  • Measure the salinity value of the water (in ppt) using a Conductivity Probe.

Sensors and Equipment

This experiment features the following Vernier sensors and equipment.

Additional Requirements

You may also need an interface and software for data collection. What do I need for data collection?

Standards Correlations

See all standards correlations for Water Quality with Vernier »

Water Quality with Vernier

See other experiments from the lab book.

4Total Solids
5Dissolved Oxygen
6Biochemical Oxygen Demand
10Ammonium Nitrogen
12Total Dissolved Solids
13Calcium and Water Hardness
14Total Water Hardness
15Chloride and Salinity
16Stream Flow
17Physical Profile of a Lake
18PAR Attenuation in Water

Experiment 15 from Water Quality with Vernier Lab Book

<i>Water Quality with Vernier</i> book cover

Included in the Lab Book

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Dev Reference: VST0366

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