Seawater is often called salt water but it contains various different salts. In this experiment you will separate some of these salts from the mixture.
This experiment is a simple one to carry out and is designed to show that seawater contains a mixture of different salts. It can be used in conjunction with Earth Science topics linked to the conveyance of mineral salts into the sea via rivers.
This experiment could be carried out early in a science course while using scientific apparatus is still a novelty, because it provides practice at using a variety of equipment and also introduces the concept of a mixture and some simple chemical tests. It is also an opportunity to reinforce safety messages eg wearing eye protection throughout and activity and the need to keep standing up.
The experiment can be carried by groups of two or three and will take about one hour to complete.
Beaker (250 cm3)
Beaker (100 cm3)
Conical flask (100 cm3)
Heat resistant mat
Seawater, 200 cm3(Note 1)
Access to hydrochloric acid, 1 M
Refer to Health & Safety and Technical notes section below for additional information.
Health & Safety and Technical notes
Wear eye protection throughout. Take care with hot apparatus and solutions.
Hydrochloric acid, HCl(aq) - see CLEAPSS Hazcard and CLEAPSS Recipe Book.
Limewater, Ca(OH)2(aq), (treat as IRRITANT) - see CLEAPSS Hazcard and CLEAPSS Recipe Book.
Calcium sulfate, hydrated, CaSO4.2H2O(s) - see CLEAPSS Hazcard.
Sodium chloride, NaCl(s) - see CLEAPSS Hazcard.
1 Although it is tempting to use genuine seawater if available, this experiment is usually more successful if the seawater is generated artificially. Genuine seawater will not always yield a full range of solids in sufficient quantities to be detected. Artificial seawater can be generated by adopting the following procedure:
- Bubble carbon dioxide through a mixture of 250 cm3 limewater plus 750 cm3 deionised water for about 20 minutes or until the cloudy precipitate disappears completely.
- Add as much solid hydrated calcium sulfate as will dissolve.
- Add about 15 g of sodium chloride.
- Stir until all the solid has dissolved, leave to settle and then decant or filter the liquid if necessary.
a Place 200 cm3 of seawater in a 250 cm3 beaker.
b Heat and boil the seawater.
c Stop heating when about 60-70 cm3 of liquid remains. Solid will be precipitated during this evaporation process.
d Allow to cool and for any solids to settle.
e Pour the clear liquid into the 100 cm3 beaker, leaving the solids behind.
f Add a few drops of hydrochloric acid to the solids left behind and observe what happens.
g Put the 100 cm3 beaker on the tripod and gauze and heat the liquid until another solid appears. This will occur when about 30-40 cm3 of liquid remains.
h Carefully filter the liquid into the conical flask.
i Wash out the 100 cm3 beaker and pour the filtrate into an evaporating basin (or beaker if the volume is too high)
j Boil the liquid yet again until there is almost none left. When a small crust of solid starts to form at the edge of the basin, turn off the Bunsen burner. Then, either allow the remaining water to evaporate at room temperature or place the basin on a beaker half full of water (a steam bath). Heat the beaker with a Bunsen and allow the remaining water in the basin to evaporate gently.
Safety note; there is a risk of tiny crystals of hot solid spitting out. Eye protection is essential at this stage.
k Let it cool and note what is observed.
Encourage the students to write down what they observe at each stage.
Teachers may wish to mark 250 cm3 beakers at the 60 cm3 level if there are no gradations already present.
The artificial seawater contains calcium hydrogen carbonate owing to the reaction of limewater with excess carbon dioxide:
Ca(OH)2 (aq) + 2CO2(g) → Ca(HCO3)2(aq)
When this solution is boiled it soon precipitates calcium carbonate:
Ca(HCO3)2(aq) → CaCO3(s) + CO2(g) + H2O(l)
This is the identity of the predominant solid first left behind when the liquid is boiled. However, some calcium sulfate will also be present.
When hydrochloric acid is added to this solid, students should observe effervescence (fizzing), since the calcium carbonate is producing carbon dioxide gas:
CaCO3(s) + 2HCl(aq) → CaCl2(aq) + CO2(g) + H2O(l)
The solid which continuously crystallises out on further evaporation is sparingly soluble calcium sulfate, which is the predominant solid filtered off when 30 cm3 of sea water remains.
The more soluble sodium chloride precipitates out during the final stages of evaporation.
Here are some questions for students.
a What evidence is there that seawater is a mixture of salts?
b What gas is likely to have been evolved when hydrochloric acid is added to the solids first collected?
c What does this tell you about the identity of these solids?
d Research the web to try to find information about the solubilities of sodium chloride and calcium sulfate – two common compounds present in seawater. Use this information to predict the possible identity of the very last solid left at the end of your experiment.
Health & Safety checked, 2016
This Practical Chemistry resource was developed by the Nuffield Foundation and the Royal Society of Chemistry.
© Nuffield Foundation and the Royal Society of Chemistry
Page last updated February 2016
This is a resource from the Practical Chemistry project, developed by the Nuffield Foundation and the Royal Society of Chemistry. This collection of over 200 practical activities demonstrates a wide range of chemical concepts and processes. Each activity contains comprehensive information for teachers and technicians, including full technical notes and step-by-step procedures. Practical Chemistry activities accompany Practical Physics and Practical Biology.