Submitted by Editor
|6.||Materials and Equipment|
This is to certify that the Project titled 'Saturated solutions: Measuring Solubility' was completed under my guidance and supervision by Roll
No. _________ a student of XII SCI, Faith
Academy within the stipulated time as prescribed by
Mrs. Sasheela Jose Head, Department of Chemistry
Faith Academy New Delhi
I gratefully acknowledge my sincere thanks to our respected chemistry teacher Mrs.Sasheela Jose for her remarkable, valuable guidance and supervision throughout the project work. I'm also most indebted to Mrs.Rao for her encouragement, help, suggestion and readily helpful service in performing the experiment.
Parichay Saxena Roll NO :
The goal of this project is to measure the solubilities of some common chemicals:
A good part of the substances we deal with in daily life, such as milk, gasoline, shampoo, wood, steel and air are mixtures. When the mixture is homogenous, that is to say, when its components are intermingled evenly, it is called a solution. There are various types of solutions, and these can be categorized by state (gas, liquid, or solid).
The chart below gives some examples of solutions in different states. Many essential chemical reactions and natural processes occur in liquid solutions, particularly those containing water (aqueous solutions) because so many things dissolve in water. In fact, water is sometimes referred to as the universal solvent. The electrical charges in water molecules help dissolve different kinds of substances. Solutions form when the force of attraction between solute and solvent is greater than the force of attraction between the particles in the solute.
Two examples of such important processes are the uptake of nutrients by plants, and the chemical weathering of minerals. Chemical weathering begins to take place when carbon dioxide in the air dissolves in rainwater. A solution called carbonic acid is formed. The process is then completed as the acidic water seeps into rocks and dissolves underground limestone deposits. Sometimes, the dissolving of soluble minerals in rocks can even lead to the formation of caves.
If one takes a moment to consider aqueous solutions, one quickly observes that they exhibit many interesting properties. For example, the tap water in your kitchen sink does not freeze at exactly 0°C. This is because tap water is not pure water; it contains dissolved solutes. Some tap water, commonly known as hard water, contains mineral solutes such as calcium carbonate, magnesium sulfate, calcium chloride, and iron sulfate. Another interesting solution property is exhibited with salt and ice.
Another example comes from the fact that salt is spread on ice collected on roads in winters. When the ice begins to melt, the salt dissolves in the water and forms salt water. The reason is that with the adition of salt the melting point of water increases and as aresult the snow melts away faster.
Even some organisms have evolved to survive freezing water temperatures with natural "antifreeze." Certain arctic fish have blood containing a high concentration of a specific protein. This protein behaves like a solute in a solution and lowers the freezing point of the blood. Going to the other end of the spectrum, one can also observe that the boiling point of a solution is affected by the addition of a solute. These two properties, namely freezing-point depression and boiling-point elevation, are called colligative properties (properties that depend on the number of molecules, but not on their chemical nature).
A saturated solution is a mixture in which no more solute can be practically dissolved in a solvent at a given temperature. It is said practical because theoretically infinite amount of solute can be added to a solvent, but after a certain limit the earlier dissolved solute particles start rearranging and come out at a constant rate. Hence overall it appears that no solute is dissolved after a given amount of solute is dissolved. This is known as a saturated solution.
In an unsaturated solution, if solute is dissolved in a solvent the solute particles dissociate and mix with the solvent without the re-arrangement of earlier dissolved solute particles.
Solubility depends on various factors like the Ksp of the salt, bond strength between the cation and anion, covalency of the bond, extent of inter and intramolecular hydrogen bonding, polarity, dipole moment etc. Out of these the concepts of H-bonding, covalency, ionic bond strength and polarity play a major role if water is taken as a solvent.
Also physical conditions like temperature and pressure also play very important roles as they affect the kinetic energy of the molecules.
Materials and Equipment
To do this experiment following materials and equipment are required:
1. Measure 100 mL of distilled water and pour into a clean, empty beaker or jar.
2. Use the kitchen balance to weigh out the suggested amount (see below) of the solute to be tested.
a. 50 g Non-iodized table salt (NaCl)
b. 50 g Epsom salts (MgSO4)
c. 250 g Sugar (sucrose, C12H22O11)
3. Add a small amount of the solute to the water and stir with a clean disposable spoon until dissolved.
4. Repeat this process, always adding a small amount until the solute will no longer dissolve.
5. Weigh the amount of solute remaining to determine how much was added to the solution.
6. Try and add more solute at the same temperature and observe changes if any.
7. Now heat the solutions and add more solute to the solutions.
|Salt||Amount of salt dissolved in 100mL water to make saturated solution.||Moles dissolved|
|NaCl (Non-iodized||36.8 grams||0.7|
|C12H22O11 (sucrose)||51.3 grams||0.15|
Adding more solute at the same temperature to the saturated solutions yielded no significant changes in NaCl and Epsom salt. Howerver at all temperatures the saturation point of sucrose could not be obtained exactly as due to the large size of the molecule the solution became thick and refraction was more prominent. Neglecting this observation in the room for error, the experiments agreed with the theory.
Adding more solute to heated solutions increased the solubility in all the 3 cases. The largest incrrease was shown by NaCl, followed by Epsom salt and sucrose. These facts too agreed with the theory as at high temperatures the kinetic enery of molecules increases and the collisions are more effective.
The solubility of NaCl is the highest as it an ionic salt and easily dissociates in water. Also since the size of both the cation and
anion are small, the collisions are more and hence probability of dissociation is high. The solubility of MgSO4 is also high as it is also an ionic salt, but due to a larger anion, collisions are not
very effective. The solubility of C12H22O11 is the least as it a very large molecule due to which hydrogen bonding with the water
molecules is not very effective. Also due to the large number of carbon and oxygen atoms, inter molecular H-bonding is more dominant than intramolecular H-bonding.
Solution of NaCl (actual photo)
^ 5. Epsom salt should be first dried in order to remove the water of crystallization (MgSO4.7H2O).
The saturated solutions of NaCl, MgSO4 and C12H22O11 were made and observed. The observations agreed with the related theory within the
range of experimental error.
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