Many alchemists already knew about hydrochloric acid. In 1774, Carl Wilhelm Scheele first produced the gaseous element at Uppsala, Sweden. He did this by heating the hydrochloric acid with the mineral pyrolusite. He observed that a dense greenish–yellow gas evolved with a choking smell. When dissolved in water to give an acid solution, he noticed that the litmus paper bleached and the leaves and flowers were decolourized. This was further investigated by Humphry Davy in 1807 and he concluded it to be not just a simple substance but truly an element. He made an announcement regarding this in 1810; but it had taken almost ten years for some chemists to accept it as an element.
As discussed earlier, Chlorine is found in combination to its compounds and hence, it is rare to find free Chlorine on the earth. The most common combination of Chlorine is with Sodium, that is, common salt. Other common combinations of Chlorine include carnallite and sylvite. Moreover, it can be obtained from chlorides through oxidizing agents and more often, by electrolysis.
Peculiar characteristics of Chlorine include:
- Chlorine has a melting point of about -100.98°C and a boiling point of about -34.6°C.
- It directly combines with almost all of the other elements and is a member of the Halogen group of elements.
- Prominently, it figures with many organic chemistry reactions, specifically in substitutions with Hydrogen.
- Its interaction in the gas form acts as an irritant for respiratory and other mucous membranes whereas its liquid form may burn the skin.
Out of the wide range of isotopes, there are two stable isotopes of Chlorine, namely 35Cl and 37Cl. Their atomic weight together is 35.45g/mol. There was some confusion in the early days of chemistry due to the half–integer value of Chlorine’s weight. However, it has been postulated that the existence of chemical isotopes were unsuspected and the atoms were composed of even units of Hydrogen. In ratio with the stable isotopes, trace amounts of radioactive 36Cl exists in the environment. The radioisotope is produced by spallation in the atmosphere of 36Ar by interactions with cosmic ray protons. In the atmosphere, the residing time of 36Cl is about one week. Hence, it is useful for dating waters less than 50 years before the present. Also, its uses can be traced in the other areas of the geological sciences, which include dating ice and sediments.
Some of the common uses of Chlorine include:
- It is commonly used for disinfecting drinking water and clean swimming pools.
- It is used in the production of textiles, paper products, dyes, petroleum products, medicines, insecticides, disinfectants, foods, solvents, plastics, paints and many other products.
- It is used in the manufacture of chlorates, carbon tetrachloride and chloroform and in the extraction of bromine.
- It was significantly utilised as a chemical warfare agent.
- Various organic chemistry processes often require Chlorine and it is commonly used as an oxidizing agent and as a substitution for Hydrogen.
As it is a highly reactive gas, Chlorine enters the body through breathing in contaminated air or consuming contaminated food or water. Chlorine affects the human respiratory system if one breathes small amounts of it for short periods of time. It irritates the skin, eyes and leads to coughing, chest pain and water retention in the lungs.