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Question

Why are alkali metals highly reactive in air?

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Solution

  • Alkali metals are highly reactive metals because of their large size and low ionization enthalpy. Their reactivity increases on moving down the group.Reactivity towards air:
  • When these metals are kept in dry air, they get tarnished due to the formation of oxides, which become hydroxides on reacting with moisture.

Alkali metals take up the leftmost side of the periodic table. The group 1 elements consist of elements:

They belong to the s-block elements of the periodic table as their outermost electron enters the s orbital giving them the electronic configuration of ns1.

As the alkali metals have only 1 electron in their valence shell, they readily lose it, making them count among the most reactive elements on earth. Thus, they are highly electropositive metals. They are called alkali metals because they form strongly alkaline hydroxides with water.


The alkali metals, found in group 1 of the periodic table (formerly known as group IA), are very reactive metals that do not occur freely in nature. These metals have only one electron in their outer shell. Therefore, they are ready to lose that one electron in ionic bonding with other elements.




Alkali metals are known for being some of the most reactive metals. This is due in part to their larger atomic radii and low ionization energies. They tend to donate their electrons in reactions and often have an oxidation state of +1. These metals are characterized as being extremely soft and silvery in color. They also have low boiling and melting points and are less dense than most elements. Li, Na, and K have the ability to float on water because of their low density. All of these characteristics can be attributed to the large atomic radii and weak metallic bonding these elements possess.

Group 1 elements have a valence electron configuration is ns1 and are good reducing agents (meaning they are easily oxidized). All of the alkali metals are found naturally in nature, but not in their pure forms. Most combine with oxygen and silica to form minerals in the Earth and are readily mined as they are of relatively low densitys and thus do not sink.


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