The elements occurring in group 2 of the periodic table are alkaline earth metals. These elements are abundant in the earth and thus acquire this name. Group 2 elements have the dipositive oxidation state (M2+) as their primary valence. The alkaline earth metals create mainly ionic compounds but are less ionic than the equivalent alkali metal compounds. This happens because of the greater nuclear charge and smaller size. Beryllium and magnesium oxides and other compounds are more covalent than those generated by the heavier and larger components (Ca, Sr, Ba).
Let us look at the different aspects of reactivity of alkaline earth metals:
M + X2 → MX2, where X represents the halogens, including fluorine, bromine, chlorine, and iodine.
Reactivity with hydrogen
Reactivity with acids
M + 2HCl → MCl2 + H2
Acting as a reducing agent
The group, two elements of the periodic table, are known as alkaline earth metals. They possess two electrons in their valence shell. Alkaline earth metals are highly reactive elements. The behaviour of alkaline earth metals is similar to that of alkali metals. However, there are distinctions since alkaline earth metals have smaller atomic and ionic sizes and higher cationic charges. Their oxides and hydroxides are less basic than those of alkali metals.