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Melting and boiling points

The alkaline earth metals have higher melting and boiling points as compared to those of alkali metals which is attributed to their small size and more close packed crystal lattice as compared to alkali metals and presence of two valence electrons.

Heat of Hydration

The heats of hydration of M2+ decreases with an increase in their ionic size and their values are greater than that of alkali metal ions.

Alkaline earth metal ions, because of their larger charge to size ratio, exert a much stronger electrostatic attraction on the oxygen of water molecule surrounding them.

Since the alkaline earth metals (except Be) tend to lose their valence electrons readily, they act as strong reducing agents as indicated by E0 red values. The particularly less negative value for Be arises from the large hydration energy associated with the small size of Be2+ and the relatively large value of heat of sublimation.

 
Solubility

Basic nature of oxides increases down the group but solubilities of sulphates and carbonates decrease as ionic size increases.

The solubility of most salts decreases with increased atomic weight, though usual trend is reversed with fluorides and hydroxides in this group.

 

Physical Properties of groups 2 elements (alkaline earth metals)

Property
Elements
Be
Mg
Ca
Sr
Ba
Ra
Atomic number
4
12
20
38
56
88
Atomic mass
9.01
24.31
40.08
87.62
137.33
226.03
Metallic radius/pm
112
160
197
215
222
-
Ionic radius/pm
51
72
100
118
135
148
Ionization enthalpy (kJ mol-1)
I
899
737
590
549
503
509
II
1757
1450
1146
1064
965
979

Enthalpy of hydration of M2+ ions (kJ mol-1)

-2494
-1921
-1577
-1443
-1305
-
Electronegativity
(Pauling Scale)
1.57
1.31
1.00
0.95
0.89
0.9
Density/g mol- at 298 K
1.85
1.74
1.55
2.63
3.62
5.5
Melting Point/K
1562
924
1124
1062
1002
973
 
Boiling point /K
2745
1363
1767
1655
2078
(1973)
(uncertain)
E°(V) at 298 K for
M2+(aq) + 2e-  M(s)
-1.97
-2.37
-2.87
 
-2.89
-2.90
-2.92
Occurrence in Lithosphere
2*
2.76**
4.6**
384*
390*
10-10**
 
* ppm (parts per million)   ** Percentage by weight
 
Reactivity and Electrode potential

All the alkaline earth metals are highly reactive elements since they have a strong tendency to lose the two valences s-electrons to form the corresponding dipositive ions having inert gas configuration. The high reactivity arises due to their low ionization energies and high negative values of their standard electrode potentials. Further, the chemical reactivity of alkaline earth metals increase on moving down the group because the I.E. decreases and electrode potentials become more and more negative with increasing atomic number from Be to Ra. Thus, beryllium is the least reactive while Ba (or Ra) is the most reactive element. Further since the ionization energies of alkaline earth metals are higher and their electrode potential is less negative than the corresponding alkali metals. They are less reactive than corresponding alkali metals.

 
Reducing Character

The alkaline earth metals are weaker reducing agents than the alkali metals. Like alkali metals, their reducing character also increases down the group. This is due to the reason that the alkaline earth metals have greater tendency to lose electrons so, they act as reducing agent but since their I.E. are higher and their electrode potentials are less negative than the corresponding alkali metals, therefore alkaline earth metals are weaker reducing agents than alkali metals. The sulphates are stable to heat whereas the carbonates decompose to give MO and CO2, the temperature of decomposition increasing from Mg to Ba. BeCO3 is kept in the atmosphere of CO2 to prevent its decomposition.

 
        BeCO3        MgCO3       CaCO3        SrCO3        BaCO3

        <100°C      540°C        900°C        1290°C       1360°C

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