Imagine you are an architect trying to build a highly stable, enduring structure. If you have massive, heavy boulders, would you use tiny pebbles to hold them together? Probably not. The structure would be wobbly and unstable. You would want large, sturdy blocks to match the boulders. This intuitive idea is the exact principle behind the thermal stability of alkaline earth metal carbonates!
Analyzing the Setup
In inorganic chemistry, the carbonate ion (CO32−) is considered a large polyatomic anion. When it forms ionic compounds with Group 2 metals (the alkaline earth metals), the stability of the resulting crystal lattice depends heavily on how well the cation and anion fit together.
As we move down Group 2 from Beryllium (Be) to Barium (Ba), the atomic and ionic radii increase due to the addition of new electron shells.
rBe2+<rMg2+<rCa2+<rSr2+<rBa2+
The Master Equation of Stability
A fundamental rule dictates that a large anion is best stabilized by a large cation. Because the Barium ion (Ba2+) is the largest in the group, it packs most efficiently with the large carbonate ion. This excellent packing leads to a highly stable crystal lattice.
Therefore, the thermal stability of the carbonates increases as we move down the group:
BeCO3<MgCO3<CaCO3<SrCO3<BaCO3
Barium carbonate (BaCO3) is so stable that it requires extremely high temperatures to decompose into Barium oxide and Carbon dioxide. This perfectly validates our Reason (R).
The Solubility Paradox
Now, let's tackle the second part of the puzzle: solubility in water. For any ionic salt to dissolve, the energy released when water molecules surround the ions (the Hydration Energy) must be greater than the energy holding the crystal together (the Lattice Energy).
Here is the catch: Hydration energy is inversely proportional to the size of the ion. Small ions like Be2+ have a very high charge density, so water molecules are strongly attracted to them, releasing a massive amount of hydration energy.
However, as we move down the group to Ba2+, the ion becomes so large that its charge density drops. Consequently, its hydration energy decreases rapidly. In fact, the hydration energy decreases much faster than the lattice energy does.
Because the hydration energy for Barium carbonate is so low, it cannot overcome the lattice energy. Thus, solubility decreases down the group, making Barium carbonate practically insoluble in water. This perfectly validates our Assertion (A).
Final Conclusion
Both the Assertion and the Reason are factually correct. More importantly, the Reason (increasing cationic size leading to higher thermal stability) is the exact scientific explanation for why Barium carbonate is so highly stable. Therefore, the correct choice is that both (A) and (R) are true, and (R) is the correct explanation of (A).