The Chemistry of Salt Hydrolysis
Imagine you are standing in a laboratory, holding a beaker of pure water. When you dissolve a salt like ammonium chloride (NH4Cl) into it, a fascinating microscopic dance begins. The salt completely dissociates into ammonium (NH4+) and chloride (Cl−) ions.
Now, not all ions are created equal. The chloride ion is the conjugate base of a very strong acid (HCl), which makes it an incredibly weak base. It acts merely as a spectator, floating aimlessly in the water. However, the ammonium ion is the conjugate acid of a weak base (NH4OH). Because it comes from a weak parent, it has a strong desire to react with water. This reaction, where the cation of the salt reacts with water to produce extra hydrogen ions (H+), is known as cationic hydrolysis.
Decoding the Nature of the Salt
Because the hydrolysis of the ammonium ion releases extra H+ ions into the solution, the delicate balance of pure water is disrupted. The solution becomes acidic.
Before we even touch a calculator, our chemical intuition tells us a crucial fact: the pH of this solution must be less than 7. This is a powerful sanity check that you should always keep in your back pocket. Whenever you have a salt formed from a strong acid and a weak base, the strong acid's character dominates the final solution.
The Master Equation for pH
To find the exact pH, we don't need to derive the equilibrium expressions from scratch every time. We have a beautifully elegant master formula for the pH of a salt of a strong acid and a weak base:
Let's gather our tools to use this formula. We are given the base dissociation constant, Kb, as 10−5. The term pKb is simply the negative logarithm of Kb:
Next, we need the concentration of the salt, C. We are given C=0.02 M. To make our upcoming logarithmic calculations smoother, it is always a smart move to convert decimals into scientific notation. So, we write C=2×10−2 M.
Executing the Calculation
Now, let's carefully substitute these values into our master formula. This is where many students make silly algebraic mistakes, so we will take it step-by-step.
We need to expand the logarithm term using the fundamental property log(a×b)=loga+logb:
log(2×10−2)=log2+log(10−2)
We are given that log2=0.301, and we know that log(10−2)=−2. Substituting these back into our equation:
Let's simplify the terms inside the bracket. Five minus two gives us three, and adding zero point three zero one gives 3.301.
The Final Sanity Check
Half of 3.301 is exactly 1.6505.
And there we have it! The final calculated pH is 5.35. Notice how this perfectly aligns with our initial theoretical prediction: the value is indeed less than 7, confirming that our strong acid-weak base salt has created an acidic environment. Always trust the math, but verify it with your physical intuition!