Analyzing the Setup
Imagine you are standing in a chemistry lab with a beaker containing exactly 1 L of a hydrochloric acid (HCl) solution
We are given a crucial piece of information: the initial pH of this solution is exactly 1. Our objective is to dilute this solution by adding pure water until its pH rises to 2.
To solve this, we must first translate the abstract concept of pH into a tangible physical quantity: molar concentration. Remember the fundamental definition of pH? It is the negative base-10 logarithm of the hydrogen ion concentration, mathematically expressed as pH=−log10[H+].
By rearranging this formula, we can easily find the concentration: [H+]=10−pH.
The Master Equation
Let's apply this to our initial state
Since the initial pH is 1, the initial molarity of hydrogen ions, which we will call M1, is 10−1 M, or 0.1 M.
Now, what about our target state? We want the final pH to be 2. This means our final molarity, M2, must be 10−2 M, which is 0.01 M. Notice how an increase of just 1 unit on the logarithmic pH scale corresponds to a massive 10-fold decrease in the actual concentration of acid!
When we add pure water to dilute a solution, the number of moles of the acid solute remains absolutely constant. Only the total volume of the solution changes. This physical reality gives us the powerful dilution equation:
Final Calculation
Let's substitute our known values into the dilution equation
We know M1=0.1 M, V1=1 L, and M2=0.01 M.
Solving for V2, we find:
There is a catch here! The question specifically asks for the volume of water added, not the final total volume. We already had 1 L of solution in the beaker initially. Therefore, the volume of pure water we need to pour in is the difference between the final volume and the initial volume.
Volume added=V2−V1=10 L−1 L=9 L
Thus, we must add exactly 9 L of water to achieve a pH of 2.