The equilibrium is represented as:
\(\text{Cr}_2\text{O}_7^{2-} \rightleftharpoons 2\text{CrO}_4^{2-}\)
This equilibrium is pH-dependent. The influence of pH on this equilibrium is as follows:
- pH and Equilibrium Shift: The balance between dichromate ions (\(\text{Cr}_2\text{O}_7^{2-}\)) and chromate ions (\(\text{CrO}_4^{2-}\)) is determined by the hydrogen ion (H+) concentration.
- Basic Medium Effects: A basic environment has a high concentration of hydroxide ions (OH-). These ions react with H+, lowering the H+ concentration. Consequently, the equilibrium shifts to the right, favoring the formation of more chromate ions (\(2\text{CrO}_4^{2-}\)) as they consume H+.
- Acidic Medium Effects: In an acidic environment, H+ ions are abundant. According to Le Chatelier's principle, an excess of H+ drives the equilibrium to consume these ions, causing a shift to the left, towards the formation of dichromate ions (\(\text{Cr}_2\text{O}_7^{2-}\)).
- Neutral and Weakly Acidic Conditions: In neutral solutions, H+ and OH- concentrations are equal, resulting in no significant equilibrium shift. Weakly acidic conditions may slightly favor dichromate formation, but to a lesser extent than strongly acidic conditions.
Conclusion: Since the equilibrium shifts to the right in a basic medium (due to OH- neutralizing H+), the correct condition is a basic medium.