This is a TSFX question (based off an article from The Age)
Effect on the c(Fe3+) and m(Fe2+) of adding water to the Fe3+(aq) + SCN-(aq) Fe(NCS)2+(aq) equilibrium at constant temperature.
Adding water instantaneously decreases all concentrations, and increases the concentration fraction. This pushes the system out of equilibrium. To return to equilibrium the concentration fraction must decrease back equal to K, so the reverse reaction dominates and the m(Fe3+) increases. Whilst this increases the c(Fe3+), equilibrium is reached again before it returns to its initial value. Overall the c(Fe3+) decreases.
Can you explain why the equilibrium 2Fe3+(aq) + Sn2+(aq) 2Fe2+(aq) + Sn4+(aq) is not pushed out of equilibrium by adding water?