Chemical Equilibria in Analysis

reaction quotient

Think of equilibrium as a destination and the reaction quotient as a snapshot of where you are right now on the road there. Take a reaction caught at any moment — not necessarily balanced — and ask, 'with the amounts present this instant, which way must it move to settle?' The reaction quotient, Q, is the number that answers it.

It is calculated with the exact same recipe as the equilibrium constant — product concentrations over reactant concentrations, each raised to its coefficient — but using the concentrations you have right now rather than the ones at equilibrium. Comparing Q to K then tells the direction: if Q is less than K the reaction runs forward to make more product; if Q is greater than K it runs backward; if Q equals K, you are already at equilibrium and nothing net changes.

For analysis, Q is the everyday decision tool. Mix two solutions and want to know whether a precipitate will appear? Compute Q for the dissolving reaction and compare it to Ksp — if Q exceeds Ksp the solution is oversaturated and solid forms. The caveat is the same one that haunts all equilibrium work: Q tells you the direction the reaction is driven, but not the speed, and for accurate work in salty samples it should be built from activities, not bare concentrations.

Mix solutions so that, the instant they meet, the product of silver and chloride concentrations is 1 x 10^-6. Since this Q far exceeds AgCl's Ksp of 1.8 x 10^-10, the solution is oversaturated and silver chloride immediately precipitates.

Q > Ksp means precipitation; Q < Ksp means the solid can still dissolve.

Q and K share an identical formula; the only difference is the moment they describe. Q is for any instant, K is for the special instant of equilibrium. At equilibrium, and only there, Q equals K.

Also called
Q反应商反應商