KP and KC describe the same equilibrium, so a fixed relationship connects them. Starting from the ideal gas equation P=(n/V)RT and noting that active mass equals molar concentration n/V, each species' partial pressure can be written as (concentration)×RT; substituting this into the KP expression and comparing with KC gives
KP=KC(RT)Δng
where Δng is the difference between the total moles of gaseous products and the total moles of gaseous reactants in the balanced equation. Three regimes follow: Δng=0 gives KP=KC exactly (e.g. H2+I2⇌2HI, or ammonia synthesis's own KC/KP=(RT)2 inverse case where Δng=−2 gives KP=KC(RT)−2, so KC/KP=(RT)2); Δng>0 gives KP>KC (e.g. PCl5⇌PCl3+Cl2, where Δng=+1, so KC/KP=1/(RT)); and Δng<0 gives KP<KC (e.g. 2SO2+O2⇌2SO3).
This relation is the standard tool for converting a measured KP into KC or vice versa -- for example, SrCO3(s)⇌SrO(s)+CO2(g) has Δng=+1 (only CO2 is gaseous), so KC=KP/(RT); at KP=2.2×10−4 atm and T=1002 K, KC=0.0821×10022.2×10−4≈2.67×10−6 mol L−1. It equally tells us, purely from the sign of Δng, whether KC must be larger or smaller than KP for a given reaction without any numbers at all -- if a gaseous homogeneous reaction has more moles of product than reactant (Δng>0), then since KP=KC(RT)Δng with RT>1 in most common units, KP>KC, i.e. KC is the smaller of the two.