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equilibrium constant
Kc = ([P1]n[P2]n)/([R1]n[R1]n)
partial pressures may also be used
homogeneous/heterogeneous equilibrium
homo - same phase
hetero - different phase
equilibrium constant (Q)
eqn. constant calculated before equilibrium is reached
Le Chatelier’s principle
high concentration → favors opposite side
high temperature → favors endothermic products
high pressure → favors side w/ fewer moles
idk?
KP = Kc(RT)∆n