Let E1,…,En and F be sets and u a mapping of E1×⋯×En into F. Let i∈{1,n}. Suppose Ei and F are given the structures of magmas. u is said to be distributive relative to the index variable i if the partial mapping
xi↦u(a1,…,ai−1,xi,ai+1,…,an)
is a homomorphism of Ei into F for all fixed aj in Ej and j=i.
If ⊤ denotes the internal laws on Ei and F, the distributivity of u is given by the equations
(1)
u(a1,…,ai−1,xi⊤xi′,ai+1,an)=u(a1,…,ai−1,xi,ai+1,…,an)⊤u(a1,…,ai−1,xi′,ai+1,…,an)
for i=1,2,…,n,a1∈E1,…,ai−1∈Ei−1,xi∈Ei,xi′∈Ei,ai+1∈Ei+1,…,an∈En.
Bourbaki puts the proof directly after the statement, so what is above is the statement and its proof together.
Nothing.