R_y(θ) = e^(−iθY/2) = [cos(θ/2) −sin(θ/2); sin(θ/2) cos(θ/2)];R_z(θ) = e^(−iθZ/2) = [e^(−iθ/2) 0; 0 e^(iθ/2)]
1. 经典对照:两层线性复合 y₂ = W₂(W₁x+b₁)+b₂ = (W₂W₁)x + (W₂b₁+b₂)——没有非线性,多层 = 单层
2. 取 θ = π:R_y(π) = [0 −1; 1 0],R_y(π)|0⟩ = (0, 1)ᵀ = |1⟩——布洛赫球北极转到南极
3. R_z(π) = diag(−i, i)(用 e^(±iπ/2) = ±i);两列 (−i,0)ᵀ、(0,i)ᵀ 内积 0、模方 1 → 幺正 ✓