In physics, the Rayleigh dissipation function, named after Lord Rayleigh, is a function used to handle the effects of velocity-proportional frictional forces in Lagrangian mechanics. It was first introduced by him in 1873. If the frictional force on a particle with velocity v → {\displaystyle {\vec {v}}} can be written as F → f = − k v → {\displaystyle {\vec {F}}_{f}=-k{\vec {v}}} , where k {\displaystyle k} is a diagonal matrix, then the Rayleigh dissipation function can be defined for a system of N {\displaystyle N} particles as
R ( v ) = 1 2 ∑ i = 1 N ( k x v i , x 2 + k y v i , y 2 + k z v i , z 2 ) . {\displaystyle R(v)={\frac {1}{2}}\sum _{i=1}^{N}(k_{x}v_{i,x}^{2}+k_{y}v_{i,y}^{2}+k_{z}v_{i,z}^{2}).}
This function represents half of the rate of energy dissipation of the system through friction. The force of friction is negative the velocity gradient of the dissipation function, F → f = − ∇ v R ( v ) {\displaystyle {\vec {F}}_{f}=-\nabla _{v}R(v)} , analogous to a force being equal to the negative position gradient of a potential. This relationship is represented in terms of the set of generalized coordinates q i = { q 1 , q 2 , … q n } {\displaystyle q_{i}=\left\{q_{1},q_{2},\ldots q_{n}\right\}} as
F f , i = − ∂ R ∂ q ˙ i {\displaystyle F_{f,i}=-{\frac {\partial R}{\partial {\dot {q}}_{i}}}} . As friction is not conservative, it is included in the Q i {\displaystyle Q_{i}} term of Lagrange's equations,
d d t ∂ L ∂ q i ˙ − ∂ L ∂ q i = Q i {\displaystyle {\frac {d}{dt}}{\frac {\partial L}{\partial {\dot {q_{i}}}}}-{\frac {\partial L}{\partial q_{i}}}=Q_{i}} . Applying of the value of the frictional force described by generalized coordinates into the Euler-Lagrange equations gives
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