Although weighted residual techniques are extremely general and may be applied to both very arbitrary linear media of highly complex anisotropic character as well as nonlinear media, there are some places where one could cite the desire to maintain a variational approach. I t is for these cases that we here address the properties of the auxiliary method for treating differing degrees of anisotropy, including but not limited to g y r o e l e c t r i c , g y r o m a g n e t i c , , c h i r a l , g y r o e l e c t r o m a g n e t i c , g y r o e l e c t r o c h i r a l , gyromagnetochiral, and gyroelectromagnetochiral. What the adjoint method is capable of doing and its limitations will be discussed in view of the auxiliary method.