Classical continuum mechanics
We consider a virtual displacement field . The virtual work is
where is the body force, is the surface traction, is the Cauchy stress tensor and is the mass density and is the current configuration.
I think the stress term ends up with an opposite sign to the body force term because it is a reactive force. This can probably be motivated by reading the section in Landau-Lifschitz where they define the stress tensor.
We do integration-by-parts to put it in the form
In classical continuum mechanics, the strain tensor is found by symmetrising . That is . The there is basically the group action of the translation group. So is there a way to generalise this to a general group ?
Generalised continuum mechanics
We consider a Cartan media configuration . To generalise the virtual work principle, we consider the “response” of a virtual displacement field and its differential and time-derivative , similarly to how , and appeared in (1).
Let denote the contraction of a covector and a vector. So if we have and , then is a scalar on (that is, it is a map ). This goes for vectors and covectors in the double tangent and codouble tangent bundles as well. So if and , then is a scalar.
Let be a -valued volume form on , we extend the notation so that for any we have that is an volume form on . If we introduce coordinates on , then we may write as
where , which transforms as a scalar density of weight and , which transforms as a tensor density of weight . We then have that
Now, let be a -valued -form on , and let
then is equal to up to sign. So absorb that sign into such that .
In coordinates, let
Now, let be a -valued -form on . In coordinates we write it as . We then define the wedge contraction as
We can then finally write down a generalisd virtual work principle
where we have ommitted the generalised surface traction for now.
The lift
Let such that . So we have that . We thus have a map , defined by . This is a dual Lie algebra field . We can thus write the contraction of and as
We define the corresponding -valued volume-form as .
In a previous note we saw that . We thus have that . So
Now, let and . Since we can write
Similarly, as we have that
We thus have
Dropping the L’s we have
:::warning Note that here is not defined over the kinematic base space , but rather just . :::
In components, we can write
We then have
Compare this to the expression we have in the paper
Cosserat systems
We have and . We also write , where is the orthonormal frame bundle.
Consider virtual displacement fields and . Collectively, we have that .
Each of the virtual displacements will give rise to a generalised body force volume form, generalised stress -form, as well as a generalised momentum volume form. Each of these will act on the virtual displacements to form a scalar volume form on .
Let us first consider the body force. Let be a -valued volume form on , then , where is the Euclidean inner product, is a scalar volume form on .
Let be a -valued volume-form on . Then is a scalar volume form on for each .
Now we move on to the stress. We need a -form that contracts and wedges with to get a scalar volume form on . In coordinates, we may write
where is defined such that , and where . We also write
We can then define the wedge inner product
Similarly, let be a -form that contracts and wedges with to get a scalar volume form on , for each .
Finally, let and be volume forms on that contracts with and to form scalar volume forms on .
We can now write down the virtual work principle
Note about vector-valued forms
Let a vector-bundle with base-space and . We denote the space of -valued -forms as .
Though a seemingly obscure object, the vector-valued -form is fairly easy to understand. For each , a regular -form on yields a linear map . An -valued -form on correspondingly yields a map , where is the fiber at . A vector-valued -form yields an antisymmetric linear map at each .
If the vector bundle is trivial, as is the case for Cartan media, the situation is simpler still. Cartan media configurations are sections on the fiber bundle . Velocities and deformation fields on Cartan media are sections on . Body forces are sections on .
:::info is the vertical bundle of the trivial fiber buncle , which which we write as . :::
Now, consider a -valued -form on . At each , is a linear map . If are coordinates on then we can expand it as
where are sections on . For any vector-field on , we have
where is now a section on .
The wedge product
Let us go back to the vector bundle . The wedge product of a -valued -form with a -valued -form is a -valued -form.
So for example, and we have and , then
The wedge contraction
In the virtual work principle, we need to wedge and then contract covector-valued -forms with vector-valued -forms.
Consider a -valued -form and a -valued -form . Their wedge product is
For each , we have that is a rank- tensor. That is, for each we have a map . The -contraction of this tensor, which yields a scalar on , is given by .
So this leads us to define the wedge contraction
such that is now a regular -valued -form on .