This page is work in progress
We identify the shell with a surface , i.e. a two-dimensional submanifold of the Euclidean point space . We suppose to be orientable, at least locally, and we shall denote by the orthogonal unit vector at .
We denote by the linear space of vectors in three dimensions. Given , we let the tangent space at
We postulate the existence of pair of tensor fields and such that the resultant force and the resultant moment exerted on a part are given by
In the above expressions, and are, respectively, the applied force and the applied couple per unit area, moreover is the position vector of with respect to a fixed origin. By writing the applied couple as the cross product of with some vector we are making it explicit that shells cannot sustain couples which have their axis parallel to . Accordingly, we can assume that .
In the boundary integrals, denotes the unit vector tangent to , orthogonal to the curve , and pointing outside at . The terms and represent, respectively, the linear densities of contect force and contact couple applied at the boundary of at . We remark that the tensor is a linear map from to , while can be taken as a linear map of into inself (since it appears always composed with the linear operation ).
We need a divergence theorem to transform integrals computed on into integrals over . To begin with, we record the following identity
Next, consider the tensor field where is a constant vector. Then
Since every tensor field can be written as , for a suitable choice of a triplet of vector fields, the identity holds for whatever tensor field . Thus, we can conveniently take
as the definition of divergence of a tensor field .
For the continuous body , Euler's axioms consist in the requirement that and be null for every part $\mathcal P \subset \mathcal S. It is not difficult, using the divergence theorem and a standard localization argument to deduce the equivalence:
A similar argument can be applied to the equilibrium of moments. However, the result of this procedure is more transparent if we start from
Then a procedure similar as above yields the following equivalence
Here is the transpose of , and hence a linear map from to , is the identity on , and is the orthogonal projection of on .
where is the Weingarten map, a tensor which can be shown to be symmetric. Since and are linear maps from to , their ranges and their domains are orthogonal to . From this fact it is not difficult to conclude that
The result is also more transparent if we introduce the decomposition
We also introduce the notation
Then we can write:
We refer to as the shear vector: its interpretation is as follows: the scalar product represents the component along of the line contact force acting across a line element from the side of .
In the linear theory the deformation of the shell is described by a displacement field and a rotation field . In the deformed configuration the typical point of the shell occupies the position , and the associated director field is . It is convenient to write the rotation as . Then the work performed by the applied couples on a virtual rotation is:
The virtual work performed by forces and couples acting on a part is:
Integration by parts by making use of the divergence theorem and of the equilibrium equations shows that
It is useful at this point to introduce the decomposition of the displacement
Then
On introducing the virtual strains: these should be symmetric
the expression of the virtual work can be written as
We refer to , , and as the virtual stretching, shearing, and bending. Observe that the variation of the direction of the normal is . Thus, the shearing can also be written as . For a Kirchhoff-Love plate, the director is constrained to be parallel to . A consequence of this requirement is that for a Kirchhoff plate. Then ,
the expression of the virtual work is
According to Ciarlet [4], for a linear Koiter shell the strain energy of a part is
where
and where , defined by
with the identity tensor on , is a linear map from the space of symmetric tangential tensors at into itself. The time derivative of the strain energy is
Then the internal power is
This leads to the constitutive equations
Note that is a symmetric tensor
Gradient and divergence on a surface
The gradient of a vector field on is a tensor field whose value at is a map from to , defined as follows: the image of a vector is computed by taking any smooth curve such that and , and by letting
This definition is independent on the particular curve chosen, as can be seen by working on a chart. The covariant derivative of is is instead a linear map from to
For a three-dimensional isotropic, linearly elastic material, the stress-strain relation has the form
where and are the Lamé constants. As discussed in Ciarlet (2005)](https://doi.org/10.1007/s10659-005-4738-8), Sec. 4.5, a rigorous argument based on asymtotic analysis shows that the mechanical response of a shell-like homogeneous linearly elastic body of thickness , made of a material obeying the stress-strain relation is captured by a shell with Lamé constants (See the discussion about the convergence
These constants are obtained by considering the in-plane response under the assumption that , which leads to the system
The divergence of a tensor field can be written as
In particular, is a vector field and is a tensor field, we have
Since and , we obtain
We also observe that since , , and ,
Hence,
By localization we obtain
For a Kirchhoff-Love plate, the director coincides with the normal . Hence Taking the variation of the identity and recalling that is a tangential vector, we obtain
whence
Whereas it is natural to project the balance equations Note that it is not natural to introduce a similar decomposition for the force balance equation at this stage.
A finite deformation of the shell is described by an one-to-one smooth map
The deformation gradient is a linear map from to , where denotes the tangent space of at . We define the strain as
Note if is a parametrization for , then the map is a parametrization for .
We denote by the normal. The Weingarten tensor on is
For a Koiter shell, the strain energy of a part is
The variation of is
The variation of is
Note that
Hence
xxxxxxxxxx\bm W\bm a_\alpha\otimes d\bm a^\alpha=-\bm W\nabla\bm v+w\bmsf W^2
References:
[1] P. Podio-Guidugli: Lezioni sulla teoria lineare dei gusci elastici sottili, Masson, 1991
[2] C. Davini: Lezioni di Teoria dei Gusci (lecture notes in Italian).
[3] P.M. Naghdi: The Theory of Shells and Plates, Handbuch der Physik VIa/2 p.425-640, Springer-Verlag, 1972
[4] P.G. Ciarlet: An introduction to differential geometry with applications to elasticity, Springer, 2005.