Step 1: Hooke's law (equation (5)) generalizes to

(13) |

Step 2a: The layer parameters are the stiffness matrix , the layer
thickness *h*, and the layer density .

Step 2b: Instead of ``springs in series'' we have
a stack of infinite flat layers with welded interfaces.
(We will assume the layering is normal to the *z* axis.)
Instead of a constant scalar spring tension
we have that
the stress normal to the layering must be the same in all layers.
Thus equation (6) becomes

(14) |

(15) |

Step 2c: The first two additive parameters are obvious ones.
The thickness *h* of each layer adds,
as does the areal density ; thus the first two
layer-group elements are trivially *h* and .

To obtain vertical displacements, which sum through the stack,
we must multiply the vertical components of strain by the layer thickness *h*.
Thus equation (7) becomes

(16) |

There is one more additive equation to find.
Think of squeezing our layercake horizontally in a vise;
all layers are forced to undergo the same horizontal distortion.
The various layers will exert differing forces on the vise blades;
to find the total traction, sum over the horizontal forces exerted by each
of the layers.
Stress is force per area, so force is area times stress. The (infinite)
horizontal dimension tangential to the vice blades is the same for all layers
and so can be factored out,
leaving only the vertical thickness *h* multiplied by the horizontal components
of stress.
We thus have

(17) |

Step 3: We can now rearrange equation (13) to segregate the additive and constant elastic terms, obtaining

(18) |

(19) |

(20) |

After a little matrix algebra we finally obtain Hooke's law in the desired form, the elastic equivalent of equation (11):

(21) |

Step 4: The somewhat complicated matrix coefficient on the constant vector parameter in equation (21),

(22) |

Does the Schoenberg-Muir system form an Abelian group? Yes.
Association and commutativity are obviously satisfied.
The inverse can be formed simply by changing the sign of *h*,
and the identity element is the layer of zero thickness.
The group is closed in the layer-group domain, although
it is possible to create representations in the layer-group domain
by layer subtraction that correspond to physically disallowed elastic media
(Schoenberg and Muir, 1989).
The group concept of subtraction coupled with the Schoenberg-Muir calculus
does provide a useful theoretical framework for decomposing observed elastic
properties into geophysically meaningful components;
for example observed orthorhombic anisotropy can be decomposed into
a transversely isotropic background with fractures
(Hood, 1991) and (Hood and Schoenberg, 1992).

11/17/1997