# Anisotropic Surface Overview

The Anisotropic Surface option can only be used in conjunction with the following material strength models:

Anisotropic Linear

Snowden Modified Anisotropic Linear

It allows you to define a surface which represents the average bedding orientation of anisotropic material regions in which the direction of anisotropy changes with location. For example, a folded bedding layer as shown in the figure below.

Given a point in space that you want to compute the anisotropic angle, Slide first computes the point on the anisotropic surface that’s closest to the point in space that you want to compute the angle.  This is not a vertically upward path like a water surface, it’s the closest point. Given the point on the anisotropic surface, Slide computes the orientation of the surface at this point and uses this as the anisotropic angle.

Anisotropic surface option, 2D schematic

An Anisotropic Surface in conjunction with the above strength options, allows the Slide compute engine to determine the local orientation of folded anisotropic regions (for example), in order to apply the correct strength properties at any location.

To add an anisotropic surface to a model use the Add Anisotropic Surface option.

NOTE: an Anisotropic Surface is an independent modeling entity and is not considered part of the model boundary geometry. It does NOT get intersected with any other boundary types, and cannot be used to define material regions. It is only used for the specific purpose of defining the direction of anisotropy for a material.

Assign Anisotropic Surface

After an anisotropic surface has been created, it must be assigned to a material using either the Anisotropic Linear or Snowden Modified Anisotropic Linear strength models.

Location of Anisotropic Surface

The exact location of the anisotropic surface is not critical, however it should be placed such that it best represents the average orientation of the bedding throughout the material.

Typically an Anisotropic Surface is defined near the "middle" of the corresponding anisotropic material region, as shown in the above figure; or it could be coincident with one of the material boundaries (e.g. either the upper or lower boundary of the anisotropic material).