Line spring elements

The line spring elements in Abaqus/Standard provide a computationally inexpensive tool for the analysis of part-through cracks in plates and shells. The basic concept was first proposed by Rice (1972) and has been further discussed by Parks and White (1982).

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Line Spring Elements for Modeling Part-through Cracks in Shells

ProductsAbaqus/Standard

The “line spring” is a series of one-dimensional finite elements placed along the part-through flaw, which allows local flexibility of one side of the flaw with respect to the other (points A and B in Figure 1). This local flexibility is calculated from existing solutions for single edge notch specimens in plane strain (Figure 2). The approach is computationally inexpensive compared to fully three-dimensional models of the vicinity of the flaw; it is also approximate because of the use of two-dimensional solutions embedded in the shell model. Practical experience with the method on typical geometries has shown that, for several important geometries, the method provides acceptable accuracy.

Figure 1. Surface geometry; line spring modeling. Side B of the element contains nodes 1, 2, and 3; and for LS6 elements side A contains nodes 4, 5, and 6.

Figure 2. Line spring compliance calibration model.

This section discusses the geometric and kinematic basis of the elements as well as the equilibrium statement and the development of the local solutions that define the constitutive relationships. The constitutive relations are expressed in terms of the forces and moments carried across the crack and the relative displacements and rotations of points on opposite sides of the crack (A and B in Figure 1), and are derived from local solutions to single edge cracked plane strain specimens. Elastic and fully plastic (limit analysis) solutions are used to construct an approximate elastic-plastic model.

At each point along the flaw a local orthonormal basis system is defined (t,n,q), with t the tangent to the shell along the flaw, n the normal to the shell, and q defined as

q=t×n.

We use the shell normal, n, to determine the side of the shell on which the flaw occurs; flaws that open on the positive n side are given positive flaw depths to indicate this, and those on the negative n side are given negative flaw depths. The relative motion between two points—A and B in Figure 1—on opposite sides of the flaw but otherwise at the same place, then defines a set of six generalized strains as follows. Side B of the element contains nodes 1, 2, 3; and for LS6 elements side A contains nodes 4, 5, and 6.

Mode I:

opening displacement  ΔuI=(uB-uA)q 
opening rotation  ΔϕI=(ϕB-ϕA)t 

Mode II: through-thickness shear is defined by the relative displacement,

ΔuII=(uB-uA)n

Mode III: antiplane shear is defined by the relative displacement,

ΔuIII=(uB-uA)t,

and by the relative rotation,

ΔϕIII=(ϕB-ϕA)q.

The relative rotation ΔϕII=(ϕB-ϕA)n plays no role in the deformation.

These relative motions form the kinematic basis of the element.

Since the line spring elements are written for geometrically linear analysis only, the first variations of these relative motions are identical to the above definitions, with the total values replaced by their variations.