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Rock Mechanics.pdf - Mining and Blasting

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Figure 6.7 Development of a finite<br />

element model of a continuum problem,<br />

<strong>and</strong> specification of element geometry<br />

<strong>and</strong> loading for a constant<br />

strain, triangular finite element.<br />

METHODS OF STRESS ANALYSIS<br />

Thus, since strain components are defined uniquely in terms of various derivatives<br />

of the displacements, the imposed displacement variation defines the state of strain<br />

throughout an element. These induced strains <strong>and</strong> the elastic properties of the medium<br />

together determine the induced stresses in an element. Superposition of the initial <strong>and</strong><br />

the induced stresses yields total stresses in the element.<br />

The assumption in the finite element method is that transmission of internal forces<br />

between the edges of adjacent elements can be represented by interactions at the<br />

nodes of the elements. It is therefore necessary to establish expressions for nodal<br />

forces which are statically equivalent to the forces acting between elements along<br />

the respective edges. Thus the procedure seeks to analyse the continuum problem<br />

(Figure 6.7a) in terms of sets of nodal forces <strong>and</strong> displacements for the discretised<br />

domain (Figure 6.7b). The solution procedure described here, for purposes of illustration,<br />

considers triangular element geometry, linear variation of displacement<br />

with respect to element intrinsic co-ordinates, <strong>and</strong> resultant constant stress within an<br />

element.<br />

6.6.1 Displacement variation<br />

In Figure 6.7c, induced nodal displacements are uxi, u yi, etc., <strong>and</strong> displacements<br />

[u] at any point within the element are to be obtained by suitable interpolation from<br />

the nodal values. Introducing a matrix of interpolation functions, [N], a suitable<br />

interpolation formula is<br />

<br />

ux<br />

[u] = = ⎡ ⎤<br />

ui<br />

[Ni][ui] = [Ni, N j, Nk] ⎣ u j ⎦ (6.36)<br />

where<br />

184<br />

u y<br />

[ui] =<br />

= [N][u e ]<br />

uxi<br />

u yi<br />

<br />

<br />

Ni 0<br />

[Ni] = Ni =<br />

0 Ni<br />

uk

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