Submitted to HEJ Manuscript no.: MET-990617-A |
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The scheme of upsetting between parallel plates is shown in Fig. 1.
Figure 1:
Work piece before and after upsetting
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The points of the deformity zone can be given in a cylindrical system of
coordinates by the points , where ,
(see Fig. 1.).
We denote the velocity field by
.
The components of can be determined by using the following model
assumptions:
1. The material is incompressible.
2. The deformation is axisymmetric, that is
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(1) |
3.The component of velocity at the contact of the piece and the plates is as follows:
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(2) |
4. At , has a point of inflexion, that is, the deformation
velocity
has an extremum at this point.
5. At the radial velocity component has a maximum when the work piece has a bilge form.
6. The upset material is homogenous and isotropic.
7. The -component of velocity can be written in the form of
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(3) |
because this function is the simplest assimetric one to describe the vwlocity field of the deformation
of the work piece.
Here , , and are provisionally unknowns to
be determined.
From Assumption 3. we get that
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(4) |
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(5) |
From Assumption 4.:
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(6) |
From equations (4, 5, 6), the values
of and can be determined, whence:
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(7) |
Assumption 1. im;ies that the velocity field is divergence free:
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(8) |
By substituting the expression of into his equation, for the
component of we obtain first-order differential equation, that
contains as a parameter. Condition 2. can be regarded as
an initial condition for this equation. So the problem given
by formulas (8) and (1) can be solved uniquely for every . It is easy to see that
the solution is as follows:
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(9) |
where is a provisionally arbitrary constant to be determined.
Introducing the nondimensional parameter by
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(10) |
Equations (7,9) can be rewritten as:
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(11) |
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(12) |
Figure 2:
Radial component of the velocity at different values of
( , , )
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In the above example, at , the work piece remains cylindrical, while at
gets bilge and at the mantle surface of the piece
becomes concave. In case of convex shape, at , the deformation velocity
has a maximum, that is, is steepest in the
point of inflexion. (Fig.3).
Figure 3:
Axial component of velocity at different values of
( , , )
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In case equations (11 and 12) gives the typical
forms of homogenous deformations, which is well-known, see e.g.
[2,3]:
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(13) |
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(14) |
The exact value of can be determined by minimization the power
requirement of the forming.
| Submitted to HEJ Manuscript no.: MET-990617-A |
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