Hookes law for stress and strain

Click For Summary
SUMMARY

The discussion centers on the application of Hooke's Law in continuous elastic media, specifically regarding the relationship between the stress tensor (σ) and the strain tensor (E). It is established that the only tensors available for constructing a linear relation in isotropic materials are the strain tensor itself and the Kronecker delta multiplied by the trace of the strain tensor. The most general linear relationship is expressed as σij = λEij + λδijkEkk, where λ represents a constant. The discussion emphasizes that this limitation is due to mathematical properties rather than directional invariance.

PREREQUISITES
  • Understanding of tensor calculus
  • Familiarity with Hooke's Law in elasticity
  • Knowledge of isotropic materials
  • Basic concepts of linear algebra, including Kronecker delta and trace
NEXT STEPS
  • Study the Cayley-Hamilton theorem and its application in tensor analysis
  • Explore the mathematical properties of the strain tensor and its invariants
  • Investigate the implications of isotropy in material science
  • Learn about tensorial functions and their representations in elasticity
USEFUL FOR

This discussion is beneficial for materials scientists, mechanical engineers, and students studying continuum mechanics or elasticity theory, particularly those seeking to deepen their understanding of stress-strain relationships in isotropic materials.

aaaa202
Messages
1,144
Reaction score
2
I need help understanding a passage in my textbook, where the form of hookes law in continuous elastic media is explained. It says:
"The absence of internal directions in isotopic matter tells us that there are only two tensors available to construct a linear relation between the the stress tensor and the strain tensor. One is the strain tensor itself and the other is the kronecker delta multiplied by the trace of the strain tensor. Consequently the most general strictly linear tensor relation between stress and strain is of the form:
Here follows a linear relation between the stress- and strain tensor involving the strain tensor and its trace in separate terms.
"
I don't really understand all this. Why is only the strain tensor and its trace avaible for constructing a linear relation between the two tensors? Does it have to do with the fact that we would like Hookes law to be invariant under change of directions, since the symmetry dictates that there are no internal directions?
 
Physics news on Phys.org
aaaa202 said:
I need help understanding a passage in my textbook, where the form of hookes law in continuous elastic media is explained. It says:
"The absence of internal directions in isotopic matter tells us that there are only two tensors available to construct a linear relation between the the stress tensor and the strain tensor. One is the strain tensor itself and the other is the kronecker delta multiplied by the trace of the strain tensor. Consequently the most general strictly linear tensor relation between stress and strain is of the form:
Here follows a linear relation between the stress- and strain tensor involving the strain tensor and its trace in separate terms.
"
I don't really understand all this. Why is only the strain tensor and its trace avaible for constructing a linear relation between the two tensors? Does it have to do with the fact that we would like Hookes law to be invariant under change of directions, since the symmetry dictates that there are no internal directions?
No. It has nothing to do with this. It's mathematical. Try to construct another tensorial form that is linear in the strain tensor.

Chet
 
I don't understand. So according to what you say we have that the most general relation is:

σij = λuij + λδijkukk

But what goes wrong if you try to put in terms proportional to other entries in the matrix u? Actually I'm not even sure if the above expression is correct.
 
aaaa202 said:
I don't understand. So according to what you say we have that the most general relation is:

σij = λuij + λδijkukk

But what goes wrong if you try to put in terms proportional to other entries in the matrix u? Actually I'm not even sure if the above expression is correct.
The above equation is the most general linear relationship (I'm assuming you are calling u the strain tensor, which I call E). If F(E) is a tensorial function of the strain tensor E, then we can use the Cayley Hamilton theorem to represent F by ##F = α I + βE+γE^2##, where α, β, and γ are functions of the invariants of E. This is linear in E only if α is a function of the trace of E (which is the only invariant that is linear in the components of E), β is a constant, and γ =0.

Chet
 

Similar threads

  • · Replies 1 ·
Replies
1
Views
3K
  • · Replies 6 ·
Replies
6
Views
1K
  • · Replies 1 ·
Replies
1
Views
3K
  • · Replies 1 ·
Replies
1
Views
4K
  • · Replies 8 ·
Replies
8
Views
1K
  • · Replies 60 ·
3
Replies
60
Views
7K
  • · Replies 2 ·
Replies
2
Views
2K
  • · Replies 9 ·
Replies
9
Views
7K
  • · Replies 2 ·
Replies
2
Views
2K
  • · Replies 9 ·
Replies
9
Views
5K