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Koenders M. A. C. - Physics Of The Deformation Of Densely Packed Granular Materials, The

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Koenders M. A. C. Physics Of The Deformation Of Densely Packed Granular Materials, The
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Appendix A
Mathematical Appendix
A.1Isotropic tensors

Literature: [Jeffreys, 1931].

A.1.1Isotropic 2-tensor

The identity is ij; its inverse is also ij.

A.1.2Isotropic 4-tensor

The identity of rank-4 tensors is such that a rank-4 tensor Aijpq, which connects two symmetric rank-2 tensors has the inverse The isotropic tensor of rank 4 is Its inverse is A2 - photo 1

The isotropic tensor of rank 4 is Its inverse is A2Integrals of strings - photo 2

The isotropic tensor of rank 4 is

Its inverse is A2Integrals of strings of unit vectors The inverse of the - photo 3

Its inverse is

A2Integrals of strings of unit vectors The inverse of the latter is the - photo 4

A.2Integrals of strings of unit vectors

The inverse of the latter is the solution of the equation and In three - photo 5

The inverse of the latter is the solution of the equation and In three dimensions the corresponding expressions are The front - photo 6 and

Physics Of The Deformation Of Densely Packed Granular Materials The - image 7

In three dimensions the corresponding expressions are

Physics Of The Deformation Of Densely Packed Granular Materials The - image 8

The front factors 2, , /4 in 2-d and 4, 4/3, 4/15 in 3-d are easily gathered in a coefficient

Physics Of The Deformation Of Densely Packed Granular Materials The - image 9

where (2m)!! = 2.4.... (2m); (2m 1)!! = 1.3.5... (2m 1), m an integer. (see [Abramowitz and Stegun, 1965], Section 6.1.49).

A very useful coefficient is

Physics Of The Deformation Of Densely Packed Granular Materials The - image 10

A.3Elastic constants

Conversion of the isotropic elastic constants in two and three dimensions. Top line: 3-D; bottom line 2-D.

and : Lam constants

E : Youngs modulus, v : contraction coefficient (Poissons ratio)

K : bulk modulus, G : shear modulus

A4Fourier transforms and harmonic density Fourier transforms are a powerful - photo 11

A.4Fourier transforms and harmonic density

Fourier transforms are a powerful tool to solve differential equations. In this section the basic theory is explored, which is required for the characterisation of the fluctuations. To begin with a one-dimensional approach is taken, in which functions depend on one variable, the time t say. In the development below it makes sense to keep the integral sign with its boundaries together with the integration variable.

The appropriate tool for describing fluctuating physical phenomena is the auto-correlation function. For a fluctuating function of time z(t) (which is zero on average) it is defined as

Physics Of The Deformation Of Densely Packed Granular Materials The - image 12

It is seen that the expectation value z2 is just equal to z(0).

The Fourier transform Physics Of The Deformation Of Densely Packed Granular Materials The - image 13 of the function z(t) is defined as

Physics Of The Deformation Of Densely Packed Granular Materials The - image 14

The inverse transform is

Physics Of The Deformation Of Densely Packed Granular Materials The - image 15

which makes the delta function (the identity)

Physics Of The Deformation Of Densely Packed Granular Materials The - image 16

The latter has meaning only in the context of another function, as follows

Physics Of The Deformation Of Densely Packed Granular Materials The - image 17

In physical processes the infinite integral boundaries do not make sense and therefore a modified definition is employed, the truncated Fourier transform

Physics Of The Deformation Of Densely Packed Granular Materials The - image 18

Now calculate the inverse Fourier transform of the quantity Physics Of The Deformation Of Densely Packed Granular Materials The - image 19

The order of the integrals may be interchanged and therefore Integrating - photo 20

The order of the integrals may be interchanged and therefore

Integrating over using the properties of the delta function gives For a - photo 21

Integrating over (using the properties of the delta function) gives

For a time record that is much longer than the correlation time the upper - photo 22

For a time record that is much longer than the correlation time the upper boundary may be replaced by and it is seen that in the limit the inverse Fourier transform Sz(t) is just equal to the correlation function z(t). This is the famous WienerKhinchin theorem. The quantity density. z() is called the spectral intensity or harmonic (spectral) density.

In two or three dimensions the formulas are easily extended, by taking the integrals over multiple variables. The Fourier frequency then becomes a vector. In a spatial setting this vector is called the wave number k.

A.5Bessel functions

Literature [Abramowitz and Stegun, 1965].

Bessel functions are very useful in the evaluation of problems that have cylinder symmetry. There are various types. The best-known is the family of ordinary Bessel functions, or Bessel functions of the first kind. They can either be defined as a series expansion

Or as an integral where v denotes the order of the Bessel function - photo 23

Or as an integral

where v denotes the order of the Bessel function indicating which member of - photo 24

where v denotes the order of the Bessel function, indicating which member of the family is meant.

The other type of cylinder functions that are useful are the Modified Bessel Functions.

Or The Bessel functions have been studied extensively There are all manner - photo 25

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