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Strona 2_redak - Instytut Agrofizyki im. Bohdana Dobrzańskiego ...

Strona 2_redak - Instytut Agrofizyki im. Bohdana Dobrzańskiego ...

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28<br />

[176] for the determination of parameters of an elasto-plastic model describing the<br />

stress-strain relation for soybeans and corn.<br />

3.3. Microstuctural models<br />

A granular material is a discontinuous random system of elementary granules.<br />

The description of phenomena occurring in such a medium can be sought on the<br />

grounds of statistical mechanics of media with discrete structure [140] The microstructural<br />

approach undertakes an attempt at deriving general laws governing the<br />

behaviour of a granular material on the basis of interactions between individual<br />

granules [165]. This approach originates from molecular dynamics which is based on<br />

the description of movement of each particle of a system. Applied here are the laws of<br />

mechanical equilibrium, with the requirement that the laws be fulfilled by all the<br />

elements of the system. Macroscopic behaviour of granular material is strictly related<br />

with interactions taking place on the micro scale. The correlation between the solution<br />

and the initial orientation of the granules caused that in the beginning the method<br />

permitted only a qualitative description of the processes under consideration.<br />

Micromechanical models derive the description of macroscopic variables –<br />

stress and strain, from analysis of microscopic variables – deformation and<br />

displacement of individual grains of the medium and distribution of forces at the<br />

points of contact between the grains. It is assumed also that the macroscopic scale<br />

of length (the whole deposit of granular material) is several orders of magnitude<br />

greater than the microscopic scale of length (a single granule of the medium).<br />

The fundamental relation between the macroscopic stress (averaged over the<br />

deposit volume V) and the distribution of the microscopic variables: forces f C at<br />

the points of contact between granules and vectors of normal directions l C is<br />

obtained by averaging, for all the points of contact between the granules, the<br />

products of vectors f C and l C :<br />

σ<br />

1<br />

= f<br />

V<br />

∑<br />

C C<br />

ij i l j . i, j =<br />

C∈V<br />

1,<br />

2,<br />

3<br />

(3.5)<br />

This relation is based on the virtual work theorem. The total work performed by<br />

the microscopic forces at the contact points of grains is equal to the work<br />

performed by the macroscopic stress [32], assuming also that the distribution of<br />

forces f C and of normal vectors at the points of contact between grains l C are known.<br />

In figure 3.9 vector l C connects the centres of granules A and B contacting each other<br />

at point C: l C = X B – X A . Granule A acts on granule B with force f AB = –f BA = f C .<br />

A s<strong>im</strong>ilar relation can be derived for macroscopic strain with displacement and<br />

rotation of individual granules [33].

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