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Next: References Up: Equations of the Hypoplastic Previous: 4. Version WU WEI
5. Version VON WOLFFERSDORF
This version was propesed in [4].
![\begin{eqnarray*}\kTb = f_b f_e \frac{1}{\tr (\hTb \cdot \hTb)} \Big[ F^2 \Db ... ...Tb^{^{\scriptstyle *}}) \vert\vert \Db \vert\vert \Big] \quad , \end{eqnarray*}](https://www2.uibk.ac.at/images/542x53/geotechnik/res/hypo_versions/img18.gif)
with

and

The factor F is

with

and
![\begin{eqnarray*}\cos 3 \theta := - \sqrt{6} \frac{\tr (\hTb^{^{\scriptstyle *... ...^{^{\scriptstyle *}}\cdot \hTb^{^{\scriptstyle *}}) \Big]^{3/2}} \end{eqnarray*}](https://www2.uibk.ac.at/images/251x75/geotechnik/res/hypo_versions/img23.gif)
The other scalar factors are:
![\begin{eqnarray*}f_d &:=& \left( \frac{e-e_d}{e_c-e_d} \right)^\alpha \ f_e &... ...\frac{e_{i0}-e_{d0}}{e_{c0}-e_{d0}} \right)^\alpha \Bigg]^{-1} \end{eqnarray*}](https://www2.uibk.ac.at/images/562x165/geotechnik/res/hypo_versions/img24.gif)
with

The void ratios must fullfill
![\begin{eqnarray*}\frac{e_i}{e_{i0}}= \frac{e_c}{e_{c0}} = \frac{e_d}{e_{d0}} = \exp \left[ - \left( \frac{3 p_s}{h_s} \right)^n \right] \quad . \end{eqnarray*}](https://www2.uibk.ac.at/images/314x53/geotechnik/res/hypo_versions/img26.gif)
This hypoplastic law has 8 parameters: the critical friktion angle , die granular hardness hs, die void ratios ei0, ec0 and ed0 the exponents n and
. They can be easily determined from simple index and/or element tests [2].
The parameters for different materials are [2]:
Material | ![]() ![]() |
hs [MPa] | n | ed0 | ec0 | ei0 | ![]() |
![]() |
Toyoura sand | 30 | 2600 | 0,27 | 0,61 | 0,98 | 1,10 | 0,18 | 1,00 |
Hochstetten sand | 33 | 1500 | 0,28 | 0,55 | 0,95 | 1,05 | 0,25 | 1,50 |
Schlabendorf sand | 33 | 1600 | 0,19 | 0,44 | 0,85 | 1,00 | 0,25 | 1,00 |
Hostun sand | 31 | 1000 | 0,29 | 0,61 | 0,91 | 1,09 | 0,13 | 2,00 |
Karlsruhe sand | 30 | 5800 | 0,28 | 0,53 | 0,84 | 1,00 | 0,13 | 1,05 |
Zbraslav sand | 31 | 5700 | 0,25 | 0,52 | 0,82 | 0,95 | 0,23 | 1,00 |
Ottawa sand | 30 | 4900 | 0,29 | 0,49 | 0,76 | 0,88 | 0,10 | 1,00 |
Ticino sand | 31 | 5800 | 0,31 | 0,60 | 0,93 | 1,05 | 0,20 | 1,00 |
SLB sand | 30 | 8900 | 0,33 | 0,49 | 0,79 | 0,90 | 0,14 | 1,00 |
Hochstetten gravel | 36 | 32000 | 0,18 | 0,26 | 0,45 | 0,50 | 0,10 | 1,80 |
plastics | 32 | 110 | 0,33 | 0,53 | 0,73 | 0,80 | 0,08 | 1,00 |
wheat | 39 | 20 | 0,37 | 0,57 | 0,84 | 0,95 | 0,02 | 1,00 |
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Next: References Up: Equations of the Hypoplastic Previous: 4. Version WU WEI Wolfgang Fellin
1999-10-01