04.07.2014 Views

download completo - SET - USP

download completo - SET - USP

download completo - SET - USP

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

A mixed BEM-FEM formulation for layered soil-superstructure interaction<br />

67<br />

⎡[<br />

H<br />

⎢<br />

⎢[<br />

H<br />

⎢<br />

⎣<br />

[ H<br />

i<br />

tt<br />

i<br />

bt<br />

i<br />

st<br />

]<br />

]<br />

]<br />

[ H<br />

[ H<br />

[ H<br />

i<br />

tb<br />

i<br />

bb<br />

i<br />

sb<br />

]<br />

]<br />

]<br />

[ H<br />

[ H<br />

[ H<br />

i<br />

ts<br />

i<br />

bs<br />

i<br />

ss<br />

] ⎤ ⎧U<br />

⎥ ⎪<br />

] ⎥ ⋅ ⎨U<br />

] ⎥ ⎪<br />

⎦ ⎩<br />

U<br />

i<br />

t<br />

i<br />

b<br />

i<br />

s<br />

⎫ ⎡<br />

i<br />

[ Gtt<br />

]<br />

⎪ ⎢ i<br />

⎬ = ⎢[<br />

Gbt<br />

]<br />

⎪ ⎢ i<br />

⎭ ⎣<br />

[ Gst<br />

]<br />

[ G<br />

[ G<br />

[ G<br />

i<br />

tb<br />

i<br />

bb<br />

i<br />

sb<br />

]<br />

]<br />

]<br />

i<br />

⎤ ⎧<br />

i<br />

[ G ⎫<br />

ts]<br />

Pt<br />

i ⎥ ⎪ i ⎪<br />

[ Gbs]<br />

⎥ ⋅ ⎨Pb<br />

⎬<br />

i ⎥ ⎪ i<br />

[ G ⎪<br />

ss]<br />

⎦ ⎩<br />

Ps<br />

⎭<br />

(7)<br />

Equilibrium and compatibility conditions can then be imposed on displacement<br />

and stresses along the boundary between the ith and (i+1) layers. For cases in which<br />

there are no relative movements between contact nodes, i.e., the case of ideal friction<br />

without the existence of prescribed forces in the interface and admitting that the side<br />

boundary is not disturbed, the relations can be expressed, respectively, as:<br />

{ u<br />

i<br />

t<br />

{ p<br />

} = { u<br />

i<br />

t<br />

i+1<br />

b<br />

} = −{<br />

p<br />

{ u } = {0}<br />

s<br />

}<br />

i+1<br />

b<br />

}<br />

(8.1)<br />

(8.2)<br />

(8.3)<br />

(8.4)<br />

{ p } = {0}<br />

s<br />

with i varying from 1 to η-1.<br />

Assuming that the lateral surface is sufficiently remote, it is possible to consider<br />

equations (8.3) and (8.4) in (7) to obtain the influence of each layer, which is given by:<br />

⎧<br />

i<br />

Pt<br />

⎨ i<br />

⎩Pb<br />

⎫ ⎡[<br />

K<br />

⎬ = ⎢<br />

⎭ ⎣[<br />

K<br />

i<br />

tt<br />

i<br />

bt<br />

]<br />

]<br />

[ K<br />

[ K<br />

i<br />

tb<br />

i<br />

bb<br />

] ⎤ ⎧U<br />

⎥ ⋅ ⎨<br />

] ⎦ ⎩U<br />

i<br />

t<br />

i<br />

b<br />

⎫<br />

⎬<br />

⎭<br />

(9)<br />

In this way, applying Eq. (9) to each layer i, and invoking equations (8.1) and<br />

(8.2), the given layer can easily be associated to the neighbouring layers.<br />

Assuming the first layer is i=1, the displacement at the base is null, describing a<br />

fixed medium and hence allowing expression (9) to be re-written as:<br />

1<br />

t<br />

{ P<br />

1<br />

b<br />

{ P<br />

1 1<br />

} = [ K ] ⋅{<br />

U }<br />

(10)<br />

tt<br />

t<br />

1 1<br />

} = [ K ] ⋅{<br />

U }<br />

(11)<br />

bt<br />

t<br />

for i=2, one has, from expression (9):<br />

2<br />

t<br />

{ P<br />

2 2 2 2<br />

} = [ K ] ⋅{<br />

U } + [ K ] ⋅{<br />

U }<br />

(12)<br />

tt<br />

t<br />

tb<br />

b<br />

Cadernos de Engenharia de Estruturas, São Carlos, v.9, n. 38, p. 63-82, 2007

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!