Thanks for mano's good material ! . *Z#cq0
hOV_Oqe4?
'oT|cmlc
These conclusions are important ,I think. ELD
+:b
?SB5b ,
3.1 Values of E' R,XD6' Q
HN^w'I'bp
Typical values may be selected from the following values: mxZ4
HD{
k:W=5{[
Wl?<c
uw00
Soft normally-consolidated clays ( 1400 - 4200 kPa) % ghJ*iHR
S[ i$e
Medium clays ( 4200 - 8400 kPa) [CsM<:C
1ME|G"$ ;
Stiff clays ( 8400 - 20000 kPa) ^75pV%<%
v)TUg0U=,
Loose normally-consolidated sands ( 7000 - 20000 kPa) *:k~g].Iz
;k-g_{M
Medium normally-consolidated sands (20000 - 40000 kPa) [+yGDMLs
T$f:[ye]Z
Dense normally-consolidated sands (40000 - 84000 kPa) PZ~`O
Bc5YW-QD
$]xE$dzJ
For over-consolidated sands, double the above values. u87=q^$
_3*: y/M_
3.2 Values of v' wrhBH;3
ik8|9m4/
Soft clay 0.35 - 0.45 c,+iU R<
4,o
%e,z
Medium clay 0.30 - 0.35 oA5<[&~<
Fa6H(L3
Stiff Clay 0.2 - 0.3 r{bgTG
+!D=SnBGs
Medium sand 0.3 - 0.35 PV5-^Y"v
jt0H5-x
These typical values should be used with caution. Soils are extremely variable materials and considerable expertise is needed to determine accurate parameters.