Thanks for mano's good material ! 3xbA]u;gp
$7,n8ddRy
RfFeAg,]/
These conclusions are important ,I think. gr yC#
r*y4Vx7
3.1 Values of E' mR?OSeeB
"c=\?
Typical values may be selected from the following values: v;irk<5
9CW .xX8
P3);R>j
Soft normally-consolidated clays ( 1400 - 4200 kPa) .DIHd/wA
,f4Hl%T;
Medium clays ( 4200 - 8400 kPa) Xq,{)G%9nM
R /iB
Stiff clays ( 8400 - 20000 kPa) t4
$cMf
-SZ^;t
Loose normally-consolidated sands ( 7000 - 20000 kPa) 4WU
6CN
vA"yy"B+ V
Medium normally-consolidated sands (20000 - 40000 kPa) Z-Zox-I1}-
0lY.z$V
Dense normally-consolidated sands (40000 - 84000 kPa) Bz]j&`
'lg6<M%#[
.z)E
For over-consolidated sands, double the above values. 8q}`4wCD$
'd'*4 )]k
3.2 Values of v' <{:$]3
q>f1V3
Soft clay 0.35 - 0.45 cl)%qIXj}H
A03,X;S+
Medium clay 0.30 - 0.35 ,}F{V>dhn
n`;=^^ B
Stiff Clay 0.2 - 0.3 x>7}>Y*(
"m(HQ5e)*
Medium sand 0.3 - 0.35 NmVc2V]I
#*XuU8q?
These typical values should be used with caution. Soils are extremely variable materials and considerable expertise is needed to determine accurate parameters.