Lab Hint- Consolidation - Oedometer Test
Transcript of Lab Hint- Consolidation - Oedometer Test
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Specimen: 19 mm thk x 75 mm dia Plan Area: 4417.9 mm2
Final thickness of soil (Hs) found by oven specimen when test end.
{Hs Hf
or Hs
}
Change ofdial gauge
reading
Stress=
R =
Table 4sFinal
reading x
0.002
R =
Table 4s
reading x
0.002
Hf= 19
mm -
R x
0.002
Hs =(see the
above)
Hv=Hf-Hs
e Hv
Hs
Initial readin
R = Final readin
R reading = Final Initial
H
s
water
soil
H
f
Hi = 19
mm
Hf Hs Hv
e
Reduced thickness (mm) =
Dial gauge reading x 0.002
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1. Compression Index, Cc
The compression index, Cc, is the slope of the straight line portion (latter part
of the loading curve) of the e-log p curve, or
where e1 and e2are the void ratios at the end of consolidation under stresses p1
andp2respectively
2. preconsolidation pressure,pc
The preconsolidation pressure,pc, is the maximum past effective overburden
pressure to which the soil specimen has been subjected. It can be determined
by using the following simple graphical procedure (Figure 8b):
1. Determine the point 0 on the e-log p curve that has the sharpest
curveature.2. Draw a horizontal line OA.
3. Draw a line OB that is tangent to the e-log p curve at O.
4. Draw a line OC that bisects the angleA OB.
Produce the straight line portion of the e-log p curve to intersect OC atD. The
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2
21
12
21
logloglog
p
p
ee
pp
eeCc
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pressure at pointD is the preconsolidation pressure,pc.
3. Swelling Index, Cs
The swelling index, Cs, is the slope of the unloadingportion of the e-log p
curve.
In most cases the values of Cs is 1/4 to 1/5 of Cc.
4. Determination of Coefficient of Consolidation Cv
a.The Root Time Method
Graph of settlement thickness (mm) vs root time t (min)
The theoretical curve is linear up to about 60% consolidation and at 90%
consolidation the abscissa (AC) is 1.15 timesthe abscissa (AB) of the
projection of the linear part of the curve.
By trial and error or draw a reference line (1.15 time)
Find thet90
Determine cvusing the following procedure:
Coefficient of Consolidation cv= 0.848H2/t90
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4
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logp
p
eeC
s
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4. Determination of Coefficient of Consolidation Cv
b.The log time method
Graph of the dial gauge readings in the oedometer test against the logarithm of
time in minutes.
The theoretical curve consists of three parts: an initial curve which approximatesclosely to a parabolic relationship, a part which is linear and an a final curve to
which the horizontal axis is an asymptote at U = 1.0 or 100%. (a100 )
1 In the experimental curve the point corresponding to U= 0 can be determined
by using the fact that the initial part of the curve represents an approximately
parabolic relationship between compression and time. Two points were on the
curve are selected (A andB in Figure 7) for which the values of t are in the
ratio of 4:1, and the vertical distance between them is measured. An equal
distance set off above the first point fixes the point (as) corresponding to
U= 0. The point corresponding to U= 0 will not generally correspond to the
point (a0) representing the initial dial gauge reading, the difference being due
mainly to the compression of small quantities of air in the soil, the degree of
saturation being marginally below 100%. This compression is called the initial
compression.
2 The point corresponding to U=50% can be located midway between theas
anda100 points and the corresponding timet50obtained
Determine cvusing the following procedure:
Coefficient of Consolidation cv= 0.196H2/t50