solved problems in soil mechanics 1
TRANSCRIPT
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Solved Problems in Soil Mechanics
Prepared By:
Ahmed S. Al-Agha
February -2015
Based on Principlesof Geotechnical Engineering, 8t Edition
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Chapter (3) & Chapter (6)
Soil Properties
&Soil Compaction
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Soil Properties & Soil CompactionSolved Problems in Soil Mechanics
Ahmed S. Al-Agha
Useful Formulas:
You should know the following formulas:
V V V V V V VW W W W 0 , W W)
G 1 e , 1 % w ,
WV ,
WV
G 1 % w1 e , G 1 eG1 e S 1
.. G 1 Gw S 1 e e Gw/1S . e G.w , S VV , at saturation S 1 w
eG
w
100%e VV
V VV , n e
1 e , n VV
G , WV , WV 9.81KN/m 62.4Ib/ft , 1ton 2000Ib , 1yd327ft3Air content A VVD e ee e
Relative CompactionR. C ,,,, 100%Vmust be constant if we want to use the borrow pit soil in a construction siteor on earth dam or anywhere else.
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1. (Mid 2014):
a)Show the saturated moisture content is: W
: solid unit weight
Solution
S . e G.w , at saturat ionS1w eG Eq.1 G 1 e e
G 1, substitute in Eq.1
w G 1
G
1
G but G
1
G
w [ 1 1].b) A geotechnical laboratory reported these results of five samples taken from a
single boring.Determine which are not correctly reported, if any, show your work.:take 9.81kN/mSample #1:w30%, 14.9 kN/m, 27 kN/m , clay
Sample #2:w20%, 18 kN/m
, 27 kN/m
, silt
Sample #3:w10%, 16 kN/m, 26 kN/m, sandSample #4:w22%, 17.3 kN/m, 28 kN/m , siltSample #5:w22%, 18 kN/m, 27 kN/m, silt
Solution
For any type of soil, the mositure content
wmust not exceeds the saturated
moisture content, so for each soil we calculate the saturated moisture content from
the derived equation in part (a) and compare it with the given water content.
Sample #1:(Given water content30%w 9.81[ 114.9
127] 29.5% < 30% not correctly reported.Sample #2:(Given water content20%
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w 9.81[ 118 1
27] 18.16% < 20% not correctly reported.Sample #3:(Given water content10%w 9.81[ 116 126]23.58%>10%correctly reported.Sample #4:(Given water content22%w 9.81[ 117.3
128] 21.67% < 22% not correctly reported.
Sample #5:(Given water content22%w 9.81[ 118
127] 18.16% < 22% not correctly reported.
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2.(Mid 2013):If a soil sample has a dry unit weight of 19.5 KN/m
3, moisture content of 8%
and a specific gravity of solids particles is 2.67. Calculate the following:
a) The void ratio.b) Moisture and saturated unit weight.
c) The mass of water to be added to cubic meter of soil to reach 80% saturation.
d) The volume of solids particles when the mass of water is 25 grams for saturation.
Solution
Givens:
19.5KN/m , %w = 8% , G=2.67a)
G 1 e 1 9 . 5 2.679.811 e e0.343 b)
1 % w 19.5 10.08 21.06 KN/m 1 % w %wmeans %w @ S 100%
S.e = G.w %w . .
. 100%12.85%
So, . . 19.510.1285 22KN/mc)
21.06 KN/m Now we want to find @ 80% Saturation so, firstly we calculate %w @80%saturation:
%w% S. eG 0.80.343
2.67 100%10.27%
,% 19.510.1027 21.5 KN/mWeight of water to be added = 21.5-21.06 = 0.44KN/mMass of water to be added = 0.44 . 44.85 Kg/m
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Another solution:
V 1m The water content before adding water (%w 8 %The water content after adding water (
%w 10.27% @80%saturation
w Weight of waterWeight of solid WW :W
WV W 19.5119.5KNW W w W, W w ,and W, W wThen, W, 19.5 0.08 1.56 KN
W, 19.5 0.1027 2 KNWeight of water to be added = 2-1.56= 0.44KNMass of water to be added = 0.44 . 44.85 Kg
d)
M 25grams for saturation S 100% %w 12.85%
W 2 5 1 0
Kg 9.811000 24.52510
KN
W Ww 24.52510
0.1285 190.8510KNNow, G 2.679.8126.2KN/m V .
. 7.28410m 72.84 cm3
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3.(Mid 2013):An earth dam require one hundred cubic meterof soil compacted with
unit weight of 20.5 KN/m3and moisture content of 8%, choose two from the three
borrow pits given in the table below, knowing that the first must be one of thetwo borrow pits, the specific gravity of solid particles is 2.7. Choose the most
economical choice.
Some Explanations about the problem:
Borrow pits:
.
Available Volume:
.
,100:
,
V.
Solution
The first step is to find the value of Vfor earth dam that must be maintained inborrow pits.
1 % w G 1 e 20.510.08 2.79.811 e e 0 . 3 9 5e V VV 0.395
1 0 0 VV V 71.68 mThe value of V 71.68 mmust be maintained on each borrow pit.
Borrow pit No. Void ratio Cost($/m3)
Available volume(m
3)
1 0.6 1 80
2 1 1.5 100
3 0.75 1.7 100
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Now we calculate the total volume of each type that required for the dam:
For borrow pit #1:
e V V
V 0 . 6 V, 71.68
71.68 V, 114.68m
For borrow pit #2:
e V VV 1 V, 71.6871.68 V, 143.36m
For borrow pit #3:
e V VV 0 . 7 5 V, 71.6871.68 V, 125.44m
,
.
Totalrequired volume from borrow pit#1 =114.68mThe availablevolume from borrow pit #1= 80mThe restrequired volume from borrow pit #1= 114.688034.68m
,
,
34.68m:solid
For the rest required from borrow pit #1:
e V VV 0 . 6 34.68V,V, V, 21.675mNow, we calculate the required volume from borrow pits 2&3 and calculate the
cost of each volume and take the lowest cost soil.
For borrow pit #2:
e V VV 1 V, 21.67521.675 V, 43.35m
Required cost =43.351.565.025$For borrow pit #3:
e V VV 0 . 7 5 V, 21.67521.675 V, 37.93m
Required cost =37.931.764.48$Choose the borrow pit #lowest costSo, the two required soils are: 80mfrom borrow pit #1and37.93 mfrom
borrow pit #3.
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4.(Mid 2012):A soil sample has avoid ratio of 0.72, moisture content = 12% and G 2.72
determine the following:
a) Dry unit weight, moist unit weight (KN/m
3
).b) Weight of water in KN/m
3to be added for 80% degree of saturation.
c) Is it possible to reach a water content of 30% without changethe present void
ratio.
d) Is it possible to compact the soil sample to a dry unit weight of 23.5 KN/m3.
Solution
Givens:e0.72 , %w = 12% , G=2.72a) G 1 e 2.729.8110.72 15.51 KN/m. 1 % w 15.51 10.12 17.374 KN/m.
b)
The original value of =17.374 KN/mThe value of@80% degree of saturation can be calculated as following:S.e = G.w %w% .... 0.2117 ,% 1 % w 15.51 10.2117 18.8 KN/m.So, the of water added= 18.817.3741.428 KN/m.c)e0.72 , %w = 30% , G=2.72 , S% ? ?We know that the max.value of S=1 so, if the value of S% > 1 its not
possible, but if S% 1 its possible.S.e = G.w S% .... 100% 1.133 > 1 Not possible.d)
, 23.5 KN/m Can we reach to this value after compaction???, toKnow this, we find the maximum possible value of=..(Zero Air Voids)
.. G 1 e e G. wS
2.720.121 0.3264
.. G 1 e 2.729.8110.3264 20.12 < 23.5 Not pssible
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5. (Mid 2011):An undisturbed sample of clayey soil is found to have a wet weight
of 285 N, a dry weight of 250 N, and a total volume of 14x103cm
3 if the specific
gravity of soil solids is 2.70, determine the water content, void ratio ,and thedegree of saturation.
Solution
Givens:
W 285N , W 250N , V 14x103cm3 , G 2.7 % w 100%
100%14% .
+, but
? ? ?
17.86KN/m
17.86 ..+ e0.483 . S.e = G.w S ... 0.781278.12%.6.(Mid 2011):
A proposed earth dam requiers 7500 m3of compacted soil with relative
density of 94% , maximim void ratio of 0.73, minimum void ratio of 0.4 and
specific gravity (G)=2.67. Four borrow pits are available as described in thefollowing table.Choose the best borrow pit with minimum cost.
Borrow PitDegree of
saturation %Moisture content
%Cost ($/m
3)
A 82 18.43 10
B 100 24.34 5
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Solution
Givens:
D 94% , e 0.73 , e 0.4 , G 2.67
V
)(
So, firstly we calculate the value of Vthat required for earth dam as following:e
, but e ? ? ? D
0 . 9 4 .
.. e 0 . 4 2 0 . 4 2 V 5281.7mthat must be maintained.
,V 5281.7For sample A :
S =82% , %w =18.43%
e V VV , but e ? ? ? e G wS 2.670.18430.82 0.6
0 . 6 V 5281.75281.7 V 8450.72 m.So, the total cost for sample A =8450.72 m 10 $ 84,507$ .For sample B :
S =100% , %w =24.34%e V VV , but e ? ? ? e G wS 2.670.24341 0.65
0 . 6 5 V 5281.75281.7 V 8714.8 m.So, the total cost for sample B =8714.8 m 5 $ 43,574$ .So, we choose the sample B beacause it has the lowest cost.
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Ahmed S. Al-Agha
7.(Mid 2010):Earth is required to be excavated from borrow pits for building an embankment as
shown in the figure below.The moisture unit weight of the borrow pits is18 kN/m3
and its water content is 8%. Estimate the quantity of earth required to be excavatedper meter length of embankment. The dry unit weight required for the embankment
is 15 kN/m3with a moisture content of 10%. Assume the specific gravity of solids
as 2.67. Also determine the degree of saturation of the embankment soil and the
volume of water in the embankment.(hint: Volume of emankment per meter length)
Solution
): (borrow pit....
(embankment),
...
V.Givens:
-For borrow pit
18kN/m3 , %w = 8% , G 2.67-For Soil of embankment
15kN/m3 , %w = 10% , G 2.67 , V From the given figure
Embankment
According to the
given slopes and
dimensions
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Required:
a)Now, for emabankment V area of the embankmenttrapezoidal/meter length
V 2 1 0 4 1 2 4m3
/m. + 1 5 ..+ e 0 . 7 4 6e 0.746
V 13.74m3/m (that must be maintained) .
Now, for borrow pit 18kN/m3 , %w = 8% , G 2.67 ,V ? ? + +. 16.67kN/m3.
+ 16.67 ..+ e 0 . 5 7
e 0 . 5 7 .. V 21.6m3
/m
`
.b)%w = 10% , G 2.67 , e0.746S.e = G.w S ... 0.35835.8%.c)
S , but V ???n , also n + .+. 0.427
V n V 0.4272410.25m3/m`V S V 0.35810.253.67m3/m`.
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8.(Mid 2010):The results of a standard compaction test for a soil having a value of
. are shown in the table below.Water Content (%) 6.2 8.1 9.8 11.5 12.3 13.2
Unit Weight (KN/m3) 16.9 18.7 19.5 20.5 20.4 20.1
Find:
The optimum water content.
The maximum dry unit weight.
The void ratio (e).
Degree of saturation (S).Moisture unit weight.
Find the weight of water need to be added to 1m3to reach 100%
degree of saturation.
Solution
Firstly, we caluculate the value of dry unit weight in the following table:
From the above table we note that the optimum water content = 11.5%And the maximum dry density = 18.4 kN/m
3and the following graph will ensure
these results:
Water Content (%) 6.2 8.19.8
11.5 12.3 13.2
Water Content (value) 0.062 0.081 0.098 0.115 0.123 0.132
Unit Weight (KN/m3) 16.9 18.7 19.5 20.5 20.4 20.1
Dry unit Weight (KN/m3) 15.91 17.3 17.76 18.4 18.17 17.76
%w100
1 w
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Now, we have the following:
18.4kN/m3 , %w =11.5% , G 2.5 Gs w1 e 18.4
2.59.811 e0.334 .
S.e = G.w S ..
. 0.8686%
.Moisture unit weight exist in the given table and equal 20.5(this part just for confusionso, trust by yourself).
The last requiered :
S=100% w% .. 0.13413.4%,% 18.410.134 20.86 KN/mWeight of water to be added = 20.8620.5 = 0.36KN/m.
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9.(Mid 2009):A sample of saturatedclay was placed in a container and weighed. The
weight was 6N. The clay in its container was placed in an oven dray for 24 hours
@ 105. The weight reduced to a constant weight of 5N. The weight of thecontainer is 1N. If G 2.7, determine:(a).Water content.
(b).Void ratio.
(c).Moist unit weight.
(d).Dry unit weight.
(e).Effective unit weight (Submerged unit weight).
Solution
Givens:W W 6N , W W 5N , W 1 N , G 2.7(a).
W Wwet WContainer WContainer 6 1 5 N .W W W W 5 1 4 N.%w W WW 100%
5 44 100%25% .
(b).
Saturated clayS=1S.e = G.w .. 0.675.(c).
,% +@+ ..+.+. 19.76 KN/m.(d).
+ .+. 15.8 KN/m.(e).Effective unit weight :
. 19.76 9.81 9.95 KN/m.
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Ahmed S. Al-Agha
10. (Mid 2009):An earth dam requires one million cubic meter of soil compacted to a
void ratio of 0.8. In the vicinity() of the proposed dam,three borrow pits
were identified as having suitable materials. The cost of purchasing the soil andthe cost of excavation are the same for each borrow pit. The only difference of
the cost for each borrow pit is the cost of transportation.
Which borrow pit would be the most economical?
Borrow pit No.Voidratio
Transportation cost($/m
3)
1 1.8 0.6
2 0.9 1
3 1.5 0.75
Solution
1:
...,V0.8 3,
V.
Firstly, we calculate the value of
Vthat required for earth dam as following:
e 0 . 8 ,, V 555,555.5mthat must be maintained.For borrow pit #1 :
e=1.8
e V VV 1 . 8 V 555,555.5555,555.5 V 1,555,555.4 m.
So, the total cost for borrow pit #1=1,555,555.4 m 0.6 $ 933,333$ .
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For borrow pit #2 :
e=0.9
e V V
V 0 . 9 V 555,555.5
555,555.5 V 1,055,555.4 m
.
So, the total cost for borrow pit #2=1,055,555.4 m 1 $ 1,055,555.4$ .For borrow pit #3 :
e=1.5
e V V
V 1 . 5 V 555,555.5
555,555.5 V 1,388,888.8 m.
So, the total cost for borrow pit #2=1,388,888.8 m 0.75 $ 1,041,666.6$ .Choose the borrow pit #1 which has the lowest cost .
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Ahmed S. Al-Agha
11. (Mid 2007):A dry sand is placed in a container having a volume of 0.3 ft
3. The dry
weight of the sample is 31 Ib. Water is carefully added to the container so as not to
disturb the condition of the sand. When the container is filled, the combinedweight of soil plus water is 38.2 Ib. From these data, compute the void ratio of soil
in the container, and the specific gravity of the soil particles.
[Hint: water density = 62.4 Ib/ft3]
Solution
...,:
..
%
100.Givens:
V 0.3ft3 , W 31Ib , S=1 , W 38.2Ib%w 100%
. 100%23.2%
. 103.33Ib/ft3
Also, + 103.33 .+ S.e = G.w 1 e 0 . 2 3 2 G
Substituting from 2 to 1103.33 .+. G 2.69.e0.232G 0.2322.690.624.
Eqn.1
Eqn.2
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Ahmed S. Al-Agha
12. (Mid 2007):The moistdensiteis and degree of saturation of a soil sample are given in the
following table:
Soil Density (Kg/m
3
) Degree of Saturation (%)1690 45
1808 75
Determine the weight of water in Kg, that will be in 7 m3of the soil when it
saturated.
Solution
Firstly, we must find the values of G , ewe know that +
+,and w .
So, the eqn. will be in this form : +.+ Case#1:
1690Kg/m3 , S = 45% , substitute in Eqn.*
1690
G 1 0 0 0 1 0.45eG
1 e
Case#2:
1808Kg/m3 , S = 75% , substitute in Eqn.*
1808 G 1 0 0 0 1 0.75eG 1 e
Now, by solving the two equations (solve by your self) the results are :G 2.49 , e0.648Now, the required is the weight of water in Kg will be added in V 7m3whenS=100%(saturated)
Eqn.*
Eqn.1
Eqn.2
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w% S eG 10.648
2.49 0.2626%.w , w , Mrequired , but M ???
Now, G 10002.492490 Kg/m3 MV M 2490V.n e1 e
0.64810.648 0.393.
n V 0.39372.751m3V V V 72.7514.25m3.So, M 2490 4.25 10582.5 Kg.Finally, M w M 0.2610582.52751.45Kg.
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13. (Mid 2006):A borrow material has a volume of 191,000 m
3and void ratio of 1.2. After
compaction its new void ratio is 0.7, find the corresponding volume?
SolutionGivens:
V, 191,000m3 , e 1.2 , V, ??, e 0.7The main idea of this problem that the value of Vis constant.Befor compaction:
e , 1 . 2 ,
V 86818.18m3After compaction:
e ,
0 . 7 ,.
. V, 147,590.9 m3
.14. (Mid 2006):The total volume of a soil soecimen is 80,000 mm
3and it weighs 150
grams. The dry weight of the specimen is 130 grams and the density of the soil
solids is 2680 Kg/m3. Find the following:
a) The water content.
b) Void Ratio.
c) Porosity.
d) Degree of saturation.e) Saturated unit weight.
f) Dry unit weight.
Solution
Givens:
V 80,000mm3 , M 150gm , M 130 gm , 2680Kg/m3a)
%w 100% 100%15.38%.
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b)
G 26801000 2.68
V 80,000mm3
80,00010 8 0 1 0m3
1625Kg/m3
G 1 e 1 6 2 5 2.681000
1 e e 0 . 6 4 9.c)
n e
1 e
0.649
10.649
0.393.d)S.e=G. w S . ... 0.63563.5% .e)
S=1 w% .. 0.24224.2,% +@+ ..+.+. 19.8KN/m3.
f) 1625Kg/m3 16259.8110 15.94KN/m3.
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15. (Mid 2005):A sample of moist soil was found to have the following characteristics:
Volume 0.01456 m3(as sampled)
Mass 25.74 Kg (as sampled)22.10 Kg (after oven drying)
Specific gravity of solids:2.69
Find the density, dry unit weight, void ratio, porosity, degree of saturation forthe soil.
What would be the moist unit weight when the degree of saturation is 80%?
Solution
Givens:
V 0.01456m3 , M 25.74 Kg , M 22.1 Kg , G 2.69
(The first required is density that means moist and dry densities)
.
. 1767.56Kg/m3.
.. 1517.86Kg/m3.
1517.86Kg/m3 1517.869.8110 14.89KN/m3. G 1 e 14.89 2.699.811 e e0.772 .S.e=G. w w ? ? 1 w 1767.561517.861 w w0.164516.45%S G. we
2.690.16450.772 0.57357.3% .
w S. eG 0.80.7722.69 0.22922.9% ++ ..+.+. 18.3KN/m3.
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16. (Final 2009):Dry soil with G 2.7is mixed with water to produce 20% water content
and compacted to produce a cylindrical sample of 40 mm diameter and 80mm long
with 5% air content. Calculate the following:A-Mass of the mixed soil that will be required.
B-Void ratio of the sample.
C-Dry, moisture and saturated unit weight.
D-Amount of water to be added for full saturation.
Solution
Givens:
V volime of the cylindrical sample 0.04
0.081.00510m3
%w=20% , air content =5% , G 2.7Important Note: Air content =
0 . 0 5 V 0.05V.
A-
M Mbecause the mixed soil is a dry soil and M Mw =
M
. M 5 M
G 10002.72700Kg/m3 M 2700 VV V V, and V
, and V V V
V V 0.05V but, V 1.00510 and 1000Kg/m3So, V 0.95V V 9 . 5 105 0.001M
Now, substitute in Eqn.2: M 0.25652.7 M Substitute in Eq. 10.25652.7 M = 5M M 0.0333Kg.M 5 0.0333 0.1665 Kg.
Eqn.1
Eqn.2
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B-
e = V 9 . 5 105 0.001M V 9 . 5 105 0.001 0.0333V 6.1710m3
V VT VS 1.005104 6.1710 3.8810m3
Then,e =.. 0.628.
C-
+ ..+. 16.27KN/m3. ++ ..+.+. 19.52KN/m3. +
+ (Saturated S 1 w
..+.. +. 20.05KN/m3.D-
Amount (KN/m3) Amount (KN) V
Amount (KN) 20.0519.52 1.00510 5.326510KN.Amount (Kg) 5.326510 . 5.429610Kg.
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Ahmed S. Al-Agha
17.Moist clayey soil has initial void ratio of 1.5, dry mass of 80gm, and specific
gravity of solid particles of 2.5.The sample is exposed to atmosphere so that the
sample volume decrease to one halfof its initial volume . Calculate the following:a) The new void ratio.
b) Mass of water if degree of saturation became 25 %.
Solution
Givens:
e 1.5 , M M 80gm , G 2.5 ,V, 0.5V,a)
Firstly, we must calculate the value of
Vthat must be the same in each case.
e , 1 . 5 , , V, ? ? ? , + ., .+. V, 8 1 0m3.So, 1.5 V 3 . 2 1 0m3.
Now, V, 0 . 5 8 1 0 4 1 0m3.e V, V
V 4 1 0 3.210
3.210 0.25.
b)
e0.25 , S=25% , G 2.5S.e = G. w w ... 0.0252.5%.w M 0 . 0 2 5 0 . 0 8 2 1 0Kg 2g m.
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Page (27)
Soil Properties & Soil CompactionSolved Problems in Soil Mechanics
Ahmed S. Al-Agha
18.Soil has been compacted in an embankment at a bulk unit weight of 2.15 t/m
3
And water content of 12% , the solid particles of soil having specific gravity of 2.65.
a) Calculate the dry unit weight, degree of saturation, and air content.b) Would it possible to compact the above soil at a water content of 13.5% to a dry
unit weight of 2 t/m3.
Solution
Givens:
2.15 t/m32.159.8121.0915KN/m3(assumeg=9.81m/s
2)
%w=12% , G 2.65a) + .+. 18.83KN/m3.
G 1 e 18.832.659.81
1 e e 0 . 3 8 .S.e = G. w S ... 0.83783.7%.Air content =
? ?
V V VV V V
w W 0.12 WG
WV G WV W G V
Substitute in Eqn. 1 W 0.12 2.65 9.81 V W 3.12 V
V W V 3.12 V9.81 0.318 V
18.83
V 0.7243 V V 0.318 0.7243 V 0.23 V
Eqn.
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Page (28)
Soil Properties & Soil CompactionSolved Problems in Soil Mechanics
Ahmed S. Al-Agha
Substitute in Eqn.*
V V Vair Vwater
V 0.7243 V V 0.23 V (Dividing by
V
1 0 . 7 2 4 3 VV 0.23 VV 0.0457 4.57% Air content.
b)
%w =13.5% , 2t/m329.8119.62KN/m3(need to check)If.. > 19.62 Ok , else Not Ok.
.. G 1 e e
G. wS
2.650.1351 0.3577
.. ..+. 19.147KN/m3
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Soil Properties & Soil CompactionSolved Problems in Soil Mechanics
Ahmed S. Al-Agha
19.A specimen of soil was immersed in mercury. The mercury which came out
was collected and its weight was 290gm. The sample was oven dreid and its
weight became 30.2gm. if the specific gravity was 2.7 and weight of soil in naturalstate was 34.6gm. Determine :
a) Tge void ratio,and porosity.
b) Water content of the original sample.
c) Degree of saturation of the original sample.
[Hint: the dnsity of mercury is 13.6 gm/cm3]
Solution
Givens:
M. 290gm , M 30.2gm , M 34.6gm , G 2.7Archimedes Law:The volume of specimen equalthe voulme of liquid came out.V . 21.32cm321.3210m3.a)
.
. 1416.51Kg/m3 G 1 e 1416.51
2.710001 e e 0 . 9 0 6.
n e1 e 0.9060.9061 0.475.b)
%w M MM 100%34.630.2
30.2 100%14.57%.c)
S.e = G. w S ... 0.434243.42%.
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Page (30)
Soil Properties & Soil CompactionSolved Problems in Soil Mechanics
Ahmed S. Al-Agha
20. (Important)The in-situ(field) moisture content of a soil is 18% and its moisture unit
weight is 105 pcf (Ib/ft3). The specific gravity of soil solids is 2.75. This soil is to
be excavated and transported to a construction site ,and then compacted to aminimum dry weight of 103.5 pcf at a moisture content of 20 %.
a) How many cubic yardsof excavated soil are needed to produce 10,000 yd3of
compacted fill?
b) How many truckloads are needed to transprt the excavated soil if each truck can
carry 20 tons?
[ Hint: 1ton = 2000Ib , 1yd3=27ft3 , 62.4pcf ](I advise you to remember these units)Solution
Givens:
For excavated soil (in-situ soil)
%w=18% , 105 pcf , G 2.75 For soil in the constrction site
%w=20% , 103.5 pcf , G 2.75..:
..
... V
W.. . (a
V, ? ? , V, 10,000yd3For constrction site soil G 1 e 103.5
2.7562.41 e e 0 . 6 5 8
e 0.658,
V 6031.36yd3(That must be maintained)Now,
for excavated soil
G 1 w 1 e 1 0 5 2.7562.410.181 e e0.9284e 0.9284 .. V 11,631.4 yd3.
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Ahmed S. Al-Agha
b)
To find the number of trucks to transport the excavated soil we need two things:
- The total volume of excavated soil (in part awe calculate it =11,631.4 yd3)
- The total volume of each truck.Each truck can carry 20 tons of excavated soil .we want to convert this weight to
volume as following:
For each truck:
V, ,
,
380.95 ft3.V, 380.95 ft3 . 14.1yd3So, # of trucks =
, ,
,.. 824.9 truck
.
Dont say 825 because you have only 90 % (0.9) of the truck.
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Page (32)
Soil Properties & Soil CompactionSolved Problems in Soil Mechanics
Ahmed S. Al-Agha
21. (Important)An embankment for a highway 30 m wide and 1.5 m thick is to be
constructed from sandy soil, trucked in from a borrow pit .The water content of the
sandy soil in the borrow pit is 15% and its void ratio is 0.69. Specifications requirethe embankment to compact to a dry weight of 18 KN/m3. Determine- for 1 km
length of embankment-the following:
a) The dry unit weight of sandy soil from the borrow pit to construct the
embankment, assuming thatG 2.7.b) The number of 10 m
3truckloads of sandy soil required to construct the
embankment.
c) The weight of water per truck load of sandy soil.
d) The degree of saturation of the in-situ sandy soil.
Solution
Givens:
For borrow pit (in-situ soil)
%w=15% , e 0.69 , G 2.7 For embankment soil
V 30 1.5 1000 45,000 m, 18 KN/m , G 2.7:
(
(borrow pit
.. V.
a)
+ ..+. 15.67KN/m3.b)
V, 10m3 but V, ? ?For embankment soil: G 1 e 1 8 2.79.811 e e0.4715.e 0.4715 , V 30,581m3(That must be maintained)
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Now, for borrow pit soil:e 0 . 6 9
,, V, 51,682m3.
So, # of trucks =,
, ,
5168.2 truck
.
c)
For each truck V, 10m3 15.67KN/m3for borrow pit soilNow, for each truck W, V, W, 1015.67156.7KN.%w=
W, 156.70.1523.5KN.
d)S.e=G. w S ... 0.58758.7%.
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Page (34)
Soil Properties & Soil CompactionSolved Problems in Soil Mechanics
Ahmed S. Al-Agha
22. ( Very Important)Your company has won a contract to provide and compact the fill material
for an earth levee((with the dimensions shown below. The
levee fill is a silty clay soil to be compacted to at least 95% of maximum standardproctor of 106pcfat an OMC of 18%. Your borrow pit has a silty clay withan in-situ moist density of 112.1pcf at 18% moisture content,and G 2.68.Whenthe soil is excavated and loaded on to your trucks, the void ratio of material is
e=1.47. Your trucks can haul 15 yd3of materials per trip.
a) Determine the volume of fill required for levee.
b) Determine the volume required from the borrow pit.
c) Determine the required number of trucks.
Solution
Givens:
For borrow pit (in-situ soil)
112.1pcf , %w=18% ,
G
2.68 For earth levee fillVDimensions, R .C 95% (Relative Compaction),,, 106pcf%w = OMC =18% (Optimum Moisture Content) G 2.68
For excavated soil (that will be loaded):e 1.47 , G 2.68 , V, 15yd3
Earth Levee
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Page (35)
Soil Properties & Soil CompactionSolved Problems in Soil Mechanics
Ahmed S. Al-Agha
..3:
... :
.. :
.
...e=1.47
..
a)Volume of Levee= (Area of trapezoidal) X (Length of Levee)
V, ( 2 0 2 0 4 0 6 0) 2 0 450 630,000ft3.b)
Forthe earth levee:R . C ,, , 0.95106100.7pcf.(Thats the true value in site) G 1 e 100.7
2.6862.41 e e 0 . 6 6
e 0 . 6 6 ,
V 379,518ft3 (That must be maintained)Now, for borrow pit soil:
++ 112.1 ..+.+ e 0.76
e 0 . 7 6 ,
, V, 667,951.7ft3 .c)
# of trucks =, , , e =1.47 for excavated soile 1 . 4 7
,, V, 937,409.5ft3
V, 15 yd3 1 5 2 7=405 ft3# of trucks =. 2314.6truck.
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Chapter (5)
Classification of Soil
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Page (37) Ahmed S. Al-Agha
Classification of SoilSolved Problems in Soil Mechanics
How to classify soil according Unified Soil Classification System
(USCS)
1. Finding Group Symbol from (Table 5.2 P.131) According the
following procedures:
a. Determine whether the soil isCoarse-grainedorFine-grained:
- If R > 50% Coarse grained soil.- If R 50% Fine grained soil
Where:R= Cumulative % retain on sieve # 200 (0.075 mm sieve opening).b. If the soil is Coarse-grained soilFollow the following:
- If > 5 0 % The soil is Gravel.- If 5 0 % The soil is Sand.Where: R= Cumulative % retain on sieve # 4 (4.75 mm sieve opening).
Coarse fraction retained on #4 seive.- If the soil is gravel Follow the following: If F < 5 % Choose Group Symbol according to values of (Cu& Cc) If F > 1 2 % Choose Group Symbol according to values of (PI) and
you may use the footnote (d) below table (5.2) if4 P I 7. If
5 % F 1 2 % Choose Group Symbol according to footnote (a)
below table (5.2).
- If the soil is sand Follow the following: If F < 5 % Choose Group Symbol according to values of (Cu& Cc) If F > 1 2 % Choose Group Symbol according to values of (PI) and
you may use the footnote (d) below table (5.2) if4 P I 7. If 5 % F 1 2 % Choose Group Symbol according to footnote (b)
below table (5.2).
Where: F200= Cumulative % passing from sieve # 200 (% Fines)Important Notes: If you have to go to footnote (d) below the table you must choose
GC-GMif the soil is gravel,and choose SC-SMif the soil is sand Aline equation PI 0.73L L 2 0If PI PIon, If PI > PIabove, If PI < PIbelow
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Classification of SoilSolved Problems in Soil Mechanics
If you have to go to footnote (a) or (b) below the table you havemore than one choice. How to find the correct symbol:
Assume that you have a gravel soil (for example) and5 % F200 12%You have to go to footnote (a) and you have the following choices:
(GW-GM, GW-GC, GP-GM, GP-GC) only one of them is true.
You will take each symbol and check it whether achieve the conditions or not
Firstly, you take GW-GM and check it you must check each part of this
dual symbol as following:
GW: check it from table 5.2 according to values of (Cu& Cc)
GM: check it from table 5.2 according to value of (PI)
If one of them doesnt achieve the condition you will reject the symbol
(GW-GM) and apply the same procedures on other symbols tillone of the
symbols achieve the conditions (each part (from the 2 parts)) achieve the
conditionsonly one symbolwill achieve the conditions.
If you check GW (for example) in GW-GM, you dont need to check it
another time in GW-GC ..Because it is the same check.
The same procedures above will apply if you have to go to footnote (b).
c. If the soil is Fine-grained soilFollow the following:- According to value of liquid limit (LL) either LL< 50or LL50.- Always we deal with inorganicsoil and dont deal with organic soil.
- If LL
< 50, Choose Group Symbol according to values of (PI) and you may
use the footnote (e) below table (5.2) if4 P I 7.- If LL 50,Choose Group Symbol according to comparison between PI ofsoil and PI from Aline.
2. Finding group name:
a. From (figure5.4 P.133)for Coarse (gravel & sand) and from (figure 5.5
P.143) for Fines(silt & clay).
b. To find group name easily you should know the following:
% Sand R R , % Gravel RThe value of (PI) >>>( in what range).Comparison between PI& PIto know (on, above or below A-line).% Plus #200 sieve = % cumulative retained on #200 sieve R.
Important Note:All values of R, Rand Fmust depend on sieve analysis>>must be cumulative (Rincrease with opening decrease and Fdecrease with
opening decrease).
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Classification of SoilSolved Problems in Soil Mechanics
23. (Mid 2013):Classify the following soils using the unified soil classification system.
give group symbol & group name.
a. A 55% of soil sample retained on sieve No.4 and 89% retained on sieve
No.200. The soil has a liquid limit (LL) =28% and plastic limit (PL) =18% ,
Cu=4.2, Cc=1.4, (A-line: PI=0.73(LL-20)).
Solution
Givens:R 55% , R 89%(R increase>> so,Comulative) ,F 1 0 0 % R 11% , LL=28% , PL=18% , PI = LL-PL=28-18=10%Cu=4.2 , Cc=1.4
1. Finding Group Symbol from Table (5.2):
a) Determine whether the soil is Coarse-grainedor Fine-grained:
R 89%>50%Coarsegrained soil.b) Determine whether the soil is gravel or sand:
100%
100%61.8%>50%The soil is Gravel.
- F 1 1 % 5 % F 1 2 % Choose Group Symbol according thefootnote (a) below table (5.2).
- The group symbol must be one of the following :GW-GM, GW-GC, GP-GM, GP-GC>> Now we check each symbol
GWaccording the values of Cu& Cc:Cu=4.2>4 AND Cc=1.4 (1 C c 3) GW is Ok.GMaccording the values of PI or A-line equation:PI=10% >4Not ok OR PI plots below A-linePI 0.732 8 2 0 5.84 < 10 above not belowGM is Not OkSo, each symbol having GM must be canceled(GW-GM & GP-GM)
Now we want to check only one of (GC and GP) to know the correct symbolbecause one of them is true and the other is false
Try GPaccording the values of Cu& Cc:Cu=4.2>4 not ok AND/OR Cc=1.4 (1 C c 3) not ok GP isNot OkGP-GC Not Ok so, the group Symbol is GW-GC.Note: (1> Cc>3) means Cc>3 OR Cc
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Page (40) Ahmed S. Al-Agha
Classification of SoilSolved Problems in Soil Mechanics
2. Finding Group Name from Figure (5.4):
% Sand R R 8 9 % 5 5 % 3 4 % > 1 5 % The group name is:Well-graded gravel with clay and sand (or silty clay and sand) .
b. 200 grams of a soil sample has a grain size distribution as shown in the table
below with a liquid limit of 32% and plastic limit of 15%.
Particle Size (mm) 4.75 2.36 1.3 0.6 0.2 0.075
Retained (grams) 12 15 13 28 20 2
Solution
Givens:
LL=32% , PL=15% , PI = LL-PL= 3215=17% , M 200 gram,From the given table we note the following:
The given is the mass retained (not percent).
The given mass is not comulative.
So, we must calculate the % comulative Retained as shown in thefollowing
table : #4 #200
Particle Size (mm) 4.75 2.36 1.3 0.6 0.2 0.075
Retained (grams) 12 15 13 28 20 2
Cumulative Retained (grams) 12 27 40 68 88 90
% Com. Retained (%) 6 13.5 20 34 44 45
% Com. Passing (%) 94 86.5 80 66 56 55
Calculation in the above table was done according the following:
Cumulative Retained (grams) 1212+15=2727+13= 4040+28=68 and so on.% Com. Retained (%) = 100%% Com. Passing (%) = 100% % Com. Retained (%)Now, from the above table R 6% , R 45% , F 55%1. Finding Group Symbol from Table (5.2):
a) Determine whether the soil is Coarse-grainedor Fine-grained:
R 45% < 50% Fine grained soil.
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Classification of SoilSolved Problems in Soil Mechanics
b) Finding group symbol from the lower part of table (5.2):
LL 3 2 < 5 0 & Inorganic soil Classify according PI and A-line P I 1 7 % > 7
PI 0.733 2 2 0 8.76 7 AND Plots above A-line Group Symbol is CL.2. Finding Group Name from Figure (5.5):
The following parameters will be used:
LL=32 , PI=17andPlots above A-line , %plus No.200 =R 45%% Sand R R 4 5 6 3 9 % , %Gravel =R 6%
Now, we find group name as following:
LL 3 2 < 5 0 I n o r g a n i c P I > 7and Plots above A-line
CL R 4 5 % > 3 0 % % S a n d 3 9 % > % G r a v e l 6 %
%G rav el6%
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Classification of SoilSolved Problems in Soil Mechanics
24. (Mid 2012):Using the unified soil classification system to classify the following soils.
(Group Symbol & Group Name).
a. A 65% of the soil sample retained on No.4 Sieve, 30% retained on No.200Sieve, Cu=3 and Cc=0.9.Also the LL = 28% and PL = 24.5% ,
(A-line: PI = 0.73(LL-20)).
Solution
Givens:
R 65% , R 6 5 % 3 0 % 9 5 % F 5%(Why)Because thevalues must be cumulative and we know that %Retain must increase ..but in this
case %Retain decrease thus, it must be cumulative by adding 65% to 30% .
LL=28% , PL=24.5% , PI = LL-PL= 2824.5=3.5 %PI 0.732 8 2 0 5.84>3.5below.1. Finding Group Symbol from Table (5.2):
a) Determine whether the soil is Coarse-grainedor Fine-grained:
R 95%>50%Coarsegrained soil.b) Determine whether the soil is gravel or sand:
100%
100%68.4%>50%The soil is Gravel.
- F 5 % 5 % F 1 2 % Choose Group Symbol according thefootnote (a) below table (5.2).- The group symbol must be one of the following :
GW-GM, GW-GC, GP-GM, GP-GC>> Now we check each symbol
GWaccording the values of Cu& Cc:Cu= 3< 4(not ok) AND Cc=0.9 not in (1 C c 3) GW is Not Ok.So, each symbol having GW must be canceled(GW-GM & GW-GC)
GMaccording the values of PI or A-line equation:PI=3.5
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Classification of SoilSolved Problems in Soil Mechanics
2. Finding Group Name from Figure (5.4):
% Sand R R 9 5 % 6 5 % 3 0 % > 1 5 % The group name is:Poorly graded gravel with silt and sand.
Now, as you see the classification is so easy, just you need some focusing, so I
will finish solving problems completely in this chapter , but I will explain some
ideas, and I give you the answer to solve the problems by yourself and check
your solution.
25. (Mid 2011):a. 86% of a soil sample passed Sieve No.4 and retained on Sieve No.200. Also
given that: Coefficient of gradation=1 , Uniformity Coefficient = 3
Solution,14%486: %
%..14200%486
4200
% )).86+14=100200
F 8 6 % R 14% , F 0.0 , R 100%Coefficient of gradation = Cc=1 , Uniformity Coefficient = Cu= 3
The group symbol is: SP
.The group name is: Poorly graded sand.b. A sieve analysis of a soil show that 97% of the soil passed sieve No.4 and 73%
passed sieve No.200. If the liquid limit of the soil is 62 and its plastic limit =34.
Solution
F 9 7 % R 3% , F 73% , R 27%LL=62% , PL=34% , PI = LL-PL= 6234=28 %
No idea in this question but you should be attention for the large value of LLbecause it will be used when you finding group symbol.
The group symbol is: MH.The group name is: Elastic silt with sand.
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Classification of SoilSolved Problems in Soil Mechanics
26. (Mid 2009):Use Unified Soil Classification System to classify the given soil knowing that
the liquid limit is 30% and plastic limit is 27%.(give group Symbol and group name)
SolutionLL=30% , PL=27% , PI = LL-PL= 3027=3 %The idea is how to calculate Ccand Cu
From the given table we note the following :
- % Finer than = % Passing
- % Passing is cumulative (if not you must make it
cumulative)
- After insuring the values are cumulative we can
take the values of D60, D30, D10from the table asfollowing : D60=1.3 , D30=0.6 , D10=0.2 thus, we can calculate Ccand Cu:
C DD 1.30.2 6.5 , C
DD D 0.6
1.30.2 1.38R 1009010% , R 1 0 0 8 9 2 % , F 8%The group symbol is: SW-SM.The group name is: Will graded sand with silt.
See AASHTO Classification System (Page 126 in your textbook)
Particle Size(mm)
% Finerthan
6 100
4.75 90
2.36 84
( D60)1.3 60
( D30)0.6 30
( D10)0.2 10
0.075 8
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Chapter (7)
Soil Permeability
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Page (46) Ahmed S. Al-Agha
Soil PermeabilitySolved Problems in Soil Mechanics
Bernoullis Equation(for Soil):
Total Head = Pressure Head + Velocity Head + Elevation Head
h
Zu: pore water pressure
v: velocity of water through the soil
Z: vertical distance of a given point above or below a datum plane.
Notes:
Pressure head is also called piezometric head.
u h .The velocity of water through soil is very small (about 0.010.001)m/sec and
when the velocity is squared the value will be very small so, the velocity headin Bernoullis equation should be canceled and the final form of bernoullis
equation will be : h Z The head loss that result from the movement of water through the soil (H
can be expressed in a nondimensional form as:
i , where:
i Hydraulic gradient (The head loss per unit length)
head
)
(
L Total length of soil or soilsthat the water passes through it
Darcys Low:Darcy found that, there are proportional relationship between velocity (v) and
hydraulic gradient (i), this relationship still valid if the flow still laminar , and in
soil the velocity is small so, the flow is always laminar.
v i v k . iK: Hydraulic conductivity of soil = Permeability of soil (m/sec)
Now, we know that: Q V A and v k . i(Darcys low)Q K . i . A
A: Cross sectional area that perpendicularto flow direction.
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Soil PermeabilitySolved Problems in Soil Mechanics
Directional Variation of Permeability:
1.Horizontal Permeability (Flow parallel to layers):
From the above graph we note the following:
All values of H and h are perpendicular to the flow .
H H h h h h Q Q. q q q ..q A A. H 1 , A h 1 , A h 1 , A h 1 ,and A h 1 H h h h h(because all layers have the same length)
i i. i i i i
Now,Q K. i. A. , q K i Aand so onK. i. A. K i A K i A K i A..K i Ai. i i i iSo we cancel itK. A. K A K A K A K AK. H 1 K h 1 K h 1 K h 1 K h 1Rearrange the last equation:
K. K h 1 K h 1 K h 1 K h 1H The final equation:
K.
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Soil PermeabilitySolved Problems in Soil Mechanics
2.Vertical Permeability (Flow perpendicular to layers):
From the above graph we note the following:
H H h h h h Q Q. q q q .. q A A. L 1 A A A A H h h h h(because flow pass through each layer) i i. i i i iNow,
q K A h .
.. (Q and A are the samecancel them)H. The final equation:
K. ++++Note: All values of H and h are parallel to the flow
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Page (49) Ahmed S. Al-Agha
Soil PermeabilitySolved Problems in Soil Mechanics
Permeability Test in the Field by Pumping from Wells:
1.
Un Confined Aquifer:The equation of un confined aquifer:
K . 2.
Confined Aquifer:The equation of confined aquifer:
K
.Important Notes about the above two cases:
Impervious layer = Impermeable layer.
Clay layer considered impermeable layer.
Always take the max.value of r as r the value of hmust be larger thanh ris the distance from the center of the well to the center of observation well. h is the elevation of water in the observation well.
The following graph explain h:In all Questions usually the value of d is given to make confusion.
d: Draw-down(Level of water below the ground surface)
) )
So,h H d H in equation of confined aquifer is the thickness of soil
layer that confined between two impermeable layers.
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Soil PermeabilitySolved Problems in Soil Mechanics
27. (Mid 2013):1. Find The total head and Pressure headat points(A-B-C-D) with respect to
given datum, Assume 3K K 1.5K 2K.2. Find the flow rate (K 3 . 5 1 0cm/secNote: All dimensions are in cm
Solution
The first step is to making the soil 2 and soil 3 as one soil by calculating the
equivalent value of K for these two layers (beacuase all layers perpendicular to
flow except these two layers)we want to make them as one layerperpendicular
to flow.
K 3K , K 2K , K 1.5K
K. K, K hH K, K h K hh h
K, 3K 2 2 K 22 2 2.5K
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Soil PermeabilitySolved Problems in Soil Mechanics
The new soil layer is shown in the figure below:
Now we can calculate K.for whole system (all layers perbendicular to the flow).K. HhK
hK hK
hK 6 1 0 86K
10K, 8K
, K, 2.5K, K 1.5K
K. 6 1 0 86K 102.5K
81.5K K. 1.565K
H 2 8 1 2 4 12cm.i. HH
126 1 0 8 0.5
Q. q q, q, and A. 4 1 A A, A(Solution Key)Point A:
h, 28no losses because no soil (Total head).h, h, h, 2 8 4 2 4 c m.(Pressure = piezometric head)h, 4 Point B: ( the soil pass through soil 1then reach point B) So,
Q. q K. i. A. K i Abut, A. A 4
K. i. K i 1.565K 0 . 5 K i i 0.7825
h, h, i h h, 280.7825623.305cm.h, h, h, 23.305419.305cm.
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Point C: (the soil pass through soil 2,3then reach point C) So,
Q. q, K. i. A. K, i, A,but, A. A, 4 K. i. K, i, 1.565K 0.52.5K i, i, 0.313
h, h, i, h, h, 23.3050.3131020.175cm
.
h, h, h, 20.175416.175cm.Point D: (the soil pass through soil 4then reach point D) So,
Q. q K. i. A. K i Abut, A. A 4 K. i. K i 1.565K 0.51.5K i i 0.5216h, h, i h h, 20.1750.5216816cm.h, 16 must be checked (h, 1 2 4 1 6 ) O K, if not equal>> youmust revise your solution because some error exist.
h, h, h, 1 6 4 1 2 c m.The second required(Dont forget it)
Q. q q q K 3 . 5 1 0cm/secQ. K. i. A.Q. 1.565K 0 . 5 4 1 1 . 5 6 5 3 . 5 1 0 0.5410.955cm/secTo check it:
q K i A
i 0.7825
3.5102 0.7825 410.955cm3/sec.Note:
If the pore water pressure (u) is required at each point >>> do the following:
At each point: u pressure head
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Soil PermeabilitySolved Problems in Soil Mechanics
28. (Mid 2013):Find the Total headat points (1 to 8), if the cross section of the system is 10 cm
2.
Knowing that: K 0.5K 3K
Solution
Its noted that all layers are perbendicular to flow(Vertical Permeability)
Now we can calculate K.for whole systemK. H
hK hK hK hK 8 1 6 4
8K 16K, 4K , K 2K, K 0.333K
K. 8 1 6 48K 162K
40.333K K. 0.9996K K. K
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Soil PermeabilitySolved Problems in Soil Mechanics
H 1 0 8 1 0 6 4 5 13cm.i. HH
138 1 6 4 0.4643
Q. q q q, and A. 10cm A A A(Solution Key)Point 1:
h, 28no losses because no soil (Total head).Point 2: ( the soil pass through the mid of soil 1then reach point 2) So,
Q. q K. i. A. K i Abut, A. A 1 0 K. i. K i K 0.4643K i i 0.4643
h, h, i 4 h, 280.4643426.1428cm
.
Point 3: ( the soil pass through all of soil 1then reach point 3) So,
Q. q K. i. A. K i Abut, A. A 1 0 K. i. K i K 0.4643K i i 0.4643h, h, i 4 h, 26.14280.4643424.2856cmOr, h, h, i 8 h, 280.4643824.2856cm.Point 4:
h, h, 24.2856 cm no losses because no soil.Point 5: ( the soil pass through 6cm of soil 2then reach point 5) So,
Q. q K. i. A. K i Abut, A. A 1 0 K. i. K i K 0.46432K i i 0.23215h, h, i 6 h, 24.28560.23215622.8927cmPoint 6: ( the soil pass through all of soil 2then reach point 6) So,
Q.
q
K.
i.
A.
K
i
Abut,
A.
A
1 0
K. i. K i K 0.46432K i i 0.23215h, h, i 1 6 6 h, 22.89270.232151020.5712cmOr,
h, h, i 1 6 h, 24.28560.232151620.5712cm.
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Soil PermeabilitySolved Problems in Soil Mechanics
Point 7:
h, h, 20.5712 cm no losses because no soil.Point 8: ( the soil pass through all of soil 3then reach point 8) So,
Q. q K. i. A. K i Abut, A. A 1 0 K. i. K i K 0.46430.333K i i 1.3929h, h, i h h, 20.57121.3929415cm.h, 15 must be checked (h, 6 4 5 1 5 ) O K, if not equal>>
you must revise your solution because some error exist.
29. (Mid 2009):An inclined premeameter tube is filled with layers of soil of different permeability
as shown below.Find the total head, elevation headand pore water pressureat points (A-B-C-D)
with respect to the given datum, Assume: .
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Soil PermeabilitySolved Problems in Soil Mechanics
Solution
The only different between this problem and problem26is to finding elevation
head.
The first step is to making the soil 1 and soil 2 as one soil by calculating theequivalent value of K for these two layers (beacuase all layers perpendicular to
flow except these two layers)we want to make them as one layerperpendicular
to flow.
K 3K , K 1.5K , K 2KK. K, K hH K,
K h K hh h
K, K 2 3 K 22 2 2KThe new soil layer is shown in the figure below :
Now we can calculate K.for whole system (all layers perpendicular to the flow).K. HhK
hK hK
hK 6 8 1 26K,
8K 12K
K. 6 8 1 262K
81.5K
122K
K. 1.814K
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Soil PermeabilitySolved Problems in Soil Mechanics
Firstly, we calculate the total head at each point.
H 3 0 1 0 7 13cm.
i. H
H 13
6 8 1 2 0.5
Q. q, q q, and A. 4 1 A, A A(Solution Key)Point A:
h, 30cmno losses because no soil (Total head).Point B: ( the soil pass through soil 1,2then reach point B) So,
Q. q, K. i. A. K, i, A,but, A. A, 4
K. i. K, i, 1.814K 0 . 5 2 K i, i, 0.4535
h, h, i, h, h, 300.4535627.279cm.Point C: (the soil pass through soil 3then reach point C) So,
Q. q K. i. A. K i Abut, A. A 4 K. i. K i 1.814K 0.51.5K i i 0.6046h, h, i h h, 27.2790.6064822.4278cm.Point D: (the soil pass through soil 4then reach point D) So,
Q. q K. i. A. K i Abut, A. A 4 K. i. K i 1.814K 0 . 5 2 K i i 0.4535h, h, i h h, 22.42780.45351217cm.h, 17 must be checked (h, 1 0 7 1 7 ) O K, if not equal>> youmust revise your solution because some error exist.
Secondly, we calculate the elevation head at each point with respect to the given
datum.
By interpolationwe calculate the elevation of each point from the datum as shownin the following graph :
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From this graph we can calculate elevation head(Z) at each point:
Z 0.0.Z6
106 8 1 2 Z 2.307 cm
.
Z6 8 106 8 1 2 Z 5.384 cm.Z 10 cm.Finally, we calculate the pore water pressure at each point:
u pressure head Point A:
h, h, h, 3 0 0 3 0 c mu 30100 9.81 2.943 KN/m.Point B:
h, h, h, 27.2792.30724.972cmu 24.972100 9.81 2.449 KN/m.Point C:
h, h, h, 22.42785.38417.0438cmu 17.0438100 9.81 1.672 KN/m.Point D:
h, h, h, 1 7 1 0 7 c mu 7100 9.810.6867KN/m.
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Soil PermeabilitySolved Problems in Soil Mechanics
30. (Mid 2005):A pumping well test was made in sands extending to a depth of 15 m where
an impermeable stratum was encountered. The initial ground-water level was at the
ground surface. Observation wells were sited at distances of 3 and 7.5 m from thepumping well. A steady state was established at about 20 hours when the discharge
was 3.8 L/s. The drawdowns at the two observation well were1.5 m and 0.35 m.
Calculate the coefficient of permeability.
K K
.
Solution
Its clear that the problem about (un confined aquifer)you should know thisbecause there exist impermeable layer below sands and no any impermeable layer
above sand.
r 7.5mlarge value , r 3msmall value, H 15 d 0.35m , d 1.5m drawdowns
r.. hd H d 150.3514.65large valueh H d 15 1.5 13.5small value
Q 3 . 8 Lsec 3600 sechr m
1000L 13.68m/hrNow, you are given two equations you must choose the coorect equation for un
confined aquifer (you must know the form of the equation of the two types)
K note: log
L n so the equation will be :
K q L n rr h h
13.68Ln7.53 14.65 13.5 0.123m/hr.
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31.A layer of sand 6 m thick lies beneath aclaystratum 5 m thick and above abed
thick shale( ) . Inorder to determine the permeability of sand, a well
was driven to the top of the shale and water pumped out at a rate of 0.01m
3
/sec.Two observation wells driven through the clay at 15m and 30 m from the pumping
well and water was found to rise to levels of 3m and 2.4 m below the ground water
surface. Calculate the permeability of soil.
Solution
Its clear that the problem about (confined aquifer)because the clay layer
considered impermeable layer an shale is a type of rock , and the sand layer exist
between these two layers.
r 30mlarge value , r 15msmall value, H 5 6 11 md 2.4m , d 3m drawdowns, below the ground water surfaceh H d 11 2.4 8.6large valueh H d 11 3 8small valueH 6mQ0.01m/sec =36m3/hr
K q l o g r
r
2 .727Hh h 36log 30
15
2.72768.68 1.1 m/hr
.
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Chapter (8)
Seepage
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SeepageSolved Problems in Soil Mechanics
Flow Net:
From the above graph the flow net consist of:
1. Flow Lines (Solid-black lines):
:
.
2. Equipotential Lines (dashed-blue lines):
:total head
90.
3. Flow Channel (::
5..
.
4. Potential Drop(
:
head
head
9:
N, , im
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SeepageSolved Problems in Soil Mechanics
Calculating the amount of flow (Rate of seepage): q k i A q k i(m3.sec/m) q k , (for one flow channel)q q q q qBut, q q q qSo, q q N k , NFinally, q k , N n (m3.sec/m)
n
bperpindicular to flow
Lparallel to flow
n
((element
1..
:
:n.
:1
..N,
.. :
,
bN.. 8.2.
:n1.
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SeepageSolved Problems in Soil Mechanics
Head calculations and the uplift force under the dam:
Calculate total, pressureand drivinghead at point A
Total Head:
headh, L H losseslosses N, N,2Ahead
=2N,:AN,A2potential drop. .
Pressure(piezometric) Head:
h, h, h,
h, L H losses L h Rearrange the equationh, Hh lossesL..h
L
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SeepageSolved Problems in Soil Mechanics
Driving Head:
,
.H)(Hhead
h, Hlosses
Uplift force under the dam:
(
)pore water pressure
,)(
.
.
u pressure head hu
Effective Stress at any point (chapter 9):
9
:
( :
(
At any point we can calculate the effective stressas following:
u uupore water pressure at any point we calculate it as mentioned above The totalvertical stress applied on a point and can be calculated as following:
)(
For example at pointAin the flow net on the last graph
, H h losses
Now, we can calculate the effective stress easily.
u
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Page (66) Ahmed S. Al-Agha
SeepageSolved Problems in Soil Mechanics
Flow Nets in Anisotropic soil:flow net
isotropick kLaplace
flow net.Laplaces Equation:
k k
0 , For isotropic soil kx kz The equation will be:
0 That is the required form to draw a trueflow net
(Lines perpendicular to each other).
Now, for anisotropic soilk kso, the first stepis to convert the two soils forone isotropicsoil (k. k. k).Laplaces equation doesnt written as the above form and the lines are not
perpendicular to each other so, the second step thatwe must rewrite the equation
to be in the required form to draw true flow net.
k k
0 (Divided by k)
/ 0
Now let x` k/kx the equation will be:`
0That is the required form to draw a trueflow net
(Lines perpendicular to each other)
Example:
For the shown soil profile under the dam. Make the soil isotropic.
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Page (67) Ahmed S. Al-Agha
SeepageSolved Problems in Soil Mechanics
Soil will be isotropic if:
k. k. kk 7 k 1 0 k
7 1 0 , k 7 1 0
7k 10k
k. k. k kk That make the soil isotropicAfter making the soil isotropic the flow net under the dam was drawn and given in
the figure below. Findall dimensions on the graph and then calculate the rate of seepage.
xLaplaceflow net
x`:x` k/kxxx`,,
x`.q:q kk HN, N n,,
seepage.
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Page (68) Ahmed S. Al-Agha
SeepageSolved Problems in Soil Mechanics
32. (Mid 2012):
For the shown flow net:
(a).Calculate the uplift force at the base of the weir , per foot of lengthPoint A and B at the corners of the concrete dam.
(b).Calculate the driving head at lines 5 and 12.
Solution
Givens:
N,#of potential drops 14 , N 4H 3 0 8 1 2 5 21ft
i N, H
N, 2114 1.5ft value of one potential drop
(a).
(A( )B)
.sheet pileB,
12 ft
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Page (69) Ahmed S. Al-Agha
SeepageSolved Problems in Soil Mechanics
Point A:
Apotential drop.
h, 3 0 8 1 1.5 36.5 ft.
u h, 36.5 62.4 2277.6 Ib/ft
Point B:
Bsheet pilepotential drops
B8.5B.
h, 3 0 8 8.5 1.5 25.25 ft.Or, h, 5 1 2 5.51.5 25.25
,
potential drops=5.5.
u h, 25.2562.41575.6 Ib/ftNow, the stress distribution under the dam as shown in figure below:And the uplift force is calculated as following:
F 2277.61575.698F 188806.8 fIb/ft`.(b).
h HlossesAt line 5, there are 5 potential drops were lost
h, Hlossesh, 2 1 5 1 . 5 1 3 . 5 f t.At line 12, there are 12 potential drops were lost
h, Hlosses
h, 2 1 1 2 1 . 5 3 f t
.
A B
2277.6
1575.6
Fuplift
98ft
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Page (70) Ahmed S. Al-Agha
SeepageSolved Problems in Soil Mechanics
33. (Mid 2011):For the flow net shown below, calculate:
a. Flow Rate per unit length.
b. Uplift force per unit length under the dam.c. Effective stress at points A and B.
d. The seepage loss for 8 m length of sheet pile (additional)
e. Pressure head at point C (from ground surfac) (additional).
f. Total head at point A (additional).
g. The exit gradiant (additional).
(k 1 1 0m/s , 19 KN/m)
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SeepageSolved Problems in Soil Mechanics
Solution
Givens:
N,#of potential drops 12 , N 4 , k 1 1 0
m/sH 10 2 8 m , 19 KN/mi N, HN, 8
12 0.667 m value of one potential dropa.
q k , N n 1 1 0 0 . 6 6 7 4 1 2 . 6 6 8 1 0m3/s.m.b.
sheet pile
.
Point 1:
1potential drop.
h, 1010.6679.333m..u h, 9.333 9.81 91.55 KN/mPoint 2:
2
4.5potential drop
5.h, 104.50.6676.998m..u h, 6.998 9.81 68.65 KN/mPoint 3:
39.5potential drop10.
h, 109.50.6673.663m..u h, 3.6639.8135.93KN/mPoint 4:
411potential drop.
h, 10110.6672.663m. .u h, 2.6639.8126.12KN/m
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SeepageSolved Problems in Soil Mechanics
Now, the stress distribution under the dam as shown in figure below:
The uplift force can be calculated as following:
F Area1Area2F 91.5568.65 2 0 35.9326.12 152067.38KN/m.sheet pilesheet pile
.
c.
Point A:
u u, 1 0 1 3 1 0 9 . 8 1 1 3 1 9 3 4 5 . 1KN/m2
A1potential drop
h, 101310.66722.333m..u 22.3339.81219.08KN/m2, 345.1219.08126 KN/m2.Point B:
, 2 1 3 2 9 . 8 1 1 3 1 9 2 6 6 . 6 2KN/m2
B
10potential droph, 1013100.66716.333m..u 16.339.81160.2KN/m2, 266.62160.2106.42KN/m2.
12 3
4
91.55
68.65
35.93
26.12
20m 15m
Fuplift
Area 1Area 2
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SeepageSolved Problems in Soil Mechanics
d.Seepage loss q length of sheet pile 2.668 10 8 2 1 . 3 4 4 1 0m3/s.e.
h,
,
.
C)( h:We note that, there are3potential drops to reach point C
h, 1 0 h 3 0 . 6 6 7 7 . 9 9 h 7.99 If the value 7.99 is negative value, that means (below the ground surface) .f.
h, 1 0 2 2 losses 1 potential drop to reach Ah, 1 0 2 2 0.667 1 31.333 m.We note that, also we can calculate pressure head from total head
h, h, h,h, 31.333 2 2 1 3 22.333m the same as calculated above.g.
i
potential drop
potential drop0.9
i
i exit losseexit distance 0.667
0.9 0.741.
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Page (74) Ahmed S. Al-Agha
SeepageSolved Problems in Soil Mechanics
34. (Final 2009)For the flow net shown below, if the coefficient of permeability of the soil
below the dam is (5.3x10-5
cm/sec) and 17.7 KN/m, find the following:A-The rate of seepage(m
3
/sec/m).B-The uplift forceunderneath the dam.
C-The driving headat point M.
D-The effective stressat points L and N.
E-If the weight of the dam is 120 KN/m2, calculate the effective stressat point O
(Assume the weight of the dam is constant with depth)
Solution
Givens:
N,#of potential drops 13 , N 4 , k 5 . 3 1 0m/sH 10 1 9 m , 17.7 KN/mi N, HN,
913 0.6923 m value of one potential drop
5m
10m
1m
8m
8m
6m 2.5m 12m 3.5m 6m
2.8m
6m
A B
C D
E F
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A-
q k , N n 5 . 3 1 0 0.6923414.6710m3/s.m.
B-((A to F
Point A:
We note that, there are 2 potential drops to reach point A
h, 10620.692314.6154m.u h, 14.6154 9.81 143.377 KN/mPoint B:
We note that, there are 4 potential drops to reach point B
h, 10640.692313.2308m.u h, 13.2308 9.81 129.794 KN/mPoint C:
We note that, there are 5 potential drops to reach point C
h, 1062.850.69239.7385m.
u h, 9.7385 9.81 95.534 KN/mPoint D:
We note that, there are 8 potential drops to reach point D
h, 1062.880.69237.6616m.u h, 7.6616 9.81 75.16 KN/mPoint E:
We note that, there are 9 potential drops to reach point E
h, 10690.69239.7693m.u h, 9.76939.8195.836 KN/m
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Point F:
We note that, there are 11 potential drops to reach point F
h, 106110.69238.3847m.u h, 8.38479.8182.254 KN/mThe stress distribution under the dam is shown in figure below:
The uplift force can be calculated as following:
F Area1Area2Area3Area4Area4F 1
2143.37129.79 6 1
2 129.7995.53 2.5
12 95.5375.16 1 2 12 75.1695.83 3 . 5 12 95.8382.25 6F 2959.51KN/m`.C-
h HlossesAt point M, there are 2 potential drops were lost
h, Hlosses
h, 9 2 0.6923 7.6154 m.
AB
C D
EF
Area1
Area3
Area5Area2
Area4
6m 2.5m 12m 3.5m 6m
143.37
129.79
95.5375.16
95.83
82.25
Fu lift
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D-
Point L:
u u
, 1 0 8 109.81817.7239.7 KN/m2
We note that, there are 2 potential drops to reach point L
h, 10820.692316.6154m.u 16.61549.81163KN/m2, 239.716376.7KN/m2.Point N:
u u
, 1 8 19.81817.7151.41 KN/m2
We note that, there are 12 potential drops to reach point N
h, 108120.69239.6924m.u 9.69249.8195.08KN/m2, 151.4195.0856.32KN/m2.E- (Additional)
O
.
O
(5+8-6+2.8) = 9.8m
Point O:
u u, 9 . 8 dam weight 9.8 17.7 120 293.46 KN/mWe note that, there are 6 potential drops to reach point O
h, 108560.692318.846m.u 18.846 9.81 184.88 KN/m
, 293.46184.88108.578 KN/m
.
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Page (78) Ahmed S. Al-Agha
SeepageSolved Problems in Soil Mechanics
35.For the flow net shown below:
a) Calculate the rate of seepage.
b) Calculate the total headat point C.c) Calculate the pressure headat point D.
d) Calculate the factor of safety against boilingat the surface AB.
(k 4 1 0m/s , 20 KN/m
:
)(
) Symmetry)
,
,2N.
Givens:
N,#of potential drops 10 , N 2 3 6 , k 4 1 0m/s H 2 2 . 5 4 . 5 m , 20 KN/mi N, HN,
4.510 0.45m value of one potential drop
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SeepageSolved Problems in Soil Mechanics
a)
q k , N n 4 1 0 0 . 4 5 6 1 . 0 8 1 0m3/s.m.b)
h, 2.2562.5 losses 4 potential drop to reach Ch, 2.2562.5 0.45 4 8.95 m.c)
D(h)h,h,.
We note that, there are8potential drops to reach point D
h, 2 . 5 2 h 8 0 . 4 5 0 . 9 h 0.9 m .If the value 0.9 is negative value, that means (below Datum).
d) (From chapter 9)
F. S i
209.819.81 1.038
i exit losseexit distance 0.450.9 0.5
F. S 1.0380.5 2.076.
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Chapter (9)
In Situ Stresses
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Total Stress (
Pore Water Pressure ( Effective Stress (
Total Stress (: Is the total weight of all layers above a certain point dividedby the area of the layers, and it is independent on seepage of water.
)(
.
Pore Water Pressure (Hydrostatic Pressure) (: Is the total weight ofthe column of water (Pressure head) divided by the area of the layers, and it is
dependent on the seepage of water (Upward or Downward).
Effective Stress (: The sum of the vertical components of all intergranularcontact forces divided by unit gross cross-sectional area.
( ,(
.
u uThe above equation is the most important equation in geotechnical engineering,
because the compressibility of soil and shearing resistance of a soil depend to a
great extent on the effective stress. Thus, the concept of effective stress is
significant in solving geotechnical engineering problems, such as the lateral earth
pressure on retaining structures, settlement of foundations, and the stability of earth
slopes.
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In Situ StressesSolved Problems in Soil Mechanics
Stresses in Saturated Soil without Seepage:
Calculate the total stress, pore water pressure, and effective stressat points A,
B, and C.
Firstly, you should note that, there are no losses in head (piezometric head) due to
the movement of water through the soil, because there is no seepage of water.
Point A:
, H u H total u H1 W H1 W 0.0Point B:
, H H u H H H1 W H2 sat H1 H2 W H2sat W.
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Page (83) Ahmed S. Al-Agha
In Situ StressesSolved Problems in Soil Mechanics
The term of is called effective unit weight or submerged unit weight(. So, the effective stress at point Bequal:H Point C:
, H z u H z H z H z z z Note:
All soils under the ground water table are saturated soils, and soils above the
ground water table are dry soils unless if there exist capillary rise on the layer
above the ground water table and we will discuss this case later.
Stresses in Saturated Soil with Upward Seepage:
We note that, there is upward seepage from upstream (point B) to downstream
(point A), also we note that, the elevation of water on the tank is remained constant
by controlling the amount of flow in and flow out.
So, due to the upward seepage through the soil, there will be losses in piezometric
head as the water move upward, and the total losses is hdue to the movement of
water in lengthH through the soil, thus, the hydraulic gradient i will be :i
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In Situ StressesSolved Problems in Soil Mechanics
Calculate the total stress, pore water pressure, and effective stressat points A,
B, and C
Firstly, you should note that, as the depth increase the piezometric (pressure) head
increase due to the upward seepage, so, pore water pressure increasewith depth.
Point A:
, H u H u H H 0.0Point B:
, H H (Not dependent on seepage of water)Dueto the upward seepage the pressure head at point B will increase by hu H H iH iH H h u H H h H H H H h H h Point C:
, H z (Not dependent on seepage of water)Dueto the upward seepage the pressure head at point B will increased by izu H z i z H z H z i z z i z Limiting Conditions:
Due to the upward seepage, as the depth increase the pore water pressure increase,
so, the effective stress will decreases with depth, and this is very dangerous
because at certain depth the effective stress may equal zero ( uand this isa limiting conditions.
Now, suppose that the effective stress will equal zero at depth z:
z i z 0.0The hydraulic gradient at this point is called the critical hydraulic gradient (
i
So,z iz i range :( 0.9 to 1.1)Now, if the value of uis larger than the value of this means the effectivestress is negativeand if we reach to this state the soil stability will lost and this
situation generally is referred to as boilingor quick condition.
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Page (85) Ahmed S. Al-Agha
In Situ StressesSolved Problems in Soil Mechanics
So, the value of z (the depth having 0) is the maximum depth can be reach toprevent boilingor quick conditionsor to prevent heave((of soil
Boiling or Quick conditions or Heave of soil:
(
)
(Mud.)
Stresses in Saturated Soil with Downward Seepage:
We note that, there is downward seepage from upstream (point A) to downstream
(point B), also we note that, the elevation of water on the tank is remained constant
by controlling the amount of flow in and flow out.
So, due to the downward seepage through the soil, there will be losses in
piezometric head as the water move downward, and the total losses is hdue tothe downward movement of water in lengthH through the soil, thus, thehydraulic gradient i will be :
i
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Page (86) Ahmed S. Al-Agha
In Situ StressesSolved Problems in Soil Mechanics
Calculate the total stress, pore water pressure, and effective stressat points A,
B, and C
Firstly, you should note that, as the depth increase the piezometric (pressure) head
decrease due to the downward seepage, so, pore water pressure decrease with depth.
Point A:
, H u H u H H 0.0Point B:
, H H (Not dependent on seepage of water)Dueto the downward seepage the pressure head at point B will decrease by hu H H iH iH H h u H H h H H H H h H h Point C:
, H z (Not dependent on seepage of water)Dueto the upward seepage the pressure head at point B will decreased by izu H z i z H z H z i z z i z It is clear that no limiting conditions exist in case of downward seepage because
the pore water pressure decreased by depth, thus, the effective stress will increase
with depth and never reach zero.
:seepage,
upward seepageboiling
..boilingdownward seepage
.. .boilingseepage
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In Situ StressesSolved Problems in Soil Mechanics
Seepage Force:Due to the seepage of water through the soil, the effective stress may increase or
decrease according the direction of seepage, so, this concept can be expressed by
seepage force by unit volume as following:In case of no seepage:
It is noted that, there is no seepage force because there is no seepage of water in
the soil. So, the only force exerted on the soil is the weight of soil layer:
P Z AIn case of Upward Seepage:
It is noted that, there is a seepage force directed upward (in the direction of flow)
and we also note that there are two forces exerted on the soil, the weight of the soil
directed downward, and the seepage force directed upward:
P Z A iz AAlso we note that, if the seepage force (
iz A) smaller than the weight of the
soil (Z A, the soil will be safe and the boiling will not occur, and the criticalcasewhen the weight of the soil equal the seepage force, but if the seepage force is
larger than the weight of the soil, the soil stability will lost and the boiling will
occur.
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Page (88) Ahmed S. Al-Agha
In Situ StressesSolved Problems in Soil Mechanics
In case of Downward Seepage:
It is noted that, there is a seepage force directed downward (in the direction of
flow) and we also note that there are two forces exerted on the soil, the weight of
the soil directed downward, and the seepage force directed downward:
P Z A iz AIt is clear that, the force exerted on the soil is always downward and the soil is
always safe.
The seepage force in the two cases having the same magnitude (iz Aand thevolume of the soil iszA, so, the seepage force can be expressed by the form of:seepage force iper unit volumeHeaving in Soil Due to Flow around Sheet Pile:If there is a sheet pile separated two levels of water (downstream and upstream),
the soil on the downstream side may be heave () due to the uplift seepage force
on the bottom of the heave zone. Terzaghi found that the heaving generally
occurred within a distance of from the sheet piles.Such that D = the depth of embedment () of sheet piles into the
permeable layer. This can be explained on the figure shown below:
A B
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In Situ StressesSolved Problems in Soil Mechanics
The first step is to draw the heave zone on the flow net (if its not drawn) and then
calculate the factor of safety:
19 9.81 9.19 KN/mThe heave zone can be enlarged as shown in figure below:
You should know how to draw this heave zone
(with dimensions)
H 1 0 2 8 m , N, 12 D = 10 mi N, HN,
812 0.667
There are 8 potential drops to reach point A
h, 80.66782.664mThere are 8.8 potential drops to reach point B
h, 80.6678.82.13mh h, h,2
2.6642.132 2.397m
i hD 2.397
10 0.2397
F . S i 9.190.23979.81 3.9
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Page (91) Ahmed S. Al-Agha
In Situ StressesSolved Problems in Soil Mechanics
Capillary Rise in Soil & the Effective Stress in the
Zone of Capillary Rise:
Capillary Rise in Soil:
h:
,
( S=100%( )0
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Page (92) Ahmed S. Al-Agha
In Situ StressesSolved Problems in Soil Mechanics
To calculate total stressresult from zone of capillary rise you should calculate the
unit weight of this layer [saturated or moist (partially saturated)] and then multiply
this unit weight by the height of this layer.
To calculate the pore water pressurefrom the zone of capillary rise:
u S100 hS Degree of saturation (%)h The height of the point under consideration measured from the groundwater....table.
Now, to find the pore water pressure at point B on the above graph you must
calculate it just before point (B) and just after point(B),because the degree of
saturation(S) is different before and after point (B)So, to find effective stress at point (B) you must calculate it just before and just
after point (B).
The negative sign in the equation is due to the points always exist above the G.W.T.
:...
,
,
.
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Page (93) Ahmed S. Al-Agha
In Situ StressesSolved Problems in Soil Mechanics
36. (Final 2012):Refer to the soil profile shown in figure below:a. Calculate the variation of , u , and with depth.
b. If the water table is rises to the top of the ground surface, what is the change inthe effective stress at the bottom of the clay layer?
c. How many meters must the ground water table rise to decrease the effective
stress by 15 KN/m2at the bottom of the clay layer?
Solution
We note that the G.W.Tis below the sand layer and above clay layer so the sand
layer is dry(No capillary rise)and the clay layer is saturated.
For Dry Sand Layer:
G 1 e 2.669.81
10.52 17.17 KN/mFor Saturated (S=1) Clay Layer:
S . e Gw w S. eG 1 12.75 0.363
2.759.8110.3631 1 18.4 KN/m
Sand
Clay
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In Situ StressesSolved Problems in Soil Mechanics
a.
Let the point Aat depth 0, point Bat depth 5m, and point Cat depth 9m.
Point A(z=0.0):
, 0.0
.
u 0.0. 0.0.Point B(z=5m):
, 5 17.17 85.85 KN/m.u 0.0. 85.85 0.0 85.85 KN/m.Point C(z=9m):
, 5 17.17 4 18.4 159.45 KN/m.u 49.8139.24KN/m. 159.45 39.24 120.21 KN/m.b.
seepage
,
.:
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Page (95) Ahmed S. Al-Agha
In Situ StressesSolved Problems in Soil Mechanics
We note that from the above graph both sand and clay layers are saturated
For Saturated (S=1) Sand Layer:
S . e Gw w S. e
G 10.52
2.660.1955
2.669.8110.195510.52 20.52 KN/mFor Saturated (S=1) Clay Layer:
18.4KN/m Calculated aboveThe required is to calculate the changeof effective stress at depth of clay layer
(point C).
From the first case: 120.21 KN/mNow, for this case:
, 5 20.52 4 18.4 176.2 KN/mu 5 9 . 8 1 4 9 . 8 1 8 8 . 2 9KN/m 176.2 88.29 87.91 KN/mNow, the change in effective stress at point C:
120.2187.9132.3KN/m .
C.
c.
C
h
.:
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Page (96) Ahmed S. Al-Agha
In Situ StressesSolved Problems in Soil Mechanics
From the first case: 120.21 KN/mand 15KN/mGivenNow, for this case:
, 5 h 17.17h20.52418.4159.453.35h
u h 9.8149.819.81h 39.24
159.453.35h 39.249.81h 120.216.46h 15120.21 120.216.46h 156.46h h 2.322m .h55.
37.For the figure shown belo