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Soil Mechanics Laboratory notebook utcb Serbulea tests
21
 Page 1 din 21 TECHNICAL UNIVERSITY OF CIVIL ENGINEERING BUCHAREST SOIL MECHANICS AND FOUNDATIONS DEPARTMENT 2013 - 2014 STUDENT’S BOOK FOR GEOTECHNICAL TESTS STUDENT: _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ FACULTY: _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ YEAR: _ _ _ _ _ GROUP: _ _ _ _ _
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Page 1: Laboratory Student_s Book

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Page 1 din 21 

TECHNICAL UNIVERSITY OF CIVIL ENGINEERING BUCHAREST

SOIL MECHANICS AND FOUNDATIONS DEPARTMENT

2013 - 2014 

STUDENT’S BOOK FOR GEOTECHNICAL TESTS 

STUDENT: _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _

FACULTY: _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _ _

YEAR: _ _ _ _ _ GROUP: _ _ _ _ _

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Contents

1  Week 2: Determination of the particle size distribution. Screening method ................................. 3 

1.1  Graphical representations: histogram, frequency curve, particle size distribution curve ...... 4 

2  Week 3: Determination of the particle size distribution. Hydrometer method .............................. 5 

2.1  Particle size distribution curve ............................................................................................... 6 

2.2  Ternary diagram representation ............................................................................................. 7 

3  Week 4: Geotechnical indices ........................................................................................................ 8 

3.1  Obtaining the density of the solid skeleton ............................................................................ 8 

3.2  Obtaining the soil density using the mould method............................................................... 8 

3.3  Obtaining the density ratio of the sand .................................................................................. 9 

4  Week 5: Plasticity Limits ............................................................................................................. 10 

5  Week 6: Determination of the permeability coefficient .............................................................. 11 

5.1  Constant head method .......................................................................................................... 11 5.2  Falling head method ............................................................................................................. 11 

6  Week 8: Oedometer test. Performing the test .............................................................................. 12 

7  Week 9: Oedometer test. Results interpretation .......................................................................... 13 

7.1  Compression –  settlement diagram ...................................................................................... 13 

7.2  Compression –  porosity diagram ......................................................................................... 14 

7.3  Consolidation diagram ......................................................................................................... 15 

8  Week 10: Direct shear test ........................................................................................................... 16 

8.1  Test results ........................................................................................................................... 16 

8.2  Failure line ........................................................................................................................... 17 

8.3  Mobilization curve ............................................................................................................... 18 

9  Week 11: Triaxial test. Performing an u.u. (unconsolidated undrained) test .............................. 19 10  Week 12: Triaxial test. Results interpretation.............................................................................. 20 

10.1  Failure line using Mohr’s circle ........................................................................................... 20 

10.2  Representation of the stress paths in MIT coordinates (s-t) ................................................ 21 

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1  Week 2: Determination of the particle size distribution. Screening method

m1

m2

m3

m j

mi

a1=m1/m*100

m- the mass of dry soil after washing

a2=m2/m*100

a3=m3/m*100

ai=mi/m*100

a j=m j/m*100

mp1=100%-a1

mp2=100%-(a1 + a2)=mp1-a2

mp3=mp2-a3

mpi=mp(i-1)-ai

mpj=mp(j-1)-a j

 

mi [g]  d [mm]  ai [%]  mp [%] 

20

108

6.3

5

4

2

1.4

1

0.85

0.63

0.5

0.315

0.25

0.18

0.125

0.09

0.063

rest: 

Total: 

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1.1   Graphi cal representations: hi stogram, frequency curve, particl e size distri buti on curve

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2  Week 3: Determination of the particle size distribution. Hydrometer method

material mass: m= 50g

specific gravity of the soil: s=2.72g/cm3 

water density: w=1g/cm3

the hydrometer rod length: Lt=16.5cmhydrometer division: div=1mm

the distance between the last reading and the bulb: L sb=1.2cm

 bulb volume: V b=100cm3 

cross section area of the cylinder: dc=30cm2 

 bulb height: h b=16.8cm

Vs=100 cm

3

 

1000t

H01005.01810d

  r 

ws 

 

cortemp

ws

s p   R 

m

100m  

 

1.4R    

R R R cor 

   

5443.2T1118.0T109T109C243-5

 

 

tcor cortemp   CR R     

101000

R 1

  cortemp  

  

   

  

     1

10divR 2LH

  cortemp

t

   

  

c

s

 br 

d

Vh5.0HH  

Time

Time

t

(s)

reading

R

meniscus

correction

R

Corrected

meniscus

reading

R cor 

temperature

correction

Ct

corrected

reading

R cortemp 

(kN/m3) 

H

(cm)

Hr

(cm)

d

(mm)

mp 

(%)

Temperature

T

(ºC)

15'' 15 1.4

30'' 30 1.4

1' 60 1.4

2' 120 1.4

4' 240 1.4

8' 480 1.4

15' 900 1.4

30' 1800 1.4

1h 3600 1.4

2h 7200 1.4

4h 14400 1.4

8h 36000 1.4

24h 86400 1.4

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2.1   Parti cle size distri buti on curve

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2.2   Ternary diagram representati on

100 0

Sa

gr.Sa

sa.Gr 

Gr 

si.Sa

cl.Sa

sa.Si

sa.cl.Si

sa.si.Cl

sa.Cl

gr.si.Sa

gr.cl.Sa

gr.sa.si.S

gr.sa.cl.S

sa.gr.si.Ssa.si.Gr 

sa.cl.Gr 

gr.sa.Sigr.sa.Cl

sa.gr.Si

sa.gr.Cl

si.Gr 

cl.Gr 

gr.Si

gr.cl.Si

gr.si.Cl

gr.Cl

Si

cl.Si

si.Cl

Cl

90 80 70 60 50 40 30 20 15 10

 Argila si Praf (<0.063mm)

     N     i   s     i   p

     (      0 .    0    6

    3 . . .    2    m   m     ) 

10

20

30

40

50

60

70

80

90

85

100

90

0

P    i     e   t    r    i     s     (     2    . . . 6    3     m   

m     )    

80

70

60

50

40

30

20

10

0

100

0

10

20

40

100

Si

cl.Si

si.Cl

Cl

Cl

Si

     A    r    g       i     l    a      (       <     0 

 .     0      0      2    m    m     )  

30

50

60

70

80

90

100 090 80 70 60 50 40 30 20 15 10

Legenda:Si - Silt - Praf 

Cl - Clay - Argila

S - Soil - Pamant

Sa - Sand - Nisip

Gr - Gravel - Pietris

cl.Si - clayey Silt - Praf argilos

si.Sa - silty Sand - Nisip prafos

si.Cl - silty Clay - Argila prafoasacl.Sa - clayey Sand - Nisip argilos

si.Gr - silty Gravel - Pietris prafos

sa.Gr - sandy Gravel - Pietris nisipos

gr.Sa - gravely Sand - Nisip cu pietris

cl.Gr - clayey Gravel - Pietris argilos

gr.Si - gravely Silt - Praf cu pietris

gr.Cl - gravely Clay - Argila cu pietris

sa.si.Gr - sandy silty Gravel - Pietris prafos cu nisip

sa.cl.Gr - sandy clayey Gravel - Pietris argilos cu nisipgr.si.Sa - silty Sand with gravel - Nisip prafos cu pietris

gr.cl.Sa - clayey Sand with gravel - Nisip argilos cu pietris

sa.cl.Si - silty Clay with sand - argila prafoasa cu nisip

gr.sa.Si - sandy Silt with gravel - Praf nisipos cu pietris

gr.sa.Cl - sandy Clay with gravel - Argila nisipoasa cu pietris

gr.sa.si.S - gravely sandy silty Soil - Pamant prafos nisipos cu pietris

gr.sa.cl.S - gravely sandy clay Soil - Pamant argilos nisipos cu pietris

sa.gr.si.S - sandy gravely silty Soil - Pamant prafos cu pietris si nisip

sa.gr.cl.S - sandy gravely clayey Soil - Pamant argilos cu pietris si nisip

sa.gr.si.S - sandy gravely silty Soil - Pamant prafos cu pietris si nisipsa.gr.cl.S - sandy gravely clayey Soil - Pamant argilos cu pietris si nisip

sa.gr.Si - gravely Silt with sand - Praf cu pietris si nisip

sa.gr.Cl - gravely Clay with sand - Argila cu pietris si nisip

gr.cl.Si -clayey Silt with gravel - Praf argilos cu pietris

gr.si.Cl - silty Clay with gravel - Argila prafoasa cu pietrissa.Si - sandy Silt - Praf nisipos

sa.Cl - sandy Clay - Argila nisipoasa

sa.cl.Si - clayey Silt with sand - Praf argilos cu nisip

sa.si.Cl - silty Clay with sand - Argila prafoasa cu nisip

sa.gr.cl.S

 

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3  Week 4: Geotechnical indices

3.1   Obtain ing the density of the soli d skeleton

COMPUTATION DATAMeasurement Picnometer No.

Unit 1 2 3

Mass of the picnometer + the material g

Mass of the picnometer m0  g

Mass of the material m1  g

Mass of the picnometer + the liquid m2  g

Mass of the picnometer + the liquid +

the materialm3  g

TEMPERATUREoC

oC

LIQUID DENSITY ρL

t

  g/cm

3

 

CORRECTION FACTOR ψL  -

 

g/cm3 

AVERAGE g/cm3 

γs=9.81ρs  kN/m3 

3.2   Obtain ing the soil density using the mould method

COMPUTATION DATAMeasurement Sample No.

Unit 1 2 3 4

Mass of the ring m2  g

Mass of the ring + the soil sample m1  g

Interior volume of the ring (soil sample's

volume)

V0  cm3

  g/cm3

Average density ρav  g/cm3

Volumic weight γ=9.81ρ  kN/cm3

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3.3   Obtain ing the density ratio of the sand

COMPUTATION DATA

Measurement

Natural state Loosest state Most dense state

Unit

Mould no.

Volume of the mould V cm3 

Mass of the mould m g

Mass of the dry sample and the mould m1  gm1-m g

  %

Average n % n= nmax= nmin=

  - e= emax= emin=

 

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4  Week 5: Plasticity Limits

UnitsNatural Moisture Content W [%] Plastic Limit Wp [%] Liquid Limit WL [%]

1 2 3 1 2 3 1 2 3

Sample number -

Weight of the wet sample A  g

Weight of the dry sample B  g

W% %

W%average %

Obs:

 

Penetr

ation

   –

Conemethod

mm

W[%]

 _ _ _ _ _ _ [%]

 _ _ _ _ _ _ 

10.0

15.0

20.0

25.0

30.0

35.0

40.0

0 2 4 6 8 10 12 14 16 18 20 22 24 26 28 30 32 34 36 38 40 42 44 46 48 50 52 54 56 58 60 62 64 66 68 70 72 74 76 78 80

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5  Week 6: Determination of the permeability coefficient

5.1   Constant head method

   

Time HeadSamplelength

Samplecross-section

Hydraulicgradient

Totaldischarge

Correctioncoefficient

Permeabilitycoefficient fortemperature t

[oC]

Permeabilitycoefficient for

20oC

T h l A i V c k t  k

[s] [cm] [cm] [cm2] [-] [cm

3] [-] [cm/s] [cm/s]

Average:

5.2   Fall ing head method

  c = _ _ _ _ _

Time1/T

Initialhead

Finalhead h1/h2  log(h1/h2) 

Permeabilitycoefficient for 20

oC

T h1  h2  k

[s] [1/s] [cm] [cm] [-] [-] [cm/s]

Average:

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6  Week 8: Oedometer test. Performing the test

dring=………cm  Aring=………cm  h0=………cm 

Sample tζ  Δh 

 

 

 

[kPa] [mm] [%] [kPa] [kPa-1]

SAND

 

12.5

25

50

100

200

300

500

12.5

LOESS

 

12.5

25

50

100

200

300

300 i

CL

AY

10''

200

20''

30''

40''

1'

2'

4'

8'

15'30'

1h

2h

4h

8h

15h

24h

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Week 9: Oedometer test. Results interpretation

7.1  

Compression –  settl ement diagr am

-2

0

2

4

6

8

10

12

14

10 100 1000

  ε   [   %   ]

ζ [kPa]

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10 100 1000

  e   [  -   ]

ζ [kPa]

7.2   Compression –  porosity diagram

e0=……… 

 

ζ  ε 

   

av 

[kPa] [%] [kPa-1]

12.5

25

50

100

200

300

500

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7.3   Consolidation diagram

Cv= _ _ _ _ _ _ _ cm2/s

  ε   [   %   ]

time

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8  Week 10: Direct shear test

n - horizontal forceSample 1

Sample

2Sample 3

δ - horizontal displacement ζ=  100 200 300 (kPa)

η - tangential stress = T/A ηfmax= (kPa)

ϕ=  °

c= (kPa)

60

     6     0

mm

    m    m

Shear Box Cross-Section

 

δ

 

8.1  

Test resultsInput data for the direct shear box

Sample 1 Sample 2 Sample 3

T T T

(kN) (mm) (kPa) (div) (mm) (kPa) (div) (mm) (kPa)

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8.2   Failure line

0

20

40

60

80

100

120

140

160

180

200

0 50 100 150 200 250 300 350 400

  η   [

   k   P  a   ]

ζ [kPa]

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8.3   Mobili zation cur ve

0

20

40

60

80

100

120

140

160

180

200

0 2 4 6 8 10 12 14

  η   [   k   P  a   ]

δ [cm]

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9  Week 11: Triaxial test. Performing an u.u. (unconsolidated undrained) test

Sample

1

Sample

2

Sample

3

°

ζ3= 100 200 300 kPa - radial stress c= kPa

75 110 150 kPa - deviator stress

ζ1=ζ3+  kPa - vertical stress

3   1

3

 

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10  Week 12: Triaxial test. Results interpretation

10.1  Failure line using Mohr’s circle

0

50

100

150

200

250

300

350

400

0 50 100 150 200 250 300 350 400

  η   [   k   P  a   ]

ζ [kPa]

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10.2  Representation of the stress paths in M IT coordinates (s-t)

s= 13

2

t= 13

2

 

0

50

100

150

200

250

300

350

400

450

500

0 50 100 150 200 250 300 350 400 450 500

   t   [   k

   P  a   ]

s [kPa]

Sample

1

Sample

2Sample 3

s= kPa

t= kPa

°

d= kPa


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