4a lapidario a#3 phase-relationships 2015-2016

24
7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016 http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 1/24 Technological University of the Philippines 1000 Ayala Boulevard, Ermita, Manila College of Engineering Civil Engineering Department CE 410 – 4A Soil Mechanics, Lec.  Assignment No. 3 Phase-Relationships LP!DR!", Ronal#o P. 11-0!-11" #ate of $u%mission& $%ly &&, &'() Engr. $es%s Ray M. Mansayon 'nstru(tor 

Upload: supertotie-landrito

Post on 24-Feb-2018

215 views

Category:

Documents


0 download

TRANSCRIPT

Page 1: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 1/24

Technological University of the Philippines

1000 Ayala Boulevard, Ermita, Manila

College of Engineering

Civil Engineering Department

CE 410 – 4A

Soil Mechanics, Lec.

 Assignment No. 3

Phase-Relationships

LP!DR!", Ronal#o P.

11-0!-11"

#ate of $u%mission& $%ly &&, &'()

Engr. $es%s Ray M. Mansayon

'nstru(tor 

Page 2: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 2/24

1. )or a given soil, s*o+ t*atγ sat =γ d+n γ w

$/'N&

γ sat =W 

γ sat =W s+W w

γ sat =γ d+W w

γ sat =γ d+γ w V w

γ sat =γ d+γ w (V v−V a )

V   

V V =V w   ,V a=0

γ sat =γ d+

γ w V v

/EE)E γ sat =γ d+nγ w

&. )or a given soil, s*o+ t*at

γ sat =γ d+(   e

1+e )γ w

$/'N&

γ sat =W 

V   

γ sat =W s+W w

V   

Page 3: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 3/24

γ sat =γ d+W w

V   

γ sat =γ d+  γ w V w

V v+V s  

γ sat =γ d+  γ w V w

eV s+V s

γ sat =γ d+  γ w V w

V s (1+e )

γ sat =γ d+γ w (V v−V a )

V s (1+e )

V V =V w   ,V a=0

γ sat =γ d+  γ w V v

V s (1+e )

γ sat =γ d+γ w(   e

1+e )

/EE)Eγ sat =γ d+(   e

1+e )γ w  

3. )or a given soil, s*o+ t*at

γ d=  eS γ w

(1+e ) w

$/'N&

γ d=W s

γ d=  W w /w

eV s+V s

Page 4: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 4/24

SAMPLE

γ d=  W w

w V s (1+e )

γ d=  γ w V w

w V s (1+e )

γ d=  γ w SV v

w V s (1+e )

γ d=  γ w SeV s

w V s (1+e )

γ d=  γ w Se

w (1+e )

/EE)E  γ d=  eS γ w

(1+e ) w  

4. A 0.4m3

 moist sam2le *as t*e follo+ing&

 Moist mass=711.2kg

 Dry mass=623.9 kg

Specific gravity of soil solids=2.68

Estimate&a. Moisture (ontent%. moist density(. #ry densityd. oid atioe. orosity

Page 5: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 5/24

5'EN&Volume (V) = 0.4 m3

Specific gravity of soil solids (Gs ) = 2.68 oist mass ( !  ) = "##.2 $g %ry mass ( s ) = 623.& $g 

E6'E#&w , ρ , e , n , ρd

$/'N&a.

w= M w

 M s=

711.2kg−623.9 kg

623.9 kg  ; w=0.1399∨13.99

%.

 ρ= M 

 =711.2 kg

0.4 m3

7  ρ=1778kg /m

3

(.

 ρd= M d

V   =

623.9 kg

0.4m3 7   ρd=1559.75 kg /m3

d.

 ρd=  Gs

1+e ρ w=1559.75

 kg

m3=

2.68

1+e (1000 kg

m3 ) 7   e=0.7182

e.

n=  e

1+e=

  0.7182

1+0.7182; n=0.4180

!. 'n its natural state, moist soil *as a volume of 0.33 ft 3

 and +eig*s 38.83 l%. /*e oven-dry

+eig*t of t*e soils is 34.!4 l%. 'fGs=2.67

, (al(ulate t*e moisture (ontent, moist unit +eig*t,

dry unit +eig*t, void ratio, 2orosity, and degree of saturation.

Page 6: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 6/24

V = 0.33ft3

5'EN&Volume (V) = 0.33 ft 3

'eigt (') = 3&.&3 l*ve+,dry !eigt (' s ) = 34.-4 lSpecific gravity of soil solids (Gs ) = 2.6" 

E6'E#&

w , γ , γ  d , e , n , S

$/'N&a.

w= M w

 M s=

39.93 lb−34.54 lb

34.54 lb  ; w=0.1516∨15.61

%.

γ =W 

 =39.93lb

0.33 ft 3

 ; γ =121lb/ ft 3

(.

γ d=W s

V  =

34.54 lb

0.33 ft 3 ; γ d=104.667 kg /m3

d.

γ d=  G s

1+e

 γ w=104.667 lb

ft 3=

2.67

1+e

 (62.4

  lb

ft 3

); e=0.5918

e.

n=  e

1+e=

  0.5918

1+0.5918; n=0.3718

f.

S=w G s

e  =

0.1561 (2.67 )0.5918

; S=0.7043

9. /*e moist +eig*t of 0.2 ft 3

 of a soil is 3 l%. /*e moisture (ontent and t*e s2e(ifi( gravity of

t*e soil solids are determined in t*e la%oratory to %e 11: and .", res2e(tively.Cal(ulate t*e follo+ing&

a. Moist unit +eig*t (lb / ft 3)

%. #ry unit +eig*t (lb / ft 3)

(. oid atio

Page 7: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 7/24

SOIL SAMPLE

d. orositye. #egree of $aturation ;:<

f. olume o((u2ied %y +ater (ft 3)

5'EN&Volume (V) = 0.2 ft 3

oist !eigt (') = 23 loisture co+te+t (!) = ##Specific gravity of soil solids (Gs ) = 2." 

E6'E#&γ , γ d , e , n , S , V  w  

$/'N&

a.

γ =W 

V  =39.93lb

0.33 ft 3  ; γ =115

 lb

ft 3

%.

γ d=  G s

1+e γ w=γ d=

  2.7

1+0.6262 (62.4  lb

ft 3 ); γ d=103.60lb / ft 

3

(.

γ =G

s

 (1+w )

1+e   ( γ w )=115 lbft 

3=2.7 (1

+0.11)

1+e   (62.4   lb

ft 3

); e=0.6262

d.

n=  e

1+e=

  0.6262

1+0.6262; n=0.3951

e.

S=w G s

e  =

0.11 (2.7 )0.6262

; S=0.4743∨47.43

f.

S=V w

V  =0.4743=

V w

0.2; V w=0.09 ft 

3

". /*e saturated unit +eig*t of a soil is 19.8 kN /m3

. /*e moisture (ontent of t*e soil is 1".1:.

#etermine t*e follo+ing&

Page 8: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 8/24

Moist Dry

S = 60%

a. #ry unit +eig*t%. $2e(ifi( gravity of soil solids(. oid atio

5'EN&

Saturated u+it !eigt (γ sat )   = #&.8 $/m3

oisture co+te+t (!) = #".#

E6'E#&γ d , Gs , e

$/'N&a.

γ d=  G s

1+e γ w=

  2.44

1+0.418 (9.81 kN 

m3 ); γ d=16.88

 kN 

m3

%.

γ sat =Gs+e

1+e  γ w=γ sat =

Gs (1+w )

1+e  γ w

19.8kN 

m3 =

G s (1+0.171 )

1+e   (9.81 kN 

m3 )

Se=w Gs

(1 ) e=Gs (0.171 ); Gs=2.44

e=0.418

=. /*e unit +eig*t of t*e soil is 95 lb / ft 3

. /*e moisture (ontent of t*is soil is 18. :. >*en t*e

degree of saturation is 90:.#etermine&

a. oid atio%. $2e(ifi( gravity of soil solids(. $aturated unit +eig*t

5'EN&

1+it !eigt   (γ )   = &- lft 3

oisture co+te+t(!) = #&.2%egree of Saturatio+(S) = 60

E6'E#&

Page 9: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 9/24

SOIL SAMPLE

e , Gs , γ s

$/'N&a.

γ =Gs+Se

1+e  γ w ;95

 lb

ft 3=

G s+0.6e

1+e   (62.4  lb

ft 3 )

%.Se=w G s ;0.6 e=0.192G s

Gs=  0.6 e

0.192

*a+   e=0.6912

;%<  Gs=2.16

(.

γ sat =Gs+e

1+e  γ w ; γ sat =

2.16+0.69121+0.6192  (62.4  lb

ft 3 ); γ sat =105.2

 lb

ft 3

8. )or a given soil, t*e follo+ing are given&Gs=2.67

7 moist unit +eig*t, γ =112lb / ft 3

7 and

moisture (ontent, w=10.8 .

#etermine&a. #ry unit +eig*t%. oid atio(. orosityd. #egree of saturation

5'EN&Specific gravity of te soil solid (Gs ) = 2.6" 

oist u+it !eigt (   γ   ) = ##2 lft 3

oisture co+te+t (!) = #0.8

E6'E#&γ d , e , n , S

$/'N&

Page 10: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 10/24

SOIL SAMPLE

a.

γ d=  G s

1+e γ w ; γ d=

  2.67

1+0.6482 (62.4 lb

ft 3 ); γ d=101.09

 lb

ft 3

%.

γ =Gs (1+w )

1+e  γ w=112

 lb

ft 

3=

2.67 (1+0.108 )1+e

  (62.4

  lb

ft 

3

); e=0.6482

(.

n=  e

1+e=

  0.6482

1+0.6482; n=0.3933

d.Se=w G s ; S (0.6482 )=(0.108 )2.67 ; S=44.49

10.efer to ro%lem 8. #etermine t*e +eig*t of +ater, in 2ounds, to %e added 2er (u%i( foot of

soil for&a.=0: degree of saturation%.100: degree of saturation 

5'EN&Specific gravity of te soil solid (Gs ) = 2.6" 

oist u+it !eigt (   γ   ) = ##2 lft 3

oisture co+te+t (!) = #0.8

E6'E#&W w at 80 , W wat 100

$/'N&a.

Se=w G s ; (0.8 )e=0.108 (2.67 )=e=0.3605

γ =Gs+Se

1+e  γ w

1=2.67+ (0.80 ) (0.3605 )

1+0.3605   (62.4  lb

ft 3 ); W =135.69 lb

W w at 80=135.69 lb−112 lb7

  W w at 80=23.69 lb

%.

Page 11: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 11/24

SOIL SAMPLE

Se=w G s ; (1 ) e=0.108 (2.67 )=e=0.28836

γ sat =Gs+e

1+e  γ w

1

=2.67+0.28836

1+0.28836  (62.4

 lb

ft 3

); W =143.28lb

W w at 100=143.28lb−112lb

W wat 80=31.28 lb

11. /*e moist density of a soil is 1680 kg/m3

. 5iven w=18  andGs=2.73

, determine&

a. #ry density%. orosity(. #egree of saturation

d. Mass of +ater, in kg /m3

, to %e added to rea(* full saturation

5'EN&

 ρ=1680kg /m3

w=18

Gs=2.73

  E6'E#&γ d , n , S , ρw if S=100

$/'N&

a.γ = ρg

γ =1680 (9.81 )

Page 12: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 12/24

γ =16480.8 N /m3

γ =Gs (1+w )

1+e  (γ w)

16480.8= 2.73 (1+0.18 )1+e

  (9810)

e=0.9175

γ d=  G s

1+e (γ w)

γ d=  2.73

1+0.9175(9810 ) ; γ d=13966.7797 N /m

3

%.

n=  e

1+e

n=  0.9175

1+0.9175; n=0.4785

(.

Se=w Gs

S (0.9175 )=(0.18 ) (2.73 ) ; S=0.5356∨53.56

d.

Se=w Gs

Page 13: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 13/24

SOIL SAMPLE

(1 ) e= (0.18 ) (2.73 )

e=0.4914

γ =Gs (1+w )

1+e  (γ w)

γ =2.73 (1+0.18 )

1+0.4914(9810)

γ =21189.442123 N /m3

γ = ρg

21189.442123= ρ(9.81)

 ρ=2159.9839 kg /m3

1. /*e dry density of a soil is 1780kg/m3

. 5ivenGs=2.68

, +*at +ould %e t*e moisture

(ontent of t*e soil +*en saturated?

5'EN&

 ρd=1780kg /m3

Gs=2.68

E6'E#&

w , if S=100

$/'N&

)or moisture (ontent,

γ d= ρd g

γ d=1780(9.81)

Page 14: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 14/24

SOIL SAMPLE

γ d=17461.8 N /m3

γ d=  G s

1+e (γ w)

17461.8=2.68

1+e (9810)

e=0.5056

Se=w Gs

1(0.5056)=w(2.68)

w=0.1887

w=18.87

13. /*e 2orosity of a soil is 0.3!. 5ivenGs=2.69

, (al(ulate&

a. $aturated unit +eig*t (kN /m3

)

%. Moisture (ontent +*en moist unit +eig*t ¿17.5 kN /m3

5'EN&

n=0.5

Gs=2.69

E6'E#&

a. γ sat  (kN /m3 )

%. w, if γ =17.5 kN /m3

Page 15: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 15/24

$/'N&

a.

e=  n

1+n

e=  0.35

1+0.35

e=0.2593

γ sat =Gs+e

1+e  (γ w)

γ sat =2.69+0.2593

1+0.2593(9.81)

γ sat =27.9752 kN  /m3

  . or moisture co+te+t if γ =17.5 kN /m3

γ =Gs (1+w )

1+e  (γ w)

17.5=2.69 (1+w )1+0.2593

(9.81)

w=0.1649

w=16.49

Page 16: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 16/24

SOIL SAMPLE

14. A saturated soil *as w=23  andGs=2.62

. #etermine its saturated and dry densities in

kg /m3

.

5'EN&

w=23

Gs=2.62

E6'E#&

a.  ρsat 

%.  ρd

$/'N&

a.

γ =γ sat 

γ =Gs (1+w )

1+e  (γ w )

γ sat =Gs+e

1+e  (γ w)

G s (1+w )

1+e  (γ w )=

G s+e

1+e  (γ w)

G s (1+w )

1+e   =

G s+e

1+e

2.62 (1+0.23 )1+e

  =2.62+e

1+e

e=0.602 6

Page 17: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 17/24

SOIL SAMPLE

γ sat =Gs+e

1+e  (γ w)

γ sat =2.62+0.6026

1+0.6026(9.81)

γ sat =19.7265 kN /m3

γ sat = ρsat g

19.7265= ρ sat (9.81)

 ρsat =2.0108 kg/m3

.

γ d=  G s

1+e (γ w)

γ d=  2.62

1+0.6026(9.81)

γ d=16.0378 kN /m3

γ d= ρd g

16.0378= ρ sat (9.81)

 ρsat =1.6348 kg/m3

1!. A soil *as e=075, w=21.5 ,  andGs=2.71

. #etermine&

a. Moist unit +eig*t ;2(f<

%. #ry unit +eig*t (lb / ft 3)

(. #egree of saturation ;:<

Page 18: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 18/24

5'EN&

e=0.75

w=21.5

Gs=2.71

E6'E#&

a.

ft 3

lb/¿γ ¿

 

%.

ft 3

lb/¿γ d ¿

(.   S

$/'N&

a.

γ =Gs (1+w )

1+e  (γ w)

γ =2.71 (1+0.215 )

1+0.75(62.4)

γ =117.4065lb / ft 3

.

γ d=  G s

1+e (γ w)

γ d=  2.71

1+0.75(62.4)

γ d=96.6309 lb/ ft 3

Page 19: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 19/24

SOIL SAMPLE

c.

Se=w Gs

S (0.75)=0.215 (2.71)

S=0.7769

S=77.69

19. /*e soil *as w=18.2 ,  Gs=2.67

 and S=80 . #etermine t*e moist and dry unit

+eig*ts of t*e soil in 2(f.

5'EN&Gs=2.67

w=18.2

S=80

E6'E#&

a.   γ 

%.  γ d

(.

$/'N&

a.

Se=w Gs

0.8(e)=0.182(2.67)

e=0.607 4

γ =Gs (1+w )

1+e  (γ w)

Page 20: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 20/24

SOIL SAMPLE

γ =2.67 (1+0.182 )1+0.6074

(62.4 )

γ =122.515 lb / ft 3

.

γ d=  G s

1+e (γ w)

γ d=  2.67

1+0.6074(62.4)

γ d=103.6506 lb/ ft 3

1". /*e moist unit +eig*t of a soil is 112.32lb / ft 3

 at a moisture (ontent of 10:. 5iven

Gs=2.7, determine&

a. e

%. $aturated unit +eig*t

5'EN&

γ =112.32lb / ft 3

Gs=2.7

w=10

E6'E#&

a.   e

%.  γ sat 

$/'N&

a.

Page 21: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 21/24

SOIL SAMPLE

γ =Gs (1+w )

1+e  (γ w )

112.32=2.7 (1+0.1 )

1+e  (62.4)

e=0.65

.

γ sat =Gs+e

1+e  (γ w)

γ sat =2.7+0.651+0.65

(62.4 )

γ sat =126.6909 lb / ft 3

1=. /*e moist unit +eig*ts and degrees of saturation of a soil are given in t*e ta%le.

γ ( pcf )   S ()10!."3 !0

11.9" "!

#etermine&

a. e

%.  Gs

5'EN&

γ ( pcf )   S ()

10!."3 !0

11.9" "!

E6'E#&

Page 22: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 22/24

SOIL SAMPLE

a.   e

%.  Gs

$/'N&

γ =Gs+Se

1+e  ( γ w )

105.73=Gs+0.5e

1+e  (62.4 )

Gs−1.194391026 e=105.73

62.4(1 )

112.67=G s+0.75 e

1+e  (62.4 )

Gs−1.055608974 e=112.67

62.4(2 )

E@uate ;1< ;<, terefore

Gs=2.6516

e=0.8014

18. efer to t*e ro%lem 1=. #etermine t*e +eig*t of +ater, in l%, t*at +ill %e in 2.5 ft 3

 of t*e

soil +*en it is saturated.

5'EN&

V s=2.5 ft 3

 +*en saturated

γ ( pcf )   S ()

10!."3 !0

Page 23: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 23/24

11.9" "!

E6'E#&

W w1 ,

W w2

$/'N&

)or +eig*t of +ater,

γ =Gs+Se

1+e  γ w

W w at 50

V s=

Gs+Se

1+e  γ w

W w at 50

2.5=

2.6516+0.5 (0.8014 )1+0.8014

(62.4)

W w at 50=264.3271lb

γ =Gs+Se

1+e

  γ w

W w at 50

V s=

Gs+Se

1+e  γ w

W w at 75

2.5=

2.6516+0.75 (0.8014 )1+0.8014

(62.4)

W w at 75=281.6773lb

Page 24: 4A Lapidario a#3 Phase-Relationships 2015-2016

7/25/2019 4A Lapidario a#3 Phase-Relationships 2015-2016

http://slidepdf.com/reader/full/4a-lapidario-a3-phase-relationships-2015-2016 24/24