Introduction to geotechnical engineering 2nd edition holtz solutions manual

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Introduction to Geotechnical Engineering 2nd Edition Holtz Solutions Manual Visit to Download in Full: https://testbankdeal.com/download/introduction-to-geotechni cal-engineering-2nd-edition-holtz-solutions-manual/

CHAPTER 2

INDEX AND CLASSIFICATION PROPERTIES OF SOILS

2-1. From memory, draw a phase diagram (like Fig. 2.2, but don’t look first!). The “phases” have a Volume side and Mass side. Label all the parts.

SOLUTION: Refer to Figure 2.2.

2-2. From memory, write out the definitions for water content, void ratio, dry density, wet or moist density, and saturated density.

SOLUTION: Refer to Section 2.2.

2-3. Assuming a value of ρs = 2.7 Mg/m3, take the range of saturated density in Table 2.1 for the six soil types and calculate/estimate the range in void ratios that one might expect for these soils.

SOLUTION: Create a spreadsheet using input values from Table 2.1 and Eq. 2.18.

(Given)(see Eq. 2.18)

ρ' - min ρ' - max emax emin (Mg/m3)(Mg/m3) 0.91.40.890.21 0.41.13.250.55 1.11.40.550.21 0.91.20.890.42 0.00.1 ∞ 16.00 0.30.84.671.13
© 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458. Introduction to Geotechnical Engineering 2nd Edition Holtz Solutions Manual Visit TestBankDeal.com to get complete for all chapters

2-4. Prepare a spreadsheet plot of dry density in Mg/m3 as the ordinate versus water content in percent as the abscissa. Assume ρs = 2.65 Mg/m3 and vary the degree of saturation, S, from 100% to 40% in 10% increments. A maximu m of 50% water content should be adequate.

SOLUTION: Solve Eq. 2.12 and Eq. 2.15 for ρd = f(ρs, w, S, Gs), or use Eq. 5.1.

Index and Classification Properties of Soils Chapter 2
ρ S w ρ = dry ρ w w+S ρs S =100908070605040302010 w ρdry ρdry ρdry ρdry ρdry ρdry ρdry ρdry ρdry ρdry (%) (Mg/m3)(Mg/m3)(Mg/m3)(Mg/m3)(Mg/m3)(Mg/m3)(Mg/m3)(Mg/m3)(Mg/m3)(Mg/m3) 0.02.652.652.652.652.652.652.652.652.652.65 5.02.342.312.272.232.172.091.991.841.591.14 10.02.092.051.991.921.841.731.591.411.140.73 15.01.901.841.771.691.591.481.331.140.890.53 20.01.731.671.591.511.411.291.140.960.730.42 25.01.591.531.451.361.261.141.000.830.610.35 30.01.481.411.331.241.141.020.890.730.530.30 35.01.371.311.231.141.040.930.800.650.470.26 40.01.291.221.141.050.960.850.730.580.420.23 45.01.211.141.060.980.890.780.670.530.380.21 50.01.141.071.000.920.830.730.610.490.350.19 Problem 2-4 0.00 0.50 1.00 1.50 2.00 2.50 3.00 0510152025303540455055 w (%) ρdry (Mg/m3 ) S=100% S=90% S=80% S=70% S=60% S=50% S=40% S=30% S=20% S=10% © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2-5a Prepare a graph like that in Problem 2.4, only use dry density units of kN/m3 and pounds per cubic feet.

2.12

2.15:

Index and Classification Properties of Soils Chapter 2
SOLUTION: ρ S w From Eq.
and Eq.
ρ = dry ρ w w+S ρs S =100908070605040302010 w γ dry γ dry γdry γ dry γ dry γdry γ dry γ dry γdry γ dry (%) (kN/m3)(kN/m3)(kN/m3)(kN/m3)(kN/m3)(kN/m3)(kN/m3)(kN/m3)(kN/m3)(kN/m3) 0.026.0026.0026.0026.0026.00 26.0026.0026.0026.0026.00 5.022.9522.6622.3021.8621.29 20.5519.5318.0315.6411.18 10.020.5520.0819.5318.8618.03 16.9915.6413.8011.187.12 15.018.6018.0317.3716.5815.6414.4813.0411.188.705.23 20.016.9916.3615.6414.7913.8012.6211.189.407.124.13 25.015.6414.9714.2213.3612.3511.189.798.106.033.41 30.014.4813.8013.0412.1711.1810.048.707.125.232.90 35.013.4912.8012.0411.1810.219.117.836.354.612.53 40.012.6211.9411.1810.349.408.337.125.734.132.24 45.011.8611.1810.449.628.707.686.535.233.732.01 50.011.1810.529.798.998.107.126.034.803.411.82 Problem 2-5a 0.00 5.00 10.00 15.00 20.00 25.00 30.00 0510152025303540455055 w (%) γ dry (kN/m3 ) S=100% S=90% S=80% S=70% S=60% S=50% S=40% S=30% S=20% S=10% © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2-5b Prepare a graph like that in Problem 2.4, only use dry density units of pounds per cubic feet.

Soils Chapter 2
Index and Classification Properties of
SOLUTION: sw dry s GS SGw γ γ= + S =100908070605040302010 w γ dry γ dry γdry γ dry γ dry γdry γ dry γ dry γdry γ dry (%) (pcf)(pcf)(pcf)(pcf)(pcf)(pcf)(pcf)(pcf)(pcf)(pcf) 0.0165.36165.36165.36165.36165.36165.36165.36165.36165.36165.36 5.0146.01144.14141.86139.04135.45130.72124.21114.7099.4671.12 10.0130.72127.75124.21119.95114.70108.0899.4687.8071.1245.30 15.0118.33114.70110.47105.4799.4692.1282.9471.1255.3533.24 20.0108.08104.0799.4694.1187.80 80.2771.1259.7745.3026.25 25.099.4695.2590.4584.9678.59 71.1262.2551.5438.3421.69 30.092.1287.8082.9477.4371.12 63.8555.3545.3033.2418.48 35.085.7981.4476.5871.1264.95 57.9249.8340.4129.3316.09 40.080.2775.9371.1265.7759.77 53.0045.3036.4826.2514.26 45.075.4271.1266.3961.1655.35 48.8541.5333.2423.7512.79 50.071.1266.8962.2557.1651.54 45.3038.3430.5321.6911.60 Problem 2-5b 0.00 20.00 40.00 60.00 80.00 100.00 120.00 140.00 160.00 180.00 0510152025303540455055 w (%) γ dry (pcf) S=100% S=90% S=80% S=70% S=60% S=50% S=40% S=30% S=20% S=10% © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.6. Prepare a graph like that in Problem 2.4, only for S = 100% and vary the density of solids from 2.60 to 2.80 Mg/m3. You decide the size of the increments you need to “satisfactorily” evaluate the relationship as ρs varies. Prepare a concluding statement of your observations.

Note: The relationship between ρdry and w is not overly sensitive to ρs

Index and Classification Properties of Soils Chapter 2
SOLUTION: ρ S w From Eq.
ρ w w+S ρs
2.12 and Eq. 2.15: ρ = dry
ρs = 2.62.652.72.752.8 w ρdry ρdry ρdry ρdry ρdry (%) (Mg/m3)(Mg/m3)(Mg/m3)(Mg/m3)(Mg/m3) 0.02.602.652.702.752.80 5.02.302.342.382.422.46 10.02.062.092.132.162.19 15.01.871.901.921.951.97 20.01.711.731.751.771.79 25.01.581.591.611.631.65 30.01.461.481.491.511.52 35.01.361.371.391.401.41 40.01.271.291.301.311.32 45.01.201.211.221.231.24 50.01.131.141.151.161.17 0.00 0.50 1.00 1.50 2.00 2.50 3.00 0510152025303540455055 w (%) ρ s (Mg/m3 ) © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.7. The dry density of a compacted sand is 1.87 Mg/m3 and the density of the solids is 2.67 Mg/m3. What is the water content of the material when saturated?

2.8. A soil that is completely saturated has a total density of 2045 kg/m3 and a water content of 24%. What is the density of the solids? What is the dry density of the soil?

b)

Index and Classification Properties of Soils Chapter 2
SOLUTION: w dry w s 3 w 33 drys S From Eq. 2-12 and Eq. 2-15: ;Note: S = 100% wS 1111 Solving for w: wS(1Mg/m)(100%)16.0% 1.87Mg/m2.67Mg/m ρ ρ= ρ + ρ ⎛⎞ ⎛⎞ =ρ−=−= ⎜⎟ ⎜⎟ ⎜⎟ ρρ ⎝⎠ ⎝⎠
SOLUTION:
Solve using equations or phase diagrams: 3 t dry w satdryw s wdry 3 s drywsat 2045 1649.2kg/m (1w)(10.24) 1 (1000)(1649.2) 2729.6kg/m (1649.210002045) ρ ρ=== ++ ⎛⎞ ρ ρ=−ρ+ρ ⎜⎟ ρ ⎝⎠ ρρ ρ=== ρ+ρ−ρ+−
a)
Solve using phase
relationships: t t w ws s twssss 3 s w ww w 3 s s s 3 s dry t assume V1.0 M2045kg M 0.24M0.24M M MMM20450.24MMM1649.19kg 0.24M M 1000V0.3958m V1000 M 1649.19 2729.6kg/m V10.3958 M 1649.19 1649.2kg/m V1 = = =→= =+→=+→= ρ==→== ρ=== ρ=== © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
diagram

2.9 What is the water content of a fully saturated soil with a dry density of 1.72 Mg/m3? Assume ρs = 2.72 Mg/m3

2-12 and Eq. 2-15: ;Note:

2.10. A dry quartz sand has a density of 1.68 Mg/m3. Determine its density when the degree of saturation is 75%. The density of solids for quartz is 2.65 Mg/m3

2.11. The dry density of a soil is 1.60 Mg/m3 and the solids have a density of 2.65 Mg/m3. Find the (a) water content, (b) void ratio, and (c) total density when the soil is saturated. SOLUTION:

From Eq. 2-12 and Eq. 2-15:

(a) Solving for w: wS(1Mg/m)(100%)24.76% 1.60Mg/m2.65Mg/m w (24.76)(2.65)

(b) From Eq. 2.15:

Index and Classification Properties of Soils Chapter 2
SOLUTION: w dry w s 3 w 33 drys S
Eq.
wS 1111 Solving for w: wS(1Mg/m)(100%)21.4% 1.72Mg/m2.72Mg/m ρ ρ= ρ + ρ ⎛⎞ ⎛⎞ =ρ−=−= ⎜⎟ ⎜⎟ ⎜⎟ ρρ ⎝⎠ ⎝⎠
From
S = 100%
SOLUTION: drydry(final) w dry w s 3 w 33 drys tdry
S
Eq. 2-12
2-15: wS 1111 Solving for w: wS(1Mg/m)(75%)16.34% 1.68Mg/m2.65Mg/m final (1 ρ=ρ ρ ρ= ρ + ρ ⎛⎞ ⎛⎞ =ρ−=−= ⎜⎟ ⎜⎟ ⎜⎟ ρρ ⎝⎠ ⎝⎠ ρ=ρ+ w)1.68(10.1634)1.95Mg/m3 =+=
Recognize that (initial)(final);S = 75%
From
and Eq.
w dry w s 3 w 33 drys s w Given: S = 100% S
wS 1111
S(100)(1 ρ ρ= ρ + ρ ⎛⎞ ⎛⎞ =ρ−=−= ⎜⎟ ⎜⎟ ⎜⎟ ρρ ⎝⎠ ⎝⎠ ρ == ρ 3 tdry 0.656 .0) (c)
=
© 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
e
(1w)1.60(10.2476)1.9962.00Mg/m
ρ=ρ+=+==

2.12. A natural deposit of soil is found to have a water content of 20% and to be 90% saturated. What is the void ratio of this soil?

SOLUTION: s s w

=

w = 20% and S = 90%; assume G2.70

w (20.0)(2.70)

===

(a) WWW625012lb

W50

W 62 (b)

(c)

12 (d) V0.1923ft 62.4

50

e =−=−= =×== γ=== γ=== === γ === γ =−=−=

wts w s t t t s dry t 3 w w w 3 s s sw vtv

G(2.64)(62.4)

====

V 0.2565 0.84510.84 V0.3035

v s

M100.0649.3150.75g

M113.27100.0613.21g

s w w s s w

M 13.21(100)

(a)w100%26.0326.0% M50.75 w 2.80(26.03)

=−= =−= =×=== ρ

===

Index and Classification Properties of Soils Chapter 2
ρ
From Eq. 2.15: e0.60 S(90)(1.0) ρ
2.13. A chunk of soil has a wet weight of 62 lb and a volume of 0.56 ft3. When dried in an oven, the soil weighs 50 lb. If the specific gravity of solids Gs = 2.64, determine the water content, wet unit weight, dry unit weight, and void ratio of the soil.
SOLUTION: Solve using phase diagram relationships.
V0.56 W
V0.56 W
W 12(100) w100%24.0%
110.7pcf
89.29pcf
W 50 V0.3035ft
VVV0.560.30350.2565
2.14. In the lab, a container of saturated soil had a mass of 113.27 g before it was placed in the oven and 100.06 g after the soil had dried. The container alone had a mass of 49.31 g. The specific gravity of solids is 2.80. Determine the void ratio and water content of the original soil sample.
SOLUTION: Solve using phase diagram relationships.
ρ © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
(b)FromEq. 2.15: e=0.72880.73 S(1)(100)

2.15. The natural water content of a sample taken from a soil deposit was found to be 12.0%. It has been calculated that the maximum density for the soil will be obtained when the water content reaches 22.0%. Compute how many grams of water must be added to each 1000 g of soil (in its natural state) in order to increase the water content to 22.0%.

SOLUTION:

w0.12M(0.12)M

MMMM0.12M1.12M1000g

M892.857g

M(0.12)(892.857)107.143g

Target state

(Note: M does not change between naturalstate and target state)

MwM(0.22)(89

2.857)196.429g

additional water necessary = 196.429107.14389.28689.29g = −==

2.16. A cubic meter of dry quartz sand (Gs = 2.65) with a porosity of 60% is immersed in an oil bath having a density of 0.92 g/cm3. If the sand contains 0.27 m3 of entrapped air, how much force is required to prevent it from sinking? Assume that a weightless membrane surrounds the specimen. (Prof. C. C. Ladd.)

VVV1.00.600.40m

MGV(2.65)(1000)(0.40m)1060kgM

Index and Classification Properties of Soils Chapter 2
w ws s tswsss s w s ws Natural state M
M
==→= =+=+== = == =×=
3 3 3 33 t 3 vt 3 stv 3 kg sssst m t kg t m t kg buoytoil m buoybuoy V1m1,000,000cm
SOLUTION:
VnV(0.6)(1.0)0.60m
M 1060 1060 V1.0
== =×== =−=−= =×ρ×=== ρ=== ρ=ρ−ρ=−= γ=ρ×== 3 3 N m 3 N buoy m Force(entrappedair)1373.40.27m370.8N =γ×=×= © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
1060920140 g(140)(9.81)1373.4

2.17. A soil sample taken from a borrow pit has a natural void ratio of 1.15. The soil will be used for a highway project where a total of 100,000 m3 of soil is needed in its compacted state; its compacted void ratio is 0.73. How much volume has to be excavated from the borrow pit to meet the job requirements?

2.18. A sample of moist soil was found to have the following characteristics:

Total volume: 0.01456 m3

Total mass: 25.74 kg

Mass after oven drying: 22.10 kg

Specific gravity of solids: 2.69

Find the density, unit weight, void ratio, porosity, and degree of saturation for the moist soil.

Index and Classification Properties of Soils Chapter 2
SOLUTION: tst v ss 3 t 3 s(emb) t s(borr)s(emb) 3 t(borr)sborr VVV V VV eee1 Embankment V100,000m 100,000 V57,803.47m 0.731 Borrow Pit V VV e1 VV(e1)(57,803.47)(1.151)124,277m ==→= + = == + == + =×+=+=
SOLUTION: 3 33 kg t m NkN tt mm 3 s s sw 3 v 25.74 (a)1767.8571768 0.01456 (b)g(1767.857)(9.81)17,342.6817.34 M 22.10 (c)V0.00822m G(2.69)(1000) V0.014560.008220.006344m 0.006344 e0.77180.77 0.00822 0.7718 (d)n 10.7 ρ=== γ=ρ×=== === ρ =−= === = + w w 10043.5643.6% 718 (e)M25.7422.103.64 3.64 V0.00364 1000 0.00364 S10057.37757.4% 0.006344 ×== =−= == =×== © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.19. A gray silty clay (CL) is sampled from a depth of 12.5 feet. The “moist” soil was extruded from a 6-inch-high brass liner with an inside diameter of 2.83 inches and weighed 777 grams. (a) Calculate the wet density in pounds per cubic feet. (b) A small chunk of the original sample had a wet weight of 140.9 grams and weighed 85.2 grams after drying. Compute the water content, using the correct number of significant figures. (c) Compute the dry density in Mg/m3 and the dry unit weight in kN/m3.

2.20. A cylindrical soil specimen is tested in the laboratory. The following properties were obtained:

VVV42.411526.54215.869in0.009184ft

Index and Classification Properties of Soils Chapter 2
SOLUTION: () ( ) () () () 3 2 3 t tt 3 3 t w wts s t dry lb dry ft 1lb 777g 453.6g M (2.83) (a)V637.741in,78.42978.4pcf 4V 1ft 37.741in 12in M 55.7 (b)MMM140.985.255.7g,w100%65.3865.4% M85.2 78.4 (c)47.40pcf (1w)(10.654) 1ft 47.4 0.3 π =×=γ==== =−=−==×=== γ γ=== ++ ρ= () () 33 33 3 kgMg mm NkN dry mm 0.4536kg 759.2880.759 048m1lb (759.288)(9.81)7448.67.45 == γ===
Sample diameter 3 inches Sample length 6 inches Wt. before drying in oven 2.95 lb Wt. after drying in oven 2.54 lb Oven temperature 110°C Drying time 24 hours Specific gravity of solids 2.65 What is the degree of saturation of this specimen? SOLUTION: 2 33 t 33 s s sw 33 vts wts 33 w w w w v (3)
4 W
V642.4115in0.02454ft
2.54 V0.01536ft26.542in G(2.65)(62.4)
WWW2.952.540.41lb
V 1 S100% V π =×== ==== γ =−=−== =−=−= ==== γ =×= 1.354 10071.5% 15.869 ×= © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
W 0.41 V0.00657ft11.354in 62.4

2.21 A sample of saturated silt is 10 cm in diameter and 2.5 cm thick. Its void ratio in this state is 1.35, and the specific gravity of solids is 2.70. The sample is compressed to a 2-cm thickness without a change in diameter.

(a) Find the density of the silt sample, in prior to being compressed.

(b) Find the void ratio after compression and the change in water content that occurred from initial to final state.

V(1.35)(83.553)112.797cmV

MV(1)(112.797)112.797g

MGV(2.70)(83.553)(1)

Index and Classification Properties of Soils Chapter 2
SOLUTION: 3 3 2 3 t w wv v vss 3 tvsssss 3 vw g www cm g sssw cm (10)
4 V S1VV V
(a)V2.5196.350cm
VeV1.35V VVV1.35VV2.35V196.350V83.553cm
π =×= ==→= =×= =+=+==→= === =ρ×== =××ρ= 33 t t gkg t cmm t 2 3 t2 3 s 3 vts final initial 225.594g M112.797225.594338.391g M 338.391 1.7231723 V196.35 (10)
V83.553cm(no change) VVV157.0883.55373.527cm 73.527 e0.88 83.553 112. (c)w = =+= ρ==== π =×= = =−=−= == = 3 wvws final 797 100%50.0% 225.594 final conditions VV73.527cm;M73.527g;M225.594g(no change) 73.527 w100%32.6% 225.594 w50.032.617.4% ×= ==== =×= Δ=−= © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
(b)V2.0157.08cm 4

2.22. A sample of sand has the following properties: total mass Mt = 160 g; total volume Vt =80 cm3; water content w = 20%; specific gravity of solids Gs =2.70. How much would the sample volume have to change to get 100% saturation, assuming the sample mass M t stayed the same? SOLUTION:

M133.33g

M(0.20)(133.33)26.667g;V(1)M26.667cm

M 133.33

V49.383cm;V8049.38330.617cm

G2.70

26.667

S100%87.10%

30.617

Desired condition: S100%

anges,butVandM remain the same

M26.667g;V26.667cm

VV(when S = 100%)

VVV49.38326.66776.053cm

V8076.0533.95cm

Soils Chapter 2
Index and Classification Properties of
3 wss tss s 3 g www cm 33 s sv sw i t
MwM(0.20)M MM0.20M160g
Vch =×= =+= = ==== ====−= ρ =×= = ss 3 ww vw 3 tsv 3
== = =+=+= Δ=−= © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.23. Draw a phase diagram and begin to fill in the blanks: A soil specimen has total volume of 80,000 mm3 and weighs 145 g. The dry weight of the specimen is 128 g, and the density of the soil solids is 2.68 Mg/m3. Find the: (a) water content, (b) void ratio, (c) porosity, (d) degree of saturation, (e) wet density, and (f) dry density. Give the answers to parts (e) and (f) in both SI and British engineering units.

SOLUTION:

(b)V47.7612cm47,761.2mm G(2.68)(1)

V80,00047,761.232,238.8mm

Index and Classification Properties of Soils Chapter 2
w w s 33 s s sw 3 v www
M
M128
(a)M14512817g
17 w100%10013.28113.3%
M 128
32,238.8 e0.67 47,761.2 32,238.8 (c)n100%40.3% 80,000
−= =×=×== ==== ρ =−= == =×= =×ρ= 33 33 3 3 33 gkg t cmm kg lbm t mft kg dry m kg l dry m 17cm17,000mm 17,000 S100%52.7% 32,238.8 145 (e)1.81251812.5 80 1 1812.5113.2(seeAppendixA) 16.018 1812.5 (f)1600.0 (10.13281) 1 1600.099.9 16.018 == =×= ρ=== ⎛⎞ ρ=×= ⎜⎟ ⎝⎠ ρ== + ⎛⎞ ρ=×= ⎜⎟ ⎝⎠ 3 bm ft (seeAppendixA) © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
(d)VM(17)(1)

2.24. A sample of soil plus container weighs 397.6 g when the initial water content is 6.3%. The container weighs 258.7 g. How much water needs to be added to the original specimen if the water content is to be increased by 3.4%? After U.S. Dept. of Interior (1990).

SOLUTION:

M397.6258.7138.9g

M0.063M

M138.9MM0.063MM1.063M

M130.668g

MwM(0.034)(130.668)4.44g

2.25. A water-content test was made on a sample of clayey silt. The weight of the wet soil plus container was 18.46 g, and the weight of the dry soil plus container was 15.03 g. Weight of the empty container was 7.63 g. Calculate the water content of the sample.

SOLUTION:

M15.037.637.40g

M18.4615.033.43g

M 3.43(100)

(a)w100%46.35146.3% M7.40

Index and Classification Properties of Soils Chapter 2
t ws twssss s w s ws
M
M w0.034
=−= = ==+=+= = Δ Δ== Δ=Δ×==
w w s
s
=−= =−= =×=== © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.26. A soil sample is dried in a microwave oven to determine its water content. From the data below, evaluate the water content and draw conclusions. The oven-dried water content is 23.7%. The mass of the dish is 146.30 grams. After U.S. Dept. of Interior (1990). SOLUTION:

CONCLUSION: The loss of additional water in the soil sample becomes negligible after 8 to 10 minutes in the microwave oven used in the experiment.

Index and Classification Properties of Soils Chapter 2
t ws ss s M231.62146.385.32g
231.62column3 column 5 = 100% 68.9733 =−= = =+ = ×
M(0.237)M 85.320.237MM M68.9733g (this value is constant throughout drying period)
GIVEN CALCULATED Time in Total Oven Mass of Mass of Water Oven Time Soil + Dish Water Content (min) (min) (g) (g) (%) 0 0 231.62 -- -3 3 217.75 13.87 20.11 1 4 216.22 15.40 22.33 1 5 215.72 15.90 23.05 1 6 215.48 16.14 23.40 1 7 215.32 16.30 23.63 1 8 215.22 16.40 23.78 1 9 215.19 16.43 23.82 1 10 215.19 16.43 23.82 19.0 20.0 21.0 22.0 23.0 24.0 25.0 01234567891011 Time in Oven (min) Water Content (% ) © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.27. The mass of a sample of silty clay soil plus container is 18.43 g and the weight of the dry soil plus container is 13.67 g. The container we ighs 8.84 g. Compute the water content of the sample.

M13.678.844.83g

M18.4313.674.76g

M 4.76(100) (a)w100%98.5% M4.83

SOLUTION: s w w s

2.28. A specimen of fully saturated clay soil that weighs 1389 g in its natural state weighs 982 g after drying. What is the natural water content of the soil?

SOLUTION:

M1389982407g

w w s

=×==

M 407(100) (a)w100%41.4% M982

2.29. The volume of water in a sample of moist soil is 0.24 m3. The volume of solids Vs is 0.25 m3. Given that the density of soil solids ρs is 2600 kg/m3, find the water content.

SOLUTION:

MV(2600)(0.25)650kg

sss www

MV(1000)(0.24)240kg

240 w100%36.9% 650

2.30. For the soil sample of Problem 2.29, compute (a) the void ratio and (b) the porosity.

SOLUTION: Assume S = 100%

s Gw (2.6)(0.3692) (a)e0.96

=== =×= +

Index and Classification Properties of Soils Chapter 2
=−= =−=
=×==
=−=
=ρ×== =×=
=ρ×==
S(1) 0.96 (b)n10050.0% 10.96 © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.31. For the soil sample of Problem 2.29, compute (a) the total or wet density and (b) the dry density. Give your answers in Mg/m3, kg/m3, and lbf/ft3

2.32. A 592-cm3 volume of moist sand weighs 1090 g. Its dry weight is 920 g and the density of solids is 2680 kg/m3. Compute the void ratio, porosity, water content, degree of saturation, and

Index and Classification Properties of Soils Chapter 2
SOLUTION: Assume S = 100% 333 333 3 t kgMg lbm t mmft kgMg lbm dry mmft (a)V0.250.240.49m 710 1448.981.4590.4 0.49 650 (b)1326.531.3382.8 0.49 =+= ρ==== ρ====
density in kg/m3 SOLUTION: 33 kgg s mcm 3 s 3 v v s w 3 w w w v 26802.68 920 V343.284cm 2.68 V592343.284248.716cm V 248.716 (a)e0.72450.72 V343.284 0.7245 (b)n100%42.0% 10.7245 (c)M1090920170g 170 V170cm V 170 S100%10068.4% V248.716 (d ρ== == =−= ==== =×= + =−= == ρ =×=×= 33 gkg t cmm 1090 )1.8411841 592 ρ=== © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
total

2.33. The saturated density γsat of a soil is 137 lbf/ft3. Find the buoyant density of this soil in both lbf/ft3 and kg/m3

2.34. A sand is composed of solid constituents having a density of 2.68 Mg/m3. The void ratio is 0.58. Compute the density of the sand when dry and when saturated and compare it with the density when submerged.

of Soils Chapter 2
Index and Classification Properties
SOLUTION: () 3 3 33 3 lbf ft kg m kg lbf ftm lbm ft '13762.474.6 16.018 '74.61195 1 γ=−= ⎛⎞ ρ== ⎜⎟ ⎜⎟ ⎝⎠
SOLUTION: 3 3 3 3 s 3 vt Mg dry m 3 wv w t Mg sat m Mg m Assume V1m V0.58,V10.581.58m 2.68 1.69621.70 1.58 For S = 100%; VV0.58m M(1)(0.58)0.58Mg M2.680.583.26Mg 3.26 2.06 1.58 '2.061.01.06 = ==+= ρ=== == == =+= ρ== ρ=−= © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.35. A sample of natural glacial till was taken fr om below the groundwater table. The water content was found to be 52%. Estimate the wet density, dry density, buoyant density, porosity, and void ratio. Clearly state any necessary assumptions.

2.36. A 1-m3 sample of moist soil weighs 2000 kg. The water content is 10%. Assume ρs = 2.70 Mg/m3. With this information, fill in all blanks in the phase diagram of Fig. P2.36.

Index and Classification Properties of Soils Chapter 2
SOLUTION: 3 3 ss ssssws t ww3 wvwv vw 3 t Mg tm dry AssumeV1m,AssumeG2.7 MGV(2.7)(1)(1)2.7Mg,MwM(0.52)(2.7)1.404Mg M2.71.4044.104Mg VM S1VV,V1.404mV V V1.4041.02.404m 4.104 (a)1.71 2.404 2.7 (b)1. 2.404 == =××ρ===×== =+= ==→==== ρ =+= ρ== ρ== 3 3 Mg m Mg m 12 (c)'1.711.00.71 1.404 (d)n100%58.4% 2.404 1.404 (e)e1.4 1.0 ρ=−= =×= ==
SOLUTION: wss tssss w s33 sw s 33 va MMw0.10M M2000M0.10M1.10MM1818.18kg M(0.10)(1818.18)181.82kg M1818.18181.82 V0.673m,V0.181m 27001000 V10.6730.327m,V0.3270.1810.146m =×= ==+=→= == ===== ρ =−==−= air water solid Mw=182 Ms=1818 M Vt=2000 w =0.18 Vs =0.67 Va =0.15 Vv=0.33 Volume(mMass(kg) 3) Vt=1.0 © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.37. For the information given in Problem 2.36, calculate (a) the void ratio, (b) the porosity, and (c) the dry density.

2.38. The void ratio of clay soil is 0.6 and the degree of saturation is 75%. Assuming the density of the solids is 2710 kg/m3, compute (a) the water content and (b) dry and wet densities in both SI and British engineering units.

Index and Classification Properties of Soils Chapter 2
SOLUTION: 3 kg drym 0.327 (a)e0.48590.49 0.673 0.327 (b)n10032.7% 1.0 1818.18 (c)1818 1.0 === =×= ρ==
SOLUTION: 3 s 33 vswv 3 t wwwsss t w s s dry t AssumeV1.0m VeV(0.6)(1.0)0.6m,VSV(0.75)(0.6)0.45m V0.61.01.6m MV(1000)(0.45)450kg,MV(2710)(1.0)2710kg M45027103160kg M450 (a)w10010016.6% M2710 (b)M27 V = =×===×== =+= =ρ×===ρ×== =+= =×=×= ρ== () () 3 3 33 3 3 3 kg m lbm kgftlbm drymft kg m tkg tm t lbm tft 101693.751694 1.6 1 1694105.8 16.018 M31601975 V1.6 1 (1975)123.3 16.018 == ⎛⎞ ρ== ⎜⎟ ⎜⎟ ⎝⎠ ρ=== ρ== © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.39. A specimen of saturated glacial clay has a water content of 38%. On the assumption that ρs = 2.70 Mg/m3, compute the void ratio, porosity, and saturated density.

(a)Fromw(38.0)(2.70)

(c)Frome(2.70)(1.0)(1.026)Eq.2.17:1.83911.84

2.40. The values of minimum e and maximum e for a pure silica sand were found to be 0.50 and 0.70, respectively. What is the corresponding range in the saturated density in kg/m3?

Index and Classification Properties of Soils Chapter 2
SOLUTION: 3 Mg sm s w swMg satm w=38%,S=100%,2.70
S(100)(1.0) e1.026
1e11.026
Eq.2.15:e1.0261.03
(b)n10010050.6%
1e11.026 ρ= ρ ==== ρ =×=×= ++ ρ+ρ + ρ==== ++ 3
SOLUTION: 3 3 sw sat Mg satm Mg satm e Eq.2.17:1e (2.70)(1.0)(0.50) maximum:2.13 10.50 (2.70)(1.0)(0.70) minimum:2.00 10.70 ρ+ρ ρ= + + ρ== + + ρ== + © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.41. Calculate the maximum possible porosity and void ratio for a collection of (a) tennis balls (assume they are 64.14 mm in diameter) and (b) tiny ball bearings 0.3 mm in diameter.

SOLUTION:

Three-dimensionalparticlearrangementofequalsphereshasbeenstudiedindepthby mathematicians,statisticians,andmaterialsscientistssincethe1600s.Aquickinternetsearch onpackingofequalsphereswillrevealnumerousmathematicaltheoriesandapproachesfor estimatingthedensestandloosestpossiblepacking.Ingeneral,theloosestarrangementof equalspheresyieldsavoidfractionofabout0.48,regardlessofspheresize.Asanaside,the densestpossiblepackingofequal-sizespheresyieldsasolidsvolumeofabout:

s V0.7405. 18 π == (Thesevaluesareapproximate–thereisnotaunifiedconsensusinthe literature.)

Densestpacking(notrequiredinproblemstatement)

2.42. A plastic-limit test has the following results:

Wet weight + container = 23.12 g

Dry weight + container = 20.84 g

Container weight = 1.46 g

Compute the PL of the soil. Can the plastic limit be evaluated by a one-point method?

SOLUTION: ws

W23.1220.842.28g,W20.841.4619.38g

W2.28

PL10010011.8

W19.38

Theplasticlimitcannotbeevaluatedusingaone-pointmethod.

2.43. During a plastic-limit test, the following data was obtained for one of the samples:

Wet weight + container = 23.13 g

Index and Classification Properties of Soils Chapter 2
tvs v max t v max s sv min Loosestpacking ForV1.0,V0.48,andV10.480.52 thus; V0.48 n10010048% V1.0 V0.48 e0.92 V0.52
0 n ===−= =×=×= === ==−= = min
1.0 0.2595 e0.35 0.7405 ×= ==
V0.7405,V1.00.74050.2595 thus;
.259510026%
w
s
=−==−=
=×=×=
© 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

Dry weight + container = 19.12 g

Container weight = 1.50 g

What is the PL of the soil?

SOLUTION:

2.44. The degree of saturation of a cohesive soil is 100%. The clay when wet weighs 1489 g and after drying weighs only 876 g. Find the water content of the soil. Draw a phase diagram and properly label it.

SOLUTION:

AssumeG2.70

2.45. For the soil in the previous problem, compute the void ratio and the porosity. Does your answer compare with what you would expect for a saturated cohesive soil?

SOLUTION:

2.46. For the soil in the previous two problems, compute (a) the total or wet density and (b) the dry density. Provide your answers in units of Mg/m3, kN/m3, and lbf/ft3

SOLUTION:

Index and Classification Properties of Soils Chapter 2
w s
=−==−= =×=×=
ws
W23.1319.124.01g,W19.121.5017.62g W4.01 PL10010022.8 W17.62
3 ts wt w s 33ww wv g wcm s s33 st sw
M876 MV
V613cm,V613cm
S100%,M1489g,M876g M1489876613g;M8766131489g M613 w10010070.0%
613613
1.0S1.0
M876
=== =−==+= =×=×= ====== ρ = ====+= ρ air water solid Mw=613 Ms=876 M Vt=1489 w =613 Vs =324 V Va v =613 Volume(cmMass(g) 3) Vt=937
thus;V324.4cm;V613324937cm G(2.7)(1.0)
vv st VV
613613 e1.89;n100%10065.4% V324V937 ====×=×=
© 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.47. A soil specimen had a buoyant density of 73 pounds per cubic foot. Calculate its wet density

SOLUTION:

and Classification Properties of Soils Chapter 2 33 33 33 33 tgMg tcmm t kNlbf tmft sgMg drycmm t kNlbf drymft M1489 (a)1.58911.59 V937 15.5999.2 M876
V937 9.1758.3 ρ==== γ== ρ==== γ==
Index
(b)0.93490.93
kg/m3
in
33 3 lblb tsatw ftft kg tm '73;'7362.4135.4 (135.4)(16.018)2169 γ=γ=γ=γ+γ=+= ρ== © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.53. The “chunk density” method is often used to determine the unit weight of a specimen of irregular shape. A specimen of cemented silty sand is treated in this way to obtain the “chunk density.” From the information given below, determine the (a) wet density, (b) dry density, (c) void ratio, and (d) degree of saturation of the sample.

Mass of specimen at natural water content in air = 181.8 g

Mass of specimen + wax coating in air = 215.9 g

Mass of specimen + wax in water = 58.9 g

Soil solid density = 2650 kg/m3

Index and Classification Properties of Soils Chapter 2
Natural water content = 2.5%
Wax
SOLUTION: 33 tst swts s s33 w swgg swcmcm wax3 waxtwaxtwax wax water MMM181.8 wM177.366gMMM181.8177.44.43g M1w1.025 MM177.366g4.43g V66.93cmV4.43cm 2.6501.0 M34.1 MMM215.9181.834.1gV36.28cm 0.940 M + =→===→=−=−= ++ ===→=== ρρ =−=−=→=== ρ displacedtwaxwaterdisplacedwaterdisplaced waterdisplaced3 twax w 3 airtwaxwaxws 3 vairwttw MMM215.958.9157.0g M157.0 V157.0cm 1.0 VVVVV157.036.284.4366.9349.36cm VVV49.364.4353.79cmVV + + + + =−→=−= === ρ =−−−=−−−= =+=+=→= 3 3 3 axwax tMg tm t sMg drym t v s w v V157.036.28120.72cm M181.8 (a)1.50 V120.72 M177.366 (b)1.47 V120.72 V53.79 (c)e0.80 V66.93 V4.43 (d)S100%1008.2% V53.79 −=−= ρ=== ρ=== === =×=×= air water solid Mw=4.43 Ms=177.4 M Vt=181.1 w =4.43 Vs =66.93 Va=49.36 Vv=53.79 Volume(cmMass(g) 3) Vt=120.72 waxM Vwax=34.1 wax =36.28 Vt+wax=157.0 © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
solid density = 940 kg/m3

2.54. A sensitive volcanic clay soil was tested in the laboratory and found to have the following properties:

(a) ρ = 1.28 Mg/m3, (b) e = 0.90, (c) S = 95%, (d) ρs = 2.75 Mg/m3, (e) w = 311%.

In rechecking the above values, one was found to be inconsistent with the rest. Find the inconsistent value and report it correctly. Show all your computations and phase diagrams.

8.558.55Thesevaluesareincorrectproportion. Consequently,theerrormustbeinthe

Index and Classification Properties of Soils Chapter 2
3 s sssws tsw t3 t t AssumeV1cm
MMM2.758.5511.30Mg M11.30 (1)V8.83cm 1.28 = =ρ×==×== =+=+= === ρ 33 w vsw w 33 tvs s t M8.55 VeV(9)(1)9cm;V8.55cm 1.0 (2)VVV9110cm8.83cm check:GwSe
SOLUTION:
MV2.75Mg;MwM(3.11)(2.75)8.55Mg
(2.65)(3.11)(0.95)(9.0)
=×===== ρ =+=+=≠ = = =→ ρ 3 3 tMg tm t Mg tm value. Re-calculateM11.301.13 V10 Solution:1.13 ρ=== ρ= air water solid Mw=8.55 Ms=2.75 M Vt=11.30 w=8.55 Vs=1.0 V Va v=9.0 Volume(mMass(Mg) 3) Vt=8.83or 10.0? © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.55. A cylinder contains 510 cm3 of loose dry sand which weighs 740 g. Under a static load of 200 kPa the volume is reduced 1%, and then by vibration it is reduced 10% of the original volume. Assume the solid density of the sand grains is 2.65 Mg/m3. Compute the void ratio, porosity, dry density, and total density corresponding to each of the following cases:

(a) Loose sand. (b) Sand under static load. (c) Vibrated and loaded sand.

(a)Loosesand-initialcondition V510cm VVV510279.24230.75cm

(b)Sandunderstaticload

M7401.471.47

(c)Vibratedandloadedsand

VV175.30175.30

e0.63;n100%10038.6% V279.24V454.54

M7401.631.63

Index and Classification Properties of Soils Chapter 2
SOLUTION: s3 st s ww 3 t 3 vts vv st s dry t M740 V279.24cm;M740g; 2.65 drysand:MV0.0
V510 ==== ρ == = =−=−= ====×=×= ρ=== 33 3 33 gMg cmm Mg drytm 3 t 3 vts vv st sgMg drycmm t d 451.45 1.45
VV230.75230.75 e0.83;n100%10045.2% V279.24V510 M7401.
510 V504.95cm 1.01 VVV504.95279.24225.71cm
VV225.71225.71
e0.81;n100%10044.2% V279.24V510
V504.95 = ρ=ρ= == =−=−= ====×=×= ρ==== ρ 3 33 Mg rytm 3 t 3 vts vv st sgMg drycmm t dryt 1.47
510 V454.54cm
1.10 VVV454.54279.24175.30cm
1.6 =ρ= == =−=−= ====×=×= ρ==== ρ=ρ= 3 Mg m 3 © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
V454.54

2.56. On five-cycle semilogarithmic paper, plot the grain-size distribution curves from the following mechanical analysis data on six soils, A through F. For each soil determine the effective size as well as the uniformity coefficient and the coefficient of curvature. Determine also the percentages of gravel, sand silt, and clay according to (a) ASTM, (b) AASHTO, (c) USCS, and (d) the British Standard.

continued next page

Index and Classification Properties of Soils Chapter 2
© 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
Chapter 2 2.56. continued. SOLUTION: () 2 6030 uc 106010 DD CC DDD == × SILT or CLAY Particle Size Distribution Grain size in millimeters 0.001 0.01 0.1 1 10 100 Percent finer by weight 0 10 20 30 40 50 60 70 80 90 100 0 10 20 30 40 50 60 70 80 90 100 SoilA SoilB SoilC SoilD SoilE SoilF SAND GRAVEL Coarse Fine Course Medium Fine Soil Type: Description: Depth: LL: PL: PI: Cu = Cc = LEGEND SoilEffective Size D30 D60 Cu Cc D10 (mm) (mm)(mm) A0.662846.72.1 B0.0050.040.0918.03.6 C0.0010.0611000.03.6 D0.160.220.31.91.0 E0.0060.0150.116.70.4 FN/DN/D0.003N/DN/D continued next page © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
Index and Classification Properties of Soils
Chapter 2
Index and Classification Properties of Soils
SoilGravelSandSiltClay (%)(%)(%)(%) A732340 B12334510 C19491814 D010000 E043498 F002971
SoilGravelSandSiltClay (%)(%)(%)(%) A801640 B18274510 C30381814 D010000 E1132498 F002971 (c)PercentagesaccordingtoUSCS. SoilGravelSandSiltClay (%)(%)(%)(%) A7323---B1233---C1949---D0100---E043---F00----
SoilGravelSandSiltClay (%)(%)(%)(%) A801640 B1827532 C30382111 D010000 E1132570 F004852 32 0 57 100 Fines (silt + clay) 4 55 32 0 57 100 Fines (silt + clay) 4 55 32 0 57 100 Fines (silt + clay) 4 55 32 0 57 100 Fines (silt + clay) 4 55 © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
2.56. continued. (a)PercentagesaccordingtoASTM.
(b)PercentagesaccordingtoAASHTO.
(d)PercentagesaccordingtotheBritishStandard.

2.58. The soils in Problem 2.56 have the following Atterberg limits and natural water contents. Determine the PI and LI for each soil and comment on their general activity.

SOLUTION: n wPL PILLPL;LI PI =−=

PropertySoil ASoil BSoil CSoil DSoil ESoil F wn(%)27141411872

LL133535--2860

PL82918NPNP28

PI56170032

LI3.8-2.5-0.24----1.38

SoilA:verysensitive,highlyactive

SoilB:mostlikelyaclayabovethewatertablethathasexperiencedadecreaseinmoisture

SoilC:mostlikelyaclayabovethewatertablethathasexperiencedadecreaseinmoisture

SoilD:mostlikelyafinesand

SoilE:mostlikelyasilt

SoilF:slightlysensitiveandactive

2.59. Comment on the validity of the results of Atterberg limits on soils G and H.

SOLUTION:

BasedonAtterberg’sdefinitions:LL>PL>SL.SoilGviolatesthedefinitionsbecausetheSL> PL(25>20).SoilHviolatesthedefinitionsbecausethePL>LL(42>38).

Index and Classification Properties of Soils Chapter 2
© 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.60. The following data were obtained from a liquid-limit test on a silty clay. Two plastic-limit determinations had water contents of 23.1% and 23.6%. Determine the LL, PI, the flow index, and the toughness index. The flow index is the slope of the water content versus log of number of blows in the liquid-limit test, and the toughness index is the PI divided by the flow index.

SOLUTION: 12

Fromtheplotbelow,LL=42.6

FlowwwIndex=slope=I10.6(fromlinearregresionofbestfitline)

use23.123.6 averagevalueofPLtests;PL23.4 2

PILLPL42.623.419.2

ToughnessI

Index and Classification Properties of Soils Chapter 2
F 2 1
N logN
== ⎛⎞ ⎜⎟ ⎝⎠ + == =−=−= F ndexPI19.21.81 I10.6 === NumberofBlows 10 Water Content (%) 30 32 34 36 38 40 42 44 46 48 50 15203040 LL=42.6 Flowindex=10.6 © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.61. Classify the following soils according to the USCS:

(a) A sample of well-graded gravel with sand has 73% fine to coarse subangular gravel, 25% fine to coarse subangular sand, and 2% fines. The maximum size of the particles is 75 mm. The coefficient of curvature is 2.7, while the uniformity coefficient is 12.4.

(b) A dark brown, wet, organic-odor soil has 100% passing the No. 200 sieve. The liquid limit is 32% (not dried, and is 21% when oven dried!) and the plastic index is 21% (not dried).

(c) This sand has 61% predominately fine sand, 23% silty fines, and 16% fine subrounded gravel size. The maximum size is 20 mm. The liquid limit is 33% and the plastic limit is 27%.

(d) This material has 74% fine to coarse subangular reddish sand and 26% organic and silty dark brown fines. The liquid limit (not dried) is 37% while it is 26% when oven dried. The plastic index (not dried) is 6.

(e) Although this soil has only 6% nonplastic silty fines, it has everything else! It has gravel content of 78% fine to coarse subrounded to subangular gravel, and 16% fine to coarse subrounded to subangular sand. The maximum size of the subrounded boulders is 500 mm. The uniformity coefficient is 40, while the coefficient of curvature is only 0.8. (After U.S. Dept. of the Interior, 1990.)

SOLUTION: RefertoTable2.7andcorrespondingfootnotes

(a)GW–Well-gradedgravelwithsand.

(b)OL--Organicclay

(c)SM–Siltysandwithgravel

(d)SM–Siltysandwithorganicfines

(e)GP-GM–Poorlygradedgravelwithsilt,sand,cobbles,andboulders(orGP-GC)

2.62.

Index and Classification Properties of Soils Chapter 2
(a)A-1-a (b)A-8 (c)A-2-4 (d)A-2-4orA-8 (e)A-1-a © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
Classify the five soils in the preceding question according to the AASHTO method of soil classification
SOLUTION:

2.63. The results of a sieve test below give the percentage passing through the sieve.

(a) Using a spreadsheet, plot the particle-size distribution.

(b) Calculate the uniformity coefficient.

(c) Calculate the coefficient of curvature.

Index and Classification Properties of Soils Chapter 2
Sieve Percent Finer by Weight ½”71 No.437 No.1032 No.2023 No.4011 No.607 No.1004 SOLUTION: () 22 6030 uc 106010 DD9.5(1.6) C24;C0.69 D0.39DD(9.5)(0.39) ====== × Grain Size Distribution Plot 2" 2"1" 1"1/2" 1/2"#4 #4#10 #10 #20 #20 #40 #40 #100 #100#200 #200 0 10 20 30 40 50 60 70 80 90 100 100.0010.001.000.100.01 Grain Diameter (mm) % Passing © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.64.Forthedatagivenbelow,classifythesoilsaccordingtotheUSCS.Foreachsoil,giveboth thelettersymbolandthenarrativedescription.

(a) 65% material retained on No. 4 sieve, 32% retained on No. 200 sieve. C u = 3, Cc = 1.

(b) 100% material passed No. 4 sieve, 90% passed No. 200 sieve. LL = 23, PL = 17.

(c) 70% material retained on No. 4 sieve, 27% retained on No. 200 sieve. C u = 5, Cc = 1.5.

SOLUTION:

(a)GP–Poorlygradedgravelwithsand

(b)CL-ML–Siltyclay

(c)GW–Well-gradedgravelwithsand

2.65. A sample of soil was tested in the laboratory and the following grain size analysis results were obtained. Classify this soil according to the USCS, providing the group symbol for it.

Index and Classification Properties of Soils Chapter 2
SieveSieve Opening (mm)Percent Coarser by WeightPercent Finer by Weight 1/2"12.73070 44.753664 102.005248 200.856436 400.4256931 600.257129 1000.157723 2000.075919 SOLUTION: () 22 6030 uc 106010 (a)PILLPL26233 DD3.9(0.4) C49;C0.51wellgraded D0.08DD(3.9)(0.08)
=−=−= ======→∴ × 70 64 48 36 3129 23 9 2" 2"1" 1"1/2" 1/2"#4 #4#10 #10 #20 #20 #40 #40 #100 #100#200 #200 0 10 20 30 40 50 60 70 80 90 100 100.0010.001.000.100.01 Grain Diameter (mm) % Passing © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.
SW-SM(Well-gradedsandwithsilt)

2.66. A minus No. 40 material had a liquidity index of 0.73, a natural water content of 44.5%, and a plasticity index of 24.7. Classify this soil according to the USCS, provide the group symbol.

SOLUTION:

2.67. A sample of soil was tested in the laboratory and the following grain size analysis results were obtained. Classify this soil according to the USCS, providing the group symbol for it.

Index and Classification Properties of Soils Chapter 2
wPL44.5PL LI0.73PL26.5 PI24.7 PILLPL;LLPIPL24.726.551.2 CH(Fatclay) ==→= =−=+=+=
Sieve No.Sieve Opening (mm)Percent Coarser by WeightPercent Finer by Weight 44.753763 102.005248 200.856436 400.4256931 600.257129 1000.157723 2000.0759010 SOLUTION: () 22 6030 uc 106010 (a)PILLPL602634 DD4.75(0.425) C63;C0.51wellgraded D0.075DD(4.75)(0.075) SW-SC(Well-gradedsandwithclay) =−=−= ======→∴ × 63 48 36 3129 23 10 2" 2"1" 1"1/2" 1/2"#4 #4#10 #10 #20 #20 #40 #40 #100 #100#200 #200 0 10 20 30 40 50 60 70 80 90 100 100.0010.001.000.100.01 Grain Diameter (mm) % Passing © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.68. A sample of soil was tested in the laboratory and the following grain size analysis results were obtained: Atterberg limits on minus No. 40 material were: LL = 36, PL = 14. Determine the USCS classification symbol for this soil. Extra credit - determine the full AASHTO classification for this soil (symbol plus group index).

SOLUTION: PILLPL361422

GI(F35)[0.20.005(LL40)]0.01(F15)(PI10)

GI(4535)[0.20.005(3640)]0.01(4515)(2210)

GI5.4

(a)USCS:SC(ClayeySand)

(b)AASHTO:A-6(5)

Index and Classification Properties of Soils Chapter 2
Sieve No.Sieve Opening (mm)Percent Finer by Weight 44.75100 102.00100 200.85100 400.42594 600.2582 1000.1566 2000.07545 Pan--0
=−=−= =−+−+−− =−+−+−− =
Grain Size Distribution Plot 2" 2"1" 1"1/2" 1/2"#4 #4#10 #10 #20 #20 #40 #40 #100 #100#200 #200 0 10 20 30 40 50 60 70 80 90 100 100.0010.001.000.100.01 Grain Diameter (mm) % Passing © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.69. Laboratory testing was performed on two soil samples (A and B).

(a) Determine the USCS classification symbol for Sample A.

(b) Determine the AASHTO classification for Sample B. Sieve

(a)PILLPL32257

(b)PILLPL523220;LL3052302232;A75

Index and Classification Properties of Soils Chapter 2
No.Sieve Opening (mm)A - Percent PassingB - Percent Passing 3inch76.2100 1.5inch38.198 0.75inch19.196 44.7577100 102.00--96 200.855594 400.425--73 1000.1530-2000.0751855 LiquidLimit3252 PlasticLimit2532 SOLUTION: ()22 6030 uc 106010
DD1.3(0.15) C29.5;C0.393poorlygraded D0.044DD(1.3)(0.044) USCSSM(Siltysandwithgravel)
GI(F35)[0.20.005(LL40) =−=−= ======→∴ × → =−=−=−=−=<∴−− =−+− ]0.01(F15)(PI10) GI(5535)[0.20.005(5240)]0.01(5515)(2010)9.2 AASHTOA-7-5(9) +−− =−+−+−−= → 10098 96 77 55 30 18 100 9694 73 55 2" 2"1" 1"1/2" 1/2"#4 #4#10 #10 #20 #20 #40 #40 #100 #100#200 #200 0 10 20 30 40 50 60 70 80 90 100 100.0010.001.000.100.01 Grain Diameter (mm) % Passing SampleASampleB © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.70. A sample of soil was tested in the laboratory and the following grain size analysis results were obtained: Atterberg limits on minus No. 40 material were: LL = 62, PL = 20. Determine the USCS letter symbol for this soil.

SOLUTION:

Index and Classification
of Soils Chapter 2
Properties
Sieve No.Sieve Opening (mm)Percent Coarser by WeightPercent Finer by Weight 44.750.0100.0 102.005.194.9 200.8510.090.0 400.42540.759.3 600.2570.229.8 1000.1584.815.2 2000.07590.59.5 Pan--100.00.0
() 22 6030 uc 106010 u PILLPL622042 DD0.43(0.25) C5.76;C1.9 D0.075DD(0.43)(0.075) TheCvalueiscloseto6.Technically,thissoilclassifiesaspoorlygraded; however,awellgradeddeterminationis =−=−= ===≅=== × notunreasonable. USCSSPSC(Poorlygradedsandwithclay) →− Grain Size Distribution Plot 100.0 94.9 90.0 59.3 29.8 15.2 9.5 2" 2"1" 1"1/2" 1/2"#4 #4#10 #10 #20 #20 #40 #40 #100 #100#200 #200 0 10 20 30 40 50 60 70 80 90 100 100.0010.001.000.100.01 Grain Diameter (mm) % Passing © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458.

2.71. A sample of a brown sandy clay was obtained to determine its Atterberg limits and then classify its soil type according to the Unified Soil Classification System. For one of the PL determinations, the wet + dish = 11.53 g and the dry weight + dish = 10.49 g. The dish only weighed 4.15 g. Compute the plastic limit. Another plastic limit was 16.9%. Three determinations of the liquid limit were made. Fo r 17 blows, the water content was 49.8%; for 26 blows, the water content was 47.5%; and for 36 blows, the water content was 46.3%. Evaluate the soil type, indicate the information on a plasticity chart, and give the Unified Soil Classification symbol.

SOLUTION:

M11.5310.491.04g

M10.494.156.34g

M1.04 wPL10010016.4

M6.34

16.416.9

PL16.65;Fromplotbelow:LL=48

2 PI4816.731

BasedonCasagrande'splasticitychart(Fig.2.13),thesoilfines

Index and Classification Properties of Soils Chapter 2
w s w PL s (avg)
=−= =−= ==×=×= + == =−= classifyasCL USCSCL(Sandyleanclay)∴→ NumberofBlows 10 Water Content (%) 40 42 44 46 48 50 52 54 56 58 60 15203040 LL=48.0 Flowindex=10.8 © 2011 Pearson Education, Inc., Upper Saddle River, NJ. All rights reserved. This publication is protected by Copyright and written permission should be obtained from the publisher prior to any prohibited reproduction, storage in a retrieval system, or transmission in any form or by any means, electronic, mechanical, photocopying, recording, or likewise. For information regarding permission(s), write to: Rights and Permissions Department, Pearson Education, Inc., Upper Saddle River, NJ 07458. Introduction to Geotechnical Engineering 2nd Edition Holtz Solutions Manual Visit TestBankDeal.com to get complete for all chapters

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