lime, cement, and lime-cemen'l' stabilizat.ion of a clay soil

64
LIME, CEMENT, AND LIME-cEMEN'l' STABILIZAT.ION OFA CLAY SOIL by- Richard Frederick Broberg Thesis submitted to the Graduate Faculty- ot the Virginia Polytechnic Institute in candidacy for the degree MASTER OFSCIENCE in Civil Engineering August, 1962 Blacksburg, Virginia

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LIME, CEMENT, AND LIME-cEMEN'l'

STABILIZAT.ION OF A CLAY SOIL

by-

Richard Frederick Broberg

Thesis submitted to the Graduate Faculty- ot the

Virginia Polytechnic Institute

in candidacy for the degree 0£

MASTER OF SCIENCE

in

Civil Engineering

August, 1962

Blacksburg, Virginia

2

TABLE or CONTE?iTS

I. Introduction•• •••• • •• • ••••••••• • •••

II. Review ot Literature.• •• •.•• •• • • •• • • • • •

III.

A. Cement Stabilization ot Soils •• • •• • • •••••

B. Lime Stabilization ot Soils ••••••• • •••••

c. Lime-Cement Stabilization of Soils

Materials •••• • •••• • • • ••

• • • •

• • • • • • • •

• • • • • • • • A. Soil • • • • • • • • • • • • • • • • • • • • • • • , •

B. Cement • • •••••••••••••• • •• • • • ••

c. Lime • • • • • • • .• • • • • • • • • • • • • • • • • •

IV. Laboratory Test Procedures • • • , • • • • • • • • • • • •

V. Results •••••••••• • .• • ••••••• • ••••

VI.

A. Preliminary Laboratory Testing Results ••••••••

B. Major Laboratoey Testing Results• •••• •••••.

c. Statistical Analysis ••• • •••

Discussion and Conclusions •••••• • • • •

• • • • • • • • • • • • • • • •

A. Atterberg Limits.••.• •••• • •• • • •••••

B. Uncured Compressive Strengths •••••••••• •.

c. Four-Day Cured Compressive Strengths ••••• • •••

D. Statistical Analyses • ••••••••••••••••

1. Lime percentages of o, ;, and 10 ••• •. • •••

2. Cement percentages ot o, S, and 10 • • ••••••

'.3. Lime-cement percentages ot 5-0, 0-5, 3-2, and 2-3 •

4. Lime-cement percentages of 10-0, 0-10, 6-4, and 4-6

Page

6

9

9

13

17

19

19

19

19

20

25

25 28

33

49

49 so 51 52 52

53 53 54

VII.

VIII.

IX. x.

TABLE or CONTENTS

5. Lime-cement percentages ot 6-4 and 4-6 • • • • • •

Page

• 54

E. Conclusions. ••• • • • • • • • • • • • • • • • • •• ss Recommendations •• • • • • Ac1cnowledgements • •.

Bibliography- •••••

Vita • • • • • • • • •

• • • •

• •

• ••• • • • • • • • • • • • • 57

• • • • • • • • • • • • • •• 58

••••••• • • •••• • •• 59

• • • • • • • • • • • • • • • • 61

LIST OF TABLES

Table Page

1. Atterberg Limits--Various Peroentagee ot Cement and Lime • • 25

2. Summary of Specimen Strengths. (O, ;, and 10 Per Cent Lime Additive) • • • • . • • • • • • • • • • • • • • • • • • 39

,3. 'l'hree-Wa.y Analysis of Variance Results for Streneth Da.ta (O, ;, and 10 Per Cent Lime Additiw) • ••• • ••• • • 40

4. Summa.ry of Specimen Strengths. (O, ;, and 10 Per Cent Cement Additive • • • • • • • • • • • • • • • • • • • . • • 4l

;. 'lhree-Way Analysis ot Variance Results for Strength Data (O, ;, and 10 Per Cent Cement Additive} • •••• • •• • 42

6. SU111DB.ry of Specimen Strengths (;-o, .o-;, ;-2, and 2-3 Per Cent Lime-Cement Additive}• ••••••• • •••••• • 43

7. 'l'hree-Way A."1alysis of Variance Results f'or Strength Data (5-o, 0-5, )-2, and 2-3 Per Cent Lime-Cement Additive) • • 44

s. Summary ot Specimen Strel'gths (10-0, 0-10, 6-4, and 4-6 Per Cent Lime-Cement Additiw) •••••••••••••• 45

9. 'lbree-Way Analysis ot Variance Results for Strength Data (10-0, 0-101 6-4, and 4-6 Per Cent Lime-Cement Addi tiff). • 46

10. Sminary of Specimen Strengths (6-4 and 4-6 Per Cent Lime-Cement Additive) • • ••••••• • • •• • • • • • • • • 47

ll. Three...Way Analysis ot Variance Results for Strength Data (6-4 and 4-6 Per Cent Lime-C..nt Additive) , •. •. • • 48

5

LIST 01'' FIGURES

figure Page

l. Effeet of lime-and cement-soil mixtures on Atterberg limits • 26

2. Effect of (cement-lime) soil mixtures on Attorberg limits • • 26a

3. St~a.ndard i?roctor and Standard Mini~ture compaction curves • , 27

4. Compacted strength-moisture-lime relationships ••••••• 29

;. Compacted strenith-1noisture-ce.r.1ent relationships •••••• 30

6. Compacted strength-moisture-(cement-1.ime) relationships ••• 31

7. Compacted strength-moisture-(celll.ent-llme) relationships.• • 32 8. Cured strength-m.oisture-lime relationships ••••••••• 35

9. CU.red strength-moisture-cement relationships •••••••• 36 10. Cu.red strength-moisture-(cement-lim.e) relationships ••••• 37

ll. Cured strength-m.oisture-(eement-lime) relationships •• • • • .38

6

I. INTRODUCTION

Foremost among road construction problems, from an economic stand-

point, is the locating of soil deposits which can be used satisfactorily

in highway eubgrades, subbases, and base courses. In some areas of the

United States, the locating of such deposits is extremely difficult, due

to the fact that abundant sand and gravel deposits are nonexistent. It

is in these areas of nonexistent base and subbase material primarily that

construction agencies are now exploring and using chemical stabilization

of substandard highway soils. In its broadest sense, chemical stabili-

zation implies improvement of a soil so that it can be used for subba.sea,

bases, and in some rare instances, surface courses. The types of admix-

tures which have been used in stabilization work include cementing agents,

modifiers, waterproofing a.gents, water-retaining agents, water-retarding

agents, and miscellaneous chemicals. Each admixture behaves vastly

different £ran the others, each has its own particular use, and, accord-

ingly, each has its own lind.ta.tions. (1)

Among the cementing materials which may be used are portland cement

and lime. Portland cement has been used with great success to improve

existing gravel roads, as well as to stabilize granular soils, silty

soils, and lean clays. This success can be attributed to the strength

gains which soil cement combinations show over the natural material.

Besides portla.nd cement, hydrated lime has been used, particularly in

the southern states to improve the engineering properties of various

soils. Lime increases soil strength primarily by pozzolanic action,

which is the formation of cem.entatious silicates a."\d aluminates. This

7

uteri.al is most efficient when used in granular materials and lean clays;

the quantity required for a proper hydration generally is relatively low.

Since they are generally susceptible to freezing and thawing action, how-

ever, lime-soil mixtures are limited in use to regions ot mild climate. (l)

This brief description of lime and cement stabilization serves to

introduce the subject matter of this thesis. In a general sense, the

effects ot adding both hydrated lime and portland cement to one particu-

lar clay soil were studied. In the case of both the lime and cement

a.ddi ti ves, a study was made ot unconfined compress! ve strength change•

following a four-day curing period in a "moist" room.. In order to make

the investigation more complete, a similar study was made by using combi-

nations of both additives with the same soil. In both cases where the

additives were added separately, the percentages used were 5 and 10 per

cent by dry weight of soil. In the additive combination study, lime-

cement percentage additions were 2-3, .3-2, 4-6, and 6-4 by dry weight ot

soil. '!he first two percentages, when added together, amount to ; per

cent stabilizing agent, while the latter two total 10 per cent. Since

these two totals were the same as those used in the separate lime and

cement studies, an analysis of strength changes when lime-cement combi-

nations, lime, and cement were added to the soil could. be ma.de.

In addition to unconfined compressive strength testing, moisture-

density relationships were established as well as changes in Atterberg

limits (liquid limit, plastic limit, and plasticity index) with varia-

tions or both the quantity and type of stabilizing a.gent used.. Atterberg

l1mi ts were first determined for lime ad.di ti ve percentages ot O, $1 and

10 by dry weight of soil, after which the limits were then run with the

same percentages of cement stabilizing agent. For the additiw combi-

nation study, Atterberg limit determinations were ma.de for lime-cement

percentages of 2-.3, .3-2, 4-6, and 6-4 by dry weight of soil.

9

II. P.EVIEW OF LIT.ERA TORE

The tremendous increases in tra.tfic on u. s. highways haw high-

lighted the importance ot the base course and subbase in modern highway

construction more than ever before. In locations where satisfactory

base course materials are readily available, construction ot such bases

presents no problem. However, a serious aggregate depletion problc has

res~ted in many states due to the heavy consumption ot aggregate in the

post-World War II construction boom. To solve this depletion problem

and stUl produce satistactoey bases and subbases, the engineer ia either

forced to employ "marginal" base course material.a or to stabilize the

soil-in-place with chemical additives.

A. Cement Stabilization of Soil.a

The origin or the idea of mixing soil and chemical additives together

to produce a structural material has not been definitely established.

'.the first record in the United States of mixing soil and cement involves

a patent for 11Soilamies 11 issued in 1917 tor highway uae. Following this

in 1920 was another patent tor "Soilcrete, 11 also tor highway use. Within

the next decade, mixing soil and cement together was tried in Iowa, Ohio,

South Dakota, and Texas. However, none or the records on experiences

mention the use ot a material ot known or predictable characteristics

that could be quantitatively evaluated by laboratory tests nor wen con-

struction procedures outlined by suitable specifications. (2)

In 1932, the South Carolina Highway Department began inwstigationa

of mixing soil and cement under the leadership ot the late Dr. c. H.

10

Moorefield. SeTeral test sections were built in 1933 and 19.34. Although

the causes ot the soil and cement reactions remained elusive, the field

performance ot these trial projects clearly' demonstrated that soil and

cement were compatible materials and that they eoul.d be mixed together

to torm a usable road. Following this, the Portla.nd Cement Association

initiated an extensive research program in Januar., ot 1935 under the

direction ot F. T. Sheets, Consulting Engineer, and M. D. Catton, Devel-

opnent Department. (2)

To confirm results of the laboratory- research, the South Carolina

State Highway Department, Bureau of Public Roads, and the Portland Cement

Aasociation cooperated in construction ot a 1.5-mile section of pavement

near JohnsonTille in the tall ot 1935. '!his project was the tirst 11cigl-

neered" soil-cement road. Following this, additional experimental

sections were constructed in South Carolina, Illinois, Michigan, Missouri,

and Wisconsin. M. D. Catton (.3) has reported on the success ot these

experimental sections. B7 1940 over 7.5 million square yards of soil-

cement had been built in the United States, mostly on roads and streets.

During the war period, 1941-1944, 22 million square yards ot soil-cement

airports were built. Following World War II, the use ot soil-cement tor

roads and streets increased rapidly. Additional uses included subbaaea

tor concrete pavements, shoulders, widening, parking and storage areas,

and linings tor reservoirs, ditches, and canals. By 1960 the annual use

or soil-cement in the United States and Canada reached 46 million square

yards with a total constructed yardage to that date ot almost 294 million

square yards. (4)

11

The first noticeable property change which takes place when cement

is mixed with moist coheain soils is a marked reduction 1n plasticity.

This reduction takes place either because of a cation exchange or a

crowing ot additional cations onto the clay, both processes acting to

change the electrical charge density around the clay particles. Clay

particles then become electrically attracted to one another, causing

flocculation or aggredation. the aggregated clay behaves like a silt,

which has a low plasticity or cohesion. Even the addition of relatively

small amounts of cement causes this aggregation to take place rather

quickly. The hydration ot the different cement constitWtnta occurs at

different rates in compacted cement-treated soil. The cementation is

mainl.7 chemical 1n nature and may be visualized as due to the developaent

of chemical bonds between adjacent cem.ent grain surtaoee, and between

cement grain surfaces and exposed soil particle surtaces. (5) ' The manner in which portland cement stabilizes soils to meet require-

ments for soil-cement differs somewhat tor tine-grained and gram1l ar

soils. In 1'1.ne-grain silty and clayey soils, the cement developa strong

linkages among and between the mineral aggregates and the soil aggregates

to tom. a matrix that ettectively encases the soil aggregates. lbe result-

ing matrix torma a honeycomb type of structure on which the strength ot

the mixture depends, since the clay aggregations within the matrix have

little strength and contribute little to the strength ot the soil-cement.

'lhe aurtace chem.cal ettect of the cement reduces the water affinity and

thus the water-holding capacity ot clayey soils. With reduced water

at1'1.n1ty, reduced water-holding capacity, and a strong matrix, an

12

encasement of the larger unpulverized raw soil aggregates is proYided.

Because of its strength and reduced water aftlnity, this encasement eervea

not only to protect the aggregates but also to prevent them trom swelling

and softening from absorption ot moisture and from sut.fering detrimental

freeze-thaw effects. (5)

With granular soils, the cementing action is aimUar to that which

takes place in concrete, with the exception that the cement paste does

not till. the voids in theaggregate. In sands, the aggregates become

cemented only at points of contact. The more densely graded the soil,

the smaller the voids, the more numerous and greater the contact areas,

and the stronger the cementing act.ion. Since well-graded granular soila

generally haTe a low swell potential and low trost susceptibil.1.ty, it is

possible to stabilize them with lesser cement contents than are needed

tor the uniformly graded sands, 'Nhich have a minimum ot contact area

between grains. For any type of soil, howeTer, the cementing process is

giwn the maxSmnm opportunity to dnelop when the mixture is hi~ coa-

pacted at a moisture content that facilitates both the densitication ot

the m:1x and the hydration of the cement.. (5)

the main requirements tor soil-cement of a prescribed quality are

that: (a) an adequate amount or cement ia mixed with the pulverized soil;

(b} the proper amount of water ia dispersed through the aoil-cement mix;

{c) the soil-cement mixture is properly denaitied; and (d) the compacted

soil-cement is protected against moisture loss and excessively low tempera-

tures during a prescribed curing period. In order tor the first three

requirements to be met, comm.only used tests and observations are now uaed

13

to predetermine control £actors. 'lb.ese tests and observations a.re ot two

types: those performed on the soil for the purpose of identification, and

those performed principally for controlling the design of the soil-cement

mix to meet specific requirements. For each of the two categories there

are several tests which a.re cormnonly used. The most commonly used soil

identification tests are liquid limit, plastic limit, and mechanical

analysis. quality control tests on soil-cement mixtures include moisture-

density relations, freeze-thaw tests, wet-dry tests, and COl'llpresaive-

atrength tests. (6)

B. Lime Stabilization of Soils

Although older types of stabilization such as bituminous, soil-cement,

and calcium chloride have been employed for years, lime stabilization, in

a modern sense, is relatively new. However, the Romans used lime exten-

sively in building roads, one of which was the Appian Way. In f'act, the

only materials used by the Romans were rock of various sizes, sand, and

lime, with lime being used in three of the five layers trom subbase to

wearing surface. 'n"ie Chinese have also used a crude form of lime stabi-

lization on the rural and village roads of China for years. Rule of thumb

mixing of lime with the soil-in-place was followed by compaction with

crude methods, with no wearing surface being used. In addition, lime has

also been used as the cementing material for earth dams constructed in

both China and India. (7) In the l920's the University of Missouri experimented with hydrated

lime on unpaved earth roads in cooperation with the Missouri Highway

Department. The only purpose of the experiments conducted then was to

14

prnent rutting and disintegration ot the earth roads during rain and snow.

Later, the u. s. Bureau or Public Roads became interested in the use of

lime tor stabilizing and conducted some field tests in South Dakota and.

Iowa. It was just two or three years later though that these roads tailed

since the stabilized base without a wearing surface had little resistance

to the abrasive action of traffic. (7) Nothing of importance was attempted with lime for road stabilization

until about 1938 when the Texas Highway Department conducted extensive

laboratory tests with varying percentages of lime on different types ot

southwestem soils. However, field work using lime was interrupted b7

World War II, even though laboratory.tests had proved lime to be generally

et.fective with clay soils. The first actual lime stabilization project

occurred in 1943 when two per cent of hydrated lime was used by the Corps

of Engineers to reduce the plasticity index of a caliche gravel in the

construction of a base course tor the runways and taxiways at Chase FJ..eld,

Texas. In spite of heavy wheel loads and considerable traffic during

World War II and for several years afterwards, the lime treated sections

showed remarkable durability. (7) It was not until August, 194.5, that lime stabilization was first

employed on a scientific basis by the Texas Highway Department. Approxi-

mately three per cent of commercial hydrated lime was used around Austin

in treating clay-gravels, granite gravels, and callche soils on tarm-to-market roads., stretches of state and u. s. highways, shoulders, and city

streets. Gradually other sections of the state tried lime, so much so that

within eight years the equivalant of about 250 miles of lime stabilized

15

roads had been constructed in Texas. EYentually-, other states began

experimenting with lime. Among these states were California, Kansas,

Arkansas, Missouri, Iowa, and Minnesota, while other states have started

to carry on laboratory and field tests, after which will come further

experimentation with lime in actual projects. (7) For the most part, lirn.e stabilization projects which have been U."'lder-

taken in recent years have been quite successful. With over 11,000 miles

of road equivalant in 35 states, lime stabilization is not experimental;

it is a well-proven road building method (8). That lime stabilization

is another 11tool 0 tor the road builder to use in complex construction

problems is evident because of its successtul and economic use on all

types ot roads, including 500 miles of interstate freeway in seven states.

'!he action of lime in soil can be explained by three distinct steps.

The first step is alteration of the water film surrounding the clay

minerals. A second step is the agglomeration of fine clay particles into

coarse, friable particles (silt and sand sizes) through a phenomenon

called base exchange (9). Base exchange involves either a cation exchange

or a crowding of additional cations onto the clay, with both processes

acting to change the electrical charge density around the clay particles.

Clay particles then become electrically attracted to one another, causing

flocculation or aggregation. Once the electrical charge density has been

changed, the clay particles behave as a silt, which has a low plasticity

or cohesion. A second chemical reaction is carbonation of lime by carbon

dioxide of the air producing calcium carbonate, a weak cement which is

deleterious to over-all strength gains. (10)

16

The third step in the action of lime in so.il can be explained as a

reaction of the lime with soil components to form new chemicals. 'lhe two

principal components of soil which react with lime are alumina and silica.

'lhis reaction is a long-term reaction and one that results in greater

strengths if lime-soil mixtures are cured for a period of time. It has

been teriued 11pozzolanic action. 11 'l'he amount of pozzolanic action which

will take place depends on such variables as qua.""'l.tity of lime, soil type,

and the length of curing time. (l)

Changes in the engineering properties or clayey soils, such as plas-

ticity, density, and strength, with addition of lime depend a.ppree,iably

on the cation originally absorbed on the clay surfaces, and on the type

ot clay (11). The nature or the exchangeable cation does not make much

difference in kaollr..i tie soils, but it makes a tremendous difference in

montmorillonitic soils. Expanding clays containing montmorUlonite react

readily with lime irr.mediately losing plasticity, and. after oom.paction

slowly gain pozzolanic strength. Clays contairdng mainly illite,. chlorite,.

or kaolinite are less effective users of lime. (9)

One of the most important functi9ne of lime is that it changes the

soil's plasticity appreciably. Lime increases both the liquid- and

plastic-1.i:mit values for soils having a plasticity index of less than

fifteen, which brings about an increase in plasticity index. For the

more plastic soils, however, lime generally decreases the liquid limit

and increases the plastic limit,. bringing about a decrease in plasticity

index. Lime-soil mixtures generally have lower compacted densities than

those of the natural soil. The decrease in density may be as much as five

17

per cent. Because of lower densities, a decrease in soil strength might

be expected. However, the reverse is true. The immediate increase in

soil strength is brought about by changes in the water films surrounding

the clay particles as well as granulation of the particles. Curing the

specimens for a period of time brings about further increases in strength.

(l) Coramonly used tests in soil-lime quality control are moisture-d.enslty

relations, freeze-thaw test, wet-dry tests, and compressive strength

tests. (12)

c. Lime-cement Stabilization of Soils

The large-scale employment of lime-cement soil stabilization is rela-

tively recent. In tact it was the success or the Texas Highway Department

in tLe field of lime stabilization which eventually bro~;ht about the firet

lime-cement stabilization project in 1950. Credit for the initial use ot

this type of si:.abilization belongs to the Fourth Army Engineers operating

out 0£ Fort Sam Houston, Texas. Around 1950, the Fourth Army Engineers

encountered areas of non-plastic materials which were not materially

affected by tLe addition of lime at Fort Sam Houston, Camp Polk, and Fine

Bluff Arsenal. In many instances these areas were interspersed with areas

having the soil portion too plastic to be mixed satisfactorily and eco-

nomically with cement unless the plastic characteristics of the clay were

changed. In order to correct this situation, a hydrated lime-cement combi-

nation plan was developed and used very effectively. By 1952, a total ot

2181000 square yards of lime-ce.~ent stabilization had either been completed

or placed under contract by the Fourth Army Engineers. (13)

In lime-cement stabilization., the lime lowers the plasticity index

of the clay, thereby making the cement combine more readily and ef.f'i-

cienUy with the soil particles. The cement combines so much more readily

that tbe Army clai.ms any extra manipulation required by using two admix-

tures separately is more than offset, since soil containing lime is much

more easily pulverized. In using this type of stabilization, the Anrty

combined two per cent hydrated lime by weight with six per cent cement

by volume. Fuller and Dabney (10) have reported on the success obtained

by using this percentage combination. In one particular case., this lime-

cei:1.e:.1t percentage was added to a. soil with a plasticity index of 25, and

a liquid limit o.f 40. After the samples had been subjected to 12 cycles

of a wet-dry test, the percent loss was 3.7. After a sample containing

eigb.t per cent cer.':ent by volume had been subjected to the same test., the

per cent loss was 8.4. Therefore, for the sample containing the additive

co.11bination, the per cent loss was but one-half the loss obtained with

the specimen containing eight r,er cent cement. (13)

19

III. MATIRIALS

'lb• clay ~11 used in all teats was taken frcm. the foundation exca-

vation for the Civil Engineering Building on the Virginia Pol:,t.echnic

Institute campus, It was reddish-brown in color, with plasticity charac-

teristics aa follows s liquid 1imi t - 67, plastic limit - 37, and

plasticity index - ,30. A mechanical. analysis which had previously- been

performed by Jan (14) showed that 96,9111, of the soil was finer than Sieve

No. 200. Classification of the soil according to the AASHO system (15)

showed it to be an A-7-5(20).

B. Lime -The quality ot the qdrated lime uaed in the experiments is coftNd

in AS'l'M Designation C-207, 'lype N. It waa manufactured by the Ripplemead.

Lime Company, Inc. of Ripplemead, Virginia.

c. Cement

An air-entraining {Type I-A) Lone Star :portland cement was ueed in

all cement additive experiments. Previous research (16) comparing the

use of normal (Type I) and air-entraining (Type I-A) cements with three

soils has shown that IGOisture-denait.y relationships and compreseive

strengths were sufficiently similar ao that the two types ot cement can

be used interchangeably in soil-cement construction,

20

IV. LABORA 'roRY TEST PROCEDURES

The major portion or this thesis is based on results obtained from

the unconfined compression of specimens ::nade with the Harvard i•liniature

Compaction apparatus (17). However, other tests were performed in con-

junction with the compression testing, and they will be described along

with any difficulties wtiich were encountered.

Tne miniature compaction mold used measures 1.313 inches inside

diameter with a length of 2.861 inches. Its volume is equal to 1/454

cubic feet. With this volwne, the weight of compacted soil in grams is

equal to the wet density in pounds per cubic feet. Before the unconfined

compression testing could be done, it was first necessary to determine

what compactive effort should be used to produce dry densities which

would be equivalant to Standard AA3HO dry deru!dties. The miniature com-

paction apparatus is equipped v,ri th a plunger attached to a spring which

compresses U.."1der a force of 40 pounds. It was found that 25 blows of this

plunger applied to three u..'tlform soil layers in the ha.rvard device yielded

dry densities which were equal to dry densities obtained by running the

Standard hASHO teat on the same soil. 'l1he opti.mull density occurred at

approximately the same moisture content in both cases, but a distinct

variance was noted in the two density-water content curves. The 11Standa.rd 11

curve re~.ained relatively flat within 3 or 4 percentage points of the

optimum moisture content on both the dry a.nd wet sides, while the "Minia-

turett curve yielded a much steeper sloJ;ie on both sides of the optimum

moisture content. Because of this much steeper slope, the miniature

compaction dry density is extremely sensitive to water content, and it

21

was found that a difference in water content of only one per cent could

create a difference in dry density of as much as two pounds per cubic foot.

It was also~sired to run unconfined. compression tests at a oom.pactift

effort equi val.ant to Modified AASHO, but this phase of the testing had

to be abandoned. 'l'"w0 different com.pa.ctive efforts were tried in an

attempt to obtain the sa.'lle dry density as the Modified AASHO test yielded

with the same soil, but in each case the dry density obtained was approxi-

mately six pounds per cubic toot less than what it should have been. It

may therefor~ be concluded tl~at Modified AASHO density cannot be obtained

with the Harvard apparatus, a.t least not with the 40 pound spring which,

along with a 20 pound spring, is part of the auxiliary equipnent that

comes with this compaction device. The desired resul.ts may have been

obtained with a heavier spring.

The unconfined compression testing was divided into two parts. In

the fir&t pa.rt, compacted specimens were tested in unconfined compression

immediately after they had been molded. A total of 81 specimens were

ma.de and tested, with nine samples being fabricated. for each additin

percentage used. 'lhree specimens were compacted at a water content on

the dry side ot the density curve, three a.t optimwn moisture content

(OMC), and three at a water content approximately three per cent greater

than OMC. When the cett.ent and lime additives were added to the aoil

separately, 5 .and 10 per cent by dry weight of soil was used. In the

additive combination study, lime-cement percentage additions were 2-3,

3-2, 4-6, and 6-4 by dry weight of soil. In the second part of the uncon-

fined compression testing, the same procedure was toll.owed, with the

22

exception that the specimens were not failed in compression until after

a tour-day storage period in a 100 per cent humidity curing room.

Prior to the compression testing, several specimens were compacted

at each stabilizing agent percentage tc determine the optimum moisture

content. With this known beforehand, "d.rr' :moisture contents were kept

about 3 per cent less than OMC while "Wet" moisture contents were kept

at appNXimateq the same percentage above OMC. For the uncured apeci-

ana, the moisture content sample included the entire tailed specimen.

J'or the cu:red specimens, however, the moisture content sample was taken

trca the soil which remained in the mixing pan after each cylinder had

been compacted. 'Dd.e water content, along v.1.th the weight ot the com-

pacted specimen, was uaed in determining the as-ccmpacted dJ7 densities.

Foll.owing the foar-day curing period, each specimen was weighed, and its

length and diameter dim.ens.ions were measured to the nearest 0.01 inch.

This was done before the unconfined compression testing. After testing,

water content determinations were again made, this time using the tailed

specimens. 'l'hese water contents, along with the weights ot the cured

specimens prior to testing were used to determine the as-cured dry' densi-

ties. In some casee during curing, overall epecimen dimensions either

increased or deereasedJ accordingly, compacted. dry densities and moisture

contents also changed scraewhat. 'ftlerefore, two dry densities-one at

compaction and one at compression testing-were detel"llined tor each cured

specimen.

caring ot the soil specimens at first presented a probl•• 'lbe

specimens were placed in gallon cans with the lids raised somewhat so

2,3

that the specimens would be exposed to the temperature and humidity con-

ditions which existed in the curing room. Ll.ds were kept over the cans

so that water would not collect on the top of the specimens. However,

attempts were first made to cure the specimens on moist porous stones

with the water level in the gallon cans kept at almost the top of the

porous stones. With the use of porous stones, water was able to rise up

into the specimens ttrough capillary action. This, in effect, increased

the water content appreciably, and hindered gains in strength which would

have developed if curing conditions had been beneficial. Since this

method of curing proved unsatisfactory, specimens were again paced inside

the gallon containers, but this time on inverted moisture cans so that

water could not penetrate into the specimens. This method of curing

proved satisfactory, and noticeable strength gains developed in those

specL'llens containing the larger amounts of stabilizing agent.

Attempts to run liquid limit tests on the soil according to ASTM

test n;.ethods after lime had been added were unsuccesstul. This can be

attributed to tbe capacity or lirne to rapidly dry out a clay soil. Hilt

and Davidson (10) have reported some degree of success in running limits

after the lim~ soil, and water mixture had been seasoned. tor two days in

a curing room. '!his procedure allowed the water to infiltrate the clay-

particles thoroughly and produce uniform wetting of the sample. Since

prelindn~y tests run by Hilt and Davidson after different storage periods

up to four days showed no perceptible daily change in the liquid and

plastic limits after two days storage, it was decided for the purposes ot

this thesis to ru.n all Atterberg limit teets after a two-day curing period..

24

With the exception of the two-day curing period., plastic limit tests

were run in accordance with AS'l'M D424-54T, "Plastic Limit and Plasticity

Index of Soils." Liquid llmit tests were run in accordance with .ASTM

D423-54T, "Liquid Limit of Soils, .. with the additional moditiea.tion that

the Casagrande grooving tool was used.

25

V. R&SULTS

A. Fr,elimiparz Laboratol"'l,l Test1A£; Results

Prior to ti:e unconfined compression testing, two other series or tests were run. Atterberg lint test results are suramarized in Table l

and reported graphically in Figures land 2. '!hese figures and table

TABLE l

ATTERBERG LIMITS-VARIOUS PERCENTAGES OF CJMENT AND LIME

ilme-Cement Liquid iliiiit Plastic Lim!t Plasticity Index Per Cent (LL) (PL) (PI)

0-0 67 37 30 0-5 66 39 27

0-10 75 47 28

5-0 64 41 23 10...0 68 4S 23

2 ... 3 63 42 2l

3-2 62 43 19

4-6 78 49 29

6-4 70 49 2l

illustrate the changes which took place in the plasticity index, as well

a.s the liquid (Lt) and plastic (PL) li.'nits• with changes in the type and

percentage of stabilizing agent added to the soil, In Figures la and lb,

the e!'fectfl of adding; and 10 per cent lime and cement separately to the

soil are shown. Similarly, significant changes which occurred in the

limits once ceno..ent-lime combinations had been added to the soil are

t fo,-------------------------. 1-" ~H i -~.,... p.r..,z;s.

L~ '1'.

.PI-.3e> J ,, 1 ~.i "' .h

35"--------------0 -5

1,,;,,e ( pt!,,. c,z,,f by tl,.7 w,!fl.-1)

t ?7

./'.I-1.8

,P.I-2.1 ,'.C-30

:JS---------------------__. 0 J /D

C4.,,,e~l(,1:n11• c:.e,,f 1,7 a-1,..1 iuqj/,1) , .,..

F;j. / £1./"~c../-o( /4',,,e.-- 0'1d CfZ~Q.,,/ -Jo// ;,, .,j /uJ..e.s on ,4/--h .. 1--/.u .. 7 J,;,.;./s

26a

t ?or--------------------=1--, I.J.-6'1 - '/4'

i,1 t ""S"• t ~I-3o

'3 H

.,.,.

PI-:u

l . ho..,,

2.-.a Ct1m,v,f-L;,,,,. ( pa; c&Af /Jy tl1-y w•iAf)

'1

t 70

u.-.1 ;-,J

'I-..

!s-• '1

'3 ,l'J-3d7

ct H ½

.3S' (,)-.::>

l'I-~1

;PI-2/

L-.3-2 a.-1-

Cen,t1M1"- L/;,,e. { p•r t:.J£11/ b)" q';.y wtaj,if)

E.f".fec.l of So// hJ/Jt.lwJ--~s on /-ll-ls;,Je.7 /,;,,,.,ifs

I 'lo

'S B;f' \)

\. . \\

v 8t:J

..... ""'

'1 t-'1 1.r +

J. 'l

a s h,,-,d',," a' ? 1--oc. for + :5A:::,nc/4,-tl ~A/q,fu;,~

+-

3/

.5,lqnd<7rd hoc../o,.,, t7/Jd .J7'-qn/4;,-d )1/l'J/4fu;.-~ compc:,c.hon cu,-,J/e.~

28

brought out 1n ftgures 2& and 2b. 'I.be second eeries ot.teata vaa an

attempt to correlate result.a obtained by using a Harvard Miniature Com-

paction apparatus with Standard AASHO dry density and moisture content

tor one particular clay soil. Figure 3 illustrate• the aueceu ot this

correlation. It may be seen that maximum densities varied by not more

than 0.5 pounds per cubic foot, while optimum moisture content (OMC)

remained at 32.4 per cent in both cases. This correlation ot the minia-

ture compaction device was obtained with a 40-pound spring-plunger

assembly. 'J.wenty-five blows of the plunger were applied to three equal

layers of soil.

B. Major Laboratoq Test!Pg Result9

The greatest portion ot the laboratory testing was concentrated on

the unconfined compression of miniature compaction specimens. For the

sake of clarity, a description of the graphical. result, presented in

Figures 4-ll will be di'Yided into two parts. '!he first part will be con-

cerned with ftgurea 4-7, which show strength curves for uncured specimens

which were tailed imudiately atter compaction. For each ot the four

figures, uncon.tined compresaiw strengths for different moisture contents

are plotted against additive percentages. In Figure 4, lime waa uaed u the additive, while 1n Figure 5., cement was used. In Figures 6 and 7,

strengths were plotted against cement-lime combinations. Detore these

plots could be made, however, moisture-atrength curves had to first be

drawn tor each additive percentage. Following this, three or tour water

contents which were within three per cent ot OMC were se.lected and the

corresponding strengths read ott the graph. Wi tn additive percenta.aea,

water contents, and strengths known, Figures 4-7 could be plotted.

»Od',----------------------,

/0

C o/np,G-fe.d' sl;-•h:,l/,-h?o/Slvre-t~e.-1-'e./,,h~n:1 A ii"~

30

9-z~~·----------------------,

.z.,ooo

.s-- /0 C11~ / ( ,PIJr Clllh/)

F_j. S' Compa?fe./ .5/;,e~,U -;770/j/-vH!--C8/#le.hf r4i/q//cn J/p.f

31

+

t,8)-- a

+(.Jf}

~•'701-------------L----------1-~ P-0 2-.3

C ftlAlll"7 /- -L /Me. { p eJ.- all I)

C on1pa(.,.fe. a" s /-;,s,yll,- n,o/f f u~ -{ceMe11l-/;;.,,e J ;.-,~ /q./,/ons/11,i?.s

3Z

t

• ~8)-a---

--------A-~~------

)1-{fo)------,c

/,IDO .___ ________ -L-------------'----' (!)-(?

Fj. 7

.s-Z Ceme11/--Liwe.(pq c.tY1I)

•-+

C om_po-c. le c/ r I-1-e,~f J. - ,,?'JO/S' lff 1-~ -{t.t!A1611l-hm ~) Alps

Figu.res 8-11 show strength cunes tor cured specimens which were

tailed atter a tour-day euring period in a 100 per cent humi.dit7 curing

room. In F.1.gure s, lime was used as the additive, while in Figure 91

cement was used. In Figures' 10 and ll~ strengths were plotted against.

cem.ent-llme combinations~ 'lb• procedure used tor determining water con-

tents and corresponding etrengtha to plot Figures 4-7 was also used for,

plotting Piguree 8-ll. Numbers in parentheses refer to water contents.

c. Statiftical Analzaia

A three-way- statistical analysis ot variance was performed on

Tarious aspects ot the unconfined compressive strength data. The three

variables upon which the analJ,sis is based included moisture condition

(A), test condition (B), and additive percentage (C). Moisture condition

refers to molded water content with relation to moisture-density curves

plotted for each additive percentage. Since specimens were compacted

at OMC, as well as on the "dry'" and "wet" aidea of the optimum moisture

content, three moisture condition• were used. Test conditions were tw

1n number-cured and uncured. Details ot the method ot a.nalyais used

and the proc.dures followed are outlined 1n Duncan ,is). In Tables 2 and 4, S1lDIU..riee ot strengths for specimens containing

lime and cenent only are presented. '!he s1gn11'1cance 0£ the three n.ria-

bles was detendned by va.l"iance ratios or "F" tests at 0.01 and o.00.l levels, and the results of the "f" tests for Tables 2 and 4 appear in

Tables 3 ands. SUl21!1B.ries ot strengths for specimens containing addi-

tives at the 5 and 10 per cent level.a, both separatelY' and in combination,

appear in Tables 6 and 8, while corresponding variance an~a are

34

described in Tables 7 and 9. The last swran.ary o.f strengths presented

in Table 10 is or.e of two additive combinations at the 10 per cent

level. The ma.in purpose of this study was to determine the ettect ot

varying the ce..-uent-lime :percentage ratio from 4-6 to 6-4. The var.lance

analysis for this phase of the study may be found in Table ll.

6606----------------------, I

/(:MJO,__ __ ---''---------'-------------~ 0 .5 /d

L,.,1",,,,,e (pa;,, c.-.,,r)

C u1-e.. al s l-1-e.~./l. - ,n,,o/s .Jw,-.e. - bme-re.lQ hon .:Ji /ps

36

+

~#DO,___ ________ _,_ _________ -'--~

0

Fij. 9

.:r C11mu f (pfrl' cc,, f.)

Cu;-e.d_ :J" f;--e.":J/l.-n-,o/.fJ~;-e... -c:e..me.nf-/-"t!-/4/-/on :5 ii,r;s

/'fl~---------------------;

tN>~·.__ ________ ...a_ ________ ...L-___,I

0-0 ~-B c....,_,,/-,t.,-;,,, .. {per- CIJ'II)

Fj. /t7 C ~,-e. ~. s l-1-~IA -/ho/:S-./-'-'1--.e.. -{~en1e~f-b me-j ;.,e, /4 I-/ on s A, j:,.:f

38

J,.OODr------,

Fj,. II

3-,2, Ca/1"/1V1/--L1;,,c. ~" c.a;,f)

C"!1-e..t/ :5/-1-e~IA -~01.:rlwJ,e--{c.e.;ne.nl-~n,e) 1-elof /on.:J'/,117s

TABLE 2

SUMMARY OF SPECIMEN S'fflENGfflS (O, 5• AND 10 PER CENT LIME ADDITIVE)

Une Une Cured Tota. s

0-0 3.255 1.150 2.480 1.045 1.415 1.200 3.345 1.815 2.480 2.910 1.760 l.,380 37.065 3.145 1.345 2.330 2.590 2.010 1.330

Lime-Cement 5-0 2.925 le'845 2.890 3.720 2.108 1.445 Percentages 2.430 1.345 3.205 3.010 2.045 1.745 42.928

2.92; 1.030 3.290 3.525 1.880 l.565

10-0 2.580 2.910 1.775 5.36; 1.960 4.020 2.870 2.360 1.940 5.560 1.880 3.870 56.780 2.990 2.460 2.10; 4.880 2.17; ;.oao

Totals 26.465 16.260 22.495 .32.605 17.233 21.715 136.773 42.725 55.100 38.948

40

TABLE 3

'l'HRE.E-WAY ANALYSIS OF VARIANCE RESULTS FOR S'lRENaffl DATA (O, 5, AHD 10 FER CENT LIME ADDITIVE)

Source of Variance F F .Ol F .OOl 51.gniricance

Moisture Condition., A 30.46 5.39 8.77 .001 leftl.

OUring, B 2.77 7.56 13.29 NS

Lime Percentage, C 43.s; 5 • .39 s.77 .001 l.evel

Interactions: AxB 47.00 5.39 8.77 .001 level

AxC s.54 4.02 6.12 .001 level

BxO 70.77 5.39 s.77 .001 level

Ax'BXC 4.15 4.02 6.12 .Ol level

TABLE 4

SUMMARY OF SFECD@l" STREl'WTHS (O, 511 AND 10 PER CENT CEMENT ADDITIVE)

Unconfined Compressive Strength, 111000 lbs. per sq. tt. ti.mum Wet

Uncured C Uncured Cured 'lbtals

0-0 3.255 1.150 2.480 1.045 1.415 1.280 3.345 1.815 2.480 2.910 1.760 1.)80 :37.065 3.145 1.345 2.330 2.590 2.010 1.330

Li.me-Cement 0-5 2.430 1.345 2.J+J..0 2.s90 2.12; 2.530 Percentages 2.540 1 • .362 2.025 3.590 2.210 3.425 42.318

2.430 1.353 2.375 2.975 2.168 2.105

0-10 3.125 10.130 2.uo 9.880 1.sso 10.010 2.83() ll.080 2.990 10.0.30 2.245 10.010 ll6.0SO .3.030 11.220 3.270 9.955 2.275 10.010

Tota.ls 26.1,30 40.800 22.;oo 45.865 18.088 42.oso 195.l;63 66.9,30 68.365 6o.l68

42

TABLE 5

THREE-WAY ANALYSIS OF VARIANCE RESULTS FOR STRENGTH DATA (O, 5, AND 10 PER CENT CEMENT ADDITIVE)

Source of Variance F F .Ol F .ool Significance

Moisture Condition., A 7.19 5.39 8.77 .ol level

Curing, B 48.20 7.56 13.29 .001 level

Cement Percentage, C 73.25 5/39 s.77 .001 level

Interactions: AxB 1.02 5.39 8.77 NS

AxC 0.77 4.02 6.12 NS

:axe 65.25 5/}9 s.77 .001 level

AxBxC o.;1 4.02 6.12 NS

TABLE 6

SUMMARY OF SPECIMEN STRENGTHS (5-0., 0-5., 3-2., AND 2-3 PER Cl!.1-IT LIME-CE."UT ADDITIVE)

Unconfinm.Compressive Strength, 1.,000 lbs._ per sq._ ft •. Moisture Condition thmm Wet Test Con · tion Curi Uncured Cured Uncured Cured Uncured Cure s

5-0 2.925 1.845 2.890 3.720 2.108 1.445 2.430 1 • .345 .3.205 3.010 2.045 1.745 42.928 2.925 1.030 3.290 .3.525 1.880 1.565

0-5 2.430 1.345 2.440 2.890 2.125 2.5.30 2.540 1.362 2.025 3,.590 2 .. 210 3.425 42.317 2.430 1.353 2.375 2.975 2.167 2.105 e;

Lime-Cement 3-2 3.090 1.645 1.695 2.090 1.960 5.070 Percentages .'.3.105 1.890 l.890 2.560 1.695 4.470 45.907

2.510 2.090 1.990 1.514 l.82J 4.820

2-3 2.810 2.840 2.225 2.520 1.462 2.060 2.960 2.645 1.975 2.450 1.595 2.160 41.955 2.845 2.743 2.uo 2 • .3.30 1.500 2.345

Totals 33.000 22.133 28.410 33.174 22.650 33.740 173.107 55.1.33 61.584 56.390

TABLE 7

'IHREE-\'IAY Ai'l'ALYSIS OF VARIANCE RESULTS FOR S'lRENGTH DATA (5-0., 0-5., 3-2, and 2-3 PER CENT LIME-CulENT ADDITIVE)

Source of Variance F F .01 F .001 Significance

Moisture Condition, A 6.53 4.9s 7.76 .Ol level

Curing, B 4.61 7.08 ll.97 NS

Lime-Ceaent Percentage, C 2.40 4.13 6.17 NS

Interactions: AxB 71.00 4.98 7.76 .001 level

AxC 37.30 3.12 4.37 .001 level

BxC 14.87 4.13 6.17 .001 level

AxBxC 17.15 :3.12 .001 level

TABLE 8

SUMMARY OF SPECIMEN STRENGTHS (10-0• 0-10• 6-4• AND 4-6 PER CEHT LIME-CEtmlT ADDITIVE)

Unconfined Compressive Strength, 1,ooo lbe. per sq • .rt. Y.10isture Condition D timum Test Con tion Cur ncured Unc

10-0 2.500 2.910 1.775 5 • .365 1~960 4.020 2.870 2.360 1.940 5.;6o 1~880 3.870 56.780 2.990 2.460 2.105 4.880 2.175 ,.oso

0-lO .3.125 10.130 2.llO 9.880 1.880 lOtPlO 2.830 ll.080 2.990 10.030 2.24; 10 .. 010 JJ.6.080 3.030 u.220 J.270 9.955 2.27; 10.010 t;

Lime-Cement 6-4 3.070 5.140 1.74; 8.8.30 1.565 7.570 Percentages 3.250 4.710 2.10; 9.210 l.815 10.uo 89.805

3.160 4.470 2.310 9.980 1.925 8.840

4-6 2.740 5.570 2.020 8.080 l.763 7.225 .3.040 6.970 1.680 9.J.1:,0 1.776 9.570 91.949 3.270 6.270 2.020 s.730 1.665 10.100

Totals 35.955 73.290 26.C170 99.96o 22.924 96.415 354.614 109.245 l26.030 ll9.J39

TABLE 9

'lHRD-WAY ANALYSIS OF VARIANCE RESULTS FOR S'l'.RENG'!H DATA (10-0, 0-10 1 6-4, AND 4-6 PER CENT LIME-CEJIENT ADDITIVE)

Source of Variance F F .Ol F .001 Sigrd.ticance

Moisture Condition, A 9.98 4.9s 7.76 .001 level

curing, B 1590.00 7.08 u.97 .001 leftl

Lime-Cement Percentage, C U0.60 4.13 6.17 .001 leftl.

Interactions: AxB 61.60 4.9s 7.76 .001 level

AxC .5.S6 3.12 4.37 .001 level

BxC 89.10 4.13 6.17 .001 level

AxBxC 10.82 3.12 4.,1 .001 level

TABLE 10

SUMMARY OF Sl'.ECIMEN S'l''RENGTHS (6-4 A.I\JD 4-6 PER CENT LIME-CEMENT ADDITIVE)

Unconfined Compressive Strength, 1,000 lbs. per sq. tt. Moisture Condition timwn Wet Test Co tion CUri Uncure Cured Uncured CUred To 8

6-4 .3.070 5.140 1.745 8.$30 1.565 · 7.570 .3.250 4.710 2.105 9.210 1.815 10.llO 89.805 !i 3.160 4.470 2.310 9.980 1.925 8.84()

Lime-cement 4-6 2.740 5.570 2.020 8.080 1.763 7.225 Percentages 3.040 6.970 l.680 9.460 1.776 9.570 91.949

3.270 6.270 2.020 s.730 l.66; 10.100

Totals 18.530 3.3.130 ll.880 54.290 10.509 53.415 181.754 51.660 66.170 63.924

48

TABLE ll

'IF.REE-WAY ANALYSIS OF VARIANCE RESULTS FOR STRENGTH DATA (6-4 AND 4-6 PER CI!:NT I.DIE-CEMENT ADDITIVE)

Source of Variance F F .Ol F .OOl Significance

Moisture Condition, A 10.S6 5.61 9.34 .001 level

Curing, B ;91.-00 7.82 14.00 .001 level

Lime-Cement Fercentage, C 0.27 7.82 ll+.00 t.!S

Interactions: AxB 46.70 5.61 9.34 .001 level

AxC 1.76 5.61 9.34 NS

BxC 0.99 7.s2 14.00 NS

AxBxC 1.s., 5.61 9.34 NS

49

VI. DISCUSSION AND CONCLUSIONS

1be results presented in the previous section will be reviewed and

discussed in the order in which they appeared. All results will be

enlarged upon through discussion, and, when possible, conclusions con-

cerning the significance of results will be presented. 'lhe statistical

analysis emphasized the more important points; hence, the majority of

the discussion will be concentrated on the £actors brought out in Tables

2-ll.

A. Atterberg Limits (Figures 2-3) All Atterberg limit specimens were cured for two days in a 100 per

cent humidity curing room prior to testing. Since previous research by

Filt and Davidson (10) subst;:ntiated the practicability of this procedure

in running limits on lime-soil mixtures, 1 t was followed by the author

after difficulty was encountered in running liquid limit tests on lime-

soil mixtures. The difficulty can be attributed to the ability ot lime

to dry out a soil immediately efter it has been added.

In order to use similar test procedures for all specimens, cement-

soil and cement-lime-soil mixtures were also cured in the same manner.

For all conditions, the plastic limit increased with increasing

additiTe percentages. '.l'tlis result is in agreement with the literature

for both lime (19) and cement (20) stabilization. However, for soils

with plasticity indexes greatet' than 15, lime and cement both will nor-

mall.y reduce the liquid limit (1)(20). This result was not achieved in

any of the tests, including those in which only lime was used. In the

;o

case ot lime however, the liquid limit only increased from 64 at 5 per

cent additive to 68 at 10 per cent additive. In all other studies the

increase in liquid limit wns more pronounced between the 5 and 10 per

cent levels, with the greatest increases occurring in the 10 per cent

cement specimen and the one containing the 6 per cent cement-4 per cent

lime combination. Since the greatest liquid limit increases at the 10

per cent additive level occurred in the samples containing the greater

percentages of cement, it may be concluded that the two-day curing period

which all specimens containing cement received was a major factor in the

erratic results obtained. A further error Fossibility is th~it hardening

had set up in these two mixtures after one day of curing; each had to be

re-worked with a spatula and the moisture content increased.

One interesting point was noticed concerning the relationship o! the

optimum moisture content to the plastic limit tor ea.ch mix. In the case

of the raw soil, its OMC exceeded the plastic limit. For additive-soil

mixtures, however, plastic limits either equalled or exc!,3eded all opti-

mum moisture contents.

B. Uncured Compressive Stre9B1hs ( F'ieu:res 4-7) Both the tr~ and amount of chemical additive in a specimen have an

immediate effect on compacted strength. This is evident in Figures 4-7.

In all cases except one, the greatest uncured strengths were obtained at

the lower water contents below OMC. The one exception was in the group

of samples containing 5 per cent lime, where the maximum strength was

achieved at OMC. This is brought out in Figure 4. In Figures 5-7, the

curves show similar trends. The lower moisture contents produced the

51

highest strengths, which decreased progressively with each moisture

increase. With regard to the four additive percentage studies (lime,

cement, and two lime-cement combinations), no definite trend was estab-

lished as to the additive percentage at which the greatest strengths

were obtained. When no curing is involved, it appears that moisture

content is extremely significant in determining the additive percent-

age at which the greatest strengths will occur.

c. Four-Day Cured Compressive ~>trengths (Figures 8-11)

Fieu.res 8-11 point out a number of interesting factors. For the

cured specimens containing nc stabilizing agent, the greatest strengths

corres;ponded to molded water contents below OMC. In those instances

where additives were used, however, highest strengths were obt,ained at

and al:.."Ove 0..'4C., with two exceptions. One exception occurred at the (3-2)

cement-lime percentage in Figure ll. At this percentage, only a small

variance in strengths exists though, and the difference in the trend may

be ignored. The other exception was at the 10 per cent cement level in

Figure 9. The reason for this will be explained later in the discussion

of the statistical. analysis presented in Tables 4 and 5.

The effects of curing and additive percentage on strengthe ma;r also

be seen in Fii'1lres S-ll. Little or no strength increases were noted at

any of the 5 per cent additive levels. The 10 per cent levels did pro-

duce notable gains however. 'lhe largest increases occurred in the

cement-stabilized samples; the smallest in those samples containing lime.

The combination-additive strength increases were inteimediate between

these two.

S2

D. Statistical An!ll:ae• (Tables 2-112

Fift indi'Vidual statistical analysea were run on the strength data

obtained in the laboratory. Two of the studies were concerned with

strengths when cement and lime were used individuall.y' as additives; two

others dealt with lime. cement, and lime-cement additives at the 5 and

10 per cent levels. 'lbe fifth study was of the tw lime-cement combi-

nations at the 10 per cent level of stabilization.

1, Lime percentages ot o, 5, and 10 (Tables 2 and .3), '!bis analy-

sis showed that the test condition (curing) of specimens, when

considered separatel7, was not significant (NS), 1,e., was not

attecting the strength data, However, judgement tells ua to

consider curing as significant when we note that there was a

very signiticant interaction between moisture and curing, Obser-

vation of the data shows that curing had no ettect at the lower

moisture contents only, Furt.her analysis shows moisture condition

and lime percentage both to be significant to the 0,001 level.

With 0.001 levels ot significance, it may be stated, with only

one chance in a thousand of being wrong, that both moisture

condition and lime percentage attected the strength data.

'lb• interaction ot AxC (moisture and per cent lime) was

also significant at the 0.001 level. The significance ot this

interaction supports the data which show that higher moiature

contents produce higher strengths only with larger amounts of

lime. The BxC interaction ( curing and per cent liae) yielded

a 0.001 level ot significance because of the tact that curing

53

was effective only after lime had been added to the samples.

Curing did nothing for samples containing O per cent lime.

2. Cement percentages of o, 5, and 10 (Tables 4 and 5). Of the

three variables, cement percentage (C) and curing (D) were the

most significant, each to the 0.001 level. The interaction of

these two, BxC, was likewise significant to the 0.001 level,

since curing made no difference at O per cent, but ma.de a great

deal of difference at 10 per cent cement. Moisture condition

(A) did not exert as much influence on the strength data as did

Band c, since it only had a 0.01 level of significance. This

is in direct contrast to the 0.001 level of aignitieance that

moisture condition had in the lime-soil analysis. It should

be pointed out here that curing was very significant when used

with cement-soil specimens, even at the lower moisture contents.

Curing was not nearly as important at the lower moisture con-

tents in the lime-soil specimens.

3. Lime-cement percentages of 5-0, 0-5, 3-2, and 2-.3 (Tables 6 and 7). Only one individual variable, moisture, had any sig-

nificance (O.Ol level). Again, as was the case in the lime-soil

study, test condition (curing) was not significant. A glance

at the data indicates that this might be because of lower cured

strengths than uncured strengths on the dry side tor each addi-

tive percentage. The interaction AxB (moisture and curing) thus

is found to be significant. Most important, the analysis shows

no significant differences in strength at the different lime-cement

;4

eom.binations. There.fore, at the 5 pe:r cent additive level, it

can be said that these tests indicate that similar results will

be obtained whether 5 per cent lime, 5 per cent cement, or a

combination of the two is used. That no great strength increases

were obtained at any of the 5 per cent levels is the probable

reason that no individual variable had outstanding significance.

4. Lime-cement percentages of 10-0, 0-10, 6-4, and 4-6 (Tables 8

and 9). The most important result of this study is that the

analysis showed ea.ch of the three variables to be significant

at least to the 0.001 level. i~1ile all three were significant,

it should be emphasized that curing was especially significant

because of its high ttF11 value. It can therefore be concluded

that moisture, curing, and lime-cement percentage all have a

pronounced effect on sample strengths. Observation of the data

would lead one to believe that cement was more effective in

raising strengths than lime. This difference was not apparent

at the 5 per cent additive percentage study.

5. Lime-cement percentages of 6-4 and 4-6 ( Tables 10 and ll) • 'Ihl.s

analysis was made primarily to determine if a variation of the

lime-cement percentage from 6-4 to 4-6 made any difference in

strengths of cured specimens. Table 11 supports the statement

that only moisture condition, test condition, and the interac-

tion between these two were significant. All other factors were

NS. 'Ihus tbe question of strength differences with the percent-

age variation of the addi.ti ves is answered. The lime-cement

;;

percentage change from 6-4 to 4-6 had no significant effect on

strengths after a four-da.y curing period.

E. Conclusions

'lhrou.ghout the discussion just presented, a number of conclusions

were either stated or implied. At this point, all conclusions which can

be made from. this laboratory study will be summarized.

1. The plastic limit of a soil can be increased with either a

cement, li..'1le, or cement-lime additive. 'l'his increase will con-

tinue with t.he a.ddi tion of more additive, at least within the

additive percentage range used.

2. Curing of lime-soil mixtures for a two-day period prior to

Atterberg li:nit testing is a satisfactory method of prepara.-

ti.on. This curing period is needed in order to _permit the

water to infiltrate the clay particles thoroughly and produce

uniform wettinG of the sample.

3. Curing .for two days as was done for the lime-soil mixes is an

unsatisfactory r.,ethod of preparation of samples containing

cement when Atterberg limit testing is to be done.

4. Standard AASHO maximum dry density and optimum moisture content

c1c.n be obt;:;.i.ned with the Harvard Miniature Compaction equipment..

Twenty-five blows of the 40-i:,ound. S}'.Jring-plun,ger asse111bly applied

to three equal soil layers in the Harvard Miniature Compaction

mold will yield an eq_uivalant maximum dry density and OMC.

5. Modified AASHO maximum dry density and OMC cannot be obtained

wlth the Harvard ¥J.niature Compaction apparatus.

S6

6. '!he type and amount or additive used will have some effect on

strength even if samples are failed immediately after compaction.

7. For cured specin1ens containing a stabilizing agent, the greatest

tour-day strengths will occur at or above OMC, in most eases.

'Ihis may not always be true in the case or cement, since moisture

condition is not as si,snificant in c~~ent stabilization as it

is in other types.

8. Control of moisture at or near OMC during field compaction

appears to be much more important in lime stabilization than

in cement stabilization if maximum strengths are to deYelop.

9. '!he variation of tbe lime-cement percenta2,--e from 6-4 to 4-6 has

no effect on tour-day cured strengths.

10. Curing had the greatest effect at the highest additive percent-

ages., since greater strengths were obtained at the higher additiw

percentages.

57

VII. RECOMMENDATIONS

Further research with lime-cement combinations as additives to

highly plastic clays is warranted, since lime will greatly improve worka-

bility and the two together will yield significant strength gains. This

type of stabilization may be particularly adaptable in northern climates

where lime stabilization has to be used with caution. This caution has

to be exercised since lime sets much more slowly than cement over a much

longer period of time. If a "hard" frost should occur only two or three

weeks after a job is completed, se1·ious damage of a perm.anent nature

could be inflicted to a lime-stabilized soil.

One last recommendation is for further study of the molded water

content-greatest cured strength relationship for all three types of

stabilization-lime, cement, and lime-cement.

58

VIII. ACKNOWLEDGEMENTS

'!he author would like to express his appreciation to Dr. Richard D.

Walker, his advisor in the Civil Engineering Department., for the guidance

he gave during the laboratory testing and the preJ,oaration of this thesis.

Without his help and valuable comments, the statistical analysis pre-

sented in Section V and discussed in Section VI would not have been

possible.

A special note of thanks is also due Dr, Robert D. Krebs, who,

tr-irough his class lectures, presented a major portion of the materiaJ.

which gave the author a minor in soil meahQ,nics.

59

IX. BIBLIOGRAPHY

. l. Yoder, E. J., Principles £! Pe.:vement Desiff Chapter 10,, nsoil Stabilization." 255-268, Wiley and Sons 959).

2. Catton, M. n., "Early Soil-Ce,nent Research and P,evolopment. 11 re A. Bulletin D42:3-18 {January 195.9).

3. Catton, M. D., "Soil-Cement Mixtures for Roads.11 HRB Proc., 18:Part II, 314-21 {1938).

4. Davidson, D. T., Ooil Stabilization with Portland Cement, "Forwa.rcl.11

HRB Bulletin 292 ~,. -

5. Highway Research Board, Soil Stabilization with Portland Cement, "lntroduction.tt HRB Bulrnn 292 (f96t~. -

. 6. American Road Builders Association, "Soil-Cement Stabilization Com-mittee Report." ARBA Technical Bulletin No. 191:7-10 (1953).

7. National Lime Association, Lime Stabilization of Roads, Chapter l, "Background of Lime Stabilization." National iline Association Bulle-tin 323:7-ll (1954).

8. National Lime Association, Lime Stabilization Pamphlet, 925 Fitteenth Street, N.W., Washington 5, D. c.

9. Davidson, D. T., and Handy, R. L., Highway ftf1neeri1': Handbook, Chapter 21, "Soil Stabilization." McGraw-Hi! {19~.

10. Hilt, G. H., and Davidson, D. T., "Linle Fixation in Clayey Soils." HRB Bulletin 262:20-24 {January, 1960).

ll.

12.

Grimm, R. E., Clay Mineralogy. McGraw-Hill {195.'.3).

National Lime Asaoeiation, Lime Stabilization of Roads, Chapter;, "Evaluation of Lime-Soil Mixes." National flm.eAssoclation Bulletin 323:21-30 {1954).

Puller, M. G., and Dabney,, G. w., 11Stabilizing Weak and Defective Bases with Hydrated Lime." Roads and Streets, 95:64-69 (March, 1952).

14. Jan, M.A., "Lime Stabilization ot a Virginia Clay Soil," Master of Science Thesis, Virginia Polytechnic Institute, Department or Cinl Engineering (1962).

15. Hennes, R. G., and Ekse, M. I., Fundamentals or Transportation Jm&!-neering, Chapter 21 "Grading the Roadbed." 2-:C.27, McGraw-Hill {IB5).

60

16. Clare, K. E., and Pollard, A. E., 11'1he Relationship Between Com-pressive Strength and Age for Soils Stabilized with Four Types of Cement.11 Magazine of Concrete Research {London), .3:8, 57-64 (December, 1951).

17. Wilson, Stanley D., "Comparative Investigation of a Miniature Com-paction Test with Field Compaction," presented before the Annual Meeting, American Society of Civil F,ngineers (January, 1950).

18. Duncan, A. J., ~tr Control and Industrial Statistics, Richard D. Irwin, Inc., omewood, Iffino1s(i9;9).

19. American Road Builders Association, Lime Stabilization Construction Manual, ''Introduction." ARBA Technical :Biiftetin 243:5-b (197,!i}.

20. Highway Research Board, Soil Stabilizat,ion with Portland Cement, Properties of Cement-Treated Soif. 11 HRB Bu!ietin 292:i2-1J (!961).

ADDITIONAL REFERENCE

l. ttAS'.IM Standards-1958, 0 American Society for Testing Materials.

The vita has been removed from the scanned document

ABSTRACT

LIME, CEMEtIT, AND LIME-CEMENT STABILIZATION OF A CLAY SOIL

The main purpose behind this thesis was to study the variations of

strength in a soil after it had been stabilized with various percentages

of lime, cement, and combinations of the two. In both cases where the

additives were added separately to the soil, the percentages used were

5 and 10 per cent by dry weight of soil. In the additive combination

study, lime-cement percentage additions were 2-3, 3-2, 4-6, and 6-4 by

dry weight of soil. The first two percentages, when added together,

amount to 5 per cent stabilizing agent, while the latter two total 10

per cent. Since these two totals were the sa.T.e a.s those used in the

separate lime and cement studies, an analysis ot strength changes when

lime, cement, and lime-cement combinations were added to the soil could

be made. Strength studies which were 1:1ade consisted of unconfined com-

pression immediately a!ter compaction and after a four-day curing period

in a 100 per cent humidity curing room. Atterberg limit tests were also

run at the various percentages of additive.

'lbe laboratory test results indicate:

1. For cured specimens containing a stabilizing agent, the greatest

four-day strengths will occur at or above OMC., in most cases. This may

not always be true in the case of cement, since moisture condition is

not as significant in caent stabilization as it is in other types.

2. Control of moisture at or near OMC during field compaction

appears to be much more important in lime stabilization than in cement

stabilization if maximum strengths are to develop. '!hie statement is

supported by a. statistical analysis which was performed on the strength

data.

3. The variation of' the lime-cement percentage trom 6-4 to 4....6 has

no effect on four-day cured strengths.