The Florida Institute of Phosphate Research was created in 1978 by the Florida Legislature(Chapter 878.101, Florida Statutes) and empowered to conduct research supportive to theresponsible development of the state’s phosphate resources. The Institute has targeted areasof research responsibility. These are: reclamation alternatives in mining and processing,including wetlands reclamation, phosphogypsum storage areas and phosphatic clay contain-ment areas; methods for more efficient, economical and environmentally balanced phosphaterecovery and processing; disposal and utilization of phosphatic clay; and environmentaleffects involving the health and welfare of the people, including those effects related to radia-tion and water consumption.
FIPR is located in Polk County, in the heart of the central Florida phosphate district. TheInstitute seeks to serve as an information center on phosphate-related topics and welcomesinformation requests made in person, by mail, or by telephone.
Executive DirectorRichard F. McFarlin
Research Directors
G. Michael Lloyd Jr.Gordon D. NifongDavid J. RobertsonHassan El-ShallRobert S. Akins
Research Staff
-Chemical Processing-Environmental Services-Reclamation-Beneficiation-Mining
Florida Institute of Phosphate Research1855 West Main StreetBartow, Florida 33830(863) 534-7160
RECLAMATION OF PHOSPHATIC CLAY WASTE PONDS BY CAPPING
VOLUME 2: CENTRIFUGAL MODELING OF THE CONSOLIDATION BEHAVIOR OFPHOSPHATIC CLAY MIXED WITH LIME OR GYPSUM
Research Project: FIPR 82-02-030
Prepared by:
Department of Civil Engineering IMC, Bartow, FloridaUniversity of Florida Agrico, Mulberry, FloridaGainesville, Florida 32611 Mobil, Nichols, Florida
Principal Investigators:
T. E. SelfridgeF. C. TownsendD. Bloomquist
Prepared for
FLORIDA INSTITUTE OF PHOSPHATE RESEARCH1855 West Main StreetBartow, Florida 33830
FIPR Project Manager: Dr. Henry L. Barwood
September, 1986
DISCLAIMER
The contents of this report are reproduced herein as receivedfrom the contractor.
The opinions, findings and conclusions expressed herein are notnecessarily those of the Florida Institute of Phosphate Research,nor does mention of company names or products constitute endorse-ment by the Florida Institute of Phosphate Research.
ii
ACKNOWLEDGMENTS
The support and sponsorship provided by the Florida Institute of
Phosphate Research for this investigation is acknowledged. The
cooperation and assistance for this project is acknowledged for:
Dr. J. E. Lawver, Inc.
Mr. Steve I. Olson, Agrico
Mr. H. H. Miller, Agrico
Mr. A. J. Propp, Mobil
This report reflects the MS thesis of Mr. Thomas E. Selfridge,
Department of Civil Engineering, University of Florida, Gainesville,
Florida, 32611. Dr. J. L. Davidson served as a committee member of this
thesis.
V
viii
ix
Reclamation of Phosphatic Clay Waste Ponds by Capping
Volume 2: Centrifugal Modeling of the Consolidation Behaviorof Phosophatic Clay Mixed With Lime or Gypsum
Research Project: FIPR 82-02-030
ABSTRACT
The phosphate mining industry is actively seeking methods to
improve the consolidation characteristics of waste clays created during
the beneficiation process in hopes of reclaiming the large amounts of
land currently used for waste clay impoundment.
This research investigates the use of lime and gypsum as additives
which might enhance the consolidation of the waste clays. The research
was divided into two stages. In the first stage, experimental tech-
niques were used to determine the appropriate quantities of lime and
gypsum to be added to the waste clays and assess the strength gains due
to these additives. The second stage involved centrifuge modeling of
the consolidation of the waste clays with the determined quantities of
lime and gypsum added.
The results of this investigation reveal that the pH test pro-
vides a rapid method for determining the minimum lime content
required for strength producing clay-lime reactions. Lime percen-
tages of approximately 12% were required to achieve the pH percentage
for the clays tested. Miniature vane shear tests showed 28-day
strength gains of 3 to 5 times that of untreated clay when 12% lime
was added while relatively small strength increases occurred for
lower lime contents. Unfortunately, the high concentrations of lime
required, and the relatively low 28-day strengths (14 to 25 psf)
x
question the feasibility of lime treatment from the standpoints of
economics or surface strength to support equipment. However, sufficient
strength to support a sand cap might be feasible, but caution is
advised. In the case of gypsum, the pH test was unsuitable for
determining the target gypsum content. Gypsum/clay ratios as high as
12:1 produced practically no strength improvement.
Centrifugal model tests revealed that addition of lime hindered the
consolidation magnitude of the clays. Apparently the lime strengthens
the soil skeleton sufficiently that little self-weight consolidation
occurs. Instead, the consolidation behavior of lime treated clay is
akin to that of sand. In the case of gypsum addition, the consolidation
magnitude was enhanced. Consolidation occurred more quickly, and final
effective clay solids contents approached those of untreated clay. The
behavior of clay/gypsum mixtures is similar to that for sand/clay mixes.
xi
CHAPTER I: INTRODUCTION
Florida supplies nearly one-third of the world's phosphate
requirements. This phosphate is the source of phosphorous in inorganic
fertilizer and represents a vital non-renewable source. The nature of
the phosphate deposits and the mineralogy of the ore or matrix combined
with the present state of the art in phosphate beneficiation give rise
to several problems related to safety and environmental acceptance.
Perhaps the most pressing problem faced by the phosphate industry is the
adequate disposal of the clay wastes generated during the beneficiation
process. The problem , simply stated, is that the volume of waste
products exceeds the mined-out volume. Historically, waste clays have
been impounded in earthen retention structures with 60% of the clays
being retained below the ground surface. The resulting retention
structures are often as large as 800 acres and have earthen dams as
high as 60 feet. There is growing public and legislative pressure
stemming from the following concerns:
1. The fear of a dam failure which could pollute the ground watersupply.
2. The rising cost of land and the fact that waste clay pondshistorically have required 10 to 30 years for reclamation.
3. The demand for potable water tied up by the mining process.
The last waste clay retention dam failure occurred in 1971. This
failure brought about the development of clay settling area regulations
under Chapter 17-9 of the Florida Administrative Code. Since then,
1
there has been increasing pressure to reduce the turnaround time between
the mining and reclamation of the land.
BENEFICIATION
Mining of the Florida phosphate deposits today is accomplished by
large electric draglines using buckets with capacities as high as 65
cubic yards. These draglines strip off the overburden and cast it
aside. The ore layer is then removed and placed in a sump where it is
slurried and pumped to the beneficiation plant at solids contents of 25%
to 40% for processing.
The washer section of the beneficiation plant separates the pebble
phosphate from the slurry in a series of screening, scrubbing, and
washing operations. The slurry that remains consists of sand, phosphate
particles, and clays. The clays are separated from the sand/phosphate
mixture by hydrocyclones and are pumped at a 3% solids content to the
large earthen retention structures. The sand is separated from the
phosphate ore by means of a flotation process. The resulting tailings
sand is pumped from the beneficiation plant at a solids content of
30%. This tailings sand is used for dam construction and land
reclamation; therefore, disposal is not a problem.
Each year a typical mine will process about 10,000,000 tons of
phosphate matrix and will produce about 2,800,000 dry tons of clay. The
increased volume of the clay at 3% to 30% solids requires that 55% to
70% of the mined land be used for waste clay settling areas.
MINERALOGY
The mineralogy of a clay greatly effects its behavior. Typical
phosphatic clays contain the following minerals: montmorillonite
2
(smectite), attapulgite (palygorskite), kaolinite, mica (illite),
quartz, appatite, and aluminum phosphates (mostly wavelite).
The basic problems associated with phosphatic clays involve the
water holding capacity and low bearing capacity of the clays. The water
holding capacity of the clay is a function of three factors: 1) water
in pore spaces, 2) water held on surfaces, and 3) water in
interlayers. The bearing capacity of a clay is related to the water
content.
The small size of the clay particles and pore spaces greatly
contributes to the water holding capacity of the clay. Often as much as
70% of the clay particles are less than 2 microns in size with an
average particle size in the colloid range. The small size of the pore
spaces combined with the presence of fibrous minerals (usually
palygorskite), which interfere with orderly stacking of the clay
particles, make dewatering of the voids difficult. Additionally, the
small particle size means that electrostatic forces prevail over the
body forces due to the large specific surface, thus hindering particle
settlement.
CLAY DISPOSAL TECHNIQUES
Dewatering methods for waste clays have been sought for many
years. Intuitively, the problem may be approached from two directions;
either modify the beneficiation process to avoid producing the slurry or
alter the produced clay slurry. Of these two methods, the latter has
generated the most interest. Research has confirmed that the poor
settling characteristics of the clays are a function of the low self-
weight consolidation forces. A logical solution to the problem is the
3
addition of tailings sand to the clay to increase the unit weight of the
material. Another solution is to provide a sand cap surcharge to
increase the effective stresses within the underlying clay slurry. In
these applications, the bearing capacity of the clay becomes a major
consideration. The initial solids content of the clay is on the order
of 2% to 6% and has insufficient strength to entrain added sand or
support a surcharge cap. Consequently, the clay must be allowed to
settle to a solids content of approximately 15% before pumping to other
disposal sites for sand addition. The use of flocculents to increase
the sedimentation rate of the particles has been investigated and holds
much promise.
LIME OR GYPSUM TREATMENT OF CLAYS
Inasmuch as gypsum is a waste by-product produced in the manufac-
ture of phosphoric acid, the feasibility of simultaneous disposal
analogous to a sand/clay mix is attractive. However, recognizing the
low pH and activity of the waste clays requires an examination of the
compatability of these materials.
Lime treatment of clays was practiced by the Romans who added burnt
limestone and volcanic ash to form a weak mortar. Accordingly, lime
treatment of waste clays would be anticipated to increase strength and
thus bearing capacity. Since gypsum can be converted to lime, the
affect of lime treatment on the consolidation and strength properties of
phosphatic clays warrants investigation.
PURPOSE OF RESEARCH
The research presented in this report investigates the effects of
the addition of lime and gypsum to the waste clay in the same manner as
4
the tailings sand. Addition of either of these two compounds to the
clays would occur after the clays had reached a solids content in the
13% to 15% range. Lime was suggested for its history of increasing the
strength and reducing the plasticity of troublesome clays. The addition
of gypsum is being investigated strictly on an experimental basis and
because disposal of by-product gypsum created in the manufacture of
fertilizers is rapidly becoming a problem.
SCOPE OF WORK
The objectives of the research are twofold. The first objective is
to experimentally estimate suitable quantities of lime and gypsum for
addition to the waste clays. The second objective is to determine the
consolidation characteristics of the waste clays with the suggested lime
and gypsum additions using centrifuge modeling techniques. Centrifuge
modeling was chosen because it permits the very lengthy consolidation
process to be modeled in a matter of hours as opposed to years.
5
CHAPTER II: BACKGROUND INFORMATION
LIME TREATMENT OF SOILS
Lime stabilization of plastic soils has become a widely accepted
method of preparing clayey soils for use as roadbeds and foundations.
Specifically, lime stabilization serves to reduce plasticity and provide
moderate strength gain. This behavior is attributed to the following
phenomena:
1. Cation Exchange,
2. Flocculation and Agglomeration,
3. Pozzolanic Reactions, and
4. Carbonation.
Cation exchange is the replacement of the exchangeable cations
(such as sodium, hydrogen, and potassium), which previously occupied the
exchange sites of the soil, by the calcium cations derived from the
lime.
An increase in grain size is created by the flocculation and
agglomeration of particles. This phenomenon is caused by suppression of
a double water layer surrounding the clay particles due to an increased
electrolyte concentration provided by the calcium cations.
Pozzolanic reactions involve the formation of cementitious minerals
from the reactions between the silica and alumina present in the soil
minerals and the calcium from the lime. These new minerals are
primarily responsible for the time dependent strength gain exhibited by
7
the lime-soil mixture. The formation of these minerals is dependent on
the amount of lime (calcium) available for reaction.
Carbonation involves the reaction of lime and atmospheric carbon
dioxide to form the cementing agent calcium carbonate. This cementing
agent is relatively weak, therefore, carbonation has only a minor
influence on the strength increase exhibited by lime addition.
MECHANISMS OF LIME TREATMENT
The following mechanisms occur as lime is added to a clay. Ini-
tially, the material becomes friable and a silty texture is attained
upon curing. This behavior is attributed to cation exchange and com-
pression of the double water layers surrounding the clay particles.
These reactions are made possible by an increase in hydrogen-ion concen-
tration (pH) of the system and an increase in calcium-ion concentration,
both made possible by the addition of lime. The plasticity of the
treated clay is subsequently reduced. The lime content at which all
cation-exchange reactions have occurred is termed the "lime fixation
point" (Townsend, 1979). This point is characterized by the increase in
pH of the lime-soil mixture to that of a calcium saturated lime slurry.
This pH approaches 12.4 for unhydrated "quick" lime. Since this point
represents the maximum modification percentage, it is the optimum
percentage generally used for lime addition to soil. Strength gains
created by the addition of percentages of lime below this optimum are
generally insignificant and are probably a result of an increase in the
angle of internal friction caused by the aggregation of the clay parti-
cles. The addition of lime in excess of the optimum percentage provides
free calcium ions which are available for further pozzolanic reactions.
8
SUITABLE SOILS FOR TREATMENT
Lime stabilization is effective for soils with silica and alumina
components available to take part in the pozzolanic reactions. Clayey
soils, with their silica tetrahedral and alumina octahedral layers,
provide a source of these ions, therefore, clayey soils generally
respond very well to lime treatment.
It has been found that plasticity, organic content, pH, and sulfate
concentration are additional factors which effect the lime reactivity of
soils (Townsend, 1979). A Plasticity Index (PI) of 12 is accepted by
the Corps of Engineers as the lower limit of soils responsive to lime
treatment. It has been reported that soils with organic contents
greater than 1% generally do not respond well to lime treatment. It has
additionally been found that acid soils are less responsive than soils
with pH greater than 7. The presence of sulfates has been proven
detrimental to lime stabilization due to the formation of minerals which
disrupt the bonding and formation of cementitious compounds.
BY-PRODUCT GYPSUM
Source of Gypsum
Calcium sulfate (gypsum) is obtained as a by-product in the manu-
facture of phosphoric acid. Phosphoric acid is the intermediate product
from which all phosphate end products are made and is created by the
reaction between sulfuric acid and ground phosphate rock. Some 4 to 5
tons of gypsum are formed for each ton of phosphoric acid (Watson,
1971).
9
Disposal and Storage
After the gypsum is separated from the phosphoric acid through
vacuum filters, it is typically slurried and pumped to settling ponds or
to the top of huge mounds of gypsum called gypsum stacks. These gypsum
stacks commonly cover areas as large as 300 acres and are often more
than 40 feet in height. The gypsum is deposited at the top of the stack
and the water is allowed to drain to a cooling pond. The water at this
point is highly corrosive, containing from 1% to 2% phosphoric acid and
having a pH of 1.5 to 2.0. Typically, only a small amount of the water
in the cooling pond is from the gypsum stack with the remainder coming
from various sources throughout the plant. This water is allowed to
cool before returning to the plant for reuse.
Uses of By-Product Gypsum
Only very limited uses have been found for by-product gypsum in the
United States because of the relatively low cost of sulfur and the
availability of good quality natural gypsum. The by-product gypsum
contains varying amounts of phosphate and fluoride impurities which must
be considered in any possible usage. Additionally, the occurrence of
small quantities of radioactive matter affects the possible usage of
this gypsum in cements and wall board in the building industry.
By-product gypsum has been used in expanding and prestressing
cements for road construction in Japan with favorable results. The
resulting concrete is said to have a better surface finish with fewer
shrinkage cracks than can be obtained with ordinary concrete. Addition-
ally, ground gypsum has been used as a soil conditioner, particularly on
grassland, to make up for calcium and sulfur deficiencies in soil. Soil
10
alkalinity is reduced with the addition of gypsum and a flocculation of
soil particles occurs, thereby improving drainage (Gutt and Smith,
1973).
CENTRIFUGE MODELING OF CONSOLIDATION BEHAVIOR
Limitations of Physical Modeling
Physical modeling is often used in engineering in an attempt to
duplicate operating and field conditions. For the model to be an ideal
representation of the prototype, similar stresses must be applied.
While geometric and material properties are often easy to duplicate in
reduced scale models, the stresses which the prototype is subjected to
are much harder to duplicate, especially in models involving soil. Soil
stresses in corresponding points of the model and prototype are a func-
tion of the height of the overlying material and its unit weight when
both model and prototype are subject to the same gravitational field.
This is the major disadvantage of physically modeling soil behavior with
a reduced scale.
Centrifuge Modeling
To overcome the stress dissimilarity of soil models previously
alluded to, the unit weight of the material in the model must be
changed. This can occur either by using a material with a higher
specific gravity, or by increasing the gravitational force. Since, in
this case, it is desired to model both material and geometric proper-
ties, the logical solution is to increase the gravitational force. This
can be accomplished by subjecting the model to high centrifugal forces.
By increasing the acceleration of the model by a scaling factor and
reducing the dimensions of the model by the same scaling factor, equal
11
stress levels at equal points in both prototype and model will be
produced.
Since the settling of a clay is a time dependent function, it
becomes necessary to study the correlation between time in the model and
time in the prototype in centrifuge modeling. When modeling the settle-
ment behavior of a slurry, the different processes of sedimentation and
consolidation must be considered.
The initial settling of clay particles is referred to as sedimenta-
tion. Bromwell and Raden (1979) state that the majority of sedimenta-
tion ends at clay solids contents of 3% to 8%. Since it is desired to
model clay slurries with relatively greater solids contents (13% to
15%), it is assumed that sedimentation will not be a major considera-
tion.
As the sedimentation process ends, the consolidation process
begins. This process is characterized by a compression of solid
particles through the dissipation of pore water pressures within the
soil mass over a period of time.
For centrifugal modeling it has been shown (Bloomquist, 1982) that
the time scaling relationship is
T P = T m x n2
This means that the model time for consolidation is increased by the
square of the scaling factor. This is obviously a major advantage of
centrifuge testing. For a centrifuge test in which the model is
accelerated to 60 times the force of gravity (i.e. n = 60), a prototype
time of 1 year can be modeled in 2.4 hours.
12
CHAPTER III: TEST PROCEDURES AND EQUIPMENT
INTRODUCTION
This chapter describes the test procedures and equipment used for
this research. In reiteration, the primary objective of this research
was to determine the consolidation properties of phosphatic waste clays
treated with lime or gypsum using centrifugal modeling techniques.
However, prior to centrifugal model tests, the optimum quantities of
lime or gypsum to be added to the clays must be determined. Thus a
series of preliminary bench tests were required. An additional
consideration was the time scaling relationships for centrifugal
modeling. Specifically, the consolidation phenomena models as N2, while
the lime/clay chemical reactions model as N1. An accelerated curing
program investigated this aspect.
From these considerations, the testing program can be divided into
four phases; (a) pH testing for optimum lime or gypsum percentage,
(b) bench tests for strength, (c) accelerated curing tests for scaling
compatibility and (d) centrifugal modeling of consolidation behavior.
pH TEST
The pH test of Eades and Grim (1966) was used to determine the
quantity of lime to be added to the waste clay. Essentially, this test
was developed to determine the minimum lime percentage required to
provide sufficient lime for clay/lime pozzolanic reactions to occur.
Since the pH of saturated lime solution is 12.4, then the percentage of
13
lime added to a clay to produce a pH of 12.4 in a clay/lime solution is
the "pH percentage." For lack of better criteria, the same tests and
concepts were used to try and estimate suitable quantities of gypsum to
be added to the waste clay. However in this case, the pH for gypsum was
about 2.8. A flowchart of the pH testing procedures followed is shown
in Figure 1, while Appendix A provides detailed procedures.
BENCH TESTS
Although the pH test provides a good indication of target lime
percentages, it does not assure "reactivity," i.e., the clay may not
react favorably to produce strength gains. Hence, the pH tests were
followed by the bench testing phase of the research to assess strength-
gaining reactivity. The target lime and gypsum quantities estimated
from the pH test data, in addition to two lower percentage quantities,
were added to the waste clays at approximately 12% to 14% solids. The
mixtures were allowed to cure at room temperature in sealed containers
underwater for periods of 0, 7, 14, and 28 days. At the end of the
specified curing periods, shear strengths of the samples were determined
using a miniature vane shear apparatus. A flowchart of the bench
testing procedures followed is shown in Figure 2, while Appendix A
provides detailed procedures.
ACCELERATED CURING TESTS
Lime stabilization is a chemical process which cannot be adequately
modeled in the centrifuge, that is to say, the time-scaling exponent for
consolidation is 2.0, while for gravity-independent chemical reactions
it is 1.0. Thus consolidation in a centrifuge model would be over many
days before the chemical reactions had occurred. Accordingly, a method
14
15
Figure 2: Flowchart of Bench Testing Procedures
16
was devised to avoid the problem associated with the time required for
the clay-lime mix to achieve adequate strength. From plots of the lime
bench test data, it was estimated that the majority of the strength
gained through the lime addition had occurred by the 16th day of
curing. The solution was to spin the suggested lime clay mixture in the
centrifuge at 60 g's for the equivalent of 16 days and then remove the
samples and allow them to cure for 16 days. Following the 16 days of
curing, the samples would be placed in the centrifuge and allowed to
consolidate to completion. Recognizing that chemical reactions can be
accelerated by heat (Townsend, 1979) to reduce the 16-day time required
for curing, two accelerated curing tests were performed to determine the
time required to reach maximum strength with a curing temperature of 105
degrees Fahrenheit. The clay was mixed with the required amount of lime
and placed in mason jars. The jars were then placed in an oven set at
105 degrees and al lowed to cure for 1, 2, 3, 4, and 5 days. At the end
of each specified curing time, a jar was removed from the oven and
tested with the vane shear device. The number of days required to reach
full strength was determined from plots of shear strength versus curing
time. A flowchart of the accelerated curing testing procedures is
presented in Figure 3, while Appendix A provides detailed procedures.
When the lime mixtures were subsequently tested in the centrifuge, the
buckets were sealed to prevent drying and placed in the oven for the
required curing time after being spun for the initial 16-day equivalent
at 60 g's. Following the curing period, the samples were placed in the
centrifuge and were allowed to consolidate to completion at 60 g's.
17
Figure 3: Flowchart of Accelerated Curing Test Procedures
18
CENTRIFUGE MODELS
The actual centrifuge testing of the waste clay mixes is a simple
but time consuming process. The consolidation behavior is determined by
visual (photographic) in-flight inspection of the slurry/supernatant
interface height. Pictures were taken at geometric time increments
(e.g. 1, 2, 4, 8, 16, 32, 64, etc. minutes) to facilitate plotting on a
logarithmic time scale. When the interface heights stabilized, the
tests were ended. The centrifuge samples were then cored and vane shear
tested to provide solids content with depth and average strength
information. The operation of the UF Centrifuge is discussed in detail
in Volume 1 of this report series (Townsend, et al. 1986) and the
centrifuge operation procedures furnished in Appendix A of this report
are for completeness.
EQUIPMENT
The equipment utilized in this research is discussed in this
section and consists of two facets; (a) bench tests for optimum lime or
gypsum content and accelerated curing, and (b) centrifugal model tests.
ADDITIVE QUANTITY DETERMINATION
Figures 4 and 5 show photographs of the pH and bench testing
equipment, respectively. Figure 4 shows the equipment used to determine
lime and gypsum fixation points while Figure 5 shows the equipment used
to determine the strength gains with time of the mixtures.
pH Meter
To determine the lime and gypsum fixation points, over a pH range
of approximately 2.6 to 12.4, a digital pH meter was used. Appropriate
buffer solutions were used for calibration, depending upon the pH range
19
Figure 5: Bench Testing Equipment
20
of interest. However, it should be mentioned that in determining pH
fixation percentages, a great deal of sensitivity is not required and
inexpensive equipment can be used.
Mason jars with sealable lids were used to contain the clay/lime or
clay/gypsum mixtures. The wide mouth of these jars allowed easy mixing
and testing with the miniature laboratory vane shear device. Mixing of
the slurries was easily accomplished using a variable speed drill with a
paint mixing attachment.
Vane Shear Device
A laboratory vane shear device was used to determine the shear
strength of the slurry mixtures at various curing times. The device
consists of a four-bladed vane which is inserted into the slurry and
rotated. The resistance to rotation, or torque, is measured. The shear
strength may subsequently be calculated from the torque required to fail
the sample.
UNIVERSITY OF FLORIDA CENTRIFUGE
Description of Centrifuge
The centrifuge used to model the consolidation behavior of the
mixtures is a Rucker Model 57-2380 shown schematically in Figure 6 and
discussed in detail elsewhere (Bloomquist, 1982; McClimans, 1984;
Townsend, et al., 1986). Power is supplied by a 2-horsepower, 3-pole,
208-volt electric motor. Two rotating arms, 180 degrees apart, each
support a platform capable of holding two samples. The distance from
the axis of rotation of the centrifuge to the centroid of each platform
is 34.5 inches. Modifications to the centrifuge arms allow a capacity
of approximately 80 pounds to an acceleration of 100 g's. A metal
21
Figure 6: Schematic Drawing of University of Florida Centrifuge
housing encloses the entire assembly. Access to the arms and platforms
is provided through a double door on the side of the centrifuge, a
hinged top panel, and a plexiglass covered viewport located on the top
of the centrifuge.
Electronic Monitoring Devices
Three devices are used to monitor and control the speed of the
centrifuge during operation: the accelerometer, the digital tachometer,
and the acceleration divergence limiter.
An Entran Miniature Damped Accelerometer (No. EGA-125f-250D)
monitors the acceleration of the samples during the tests. The output
voltage is converted to g units and displayed on the LED panel of a
Doric Series 420 Digital Transducer Indicator after passing through a
slip ring on the centrifuge spindle. The accelerometer is mounted on
one of the sample bucket housings at a distance of 37.5 inches from the
center of rotation of the centrifuge. This distance differs from the
center of gravity of the sample necessitating the calculation of an
operational offset acceleration.
For redundancy, a digital bench tachometer (Power Instruments,
Model 1723) is used to monitor the model acceleration. The tachometer
measures the speed (RPM) of the centrifuge by means of a photo-electric
pickoff monitoring the spindle. The rotational speed of the model is
displayed on the LED panel of the tachometer. Knowing the rotational
speed of the centrifuge and the radial distance to the model point of
interest, the correct acceleration of the model may be calculated.
An Acceleration Divergence Limiter (ADL) was developed by the
Digital Design Facility of the University of Florida's College of
23
Engineering. The ADL provides a means of controlling the acceleration
of the centrifuge for safety purposes and to allow overnight testing to
occur without the presence of an operator. The device allows the
selection of an appropriate acceleration level and operating window.
When the acceleration of the centrifuge increases beyond or falls below
the specified operating window, the centrifuge automatically shuts
off. This device therefore protects against damage due to overheating
of bearings, unauthorized adjustment of the speed control, and possible
breakage of the platform or sample housings during the test.
Specimen Container Assembly
For proper correlation between stresses in the prototype and model,
centrifuge modeling requires proper inflight orientation of the sample
to be modeled. The consolidation process occurs vertically in the
field, however, the increased centrifugal forces which, make
model/prototype correlation possible, occur horizontally. The sample
must therefore be oriented horizontally in flight. This orientation is
made possible by the use of platforms which allow the models to pivot
freely. This design allows the acceleration vector to pass through the
bottom of the sample at all times. The components of the mounting
assembly include the aluminum bucket housings, the aluminum buckets, the
pivot bolts, and the plexiglass containers. The components of the
mounting assembly include the plexiglass containers, aluminum buckets,
pivot bolts, and aluminum bucket housings.
Since movement of the slurry/supernatant level must be monitored
during the test, transparent plexiglass containers, 5.5-in. ID by 6 in.
high, were used to carry the samples. Transparent metric scales with
24
millimeter divisions were attached to the outside of the container for
accurate measurement of interface heights.
Since high stresses are developed in the centrifuge, the plexiglass
containers alone would not be strong enough and some means of support is
required. Accordingly, an aluminum bucket was fabricated from 6 9/16-
in. OD by 1/4-in. thick pipe with 1/4-in. plate heliarc welded to the
bottom. A 1 in. by 4-in. cut-out in the bucket permits viewing of the
plexiglass slurry container. Two 3/4-in. holes drilled through the top
of the bucket allow mounting of the bucket to the container housing by a
pivot bolt.
A 3/4-in. high-strength steel bolt is used to mount the buckets to
the housing. The bolts pass through the bucket and allow them to rotate
upward into a horizontal position upon centrifugal loading. The bolts
are slightly offset to allow the buckets to overswing and rest against a
restraining bracket mounted on the bucket housing. This design insures
that the resultant acceleration vector is always perpendicular to the
model's interface (Bloomquist, Davidson, and Townsend, 1984).
Two aluminum bucket housings provide a support system for the
buckets to be mounted to the centrifuge arm, and allow simultaneous
modeling of four samples.
Data Acquisition
Data acquisition is a photographic record using a stroboscope and a
Polaroid camera. The major components of the system include the strobe,
the flash delay, the camera, and the camera mount.
25
A Stroboslave Model 1539-A manufactured by General Radio Company is
used to provide high intensity light flashes of short duration. The
strobe is connected with one of two photoelectric pickoffs mounted on
top of the centrifuge. An external trigger allows just one flash to
occur, thus eliminating multiple exposures.
A model 1531-P2 Flash Delay allows the rotating samples to be
oriented directly underneath the camera as a flash occurs. This flash
delay allows the proper orientation of the samples with the flashing
light source and camera and permits minor adjustments to compensate for
fluctuations in centrifuge speed.
A Polaroid camera (Model 600 SE) was chosen because of its ability
to take close-up, instant photographs. The model features an
interchangeable lens but a close-up lens set was added to enable
accurate readings of the metric scale on the side of the plexiglass
buckets. High-speed film (ASA 3000) is used and provides excellent
photographs as illustrated in Figure 7.
Camera Mount. Since the centrifuge vibrates during operation, the
camera is mounted to a platform anchored to the ceiling joists directly
over the view port. A tube extends down from the platform and allows
the camera to be lowered into place over the opened viewport for
pictures to be taken. An adjustable mechanism allows the camera to be
raised and lowered vertically along the tube or three inches
horizontally.
26
Figure 7: Example of Photographic Monitoring
CHAPTER IV: PRESENTATION AND DISCUSSION OF RESULTS
INTRODUCTION
The testing performed on the phosphatic waste clays may be divided
into four phases:
1. The pH testing phase, where stabilization concentrations oflime and gypsum to be added to the waste clays were determined,
2. The bench testing phase, where strengths of the proposed claymixtures were determined after certain curing periods,
3. The accelerated curing test phase, where lime/clay mixtureswere subjected to increased temperature to decrease the curingtime required for adequate strength gain of centrifuge samples,and
4. The centrifuge testing phase, where the consolidation charac-teristics of phosphatic waste clays mixed with lime and gypsumwere observed.
pH TESTS
The pH test developed by Eades and Grim (1966) was used to
determine the percentages of lime and gypsum required for stabilization
of the waste clays. A total of six waste clays from different mines in
Florida were tested, including I.M.C.- Kingsford, Occidental-Suwannee
River, Agrico-Ft. Green, Amax-Big Four, Brewster-Haynsworth, and CF
Mining-Hardee. Table 1 presents the results of the pH testing and shows
the percent lime or gypsum (by weight of clay solids) required to
achieve a pH value of approximately 12.4 or 2.8, respectively. The pH
of the untreated clays ranged from 7.2 to 7.8.
29
Lime Addition
Relatively large quantities of lime were required to increase the
pH of the waste clays to the target pH. In general, six percent lime is
accepted as being the cut-off point for cost effective stabilization.
Lime percentages of from 12 to 14 were required to bring the waste clays
up to the target pH, which ranged from 12.2 to 12.4 depending on the
degree of hydration of the lime used. Typical liquid limits (LL) of the
phosphatic waste clays are well over 200. Typical plasticity indices
(PI) of the clays range from 140 to 180. Some restrictions which have
been placed on the LL and PI of clayey soils suitable for effective lime
stabilization are a liquid limit not less than 40 and a plasticity index
not less than 20 (Townsend and Donaghe, 1976). According to these
criteria, lime stabilization of phosphatic waste clays should be
30
successful. A possible reason that such large quantities of lime are
required to achieve this pH percentage could be the organic content of
the clays. In general, clays with organic contents greater than 1% do
not respond well to lime stabilization. A typical organic content of
phosphatic waste clays is on the order of 2% (Bloomquist, 1982). With
these facts in mind, it was decided to proceed to the bench testing
phase using the experimental target lime percentage and two lower lime
percentages to test the validity of the pH testing phase.
Gypsum Addition
The addition of gypsum as a stabilizing agent is being investigated
on an experimental basis. While gypsum has been used as a soil
conditioner, documentation of its use as a soil additive for stabili-
zation purposes is nonexistent.
For lack of better criteria, the pH test of Eades and Grimm, which
was developed to determine lime stabilization concentrations was used to
determine the quantity of gypsum required for waste clay
stabilization. Gypsum concentrations of from 700% to 1200% were
required to bring the clay to the target pH, which ranged from 2.8 to
2.85, using Eades and Grimm criteria. Obviously, the stabilization
processes of lime and gypsum are different and require different tests,
assuming that gypsum indeed acts as a soil stabilizer.
It was decided to use the same approach adopted for lime in the
gypsum bench testing phase. The target pH additive concentration would
be tested as well as two lower percentages.
31
BENCH TESTS
Introduction
The bench testing technique outlined in the previous chapter was
used to determine 28-day strengths of the phosphatic waste clay mixed
with lime and gypsum. In typical lime stabilization laboratory
investigations, the soil is mixed with the required lime percentage at
the appropriate water content and then compacted in a Harvard miniature
or Proctor mold. The resulting sample is generally cured for a
specified time and then tested in unconfined compression. The nature of
phosphatic waste clays, however, requires a different testing
procedure. Compaction of the slurry cannot occur in the field, and the
slurry form of the clay prevents the use of the unconfined compression
device. It was therefore necessary to employ the miniature vane shear
device to provide a measure of the undrained shear strength of the cured
phosphatic clay mixtures. The samples were cured at room temperature
(20-25 degrees Celsius).
The six phosphatic waste clays which were tested in the pH testing
phase were also tested in this phase of the research. Table 2 presents
a summary of the 28-day strengths of the various clay mixtures.
Shear Strength versus Curing Time Curves
In addition to the 28-day strengths, the undrained shear strength
was measured at 7 and 14 days as well as immediately after mixing with
lime or gypsum. When the shear strengths are plotted against the curing
time, the plots give an indication of the curing behavior, i.e. chemical
reactions of the particular mix.
32
Table 2.
Summary of 28-Day Strengths from Bench Tests
MINE % SOLIDS ADDITIVE % ADDED 28-DAY
STRENGTH (PSF)
I.M.C. KINGSFORD 13.6
OCCIDENTAL SUWANNEE RIVER
AGRICO-FT. GREEN 13.3
AMAX-BIG FOUR 12.7
BREWSTER HAYNSWORTH
CF MI NING-HARDEE
12.5
12.2
13.1
LIME LIME LIME
GYPSUM GYPSUM GYPSUM LIME LIME LIME
GYPSUM GYPSUM GYPSUM
LIME LIME LIME
GYPSUM GYPSUM GYPSUM LIME LIME LIME
GYPSUM GYPSUM GYPSUM
LIME LIME LIME
GYPSUM GYPSUM GYPSUM
LIME LIME LIME
GYPSUM GYPSUM GYPSUM
i 12
100 300 700
: 14
300 500 700
5 7
12 400 800
1200 4 8
12 400 800
1200 4
1: 400 800
1200 4 8
12 400 800
1200
;*i 25:2 4.5 4.0 4.7 4.5 5.4
15.8 3.5 6.2 8.4 4.1 4.6
14.3 4.8 6.5
10.2 3.7 4.5
21.1, 4.4 7.5 8.9 3.3
1::; 4.0 7.5
i-i 8:l
17.7 5.5 7.9
10.6
33
Figures 8 through 13 present the curves for each clay type that
lime was added to. In general, the addition of lime below the target
value produced very little strength gain in any of the samples. The
addition of the target concentration, however, produced strength gains
as high as 5 times the initial strength of the slurry with the average
strength gain being approximately 3 times the initial strength. The
strength gains with time observed for the target pH percentages indicate
that chemical reactions are occurring with the clay/lime mixture. They
also verify the validity of the pH test for rapidly determining the lime
contents required for stabilizing reactions.
In all of the samples that lime was added to, there was a
noticeable reduction in plasticity during the initial mixing. The time
required for the maximum strength gain varied widely between the samples
as seen in the figures. Samples from Agrico, Occidental, and Brewster
reached a plateau in strength gain between 16 and 20 days. In contrast,
samples from I.M.C., CF Mining, and Big Four exhibited strength gains
throughout the 28-day period. These samples also exhibited the highest
strength gains of the lime treated clays, indicating that they react
more favorably to lime stabilization.
Figures 14 through 19 present the curing curves for the samples to
which gypsum was added. Strength gains were minimal in comparison with
the lime samples, even when gypsum-clay ratios of 12:1 were tested. The
highest strength gains were from approximately 5 psf to 10 psf. While
this represents a doubling of strength over the 28-day period, the gain
of 5 psf is negligible in terms of improving the bearing capacity of the
clay. Furthermore, the addition of gypsum to the clay slurry initially
34
Figure 8: Shear Strength vs Curing Time, I.M.C. Lime Samples
Figure 9: Shear Strength vs Curing Time, Occidental Lime Samples
Figure 10: Shear Strength vs Curing Time, Agrico Lime Samples
Figure 13: Shear Strength vs Curing Time, CF Mining Lime Samples
Figure 14: Shear Strength vs Curing Time, I.M.C. Gypsum Samples
Figure 15: Shear Strength vs Curing Time, Occidental Gypsum Samples
Figure 16: Shear Strength vs Curing Time, Agrico Gypsum Samples
Figure 17: Shear Strength vs Curing Time, Big Four Gypsum Samples
Figure 18: Shear Strength vs Curing Time, Brewster Gypsum Samples
)
Figure 19: Shear Strength vs Curing Time, CF Mining Gypsum Samples
tended to decrease the viscosity of the mixture, making it flow more
readily and reducing the strength to below that of an untreated clay
slurry of the same clay solids content. This phenomenon was observed
even when adding a 12:1 gypsum to clay ratio. It is difficult to
discern whether these minor strength gains are chemical or mechanical
reactions or a combination. The time-related strength gains are
indicative of chemical reactions and were observed for all gypsum
mixtures. Although quite small, in all of the gypsum samples, the
majority of the strength gains occurred within 12 to 16 days.
ACCELERATED CURING TESTS
It was found that the majority of the strength gain in the lime
samples occurred within 16 to 20 days. This is a time dependent, i.e.,
chemical, process that cannot be modeled or accelerated in the
centrifuge. In order to examine centrifugally the consolidation
behavior of these clay/lime mixtures, a method of circumventing this
problem was devised in which the lime-clay mixtures would be accelerated
in the centrifuge for the equivalent of the 16 days required for
strength gain, removed from the centrifuge, allowed to cure for the 16-
day period, and then re-accelerated to completion in the centrifuge.
The major problem with this method was the 16-day period required for
curing the samples. In order to reduce the curing time and to quicken
the total testing process, accelerated curing tests were performed as
outlined in the previous chapter. A curing temperature of 105 degrees
Fahrenheit was used and samples from Agrico-Ft. Green and Occidental-
Suwannee River mines were tested. Lime concentrations of 12% were added
to the samples since it was proven that the addition of lime in lower
47
percentages produces little or no strength gain. Figures 20 and 21
present the results from these curing tests. From the figures, it is
clear that the majority of the strength gain occurs after 2 days of oven
curing. The centrifuge buckets were therefore allowed to cure for 2
days at 105 degrees Fahrenheit after initial spinning. It is curious to
note that the strength gains for the bench test specimens during
accelerated curing were as much as 100% higher than the specimens that
were cured at room temperature. This increased strength could be due to
a change in the pozzolanic reaction products brought about by the
increased temperature (Townsend and Donaghe, 1976).
CENTRIFUGE TESTS
Introduction
The final phase of the research involved the actual centrifuge
modeling of the consolidation behavior of phosphatic waste clays mixed
with lime and gypsum. A total of four clays from different mines were
tested; specifically, Agrico-Ft. Green, Occidental-Suwannee River, Amax-
Big Four, and Brewster-Haynsworth. A total of 16 tests were per-
formed. Four tests each were performed on untreated and lime treated
clays, while eight tests were performed on gypsum treated clays.
Untreated clay was tested to provide a baseline against which the
consolidation characteristics of lime and gypsum treated clays may be
compared. Twelve percent lime was added to the lime treated clay
samples as predicted by the pH and bench testing phases. Gypsum to clay
ratios of 8:1 and 2:1 were tested. It was decided to use these lower
quantities of gypsum rather than the 12:1 ratio determined in the pH
testing phase because it was felt that adding such large quantities of
48
Figure 20: Accelerated Curing Test Results, Occidental Samples
material to the clay would be economically infeasible. Initially, the
8:1 ratio was tested but subsequently discarded as sand clay mix tests
showed this ratio was not beneficial (McClimans, 1984). Then it was
decided to test a 2:1 ratio in an attempt to lower the final interface
height and enhance consolidation of the clay. Table 3 provides a brief
summary of the centrifuge tests performed. All tests were performed at
60 g's and had initial interface heights of approximately 8 centi-
meters. Additionally, all samples had initial clay solids contents of
approximately 13%.
Consolidation Characteristics of Treated Clays
The objectives of this modeling were to determine the effects of
the addition of lime and gypsum on consolidation behavior of the phos-
phatic waste clays mentioned above. Figures 22 through 25 present plots
of average effective clay solids content versus elapsed model time on a
log scale. The average effective clay solids content was determined
from the photographs of the interface heights and the following equation
derived by McClimans (1984):
51
53
n
54
55
56
Effect of Lime Addition on Consolidation Behavior
Figures 22 through 25 show that the addition of lime did nothing to
enhance the consolidation behavior of the phosphatic waste clays. The
addition of lime in fact hindered the consolidation when compared to the
untreated samples. This behavior is probably explained by the phenomena
of flocculation and agglomeration which occurs in the lime stabilization
process. An increase in grain size is produced by the suppression of
the double water layer. While increased grain size intuitively means
better drainage, it also means a stronger soil skeleton which resists
consolidation. An analogy to testing a lime-clay mix is placing a
sample of sand in the centrifuge and attempting to consolidate it. At a
certain point, the soil skeleton will resist further movement. It is
believed that this phenomenon as well as a drastic reduction in
plasticity on addition of the lime to the clay caused the observed
consolidation behavior.
Effect of Gypsum Addition on Consolidation Behavior
Figures 22 through 25 also show that the addition of gypsum in the
2:1 ratio greatly improved the consolidation behavior of the four clays
tested. The final interface height was reached an average of two times
faster in the gypsum treated samples. Additionally, the figures show
that similar intermediate clay solids contents were reached up to six
times faster in the gypsum treated waste clays. A possible explanation
for this behavior is the hypothesis that gypsum might act as a
flocculent in phosphatic waste clays. Unlike lime, which also produces
a flocculation of particles, a strengthening of the soil skeleton
probably does not occur. This was proven in the bench testing phase of
57
the research as negligible strength gain occurred even at 12:1 gypsum to
clay ratios. A flocculation of the particles could produce the enhanced
consolidation behavior observed in the gypsum samples.
More than likely, however, the gypsum particles serve to increase
self-weight and enhance drainage in much the same way as the tailings
sand in sand/clay mixes. Similar consolidation behavior is evident in
work performed by McClimans (1984) reported in Volume 1 (Townsend, et
al., 1986) in which sand/clay mixes were tested in the centrifuge.
Unlike sand, however, the gypsum seems to be very soluble in water and
drastically reduces the viscosity of the clay when mixed with it. In
order to fully understand the reaction between the gypsum and the waste
clay, further research should be conducted to prove or disprove the
theory that gypsum acts as a flocculent when mixed with phosphatic waste
clays. It is clear, however, that gypsum aids the consolidation process
of phosphatic waste clays.
Final Sample Analysis. After the completion of testing in the
centrifuge, each sample was removed and cored as outlined in the
previous chapter. Additionally, two vane shear tests were performed on
each sample to determine the final average shear strength. Table 3
shown on page 52 also presents a summary of the final analysis data. It
is interesting to note that the highest strength gain occurs in the
gypsum treated samples. The gypsum treated samples consolidated to
final model heights which were roughly equivalent to the final heights
of the untreated samples; however, the final strengths of the gypsum
treated samples ranged from 1.5 to 1.9 times higher than the untreated
samples, with shear strengths in the 30 psf range. This strength gain
58
is due to the increase in total solids content created by the addition
of gypsum since both the untreated and gypsum treated samples
consolidated to roughly the same final clay solids content.
The addition of lime to the waste clay obviously hindered the
consolidation process. Final clay solids contents of only 60% to 80% of
the final solids contents achieved in the untreated clay centrifuge
tests were attained. Final strengths were highly variable and
significant gains were noted only in the Agrico and Occidental waste
clays. The final strengths of the lime treated samples were generally
less than the untreated samples, however, this is understandable because
of the lower clay solids content achieved by the lime treated samples.
Figures 26 through 29 present plots of the final total solids
content with depth of each of the untreated centrifuge samples. The
untreated samples showed consistent profiles of increasing solids
content with depth. These solids contents were relatively variable from
top to bottom, differing by as much as 15%.
Figures 30 through 33 present similar plots of the lime treated
soils. The trend showed in these figures is a similar increasing solids
content with depth. The magnitude of the overall increase with depth is
much less than the untreated samples, differing by only 4% or less.
This perhaps indicates an overall strengthening or stiffening of the
clay from top to bottom, when the lime is added.
Figures 34 through 37 show plots of the final total solids content
profiles of the gypsum treated samples. Again, the observed trend of
increasing solids content with depth is present. Like the untreated
samples, there is a relatively high difference between the solids
60
61
63
contents at the top and bottom of the gypsum treated samples. This
could be indicative of migration of the gypsum particles to the bottom
of the containers during testing especially in the Amax-Big Four sample
which has a solids content variation of 36% from top to bottom. Because
of the degree of consolidation achieved by the gypsum treated samples,
and by work done by McClimans, 1984, (Townsend, et al., 1986) in which
it was shown that significant migration of sand particles through the
clay during centrifuge testing does not occur, it is believed that the
gypsum to clay ratio with depth stayed relatively intact. Since the
cored sections were not washed through a sieve to determine the
gypsum/clay ratio profile, there is no sure way of proving or disproving
this belief.
64
Figure 30: Solids Content With Depth, Agrico Lime Treated Clay Centrifuge Samples
Figure 31: Solids Content With Depth, Occidental Lime Treated Clay Centrifuge Samples
Figure 32: Solids Content With Depth, Big Four Lime Treated Clay Centrifuge Samples
Figure 34: Solids Content With Depth, Agrico Gypsum Treated Clay Centrifuge Samples
Figure 35: Solids Content With Depth, Occidental Gypsum Treated Clay Centrifuge Samples
Figure 36: Solids Content With Depth, Big Four Gypsum Treated Clay Centrifuge Samples
Figure 37: Solids Content With Depth, Brewster Gypsum Treated Clay Centrifuge Samples
CHAPTER V: CONCLUSIONS
LIME ADDITION TO WASTE CLAYS
The pH testing phase revealed that the pH test provides a rapid
assessment of minimum lime contents required for strength gains.
Percentages of lime were approximately 12% for the clays tested. The
bench testing phase of the research showed that relatively high strength
gains were achieved in waste clay samples where lime concentrations of
12% were added and relatively little improvement was obtained at lower
lime contents. Unfortunately, the magnitude of the 28-day strengths
could prove inadequate in bearing capacity considerations for supporting
equipment. However, the concept of using lime to strengthen the upper
few feet of a waste pond to provide a working platform for supporting a
sand cap may be feasible, but caution is advised. Given the relatively
high percentage of lime required for stabilization of the waste clays
and the magnitude of the strength gain resulting from the addition of
lime, lime stabilization is probably unsuitable for natural phosphatic
waste clays.
The addition of lime to the waste clays tended to hinder the
consolidation process. This is probably due to the decrease in
plasticity of the clay occurring as the lime is added and the curing
process proceeds. An overall strengthening of the soil skeleton occurs,
although final strengths after consolidation are weaker than untreated
clay after consolidation due to relatively lower clay solids contents.
73
The addition of lime to the clay seems to liken the consolidation
behavior to thatof sand which resists consolidation after
grain contact is made.
GYPSUM ADDITION TO WASTE CLAYS
grain to
The pH testing phase of the research showed that relatively large
quantities of gypsum were required to stabilize the waste clays when
using Eades and Grimm criteria. Since little time-dependent strength
increases indicative of chemical reactions occurred for clay/gypsum
mixes, this testing method is unsuitable for gypsum, which reacts
differently than lime with the clay.
The bench testing phase of the research showed that initial mixing
of gypsum with the waste clay dramatically decreased the viscosity of
the clay. This phenomenon is probably a key to the behavior observed in
the centrifuge testing phase of the research and should be investigated
further. It is assumed that a flocculation of particles occurs after a
certain period of time and results in an increased effective grain size
without the strength gain observed in lime stabilization. After
approximately 12 days of room temperature curing, maximum strengths were
achieved. These strengths were relatively low and probably insufficient
for bearing capacity considerations, even when 12:1 gypsum to clay
solids ratios were added.
The addition of gypsum to the waste clays had a marked effect on
the consolidation behavior of the clays. When compared to untreated
waste clays subjected to the same centrifugal acceleration, consoli-
dation to similar intermediate clay solids contents occurred much faster
and final solids contents were reached an average of 2 times faster when
74
a 2:1 gypsum to clay solids ratio was tested. It is believed that this
behavior is caused by a combination of the flocculation of clay and
gypsum particles and an increased self-weight and enhanced drainage of
the mixture similar to mixing sand with the waste clay. To fully
understand the reactions or mechanisms that occur, further research
should be conducted. Different gypsum to clay ratios should be tested
to determine an optimum additive concentration for consolidation
enhancement. Additionally, the environmental impact of adding gypsum to
the clays should be studied. After the gypsum centrifuge tests were
completed, a measure of the supernatant pH indicated a highly acidic
solution with pH values ranging from 2.5 to 2.9. This could have a
detrimental effect on the groundwater supply if unchecked seepage
occurs.
75
REFERENCES
Bloomquist, D.G. 1982. Centrifuge Modeling of Large StrainConsolidation Phenomena in Phosphatic Clay Retention Ponds, Ph.D.Dissertation, University of Florida.
Bloomquist, D.G., J.L. Davidson and F.C. Townsend. 1984. PlatformOrientation and Start-up Time During Centrifuge Testing.Engineering and Industrial Experiment Station, University ofFlorida. Research Report 242 W18.
Bromwell, L.G. and D.J. Raden. 1979. Disposal of Phosphate MiningWastes (Current Geotechnical Practice in Mine Waste Disposal).ASCE Geotechnical Division Special Publication.
Eades, J.L. and R.E. Grim. 1966. A Quick Test to Determine LimeRequirements for Lime Stabilization. National Academy of Sciences,National Research Council, Highway Research Board, Washington,D.C. Highway Research Record No. 3.
Gutt, W. and M.A. Smith. 1973. Utilization of By-Product CalciumSulphate. Chemistry and Industry. 63-65.
McClimans, S.A. 1984. Centrifugal Model Evaluation of theConsolidation Behavior of Sand/Phosphatic Clay Mixes. ReportSubmitted in Partial Fulfillment of Requirements for the Degree ofMaster of Engineering, University of Florida.
Townsend, F.C. 1979. Use of Lime in Levee Restoration. U.S. ArmyEngineer Waterways Experiment Station, CE, Vicksburg, Miss.Technical Report GL-79-12.
Townsend, F.C. and R.T. Donaghe. 1976. Investigation of AcceleratedCuring of Soil-Lime and Lime-Flyash-Aggregate Mixtures. U.S. ArmyEngineer Waterways Experiment Station, CE, Vicksburg, Miss.Technical Report S-76-6.
Townsend, F.C., S.A. McClimans, D. Bloomquist, and M.C. McVay. 1986.Reclamation of Phosphatic Waste Clay Ponds by Capping, Vol. 1:Centrifugal Model Evaluation of Reclamation Schemes for PhosphaticWaste Clay Ponds. Florida Institute of Phosphate Research, Bartow,Florida. FIPR Research Report 82-02-030.
Watson, G.V. 1971. The Disposal of Gypsum from Phosphoric AcidPlants. Chemistry and Industry. 78-84.
77
APPENDIX A
INTRODUCTION
This appendix details via step by step and flowcharts the
procedures follow for:
a. pH Tests
b. Bench Tests
c. Accelerated Lime/Clay Tests
and d. Centrifuge Testing
pH TESTING PROCEDURES (Figure A-1)
1. Standardize the pH meter with a buffer of known pH.
2. Prepare lime and gypsum slurries to determine target pH values in
clay mixes. This step calibrates divergences in pH from 12.4 or 2.8
due to pH meter, local water, and quality of lime or gypsum being
used in the test program.
a. Weigh approximately 40 grams of lime and gypsum.
b. Place lime and gypsum in two plastic 200-ml bottles.
c. Add water to bottles to 200-ml mark.
d. Mix thoroughly by shaking bottles every 10 minutes for an hour.
e. Measure the pH of the slurries with the pH meter. This is the
target pH.
3. Determine bulk solids content of clay to be tested.
a. Thoroughly mix the clay to be tested.
b. Weigh three tare to nearest .01 gram.
A-1
STANDARDIZE' pH METER
1 PREPARE LIME &
GYPSUM SLURRIES
L MEASURE TARGET pH OF SLURRIES 4
I
. PLACE CLAY IN
PLASTIC BOTTLES
I c ADD WATER I TO 200 ml MARK
i SHAKE BOTTLES EVERY 1 10 MINUTES FOR 1 HOUR1
I 1
1 MEASURE pH OF MIXTURES 1
1 DETERMINE TARGET PERCENTAGES 1 I +
[PROCEED TO BENCH TESTS 1
Figure A-l: Flowchart of pH Testing Procedures
A-2
c. Place clay in tare and weigh.
d. Place tare cans in oven set at 110 degrees Fahrenheit for 24
hours.
e. Remove tare cans from oven and weigh.
f. Determine solids content from S% = W solids/W total.
4. Prepare clay slurry mixtures with lime and gypsum.
a. Weigh six clay samples and place in plastic bottles.
b. Add lime percentages of 4, 6, 8, 10, 12, and 14 (% of clay
solids), or gypsum to clay solids ratios of 4:1, 6:1, 8:1, 10:l,
12:1, and 14:1.
c. Add water to 200-ml mark.
d. Shake bottles every ten minutes for an hour to mix thoroughly.
5. Measure and record the pH of the mixtures. The percentage of lime
or ratio of gypsum at which the target pH is reached is the
percentage required for stabilization.
6. Repeat procedure for another clay.
BENCH TEST PROCEDURES (Figure A-2)
1. Thoroughly mix bulk sample of waste clay and obtain solids content
as previously outlined. If solids content is between 12% and 14%
continue, otherwise add water and remix.
2. Weigh clay samples into mason jars using tare function on electric
balance. Eighteen jars are required for 1 set of lime or gypsum
bench tests.
3. Calculate weight of solids in jar based on determined solids
content.
A-3
ADD SUGGESTED PERCENTAGES OF LIME AND GYPSUM TO JARS
1 MIX CLAY AND ADDITIVE IN
EACH JAR FOR 2 MINUTES
1 LABEL SAMPLE JARS WITH SUGGESTED INFORMATION
1 ALLOW JARS TO CURE FOR
PRESCRIBED PERIODS
1 DETERMINE SHEAR STRENGTH
OF SAMPLES AT END OF CURING PERIODS
I . PLOT SHEAR STRENGTH
VERSUS CURING TIME
1 , REPEAT pti & BENCH TESTS
FOR ANOTHER CLAY
Figure A-2: Flowchart of Bench Testing Procedures
A-4
4. Add target pH percentage of lime or ratio of gypsum to 6 jars based
on weight of solids, again using the tare function.
5. Add two lower percentages or ratios to remaining 12 jars.
6. Thoroughly mix each sample for approximately 2 minutes with drill
mixer.
7. Label each sample with the following information:
a. where the clay is from
b. the additive used (lime or gypsum)
c. the percentage or ratio added
d. the curing time (7, 14, or 28 days)
e. the test number (two tests for each curing time)
8. Immediately test the vane shear strength of the 7-day samples for a
measure of the initial shear strength of the mixes.
a. Place the jar on the raised platform of the device.
b. Lower the vane down into the clay mixture by turning the top
crank.
C. When vane is inserted to a predetermined depth, turn crank on
the side of the device to rotate the vane and obtain the shear
strength.
9. Remix the 7-day samples immediately after testing O-day vane shear
strengths.
10. Allow jars to cure for prescribed periods, testing each as
previously outlined on the required dates.
11. When all tests are complete, plot shear strength versus curing time.
12. Repeat procedure for another clay.
A-5
ACCELERATED CURING TEST PROCEDURES (FOR LIME ONLY) (Figure A-3)
1. Mix bulk sample of waste clay and determine batch solids content as
previously outlined.
2. Weigh samples of clay into 5 mason jars using tare function.
3. Determine weight of solids in jar from solids content.
4. Add target pH percentage of lime to clay and mix thoroughly with
drill mixer.
5. Place jars in 105 degree Fahrenheit oven.
6. Remove one jar each day for 5 days and
as previously outlined.
7. Plot shear strength versus curing time
time required for adequate strength gain.
CENTRIFUGE TESTING PROCEDURES (Figures A-4
1. Adjust centrifuge for testing.
test the vane shear strength
for five samples to determine
and A-5)
a. Calculate offset acceleration by the following equation:
Ao = (Ra/Rs) x At
where: Ao = offset acceleration
Ra = radius to accelerometer = 37.5 inches
Rs = radius to the center of gravity of the sample
At = test acceleration
b. Place 8 centimeters of water in the four plexiglass containers.
c. Place the plexiglass containers in the aluminum buckets and
secure the buckets to the bucket housings with the pivot bolts.
A-6
I DETERMINE BULK SOLIDS CONTENT OF CLAY I
IADD 12% LIME ~0 CLAYI
Figure A-3: Flowchart of Accelerated Curing Test Procedures
A-7
CALCULATE OFFSET ACCELEFUWON
I PLACE 8 cm OF WATER
IN PLEXIGLASS CONTAINERS
I PLACE CONTAINERS
IN CENTRIFUGE
4 a REMOVE DEBRIS FROM
CENTRIFUGE INTERIOR
1 1 TURN ON POWER/
I +
ACCELERATE WATER SAIYPLES TO OFFSET ACCELERATION
I +
ADJUST OVERSWING ADJUSTMENT BOLTS AS OUTLINED L
I +
[ADJUST ADL AS OUTLINED] I 1
Figure A-4: Flowchart of Centrifuge Preparation Procedures
A-8
/MIX WASTE CLAY
I
/CHECK on LEVEL1
[DETERMINE % SOLIDS], 1
I
ICLEAR INTERIOR
I #IX CLAY WITH LIME
OR GYPSUM 1 SECURE ACCESS DOORS)
I I
ADD CLAY TO PLEXIGLASS f tUtIN POWER ON]
CONTAINERS 1
I
4 ICOMPRESSED AIR ONI
c PLACE CONTAINERS IN I
ALUMINUM BUCKETS
I
[START CENTRIFUGE 1
'PLACE BUCKETS I
INCREASE SPEED TO IN HOUSING OFFSET ACCELERATION
I TAKE PHOTOGRAPHS
,
AT PRESCRIBED TIMES
c 1 END TEST WHEN
INTERFACE STABILIZES I
CLEAN CAMERA CLOSE-UP LENS
I 'INSERT FILM
PACKET
I LOWER CAMERA
TO TEST POSITION
1 ----{STOP CENTRIF=]p
* 1 REMOVE CONTAINERS]
' DETERMINE INTERMEDIATE 1
PERFORM VANE ~ CLAY SOLIDS CONTENT SHEAR TESTS
1
L
I PLOT VERSUS ELAPSED
MODEL TIME 1 CORE SAMPLES 1
I
Figure A-5: Flowchart of Centrifuge Operations
A-9
d. Remove tools and loose debris from inside of centrifuge and
secure access door.
e. Turn on the main power at the circuit breaker.
f. Turn on the compressed air to cool the main spindle housing.
g. Adjust the overswing adjustment bolts in the restraining
brackets across each bucket housing. This is an iterative
procedure in which the water samples are spun-up to the required
offset acceleration. The heights of the water interfaces are
observed and the centrifuge is stopped. Adjustments are made to
the bolts if the interface deviates from the known 8
centimeters. If the water level is too high, the bucket has
under-rotated and the screw should be raised. If the water
level is too low, the bucket has over-rotated and the screw
should be lowered. Once the proper interface level is obtained,
for the given accelerationno further adjustment
level.
h. Adjust Acceleration
is necessary
Divergence Limiter (ADL). This is another
iterative procedure in which the acceleration level and
operating window are adjusted. After each adjustment, the
acceleration is increased and decreased from the given offset
acceleration to determine where the centrifuge shuts off (the
operating window) when the device is turned on. Once the
desired window is obtained no further adjustments are necessary
for the particular offset acceleration. A window of plus or
minus 5 g's was used for this testing.
A-10
2. Prepare samples.
a. Thoroughly mix clay samples from four different sites in four 10
gallon buckets. (Note: solids content of clays at this time
must be greater than desired test solids content.)
b. Determine the solids content of the clays as previously
outlined.
c. Place approximately 1000 grams of clay in a container, weighing
to the nearest .01 gram (WC).
d. Knowing batch solids content (%Sb) and desired test solids
content (%Sd), determine the quantity of water to be added (Ww)
by the equation:
Ww = (WC x %Sb/%Sd) - Wc.
e. Determine quantity of lime or gypsum to be added (%A) by the
following equation:
%A = (Wc + Ww) x %Sd x (%T/100).
where %T = 12 for lime or 200 for gypsum
f. Make the required additions to the clay and m
egg beater.
ix thoroughly with
g. Add clay to plexiglass container to initial model height of 8
centimeters. Actual initial model height should be determined
from the first centrifuge photographs.
h. Repeat procedures for three other clay samples.
A-11
3. Prepare the centrifuge for testing.
a. Check oil level in main spindle housing under centrifuge. Add
oil if necessary.
b. Place plexiglass containers in aluminum buckets.
c. Place aluminum buckets in bucket housings, securing with pivot
bolts.
d. Inspect inside of centrifuge. Remove all tools and loose
debris.
e. Secure access door by inserting locking rod.
f. Start centrifuge and increase acceleration to offset value.
g. Lower camera into position over viewport.
h. Begin taking photographs one minute after the offset
acceleration is reached.
i. Take following photographs in geometrically increasing time
increments to allow logarithmic plots with equally spaced data
(e.g., 1, 2, 4, 8, 16, 32, etc.)
j. If centrifuge is left unattended while operating, ADL should be
engaged. The switch is set such that the indicator light is
off.
k. Test is completed when two sequential photographs of the same
sample indicate no movement of the interface.
4. Analyze centrifuge samples.
a. Remove the plexiglass buckets from the centrifuge and decant the
supernatant.
A-12
b. Obtain the average shear strength of the sample with the vane
shear apparatus, testing the sample in two different locations
(see Figure A-6).
c. Obtain the final solids content with depth of the sample by
making a coring with the modified syringe. The coring should be
sectioned into approximately 1 centimeter thick samples. The
solids content of the samples should be determined as previously
outlined and plotted versus average depth.
A-13