MA1009-SY120713GEOTECHNICAL ENGINEERING STUDY
LAKE AND CHANNEL INVESTIGATION
ANDY BROWN PARK
PARKVIEW BOULEVARD
COPPELL, TEXAS
Presented To;
Teague Nall and Perkins, Inc.
July 2012
PROJECT NO. 131 -'I 2 -i 16
CAV ENGINEERING, INC.
July 5, 2012
Report No, 131 -12 -116
Teague Nall and Perkins, Inc.
1100 Macon Street
Fort Worth, Texas 76102
Attn:: Mr, Kyle Dykes, P.E.
GEOTECHNICAL ENGINEERING STUDY
LAKE AND CHANNEL INVESTIGATION
ANDY BROWN PARK
PARKVIEW BOULEVARD
COPPELL, TEXAS
Dear Mr, Dykes:
7636 Pebble Drive
Fort Worth, Texas 76118
www.cmjengr.com
Submitted here are the results of a geotechnical engineering study for the referenced project. This
study was performed in general accordance with CMJ Proposal 11 -3524 dated April 12, 2012.
Formal authorization to initiate the geotechnical services was provided by Mr. Michael A, Jones,
P.E., President of Teague Nall and Perkins, Inc. on May 2, 2012.
Engineering analyses and recommendations are contained in the text section of the report.. Results
of our field and laboratory services are included in the appendix of the report. We would
appreciate the opportunity to be considered for providing geotechnical engineering services for any
future projects.
We appreciate the opportunity to be of service to Teague Nall and Perkins, Inc.. Please contact us
if you have any questions or if we may be of further service at this time.
Respectfully submitted,
CMJ ENGINEERING, INC.
TEXAS FIRM REGIS IRATION NO. F -9177
James P. Sappington IV, P,E.
Project Engineer
Texas o. 97402
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copies submitted (3) Mr. Kyle Dykes, P.E.; Teague Nall and Perkins, Inc. (mail)
(1) Mr. Kyle Dykes, P E., Teague Nall and Perkins, Inc. (email)
Phone (817) 284 -9400 Fk (817) 5589 -9993 ?ylct:o (817) 589 =9992
TABLE OF CONTENTS
Page
1.0 INTRODUCTION -------------------------------------------------------------------------------------------------- - - - - -1
2.0 FIELD EXPLORATION AND LABORATORY TESTING ------------------------------------------------ - - - - -- 2
3.0 SUBSURFACE CONDITIONS---------------------------------------------------------------------------------- - - - - -3
4.0 FOUNDATION RECOMMENDATIONS --------------------------------------------------------------------- - - - - -- 5
5,0 SLOPE STABILITY ANALYSIS -------------------------------------------------------- ..._. ...---------------------- - - - - -9
6..0 EARTHWORK ----------------------------------------------------------------------------------------------------- - - - -11
7.0 CONSTRUCTION OBSERVATIONS ------------------------------------------------------------------------ - - - -15
8.0 REPORT CLOSURE --------------------------------------------------------------------------------------------- - - - -15
APPENDIX A
Plate
Planof Borings ------------------------------------------------------------------------------------------------------------ - - -A.1
Unified Soil Classification System ---------------------------------------------------------------------------------------- A.2
Key to Classification and Symbols ----------------------------------------------------------------------- — -------------- A..3
Logsof Borings ----------------------------------------------------------------------------------------------- - - - - -- A.4 — A.10
Particle Size Distribution Reports ------------------------------------------------------ ---------- ------ - - - --- A.11 —A.12
Direct Shear Test Reports ------------------------------------------------------------------------------- - - - - -- A..13 — A..18
APPENDIX B
Plate
SlopeStability Analyses -------------------------------------------------------------------------------------------- B.. 1 — B.
1.0 INTRODUCTION
1.1 General
The project site is located within Andy Brown Park East at 260 East Parkway Boulevard in Coppell,
Texas. The project, as currently planned, consists of investigating the existing slope slippage and
erosion areas occurring along the banks of the large lake within the park. New lake edge treatment with
either modular block wall or turf reinforcement is planned, along with stabilization of both the existing
spillway and inlet channel between the large lake and Parkway Boulevard. New walls on the order of 4
feet are anticipated around the southern lake shore. Plate A.1, Plan of Borings, depicts the project
vicinity and location of the exploration borings..
The purpose of this geotechnical engineering study has been to determine the general subsurface
conditions, evaluate the engineering characteristics of the subsurface materials encountered,
analyze slope conditions, and provide recommendations and geotechnical design parameters for
remedial measures to be designed by Teague Nall and Perkins, Inc.
To accomplish its intended purposes, the study has been conducted in the following phases: (1)
drilling sample borings to determine the general subsurface conditions and to obtain samples for
testing; (2) performing laboratory tests on appropriate samples to determine pertinent engineering
properties of the subsurface materials; and (3) performing engineering analyses, using the field
and laboratory data, to develop geotechnical recommendations for the proposed construction..
The design is currently in progress and the locations and /or elevations of the structure could
change.. The recommendations contained in this report are based on data supplied by Teague Nall
and Perkins, Inc. Once the final design is near completion (80- percent to 90- percent stage), it is
recommended that CiUiJ Engineering, inc.. be retained to review those portions of the construction
documents pertaining to the geotechnical recommendations, as a means to determine that our
recommendations have been interpreted as intended.
1.3 Report Format
The text of the report is contained in Sections 1 through 8.. All plates and large tables are
contained in Appendix A. The alpha- numeric plate and table numbers identify the appendix in
Report Igo 131-12-116 CMJ ENGINEERING, INC.
which they appear.. Small tables of less than one page in length may appear in the body of the text
and are numbered according to the section in which they occur..
Units used in the report are based on the English system and may include tons per square foot
(tsf), kips (1 kip = 1,000 pounds), kips per square foot (ksf), pounds per square foot (psf), pounds
per cubic foot (pcf), and pounds per square inch (psi)..
2.1 Field Exploration
Subsurface materials at the project site were explored by seven (7) vertical soil borings.. Borings
B -1 and B -2 were drilled to depths of 40 to 50 feet while the remaining borings were drilled to 20
feet.. The borings were drilled using continuous and intermittent sampling and continuous flight
auger methods at the approximate locations shown on the Plan of Borings, Plate A.1. The boring
logs are included on Plates AA through A..10 and keys to classifications and symbols used on the
logs are provided on Plates A..2 and A..3..
Undisturbed samples of cohesive soils were obtained with nominal 3 -inch diameter thin - walled
(Shelby) tube samplers at the locations shown on the logs of borings. The Shelby tube sampler
consists of a thin - walled steel tube with a sharp cutting edge connected to a head equipped with a
ball valve threaded for rod connection. The tube is pushed into the soil by the hydraulic pulldown
of the drilling rig. The soil specimens were extruded from the tube in the field, logged, tested for
consistency with a hand penetrometer, sealed, and packaged to limit loss of moisture.
The consistency of cohesive soil samples was evaluated in the field using a calibrated hand
penetrometer. In this test a 0..25 -inch diameter piston is pushed into the relatively undisturbed
sample at a constant rate to a depth of 0.25 inch. The results of these tests, in tsf, are tabulated at
respective sample depths on the log.. When the capacity of the penetrometer is exceeded, the
value is tabulated as 4.5+
To evaluate the relative density and consistency of the harder formations, a modified version of the
Texas Cone Penetration test was performed at selected locations.. Texas Department of
Transportation (TXDOT) Test Method Tex -132 -E specifies driving a 3 -inch diameter cone with a
170 -pound hammer freely falling 24 inches. This results in 340 foot - pounds of energy for each
Report No. 131 -12 -118 CMJ ENGINEERING, INC.
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blow.. This method was modified by utilizing a 140 -pound hammer freely falling 30 inches. This
results in 350 foot - pounds of energy for each hammer blow.. In relatively soft materials, the
penetrometer cone is driven 1 foot and the number of blows required for each 6 -inch penetration is
tabulated at respective test depths, as blows per 6 inches on the logs.. In hard materials (rock or
rock - like), the penetrometer cone is driven with the resulting penetrations, in inches, recorded for
the first and second 50 blows, a total of 100 blows.. The penetration for the total 100 blows is
recorded at the respective testing depths on the boring logs.
Ground -water observations during and after completion of the borings are shown on the upper right
of the boring logs.. Upon completion of the borings, the bore holes were backfilled with soil cuttings
and plugged at the surface by hand tamping.
2.2 Laboratory Testing
Laboratory soil tests were performed on selected representative samples recovered from the
borings.. In addition to the classification tests (liquid limits, plastic limits, and gradations), moisture
content, unconfined compressive strength, and unit weight tests were performed.. Results of the
laboratory classification tests, moisture content, unconfined compressive strength, and unit weight
tests conducted for this project are included on the boring logs. Particle size analyses are included
on Plates A..11 and A.12.
Three direct shear tests with associated residual direct shear tests were performed within the
overburden soils. The shear tests were performed in order to obtain strength parameters of the
soils in their existing state. The results of the direct shear tests are presented on Plates A..13
through A..18..
The above laboratory tests were performed in general accordance with applicable ASTIR
procedures, or generally accepted practice.
3.0 SUBSURFACE CONDITIONS
3.1 Soil Conditions
Specific types and depths of subsurface strata encountered at the boring locations are shown on
�
the boring logs in Appendix A. The generalized subsurface stratigraphy encountered in the borings
are discussed below. Note that depths on the borings refer to the depth from the existing grade or
Report No, 131 -12 -116 CMJ ENGINEERING,. INC..
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ground surface present at the time of the investigation, and the boundaries between the various
soil types are approximate.
Fill materials are noted at the surface in Boring B -1 extending to a depth of 7 feet.. The fill consists
of dark brown and reddish brown sandy clays with gravel.. Natural soils encountered consist of
dark brown and brown silty clays and clays overlying brown, light brown and gray sandy clays, silty
sandy clays, and clayey sands.. Calcareous nodules are typically present with few exceptions
throughout the soils encountered, with select zones containing ironstone nodules. Borings B -3
through B -7 were terminated within the sandy clays, silty sandy clays, and clayey sands at 20 feet.
Gravel with sand is noted from 32 to 33 feet in Boring B -2.
The clay soils encountered are stiff to hard in consistency (soil basis), with pocket penetrometer
values of 1..5 to over 4..5 tsf. Soft to firm soils are noted at the 19- to 20 -foot depth in Borings B -3,
B -4, and B -7, with pocket penetrometer readings of 0..5 to 1..25 tsf. The various soils encountered
in the borings had tested Liquid Limits (LL) ranging from 27 to 61 with Plasticity Indices (PI)
ranging from 14 to 42 and are classified as SC, CL and CH by the USCS.. Tested unit weight
values were 90 to 114 pcf and unconfined compressive strengths varied from 2,000 to 4,410 psf.
Dark gray shale is present in Borings B -1 and B -2 at depths of 23'/2 and 33 feet below existing
grade, respectively. The dark gray shale contains limestone seams below 37 feet in Boring B -2
and is soft to moderately hard (sedimentary rock basis) with Texas Cone Penetrometer values of
2% to 6 inches per 100 blows.. Borings B -1 and B -2 were terminated within the dark gray shale at
40 to 50 feet.
3.2 Ground -Water Observations
The borings were drilled using continuous flight augers in order to observe ground -water seepage
during drilling. Ground -water seepage was encountered during drilling in Borings B -1 through B -5
at 10 to 18 feet below existing grade. Ground -water also was observed in these borings at the
completion of drilling operations at 8 to 12 feet.. Borings B -6 and B -7 were dry during drilling and at
completion of drilling operations.. Table 3..2 -1 summarizes water level data. While it is not possible
to accurately predict the magnitude of subsurface water fluctuation that might occur based upon
these short -term observations, it should be recognized that ground -water conditions will vary with
fluctuations in rainfall. Seepage near the observed levels should be anticipated throughout the
year.
Report No. 131 -12 -116
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CMJ ENGINEERING, INC.
TABLE 3.2 -1
Ground -Water Observations
Boring
No.
Seepage During
Drilling (ft.)
Water at
Completion (ft.)
B -1
11
12
B -2
18
12
B -3
10
8
B-4
12'/2
9
B -5
10'/2
11
B -6
Dry
Dry
B -7
Dry
Dry
Ground -water may occur within granular zones or particularly after periods of extended rainfall..
Ground -water encountered with depth may possess moderate hydrostatic pressure, as indicated
by water level readings in Borings B -2 through 134. Fluctuations of the ground -water level can
occur due to seasonal variations in the amount of rainfall; site topography and runoff; hydraulic
conductivity of soil strata; and other factors not evident at the time the borings were performed.
During wet periods of the year, seepage can occur in more permeable strata. The possibility of
ground -water level fluctuations should be considered when developing the design and construction
plans for the project.
Due to the variable subsurface conditions, long -term observations would be necessary to more
accurately evaluate the ground -water level.. Such observations would require installation of
piezometer or observation wells which are sealed to prevent the influence of surface water.
4.1 Expansive Soil Movements
The expansive soils encountered at this site can shrink and swell considerably as the soil moisture
content fluctuates during seasonal wet and dry cycles. Additionally, the site environment is
impacted by grading and drainage, landscaping, ground -water conditions, paving and many other
factors which affect the structure during and after construction.. Therefore, the amount of soil
movement is difficult to determine due to the many unpredictable variables involved.
Estimates of soil movements for this site have been performed using data from the Texas
Department of Transportation (TX -Dot ) procedure TEX- 1 24 -E for estimating Potential Vertical Rise
Report No,, 131 -12 -116 CMJ ENGINEERING, INC.
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(PVR) and using engineering judgment and experience.. Vertical soil movements on the order of
3'/2 to 4'/2 inches or less have been estimated for the soils encountered, as the soils undergo
moisture changes. Below depths of 3 to 4 feet around the lake shore, expansive soil movements
are estimated at 13/4 inches.
4.2 Retaining Structures
4.2.1 General Retaining Wall Considerations
Five geotechnical design criteria must be satisfied in the selection of the type and configuration of
the retaining walls. These criteria are; the wall must have an acceptable factor of safety with
respect to (1) overturning failure, (2) a sliding (translation) failure, (3) a bearing capacity failure, and
(4) a global (deep- seated) slope failure. In addition, (5) the deformation of the wall caused by
deflection from earth pressure, and from settlement or heave of the foundation soils or backfill
soils, must be within tolerable limits during the functional life of the structure.
4.2.2 Foundations
The retaining wall foundations may be founded atop natural soils which will be firm to stiff using
shallow spread or continuous footings. The retaining wall foundations may be designed for an
allowable bearing pressure of 1.5 ksf. A minimum footing dimension of 2 teet is recommenaea.. in
addition, the footing should be placed a minimum of 2 feet below lowest adjacent grade..
Excavation for the footing base will need to incorporate dewatering to keep the excavation free of
excess water. In addition, the water table should be lowered to a depth of 2 feet below the
proposed excavation to prevent excavation base sands from becoming a "quick condition. It
should be noted that retaining wall foundations are typically subjected to non - uniform pressure
across the foundation, and possibly negative pressure (separation of foundation from soil) under a
portion of the foundation, due to the overturning moment induced by the lateral earth pressures.
The allowable foundation pressures given above are for the maximum pressure induced by the
foundation loads, and not the average pressure under the foundation base..
The horizontal bases of the footings will develop resistance to sliding by means of a combination of
friction and adhesion (for cohesive foundation materials). Given the nature of the foundation
materials, an adhesion of 400 psf may be used for earth formed footings. An ultimate friction factor
of 0.3 may be used to calculate sliding resistance of the footings bearing on site soils.. Passive
earth pressure resistance should be neglected..
Report No. 131 -12 -116
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CMJ ENGINEERING, INC.
Foundations for the retaining walls designed in accordance with these recommendations will have
a minimum factor of safety of 3 with respect to a bearing capacity failure, and should experience a
total settlement of 1 inch or less and a differential settlement of Y2 inch or less, after construction..
4.3 Lateral Earth Pressure
4.3.1 Equivalent Fluid Pressures
Lateral earth pressures on retaining walls will depend on a variety of factors, including the type of
soils behind the wall, the condition of the soils, and the drainage conditions behind the wall.
Recommended lateral earth pressures expressed as equivalent fluid pressures, per foot of wall
height, are presented in Table 4.3..1 -1 for a wall with a level backfill behind the top of the wall. The
equivalent fluid pressure for an undrained condition should be used if a drainage system is not
present to remove water trapped in the backfill and behind the wall. Pressures are provided for at-
rest and active earth pressure conditions. In order to allow for an active condition the top of the
wall(s) must deflect on the order of 0..4 percent.
For the select fill or free draining granular backfill these values assume that a "full' wedge of the
material is present behind the wall.. The wedge is defined where the wall backfill limits extend
outward at least 2 feet from the base of the wall and then upward on a 1 H:2V slope. For narrower
backfill widths of granular or select fill soils, the equivalent fluid pressures for the on -site soils
should be used.
TABLE 4.3.1 -1 — Equivalent Fluid Pressures
At -Rest Equivalent
Active Equivalent
Backfill Material
Fluid Pressure (pcf)
Fluid Pressure (pcf)
Drained
Undrained
Drained
Undrained
Excavated on -site clay or clay fill
100
110
85
100
material
Select fill or on -site soils meeting
65
90
50
85
material specifications
Free draining granular backfill
50
90
35
80
material
4.3.2 Wall Backfill Material Requirements
Granular Wall Backfill. All free draining granular wall backfill material should be a crushed stone,
sandigravei mixture, or sand /crushed stone mixture. The material should have less than 3 percent
Report Na. 131 - 12-116 CMJ ENGINEERING, INC..
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passing the No.. 200 sieve and less than 30 percent passing the No. 40 sieve.. The minus No. 40
sieve material should be non - plastic.. Granular wall backfill should not be water jetted during
installation.
Select Fill: All wall select backfill should consist of clayey sand and /or sandy clay material with a
plasticity index of 16 or less, with a liquid limit not exceeding 35. The select fill should be placed in
maximum 8 -inch lifts and compacted to between 95 and 100 percent of Standard Proctor density
(ASTM D 698) within a moisture range of plus to minus 3 percentage points of the optimum
moisture.. Compaction within five feet of the walls should be accomplished using hand compaction
equipment and should be compacted between 90 and 95 percent of the Standard Proctor Density.
On -Site Soil Backfill:: For wall backfill areas with site - excavated materials or similar imported
materials, all oversized fragments larger than four inches in maximum dimension should be
removed from the backfill materials prior to placement.. The backfill should be free of all organic
and deleterious materials, and should be placed in maximum 8 -inch compacted lifts at a minimum
of 95 percent of Standard Proctor density (ASTM D 698) within a moisture range of plus to minus
3 percentage points of optimum moisture. Compaction within five feet of the walls should be
accomplished using hand compaction equipment, and should be between 90 and 95 percent of the
Standard Proctor Density..
4.3.3 Wall Backfill Settlement
Settlement of the wall backfill should be anticipated. Piping and conduits through the fill should be
designed for potential soil loading due to fill settlement.. On -grade slabs, sidewalks, and
pavements over fills also may settle.. Backfill compacted to the density recommended above is
anticipated to settle on the order of 0..2 to 0..5 percent of the fill thickness..
4.3.4 Below -Grade Drainage Requirements
Pervious walls require a geotextile for separation between the backfill and the back face of the
wall. In order to achieve the "drained" condition, the entire backfill material must be free draining,
or the backfill -wall geometry must be such that the backfill will not become saturated from rainfall,
ground water, adjacent water courses, or other sources.. It should be noted that non - expansive
earth fill and general earth fill are not -free draining.
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CMJ ENGINEERING, INC.
5.0 SLOPE STABILITY ANALYSIS
5.1 General Comments
Retaining walls are proposed in various locations to establish an erosion control feature around the
large lake and channel„ An additional focus of this investigation was to determine if there exists an
ample safety factor for construction of retaining walls at this site and also to perform a check of the
existing channel slope between the large lake and Parkway Boulevard. These analyses check
only for global slope failure.. The internal stability, overturning, and sliding failure check should be
performed by the wall designer, based on specific soil and product information..
5.2 Slope Stability Analysis System- Computer Solutions
CMJ Engineering, Inc. selected GSTABL7 with STEDwin to perform the slope stability analyses for
this project.. GSTABL7 with STEDwin is a combination of GSTABL7, an off shoot based on the
original PCSTABL6 -1986 developed at Purdue University.. It is a two - dimensional, limit equilibrium
slope stability program developed and enhanced by Garry H. Gregory, P.E. and Harold W.
VanAller, P.E. CMJ Engineering, Inc. utilized GSTABL7, Version 2.
This slope stability analysis utilizes Modified Bishop, Simplified Janbu, or the Spencer Method of
Slices for analysis.. Circular, random, and sliding block search routines are available for analysis.
Analysis also allows the utilization of anisotropic soil strength parameters which aid in modeling
tension cracks of bedding planes as well as different soil strength in different directions.. The
system overall allows analyses of hundreds of search options and potential failure surfaces and
results in a print out showing the geometry, soil parameter summary, and listing of the ten most
critical failure surfaces analyzed, focusing and highlighting the most critical surface with the lowest
safety factor.
5.3 Analyseslinput Parameters
Numerous analyses were conducted by CMJ Engineering, Inc. to identify the worst -case
methodology to use in analysis as well as the appropriate soil parameters, which affect the slope
stability.. Slope stability analyses were conducted based on geometrics of the proposed walls and
slope cross section information provided by Teague Nail and Perkins, Inc. The assumed soil
properties utilized for analysis are denoted in the table in the upper left on Plates B.1 through 8.3.
The soil type below each profile line is denoted with a number that corresponds to the table in the
upper left. The table lists the assumed unit weight and strength properties for each soil type.. The
Report No. 131 -12 -115 CMJ ENGINEERING, INC.
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method for determining the strength of the slope soils was laboratory soil testing.. The strength
tests consisted of both unconfined compressive tests and direct shear tests.
The soil zones selected for modeling consist of the following::
• Upper Soil Zones with generally stiff clay and silty clay soil conditions, exhibiting relatively
moderate cohesive strength
• Lower Soil Zones — sandy clays and clayey sands, possessing significantly increased
internal angle of friction parameters and reduced cohesion over Upper Soils.
• The depth to dark gray shale was considered too deep to affect the slope analyses
conducted herein, and was therefore not included.
Plates B..1 and B.2 depicts two cross sections taken from the channel section between the large
lake and Parkway Boulevard, with approximate overall heights of 10 to 12 feet and slope angles
varying from 3HAV to 2HAV. These two sections are referred to as Sections 1085 and 1320,
respectively. Topographic information utilized in developing the lake shore cross section on Plate
B..3 was provided from a plan sheet entitled "Central Activity Lake Concept Plan" dated June 2012
by Teague Nall and Perkins, Inc..
Long -term acceptable factors of safety for slope stability are considered to be 1.5 or above. In
other words, the resisting forces to failure are 50 percent greater than the driving forces. A factor
of safety of 1.0 indicates impending failure.
5.4 Slope Stability Results and Comments
Based on field observations of the existing slope and in -situ and laboratory test results, the existing
onsite soils presently possess moderate shear strength (soil basis).. Slope stability analyses
resulted in higher than acceptable factors of safety, on the order of 3.8 and up to 6.5, for in -situ
moisture and soil strength conditions in all three cross sections analyzed.. These analyses imply
the existing slope between the large lake and Parkway Boulevard should remain stable in its pre-
existing orientation, without considering erosion and surface skin sliding effects. In addition, the
planned lake shoreline walls should also be stable with respect to global slope stability The
results of slope stability analyses indicate that deep - seated instability is not a concern in any of
these three cases. Most likely any surficial sloughing or minor slope slippage noted on -site have
been caused to erosion related problems.
Report No 131.17.116 CMJ ENGINEERING, INC.
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Although the analyses indicates that a satisfactory safety factor exists regarding slope stability; it is
imperative that trained field personnel be vigilant to observing anomalies that may occur in the
subsurface conditions during the excavation and placement of the slope protection and /or retaining
walls.. Any anomalous conditions should be brought to the attention of the engineers on this
project for evaluation and potential remediation, as necessary.. Onsite materials are known to vary
in soil type and consistency. Isolated zones of loosely packed or soft materials can exist and their
potential should be carefully observed by trained construction personnel.
6.1 Site Preparation
The subgrade should be firm and able to support the construction equipment without displacement.
Soft or yielding subgrade should be corrected and made stable before construction proceeds. The
subgrade should be proof rolled to detect soft spots, which if exist, should be reworked to provide a
firm and otherwise suitable subgrade.. Proof rolling should be performed using a heavy pneumatic
tired roller, loaded dump truck, or similar piece of equipment. The proof rolling operations should
be observed by the project geotechnical engineer or his /her representative. Prior to fill placement,
the subgrade should be scarified to a minimum depth of 8 inches, its moisture content adjusted,
and recompacted to the moisture and density recommended for fill.
6.2 Placement and Compaction
Fill material should be placed in loose lifts not exceeding 8 inches in uncompacted thickness. The
uncompacted lift thickness should be reduced to 4 inches for structure backfill zones requiring
hand - operated power compactors or small self - propelled compactors. The fill material should be
uniform with respect to material type and moisture content. Clods and chunks of material should
be broken down and the fill material mixed by disking, blading, or plowing, as necessary, so that a
material of uniform moisture and density is obtained for each lift.. Water required for sprinkling to
bring the fill material to the proper moisture content should be applied evenly through each layer..
The on -site soils are suitable for use in site grading. Imported fill material should be clean soil with
a Liquid Limit less than 45 and no rock greater than 4 inches in maximum dimension. The fill
materials should be free of vegetation and debris..
Report No. 131- 12-116
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CMJ ENGINEERING, INC..
The fill material should be compacted to a minimum of 95 percent of the maximum dry density
determined by the Standard Proctor test, ASTM D 698. In conjunction with the compacting
operation, the fill material should be brought to the proper moisture content.. The moisture content
for general earth fill should range from 2 percentage points below optimum to 5 percentage points
above optimum ( -2 to +5). These ranges of moisture contents are given as maximum
recommended ranges.. For some soils and under some conditions, the contractor may have to
maintain a more narrow range of moisture content (within the recommended range) in order to
consistently achieve the recommended density.
Field density tests should be taken as each lift of fill material is placed.. As a guide, one field
density test per lift for each 5,000 square feet of compacted area is recommended. For small
areas or critical areas the frequency of testing may need to be increased to one test per 2,500
square feet. A minimum of 2 tests per lift should be required.. The earthwork operations should be
observed and tested on a continuing basis by an experienced geotechnician working in conjunction
with the project geotechnical engineer.
Each lift should be compacted, tested, and approved before another lift is added. The purpose of
the field density tests is to provide some indication that uniform and adequate compaction is being
obtained. The actual quality of the fill, as compacted, should be the responsibility of the contractor
and satisfactory results from the tests should not be considered as a guarantee of the quality of the
contractor's filling operations.
6.3 General Slope Recommendations
Special site preparation procedures will be imperative to reduce the possibility of slope sliding,
settlement of fill soils, and otherwise undue soil movements.. In addition, where existing slopes
may be re- worked, cuts and fills will be required to properly blend new fill materials to existing
materials. These procedures are outlined below, but generally consist of proper removal of
existing vegetation, proof rolling the site area to receive fill, benching new fill into the existing fill to
prevent a direct slide plane at this interface, and general grading at existing, specific erosion and
drainage areas.
Specific recommended procedures are provided in this report section to emphasize the importance
of these procedures If these procedures are adhered to during the construction phase, the
Report No. 131- 12 -1i& CMJ ENGINEERING, INC.
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potential for slides, undue settlement, and otherwise problematic soil movements are greatly
reduced.. The following specific recommendations are provided,
1.. Grub all areas in which earth fill operations will take place. This requires the proper
removal and disposal of all trees, brush, and vegetation.. It also requires the grubbing
of all roots in excess of 1 inch and disposing of them properly away from the site.
2.. All organic topsoil, trash, debris, or other deleterious materials should be removed
from the fill.. Any rock fragments larger than 6 -inch size should likewise be removed.
3. In areas to receive fill, the surface should be proof rolled to locate any soft or
compressible materials. Should said materials be encountered, they should be
removed and backfilled with acceptable soil materials.
4. The fill materials should be placed from the bottom leading upwards.. The surface
soils should be lightly scarified to allow bonding of new fill to either natural soils or
existing fill. The initial lift of fill should be at least 12 feet wide and placed on a
horizontal plane. As additional fill is placed, the fill should be benched into the natural
soil for every 1 -foot thickness of fill placed. The benches should continue to work
uphill to prevent a continuous plane from occurring at the new fill /old fill /natural soil
interface.
The onsite soil may be used as fill for re- working of slopes; however, if a mass grading deficit
occurs, then offsite soil should be brought in as fill to this site.. Any off site borrow fill should consist
of silty clays, sandy clays, or clayey sands with a Liquid Limit less than 45 and a Plasticity Index
between 4 and 25. These acceptable soils are classified as CL or SC per the Unified Soil
Classification System.. Clean sands, silts, gravels, and highly plastic clays should be discarded. In
addition, fill materials should be placed, pulverized as required, uniformly moistened as required,
compacted to those standards listed above and reiterated in Section 6.2, and each lift tested to
assure proper compaction.. Any fill not meeting specifications should be reworked /recompacted as
necessary.. In addition, light scarification should be performed on the surface of the accepted fill
prior to placing the next lift of fill in order to bond the fill lifts satisfactorily..
6.4 Slope Considerations
We recommend the proposed slopes along the north side of the large lake incorporate 3 horizontal
to 1 vertical slope angles or flatter. These slope angles are generally considered acceptable in the
Dallas /Fort Worth Metroplex area for the given height.. Selected zones of onsite soils may be soft
and creep movement can occur on slopes, particularly along the channel slope between the large
lake and Parkway Boulevard. Creep phenomenon usually manifest as slow to very slow soil
RepoTt No. 131 -12 -115 CNMJ ENGINEERING, INC.
13
movements or skin slides which may require periodic maintenance. Maintenance of shallow creep
movement can be accomplished via the itemized process in Section 6..3. Slopes steeper than 3
horizontal to 1 vertical are specifically not recommended..
6.5 Excavation
The side slopes of excavations through the overburden soils should be made in such a manner to
provide for their stability during construction. Existing structures, pipelines or other facilities, which
are constructed prior to or during the currently proposed construction and which require
excavation, should be protected from loss of end bearing or lateral support..
Temporary construction slopes and /or permanent embankment slopes should be protected from
surface runoff water. Site grading should be designed to allow drainage at planned areas where
erosion protection is provided, instead of allowing surface water to flow down unprotected slopes.
Trench safety recommendations are beyond the scope of this report. The contractor must comply
with all applicable safety regulations concerning trench safety and excavations including, but not
limited to, OSHA regulations.
6.6 Soil Corrosion Potential
Specific testing for soil corrosion potential was not included in the scope of this study. However,
based upon past experience on other projects in the vicinity, the soils at this site may be corrosive..
Standard construction practices for protecting metal pipe and similar facilities in contact with these
soils should be used.
6.7 Erosion and Sediment Control
All disturbed areas should be protected from erosion and sedimentation during construction, and
all permanent slopes and other areas subject to erosion or sedimentation should be provided with
permanent erosion and sediment control facilities.. All applicable ordinances and codes regarding
erosion and sediment control should be followed.
Plates A.11 and A..12 present sieve /hydrometer grain size analyses for typical onsite soils.. The
following table provides grain size for erosion analyses.
Report No., 131- 12-116
14
CMJ ENGINEERING, INC.
Table 6.7 -1 Grain Size Values
7.0 CONSTRUCTION OBSERVATIONS
In any geotechnical investigation, the design recommendations are based on a limited amount of
information about the subsurface conditions„ In the analysis, the geotechnical engineer must
assume the subsurface conditions are similar to the conditions encountered in the borings..
However, quite often during construction, anomalies in the subsurface conditions are revealed..
Therefore, it is recommended that CMJ Engineering, Inc. be retained to observe any additional
earthwork and perform materials evaluation during the construction phase of the project. This
enables the geotechnical engineer to stay abreast of the project and to be readily available to
evaluate unanticipated conditions, to conduct additional tests if required and, when necessary, to
recommend alternative solutions to unanticipated conditions..
It is proposed that construction phase observation and materials observation commence by the
project geotechnical engineer at the outset of the project. Experience has shown that the most
suitable method for procuring these services is for the owner or the owner's design engineers to
contract directly with the project geotechnical engineer.. This results in a clear, direct line of
communication between the owner and the owner's design engineers and the geotechnical
engineer..
The locations and elevations of the borings should be considered accurate only to the degree
implied by the methods used in their determination„ The boring logs shown in this report contain
information related to the types of soil encountered at specific locations and times and show lines
delineating the interface between these materials. The logs also contain our field representative's
interpretation of conditions that are believed to exist in those depth intervals between the actual
samples taken. Therefore, these boring logs contain both factual and interpretive information..
Laboratory soil classification tests were also performed on samples from selected depths in the
borings. The results of these tests, along with visuai- manual procedures, were used to generally
Report No. 131 -12 -113 CM! ENGINEERING, INC.
15
Grain Size (mm)
Boring No.
Depth (Ft.) D5o
D95
B -3
2 -3 0.0030
0.2840
B -4
1 -2 0.0034
0.2820
7.0 CONSTRUCTION OBSERVATIONS
In any geotechnical investigation, the design recommendations are based on a limited amount of
information about the subsurface conditions„ In the analysis, the geotechnical engineer must
assume the subsurface conditions are similar to the conditions encountered in the borings..
However, quite often during construction, anomalies in the subsurface conditions are revealed..
Therefore, it is recommended that CMJ Engineering, Inc. be retained to observe any additional
earthwork and perform materials evaluation during the construction phase of the project. This
enables the geotechnical engineer to stay abreast of the project and to be readily available to
evaluate unanticipated conditions, to conduct additional tests if required and, when necessary, to
recommend alternative solutions to unanticipated conditions..
It is proposed that construction phase observation and materials observation commence by the
project geotechnical engineer at the outset of the project. Experience has shown that the most
suitable method for procuring these services is for the owner or the owner's design engineers to
contract directly with the project geotechnical engineer.. This results in a clear, direct line of
communication between the owner and the owner's design engineers and the geotechnical
engineer..
The locations and elevations of the borings should be considered accurate only to the degree
implied by the methods used in their determination„ The boring logs shown in this report contain
information related to the types of soil encountered at specific locations and times and show lines
delineating the interface between these materials. The logs also contain our field representative's
interpretation of conditions that are believed to exist in those depth intervals between the actual
samples taken. Therefore, these boring logs contain both factual and interpretive information..
Laboratory soil classification tests were also performed on samples from selected depths in the
borings. The results of these tests, along with visuai- manual procedures, were used to generally
Report No. 131 -12 -113 CM! ENGINEERING, INC.
15
classify each stratum.. Therefore, it should be understood that the classification data on the logs of
borings represent visual estimates of classifications for those portions of each stratum on which the
full range of laboratory soil classification tests were not performed.. It is not implied that these logs
are representative of subsurface conditions at other locations and times..
With regard to ground -water conditions, this report presents data on ground -water levels as they
were observed during the course of the field work.. In particular, water level readings have been
made in the borings at the times and under conditions stated in the text of the report and on the
boring logs.. It should be noted that fluctuations in the level of the ground -water table can occur with
passage of time due to variations in rainfall, temperature and other factors. Also, this report does
not include quantitative information on rates of flow of ground water into excavations, on pumping
capacities necessary to dewater the excavations, or on methods of dewatering excavations.
Unanticipated soil conditions at a construction site are commonly encountered and cannot be fully
predicted by mere soil samples, test borings or test pits. Such unexpected conditions frequently
require that additional expenditures be made by the owner to attain a properly designed and
constructed project. Therefore, provision for some contingency fund is recommended to
accommodate such potential extra cost.
The analyses, conclusions and recommendations contained in this report are based on site
conditions as they existed at the time of our field investigation and further on the assumption that
the exploratory borings are representative of the subsurface conditions throughout the site; that is,
the subsurface conditions everywhere are not significantly different from those disclosed by the
borings at the time they were completed.. If, during construction, different subsurface conditions
from those encountered in our borings are observed, or appear to be present in excavations, we
must be advised promptly so that we can review these conditions and reconsider our
recommendations where necessary.. If there is a substantial lapse of time between submission of
this report and the start of the work at the site, if conditions have changed due either to natural
causes or to construction operations at or adjacent to the site, or if structure locations, structural
loads or finish grades are changed, we urge that we be promptly informed and retained to review
our report to determine the applicability of the conclusions and recommendations, considering the
changed conditions and /or time lapse..
Report No. 131 -12 -116 CMJ ENcLNEER1NC,1NC.
16
Further, it is urged that CMJ Engineering, Inc.. be retained to review those portions of the plans and
specifications for this particular project that pertain to earthwork as a means to determine whether
the plans and specifications are consistent with the recommendations contained in this report.. In
addition, we are available to observe construction, particularly the compaction of structural fill, or
backfili as recommended in the report, and such other field observations as might be necessary.
The scope of our services did not include any environmental assessment or investigation for the
presence or absence of wetlands or hazardous or toxic materials in the soil, surface water, ground
water or air, on or below or around the site. The scope of services also did not include any
assessment of the site for suitability for the proposed construction or use, related to items or
conditions other than those specifically addressed in this report..
This report has been prepared for use in developing an overall design concept. Paragraphs,
statements, test results, boring logs, diagrams, etc, should not be taken out of context, nor utilized
without a knowledge and awareness of their intent within the overall concept of this report. The
reproduction of this report, or any part thereof, supplied to persons other than the owner, should
indicate that this study was made for design purposes only and that verification of the subsurface
conditions for purposes of determining difficulty of excavation, trafficability, etc. are responsibilities
of the contractor.
This report has been prepared for the exclusive use of the Teague Nall and Perkins, Inc. for
specific application to design of this project.. The only warranty made by us in connection with the
services provided is that we have used that degree of care and skill ordinarily exercised under
similar conditions by reputable members of our profession practicing in the same or similar locality..
No other warranty, expressed or implied, is made or intended.
Report Flo. 131-12-116
17
CMJ ENGINEERING, INC.
U
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Typical Names
Laboratory Classification Criteria
Well- graded gravels, gravel-
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sand mixtures, little or no
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C„= - - - -- greater than 4: Cc= -------- - - - - -- between 1 and 3
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below "A" line or P i.
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omixtures
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greater than 4
plotting in hatched zone
Z
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Poorly graded sands;
a)
C
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gravelly sands, little or no
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Not meeting all gradation requirements for SW
4 L= >
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sands, rock flour, silty or
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clayey fine sands, or clayey
silts with slight plasticity
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clays, sandy clays, silty clays,
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Plasticity Chart
a,
soils
110
I
jUNIFiED SOIL CLASSIFICATION SYSTEM PLATE A. �
SOIL OR ROCK TYPES
®®
GRAVEL
LEAN CLAY
LIMESTONE
• •
SAND
• •
SANDY
—
SHALE
• 0%
• •
SILT
SILTY
SANDSTONE
CLAYEY
HIGHLY
PLASTIC CLAY
CONGLOMERATE
Shelby
Tube
Auger
Split
Spoon
Rock
Core
Cone
Pen
No
Recovery
TERMS DESCRIBING CONSISTENCY, CONDITION, AND STRUCTURE OF SOIL
Fine Grained Soils (More than 50% Passing No 200 Sieve)
Descriptive Item
Penetrometer Reading, (tsf)
Soft
0.0 to 1.0
Firm
1.0 to 1.5
Stiff
1,5 to 10
Very Stiff
3.0 to 4.5
Hard
4.5+
Coarse Grained Soils (More than 50% Retained on No 200 Sieve)
Penetration Resistance
Descriptive Item Relative Density
(blows /foot)
0 to 4
Very Loose 0 to 20%
4 to 10
Loose 20 to 40%
10 to 30
Medium Dense 40 to 70%
30 to 50
Dense 70 to 90%
Over 50
Very Dense 90 to 100%
Soil Structure
Calcareous
Contains appreciable deposits of calcium carbonate; generally nodular
Slickensided
Having inclined planes of weakness that are slick and glossy in appearance
Laminated
Composed of thin layers of varying color or texture
Fissured
Containing cracks, sometimes filled with fine sand or silt
Interbedded
Composed of alternate layers of different soil types, usually in approximately equal proportions
TERMS DESCRIBING PHYSICAL PROPERTIES OF ROCK
Hardness and Degree of Cementation
Very Soft or Plastic
Can be remolded in hand; corresponds in consistency up to very stiff in soils
Soft
Can be scratched with fingernail
Moderately Hard
Can be scratched easily with knife; cannot be scratched with fingernail
Hard
Difficult to scratch with knife
Very Hard
Cannot be scratched with knife
Poorly Cemented or Friable
Easily crumbled
Cemented
Bound together by chemically precipitated material; Quartz, calcite, dolomite, siderite,
and iron oxide are common cementing materials and iron oxide are common cementing materials.
Degree of Weathering
Unweathered
Rock in its natural state before being exposed to atmospheric agents
Slightly Weathered
Noted predominantly by color change with no disintegrated zones
Weathered
Complete color change with zones of slightly decomposed rock j
Extremely Weathered
Complete color change with consistency, texture, and general appearance approaching soil II
Ia r= TO `I ACCIII'ATInki Akin SVRi PALC PLATE A.
IKE V9e rA ION r14—
Project No
131 -12 -116
Boring No
B -1
Project Lake and Channel Investigation - Andy Brown Park
Parkview Boulevard - Coppell, Texas
Location
See Plate A.1
Water Observations
Seepage at 11' during drilling; water at 10' and cave -in at 17' at
Completion
Completion
Depth 40.0'
Completion
Date 5 -21 -12
LL
fl
o
T
N
Qpj
m-o
Surface Elevation
Type
B -53, w/ CFA
o
U
w
o
CI
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Z
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m.�
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_
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a� ti rn
00E5
c o 0
Stratum Description
5
1
15
2
25
30
35
SANDY CLAY, dark brown, stiff to very stiff (FILL)
-w/ reddish brown, gravel, below 2'
I
225
16
3.25
15
2.25
13
114
2000
2,5
14
3.25
15
CLAY / SILTY CLAY, dark brown, stiff
2.0
52
25
27
31
90
1.5
27
95
2190
SAND / CLAYEY SAND, brown and gray
15
26
SANDY CLAY, brown and gray
26
—_—
—
--
=-
—
— —_
SHALE, dark gray, moderately hard
00/2.25'
10012.5"
LOG OF BORING NO -1 'LATE A.4 I
Project No
131 -12 -116
Boring No
B -2
Project Lake and Channel Investigation -Andy Brown Park ivi� LtVVII���I ttw ltV�
Parkview Boulevard - Coppell, Texas
Location
See Plate A.1
Water Observations
Seepage at 18' during drilling; water at 12' at completion
Completion
Depth 50.0'
Completion
Date 5 -18 -12
LL
o
9
E
U
a
Surface Elevation
Type
CME -55, w/ CFA
U
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d
rn
LL
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0 0
U
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r6
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_
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o
= N `�
o 0.a
c)EO
c o o
Stratum Description
5
1
15
20
25
3
35
4
5
CLAY / SILTY CLAY, dark brown, w/ calcareous
nodules, hard
4.5+
15
4.5+
16
4.5+
14
4.5+
13
CLAY / SILTY SANDY CLAY, brown to dark brown,
w/ calcareous nodules, very stiff to hard
-stiff to very stiff below 9'
3.75
15
4.5+
61
19
42
23
102
3.25
24
2.5
24
102
4050
CLAYEY SAND, light brown and gray
1.5
27
13
14
16
114
1.25
47
17
0.25
23
GRAVEL, w/ sand
_—
— _
SHALE, dark gray, soft to moderately hard
-w/ limestone seams below 37'
----------------- - - - -
100/5.5"
--
_
— —_
--
100/4"
00/4.25'
LOG OF BORING NO —2 PLATE Ao5 I
Project No
131 -12 -116
Boring No
B -3
Project Lake and Channel Investigation - Andy Brown Park
Parkview Boulevard - Coppell, Texas
Location
See Plate A.1
Water Observations
Seepage at 10' during drilling; water at Vat completion
Completion
Depth 20.0'
Completion
1 Date 5 -18 -12
LL
Q-
o
T
a
E
Surface Elevation
Type
CME -55, w/ CFA
o
U
W
�
o
C�
Q'
_0
�= LL
O N V!
mdh
0
0
Z
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7 ±:
O' >=
JJ
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z=
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C-0
c ti
N N a
U 7
C O O
Stratum Description
5
10
15
20
r
i
)
1
CLAY / SILTY CLAY, dark brown, w/ calcareous
nodules, very stiff to hard
-w/ ironstone nodules below 4'
I
45+
12
45+
13
425
51
20
31
20
3,25
21
3.5
20
111
4410
SANDY CLAY, light brown and gray, w/ calcareous
nodules and ironstone nodules, stiff
soft below 19'
-----------------------
1 5
21
2.0 1
55
30
13
17
15
2.75
16
0.5
19
LOG OF BORING NO B -3 PLATE An6
C-'MT ENGINEERING INC
Project No
N o
Project Lake and Channel Investigation - Andy Brown Park
131 -12 -116
�Boriing
B -4
Parkview Boulevard - Coppell, Texas
Location
Water Observations
See Plate A.1
Seepage at 12.5' during drilling; water at 9' at completion
Completion
Completion
Depth 20 W '
Date 5 -18 -12
Surface Elevation
Type
CME -55, wl CFA
_
LL
O
E
N
-a
o
o
N
0
_
�LL
O LL
a
E
stratum Description
o
Z
w
oL
W yU)
0
0c� U
0
2i C
>
X N
N C
� U
o U Q
O
CJ
O N�
COdH
2
dU
JJ
dJ
0-.E
0 0
220
DJ
C 00
CLAY / SILTY CLAY, dark brown, w/ calcareous
4.5+
15
4.5+
51
20
31
13
nodules, hard
4.5+
12
-stiff to very stiff below 3'
225
25
100
3380
3.0
24
5
SANDY CLAY, light brown and gray, w/ calcareous
325
19
nodules and ironstone nodules, stiff to very stiff
275
19
113
3230
10
2.25
66
34
13
21
18
15
firm below 19'
1 25
21
2
-----------------------
N
M
n
I
�
I
N
M
LL
° 1 ,,� r,C Qnaitlir Kin -� PLATE A
Project No.
Boring No
L1V1� G1VViiVGGl i1v� i v`
Project Lake and Channel Investigation - Andy Brown Park
131 -12 -116
B -5
Parkview Boulevard - Coppell, Texas
Location
Water Observations
See Plate A.1
Seepage at 10.5' during drilling; water at 11' at completion
Completion
Completion
Depth 20.0'
Date 5 -18 -12
Surface Elevation
Type
CME -55, w/ CFA
Stratum Description
LL
CL
o
O
.fl
T
a
N
o
w
W
o
C1
W
'6
v�D LL
-2 a)
mo.F—
0
O
N
Z
��
a)
m
CL U)
o
rr
o_
iaE
a_,
x
as-6
a5
°
m
o
20
_
LL
:0!-- V
�
_J
c LL
y Cn Cr
v
o ac
cob
:DUO-
CLAY / SILTY CLAY, dark brown, w/ calcareous
45+
10
4.5+
13
nodules, hard
-stiff to very stiff below 2'
225
25
101
3630
2.25
27
2.0
27
5
2.25
58
17
41
26
325 1
1
22
10
SANDY CLAY, light brown and gray, w/ calcareous
nodules and ironstone nodules, stiff
-w/ brown below 13'
2.75
19
15
1.5
20
2
— — — — — — — — — — — — — — — — — — — — — — —
i
J
I
I
i
I
LOG OF BORING No -5 PLATE A•8
- .TT -
Project No
Boring No.
Project Lake and Channel Investigation - Andy Brown Park
131 -12 -116
B -6
Parkview Boulevard - Coppell, Texas
Location
Water Observations
See Plate A.1
Dry during drilling; dry at completion
Completion
Completion
Depth 20.0'
Date 6 -22 -12
Surface Elevation
Type
B -47, w/ CFA
_
L
N
fl
o
Stratum Description
CU
U
�u>
3a�W
X�c
E �
W
C3
Y
o
mo_F-
m. a)
(L
f
m E
m
:EU
»
c o
o
DUO -
SILTY CLAY, dark brown, w/ calcareous nodules,
4.5+
15
45+
13
hard
-stiff below 2'
1 75
23
2 5
24
103
2950
2.5
48
19
29
22
5
SILTY SANDY CLAY, light brown and gray, w/
375
18
ironstone nodules, stiff to very stiff
1.75
17
1
1.75
18
15
1.5
16
20
— — — — — — — — — — — — — — — — — — — — — — —
V
n
I
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y
M
0
Z
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0
co
0I PLATE
I (�G OF BORING NO B-6
n -- - - __
,-'A TT
Project No
No .
Project Lake and Channel Investigation - Andy Brown Park
131 -12 -116
�Boring
-%
Parkview Boulevard - Coppell, Texas
Location
Water Observations
See Plate A.1
Dry during drilling; dry at completion
Completion
Completion
Depth 20.0'
1 Date 5 -22 -12
Surface Elevation
Type
B-47, wl CFA
ii
w
o
s
E
a
°.
0
04
0
�ti
c ii
g
nto
Q
E
`)
Stratum Description
o
a
�a)
Z
o�
_��
M
o
U
3�u
N>
�.-
N.=
axi
n c
- ui
'E
v E
w
CJ
W
o ac) C/5
mdH
m.Lp
(L W
a-E
JJ
_� E
dJ
m�
d S
o o
20
Q
Z) -3
c o o
Z) Ud
SILTY CLAY / CLAY, dark brown, w/ calcareous
4.5+
17
45+
18
nodules, hard
-firm to stiff below 2'
1-75
26
100
2170
1 5
28
1.25
29
5
25
22
SILTY SANDY CLAY, light brown and gray, w/
2.0
39
13
26
17
10—
calcareous nodules and ironstone nodules, firm to
stiff
2.0
16
15
1.25
18
20
-----------------------
n
J
I
a
�I
II
O
Z
0
O
al
I nr- np RnRINr. Nn 13- PLATE .�
J
100
90
80
70
0� 60
w
Z
LL
Z 50
W
U
0Y
w 40
CL
30
20
10
0
Particle Size Distribution Report
GRAIN SIZE - mm.
%+3" % Gravel % Sand %m Fines
CoarseFine Coarse Medium -- Fine Silt Clay
0.0 0.0 0.0 0.4 0.6 17.5 26.4 1 55.1
0 51 20 0.1126 0.0065 0.0030
Material Description USCS i AASHTO
o Silty Clay, dark brown w/ calcareous nodules
Project No. 131 -12 -116 Client: Teague Nall and Perkins, Inc.
Project: Andy Brown Park - Lake & Channel
110 Sample Number: B -3 2 -3
CIVIJ ENGINEERING, INC.
Fort Worth, Texas
Remarks:
4 ,, 0,.. AA11 iii ,iAT� A 11
I esied BY: IVIK' �12t;%'ftCU say. svire ,
100
90
80
70
W
60
Z
LL
Z 50
W
U
ry
W 4C
a
3(
2C
1C
Particle Size Distribution Report
GRAIN SIZE - mm
% Gravel % Sand % Fines
Coarse I Fine Coarse, Medium Fine Silt Clay
0.0
0'.00.0 0.2 0.4 15.5 29.9 54.0
D D D D C
LL PL D
51 20 0.0796 0.0082 0.0034
Material Description SCS AASHTO
Silty Clay, dark brown w/ calcareous nodules
Project No. 131 -12 -116 Client: Teague Nall and Perkins, Inc. RemarKs:
Project: Andy Brown Park - Lake & Channel
o Sample Number: B -4 1 -2
Fort -
Tested By: iv1K PLATE A,.12
-0
-0
c
-0
0
0
aD
0
U
N
1
1500
1250
1000
CL
a)
750
CU
a)
U) 500
250
Strain, %
I I! I I I I I i I I —14--1 I
� �I
]II 25 5 75 10
Strain, %
Sample Type: Shelby Tube
Description: Silty Clay, dark brown
LL.= 52 PL= 25 Pl= 27
Assumed Specific Gravity= 2..7
Remarks:
1
3
2
6000
4000
r5
CL
m
L6
LL
2000
0
Sample No..
3 Water Content, %
2 Dry Density, pcf
Saturation, %
c: Void Ratio
1 Diameter, in.
Height, in.
Water Content, %
Dry Density, pcf
ISaturation, %
Q Void Ratio
Diameter, in..
Height, in.
Normal Stress, psf
Fail.. Stress, psf
Strain, %
Ult. Stress, psf
Strain, %
Strain rate, in.. /min.
Normal Stress, psf
1
Results
3
30,.6
30,.6
30.6
85.3
—
-
—
C, psf
797
0,9752
0,.8773
0„8854
2„50
2,.50
2.50
—
0.75
�, deg
12.0
313
—
853
—
Tan(o)
0.21
963
87.0
0„9752
0..8773
0,.8854
2.50
2..50
2.50
0.75
0.75
0.75
1000
2000
3000
973
1297
1399
4.0
4 „0
2.8
I
L
- -, -- . -
I
I
�I
7
01
2000 4000 6000
Sample No..
3 Water Content, %
2 Dry Density, pcf
Saturation, %
c: Void Ratio
1 Diameter, in.
Height, in.
Water Content, %
Dry Density, pcf
ISaturation, %
Q Void Ratio
Diameter, in..
Height, in.
Normal Stress, psf
Fail.. Stress, psf
Strain, %
Ult. Stress, psf
Strain, %
Strain rate, in.. /min.
Normal Stress, psf
1
2
3
30,.6
30,.6
30.6
85.3
89.8
89.4
84,.7
94.2
93.3
0,9752
0,.8773
0„8854
2„50
2,.50
2.50
0.75
0.75
0.75
34..4
313
28..5
853
89„8
89.4
952
963
87.0
0„9752
0..8773
0,.8854
2.50
2..50
2.50
0.75
0.75
0.75
1000
2000
3000
973
1297
1399
4.0
4 „0
2.8
0,69 N/A N/A
Client: Teague Nall and Perkins, Inc.
Project: Andy Brown Park - Lake & Channel
Sample Number: B -1 Depth: 7 -8
Proj. No.: 131 -12 -116 Date: 6/12/2012
DIRECT SHEAR TEST REPORT
Tested Bv: MK Checked Bv: MK ICI A.TF A 1
-0
-0
c
c -0
0
.7�
E
L
0
M
n
_U
a�
0
1500
1250
1000
n
m
750
c�
(D
U) 500
250
0
Strain, %
1
2
3
6000
4000
a
''L^^
VJ
M
LL
2000
0
Sample No..
Water Content, %
3 Dry Density, pcf
Saturation, %
2 Void Ratio
Diameter, in..
Height, in.
I Water Content, %
Dry Density, pcf
Saturation, %
Q Void Ratio
Diameter, in.
Heiaht. in.
Normal Stress, psf
Fail. Stress, psf
0 5 10 15 20 Strain, %
Strain, % Ult. Stress, psf
Strain, %
Strain rate, in.. /min..
Sample Type: Shelby Tube
Description: Silty Clay, dark brown
LL= 52 PL= 25 PI= 27
Assumed Specific Gravity= 2.7
I Remarks: Residual
■
Normal Stress, psf
1
2
3
30.6
30„6
30.6
85.3
89„8
89.4
84.7
942
93.3
0,9752
0,.8773
0..8854
2,.50
2.50
2.50
0.75
0.75
0.75
34..4
31.3
28..5
85..3
89„8
89.4
9.5.2
96.3
87.0
0,9752
0.8773
0.8854
2,.50
2.50
2..50
0.75
0.75
0.75
1000
2000
3000
709
1044
1196
9.6
10A
8,.0
N/A N/A N/A
Client: Teague Nall and Perkins, Inc.
Project: Andy Brown Park - Lake & Channel
Sample Number: B -1 Depth: 7 -8
Proj. No.: 131 -12 -116 Date: 6/12/2012
DIRECT SHEAR TEST REPORT
U M J i E rilN , 1 U.
Tested Bv: MK Checked Bv: MK Pt ATF A 1A
C
C
0
.6
E
L
0
U_
a)
6000
5000
4000
CL
0
v
3000
M
a>
U) 2000
1000
Strain, %
Strain, %
Sample 'Type: Shelby Tube
Description: Silty Sandy Clay, dark brown w/
calcareous nodules
LL= 61 PL= 19 Pl= 42
Assumed Specific Gravity= 2.8
Remarks:
2
1
3
6000
4000
C
Q
U)
U)
Vl
CU
LL
2000
0
Sample No
Water Content, %
Dry Density, pcf
Saturation, %
` Void Ratio
Diameter, in.
Height, in.
3 Water Content, %
2 Dry Density, pcf
1 )
a) Saturation, %
Q Void Ratio
Diameter, in
Height, in.
Normal Stress, psf
Fail. Stress, psf
Strain, %
Ult Stress, psf
Strain, %
Strain rate, in. /min.
Normal Stress, psf
1
2
3
22.7
22.7
22„7
101.8
102.1
101..4
88.7
89.5
88..0
0.7177
0„7119
0.7240
2.50
2.50
2.,50
0.75
0.75
0.75
25..2
25.,3
24„8
101..8
102,1
101.4
98„4
99„3
95.8
0.7177
0.7119
0.7240
2.50
2.50
2.50
0.75
0.75
0.75
1000
2000
3000
2351
2666
3061
32
8.,8
3.6
N/A N/A N/A
Client: Teague Nall and Perkins, Inc.
Project: Andy Brown Park - Lake & Channel
Sample Number: B-2 Depth: 7 -8
Proj. No.: 131 -12 -116 Date: 6/13/2012
DIRECT SHEAR TEST REPORT
CMJ ENGINEERING, INC.
Tested By: MK — ____ -- Checked By: MK
C
0
E
`o
ro
0
ca
U_
3000
2500
2000
a
M
fn
v
1500
m
m
(n 1000
500
Strain, %
1i
T -T
'
-1.
22.7
-
-
-- - -
-�I
1696
89.5
- - -
' It
0..7177
-�, deg
- 19.5
2.50
2.50
2.50
TanO
0.35
-
--
253
24..8
4-
102..1
74-
98.5
99.3
95.8
0••7177
-r
0••7240
2.50
2.50
2.50
_4
0.75
0.75
1000
2000
3000
2068
2372
2777
11.2
17.6
12.0
N/A
N/A
N/A
:
0 5
10� 15� 20
Strain, %
Sample Type: Shelby Tube
Description: Silty Sandy Clay, dark brown w/
calcareous nodules
LL= 61 PL= 19 Pl= 42
Assumed Specific Gravity= 2.8
Remarks: Residual
Tested Sy: MK
1
3
2
6000
4000
a
Cn
U)
P
U)
CIO
LL
2000
0
Sample No,
3
Water Content, %
Dry Density, pcf
2
_ Saturation, %
1 E Void Ratio
Diameter, in
Hei ht, in.
Water Content, %
w. Dry Density, pcf
Saturation, %
Q Void Ratio
Diameter, in..
Height, in.
Normal Stress, psf
Fail , Stress, psf
Strain, %
Ult. Stress, psf
Strain, %
Strain rate, in /min
i
Normal Stress, psf
1
Results
3
22••7
22.7
22.7
-
-
C, psf
1696
89.5
- - -
' It
0..7177
-�, deg
- 19.5
2.50
2.50
2.50
TanO
0.35
-
--
253
24..8
101.8
102..1
101.4
98.5
99.3
95.8
0••7177
0•,7119
0••7240
2.50
2.50
2.50
_ 0.75
0.75
0.75
1000
2000
3000
2068
2372
2777
11.2
17.6
12.0
N/A
N/A
N/A
Sample No,
3
Water Content, %
Dry Density, pcf
2
_ Saturation, %
1 E Void Ratio
Diameter, in
Hei ht, in.
Water Content, %
w. Dry Density, pcf
Saturation, %
Q Void Ratio
Diameter, in..
Height, in.
Normal Stress, psf
Fail , Stress, psf
Strain, %
Ult. Stress, psf
Strain, %
Strain rate, in /min
i
Normal Stress, psf
1
2
3
22••7
22.7
22.7
101 ..8
102 1
101.4
88.7
89.5
88..0
0..7177
0.7119
0.7240
2.50
2.50
2.50
0.75
0.75
0.75
25.3
253
24..8
101.8
102..1
101.4
98.5
99.3
95.8
0••7177
0•,7119
0••7240
2.50
2.50
2.50
_ 0.75
0.75
0.75
1000
2000
3000
2068
2372
2777
11.2
17.6
12.0
N/A
N/A
N/A
Client: Teague Nall and Perkins, Inc.
Project: Andy Brown Park - Lake & Channel
Sample Number: B -2 Depth: 7 -8
Proj. No.: 131 -12 -116 Date: 6/13/2012
DIRECT SHEAR TEST REPORT
CMJ NGINF IN r !N "-
Checked By: MK
X18 A TR_ A A !�
-0
.S
-0
0
.1�
E
0
a�
U
N 0
3000
2500
2000
CL
1500
m
a�
U) 1000
500
Strain, %
Strain, %
Sample Type: Shelby Tube
Description: Clayey Sand, gray and light brown
LL= 27 PL= 13 P1= 14
,assumed Specific Gravity= 2.7
Remarks.
Tested By: MK
7
2
3
,.o1�
4000
U)
CL
vi
aD
M
(6
LL
2000
0
Results
3
-
16..3
-
-
709
113.7
90.6
-- - -
91,3
�, deg --
23.3
0.4822
2.50
2.50
2.,50
TanO
0.43
0.75
16.7
15.1
-'
113.4
113.8
1137
92.6
85.1
83.0
0„4859
0„4807
0.4822
2.50
2.50
�
0.75
0.75
0.75
y
2000
_
1135
1581
1997
4.8
6.4
20,0
G
F
N/A
4
=
I __'I
r
!r _
i
j
-
r
0 5
10
15
20
Strain, %
Sample Type: Shelby Tube
Description: Clayey Sand, gray and light brown
LL= 27 PL= 13 P1= 14
,assumed Specific Gravity= 2.7
Remarks.
Tested By: MK
7
2
3
,.o1�
4000
U)
CL
vi
aD
M
(6
LL
2000
0
n
Sample No
Water Content, %
Dry Density, pcf
Saturation, %
3 Void Ratio
Diameter, in
2 Height, in.
Water Content, %
Dry Density, pcf
1 � Saturation, %
Q Void Ratio
Diameter, in
Height, in.
Normal Stress, psf
Fail Stress, psf
Strain, %
Ult. Stress, psf
Strain, %
Strain rate, in./min.
Normal Stress, psf
1
Results
3
-
16..3
-
C, psf
709
113.7
90.6
-- - -
91,3
�, deg --
23.3
0.4822
2.50
2.50
2.,50
TanO
0.43
0.75
16.7
15.1
-'
113.4
113.8
1137
92.6
85.1
83.0
0„4859
0„4807
0.4822
2.50
2.50
�
0.75
0.75
0.75
y
2000
3000
1135
1581
1997
4.8
6.4
n
Sample No
Water Content, %
Dry Density, pcf
Saturation, %
3 Void Ratio
Diameter, in
2 Height, in.
Water Content, %
Dry Density, pcf
1 � Saturation, %
Q Void Ratio
Diameter, in
Height, in.
Normal Stress, psf
Fail Stress, psf
Strain, %
Ult. Stress, psf
Strain, %
Strain rate, in./min.
Normal Stress, psf
1
2
3
163
16..3
16.3
113.4
113.8
113.7
90.6
91.6
91,3
0.4859
0.4807
0.4822
2.50
2.50
2.,50
0.75
0.75
0.75
16.7
15.1
14.8
113.4
113.8
1137
92.6
85.1
83.0
0„4859
0„4807
0.4822
2.50
2.50
2.50
0.75
0.75
0.75
1000
2000
3000
1135
1581
1997
4.8
6.4
20,0
N/A
N/A
N/A
Client: Teague Nall and Perkins, Inc.
Project: Andy Brown Park - Lake & Channel
Sample Number: B -2 Depth: 19 -20
Proj. No.: 131 -12 -116 Date: 6/13/2012
DIRECT SHEAR TEST REPORT
MJ ENGINE RIlV r UNC.
Checked By: MK
PLATE A.17
-0
C
-0.
0
.5
E
0
i
m
_0
m
0
0
3000
2500
N 2000
CL
0
U)
v
1500
m
0
U) 1000
500
Strain, %
5 10 151 20
Strain, %
Sample Type: Shelby Tube
Description: Clayey Sand, gray and light brown
LL= 27 PL= 13 P1= 14
Assumed Specific Gravity= 17
Remarks: Residual
Tested By: MK
1
2
3
6000
4000
a
M
LL
2000
Results
C, psf 568
�, deg 22.6
Tan() 0.42
we
Sample No.
Water Content, %
Dry Density, pcf
Saturation, %
Void Ratio
3 Diameter, in..
Height, in.
2 Water Content, %
Dry Density, pcf
a) Saturation, %
Q Void Ratio
Diameter, in.,
Height, in.
F rmal Stress, psf
il. Stress, psf
Strain, %
Ult. Stress, psf
Strain, %
Strain rate, in. /min..
2000
4000
Normal Stress, psf
1
2
3
16.3
16.3
163
113.4
1118
113.7
90..6
91.6
91.3
0.4859
0„4807
0.4822
2.50
2.50
2,,50
0.75
0.75
0.75
16 „6
15.1
14.8
113.4
113.8
1117
92.5
85.1
83 .O
0.4859
0.4807
0.4822
2.50
2.50
2.50
0.75
0.75
0.75
1000
2000
3000
973
1419
1804
8..8
20.0
18.4
N/A
N/A
N/A
6000
Client: Teague Nall and Perkins, Inc.
Project: Andy Brown Park - Lake & Channel
Sample Number: B -2 Depth: 19 -20
Proj. No.: 131 -12 -116 Date: 6/13/2012
DIRECT SHEAR TEST REPORT
MJ ENGINEERING, Nu.
Checked By: MK
Al A Tr A A n go
0
O
y
r%
t
s
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co
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