HomeMy WebLinkAbout3156; JEFFERSON STREET BIKE PATH; GEOTECHNICAL INVESTIGATION; 1994-09-26<5- _C~ SOUTHERN CALIFORNIA
T> SOIL & TESTING, INC.
6280 Riverdale Street, San Diego, CA 92120
P.O. Box 600627, San Diego, CA 92160-0627
619-280-4321, FAX 619-280-4717
September 26, 1994
City of Carlsbad Engineering Department SCS&T 9311049
2075 Las Palmas Drive Report No. 3
Carlsbad, California 92009-1576
SUBJECT: Revised Additional Recommendations, Jefferson Street Bicycle Lane, Carlsbad,
California.
REFERENCES: 1) Additional Recommendations, Jefferson Street Bicycle Lane;" Southern
California Soil and Testing, Inc.; May 7, 1993.
2) "Report of Geotechnical Investigation, Jefferson Street Bicycle Lane;"
Southern California Soil and Testing, Inc.; April 6, 1993.
Gentlemen:
In accordance with your request we have prepared this report to provide revised additional
recommendations for the subject project. These recommendations are based on a review of a
cribwall detail (Section A-A), conversations with Mr. Albert Virgilio and a review of the
referenced reports.
RECOMMENDATIONS
BEARING CAPACITY: A bearing capacity of 3000 psf may be utilized for cribwall design.
This value may be increased by one-third when considering wind and/or seismic loads.
SETTLEMENT: Based on the aforementioned cribwall detail the net pressure of the existing
foundation soils will not exceed about 200 psf to 400 psf. It is estimated that the total and
differential settlements for the proposed cribwall will be approximately one-inch and half-inch,
respectfully.
If you should have any questions regarding this report, please do not hesitate to contact this office.
This opportunity to be of professional service is sincerely appreciated.
Respectfully submitted,
SOU ERN CAVFORNIA SOIL AND TESTING, INC. o%OESSIO4,
NO, 36037
Daniel 11,R.C3
DBA:mw
cc: (6) Submitted
REPORT OF
GEOTECHNICAL INVESTIGATION
JEFFERSON STREET BICYCLE LANE
JEFFERSON STREET
CARLSBAD, CALIFORNIA
PREPARED FOR: oqzc~ej
OR CITY OF CARLSBAD 071993
ENGINEERING DEPARTMENT
2075 LAS PALMAS DRIVE
CARLSBAD, CALIFORNIA 92009-1576
PREPARED BY:
SOUTHERN CALIFORNIA SOIL AND TESTING, INC.
6280 RIVERDALE STREET
SAN DIEGO, CALIFORNIA 92120
Providing Professional Engineering Services Since 1959
5—C, SOUTHERN CALIFORNIA 1 SOIL & TESTING, INC.
6280 Riverdale Street, San Diego, CA 92120
I P.O. Box 600627, San Diego, CA 92160-0627
619-280-4321, FAX 619-280-4717
I April 6, 1993
I City of Carlsbad
Engineering Department
I 2075 Las Palmas Drive
Carlsbad, California 92009-1576
SCS&T 9311049
Report No. 1
ATTENTION: Mr. Alphonse Virgilio
U SUBJECT: Report of Geotechnical Investigation, Jefferson Street Bicycle Lane, Jefferson
Street, Carlsbad, California.
Gentlemen:
In accordance with your request, we have completed a geotechnical investigation for the proposed
I project. We are presenting herewith our findings and recommendations.
I The findings of this study indicate that the site is suitable for the proposed development provided
the recommendations presented in the attached report are followed.
I
If you have any questions after reviewing the findings and recommendations contained in the
I attached report, please do not hesitate to contact this office. This opportunity to be of professional
service is sincerely appreciated.
I Respectfully submitted,
I SOUTHERN LIFORNIA SOIL & TESTING, INC.
I Daniel B. Adler, .E.#36O3
AL
John/R. High/C.E.
ç EcYQ
I DBA:JRH:mw B.4%R.
cc: (6) Submitted /
1 NO.
I
I CERTIFIED I -
I 36 037 I
I EXP.6-3 ENGiNEERING0 9G *1 \GEOLOGIST /
'WI 6-30-94
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I TABLE OF CONTENTS
PAGE
I Introduction and Project Description ........................................
ProjectScope ....................................................2
1
Findings......................................................2
I Site Description ...................................................2
General Geology and Subsurface Conditions ................................3
Geologic Setting and Soil Description .................................3
WaterTable .................................................3
Tectonic Setting ...............................................4
Geologic Hazards .................................................4
I
General.....................................................4
Groundshaking ................................................4
Liquefaction ..................................................5
I
Flooding...................................................5
Landslides ..................................................5
Ground Cracking and Surface Rupture .................................6
Tsunamis and Seiches ...........................................6
Conclusions and Recommendations ........................................6
General....................................................6
Site Preparation ..................................................7
General ..................................................... 7 I Import1Fill .................................................7
Sheet Pile Design Parameters .........................................8
I Lateral Pressures ..................................................8
Passive Pressure ...............................................8
Surcharge Load ...............................................9
Factor of Safety ...............................................9
Limitations.....................................................9
Review, Observation and Testing .......................................9
Uniformity of Conditions ............................................9
Changein Scope ................................................10
Time Limitations ................................................10
• I Professional Standard .............................................10
Client's Responsibility .............................................10
Field Explorations ................. .................................... 11
I
Laboratory Testing .................................................11
AFACIIMENTS
FIGURES
I Figure 1 Site Vicinity Map, Follows Page 1
Figure 2 Resultant Earth Pressure Diagram, Page 8
I PLATES
Plates IA, 1B,
& 1C Site Configuration, Topography and Trench Locations I Plate 2 Unified Soil Classification Chart
Plates 3-8 Boring Logs
Plates 9-16 Grain Size Distribution I Plate 17 Direct Shear
Plate 18 Single Point Consolidation
I
SOUTHERN CALIFORNIA I Q SOIL & TESTING, INC.
6280 Riverdale Street, San Diego, CA 92120 I P.O. Box 600627, San Diego, CA 92160-0627
619-280-4321, FAX 619-280-4717
GEOTECHNICAL INVESTIGATION
JEFFERSON STREET BICYCLE LANE
JEFFERSON STREET CARLSBAD, CALIFORNIA
INTRODUCTION AND PROJECT DESCRIPTION
This report presents the results of our geotechnical investigation for the proposed bicycle lane to be
I . located adjacent and northwest to Jefferson Street, in the City of Carlsbad, California. The site location
is illustrated on the following Figure Number 1.
I The subject project will consist of the construction of bicycle lanes on both sides of Jefferson Street, west
of Marron Road for a distance of approximately 2,450 feet. The subject area of this report is the north
side of Jefferson Street, in particular a 260-foot long section that will require an earth retaining structure.
The retained height should not exceed three feet.
I
To assist in the preparation of this report, we were provided with a set of undated improvement plans
I prepared by Keltner & Associates, Inc. The site configuration, topography and approximate locations
of our borings are provided on the attached Plates Number IA, lB and I.C.
I
PROJECT SCOPE
The investigation consisted of: surface reconnaissance, subsurface explorations, obtaining representative
I disturbed and undisturbed samples, laboratory testing, analysis of the field and laboratory data, research
of available geologic literature pertaining to the site, and preparation of this report. More specifically,
the intent of this analysis was to:
a) Explore the subsurface conditions to the depths influenced by the proposed construction.
I b) Describe the general geology at the site, including geologic hazards which could have an
effect on the site development.
I
I By: IJBA
JEFFERSON ET BICYCLE LANE
DATE: 040693
SOUTHERN CALIFORNIA
SOIL a TESTINQ,INC.
I UMBER: 9311049 IFIGURE NO. 1
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1 SCS&T 9311049 April 6, 1993 Page 2
C) Develop soil engineering criteria for site grading and provide design information regarding
the stability of existing slopes.
d) Address potential construction difficulties and provide recommendations concerning these
I problems.
I e) Recommend an appropriate foundation system for a sheet pile and "H" pile and wooden
lagging earth retaining structure anticipated and develop soil engineering design criteria for
I the recommended foundation design.
I FINDINGS
I SITE DESCRIPTION
The project site is comprised of a narrow strip of land located between Marron Road and Interstate
Highway 5 within the northern portion of the easement for Jefferson Street in the City of Carlsbad,
I California. The project area is located immediately north of and adjacent to the paved portion of
Jefferson Street. The site is bounded on the east by Marron Road, on the west by Highway 5 and Buena
I Vista Lagoon on the north. Topographically, the project area slopes gently downward toward the
northeast and is approximately the same elevation as the adjacent paved portions of Jefferson Street. A
I northerly descending slope parallels the northerly boundary of the project area and extends down to the
water level of the adjacent lagoon. The slope ranges up to approximately 30 feet in height with
I inclinations varying from approximately 1:1 to 2:1, horizontal to vertical. The tallest portions of the
slope are located on the southwesterly end of the project area. The. slope decreases in height toward
l Marron Road (northeast). The slope in the vicinity of proposed earth retaining structure (boring B-3 and
B-4) ranges up to approximately six feet in height at inclinations varying from approximately 1:1 to 2:1,
I horizontal to vertical. The width of the narrow strip of land (proposed bike lane) between the curb of
Jefferson Street and the top of the slope ranges from approximately five feet to approximately 25 feet.
The water level of the lagoon is primarily at the base of the northerly slope that parallels the proposed
I bike lane.
I Vegetation within the project area and the adjacent slope is comprised of dense native grasses, shrubs and
mature trees. No structures were noted north of the existing curb, within the proposed bike lane.
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1 SCS&T 9311049 April 6, 1993 Page 3
GENERAL GEOLOGY AND SUBSURFACE CONDITIONS
GEOLOGIC SETTING AND SOIL DESCRIPTION: The subject Site is located in the Coastal Plains
Physiographic Province of San Diego County and is underlain by the Tertiary-age Santiago Formation,
Quaternary-age alluvium and artificial fill.
The project area is located within the easement of Jefferson Street and is immediately underlain by fill
associated with the construction of the street. The fill encountered ranged up to approximately six feet
in depth. The fill was generally loose and was comprised of medium brown, silty sand and clayey sand.
The fill in boring, numbers B-3 and B-4 becomes wet to saturated at depths of approximately four feet
below the existing ground surface.
Alluvial deposits were encountered underlying the fill in borings B72, B-3 and B-4. In boring B-2 the
alluvium extended down to approximately nine feet below the existing grade. The alluvium appears to
extend to depths of approximately 32 feet and 37 feet below the existing ground surface in borings B-3
and B-4, respectively. The alluvium in boring B-2 appeared to be medium stiff to stiff, moist, pale
green, clayey silt. The alluvium in boring B-3 was generally loose to medium dense and stiff to a depth
of approximately 20 feet. In boring B-4 the alluvium was loose and soft to medium stiff to a depth of
approximately 25 feet. Below these depths the alluvium appears to become medium dense. The alluvium
in boring B-3 consists-of olive green, light grey and yellowish tan, silty clays, silty sands. slightly silty
sands, and sandy conglomerate. Some of these deposits are interbedded. The alluvium in boring B-4
consists of interbedded greenish grey, yellowish tan, and medium to dark grey, minor organic clays, silty
clays, clayey sands and silty sands.
The Santiago Formation was encountered underlying the artificial fill and the alluvial deposits. The
formational soils are comprised of dense to very dense, moist, yellowish tan to pale green, silty sand.
In addition, it was noted that the face of the northerly descending slope exposes fill debris and appears
to be relatively loose. This slope face does not appear to have been compacted and minor sloughing and
erosion was noted.
WATER TABLE: The water table was encountered in borings B-i, B-2, B-3 and B-4 at a depth of 10.5.
feet, ten feet, five feet and .4.5 feet, respectively.
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SCS&T 9311049 April 6, 1993 Page 4
TECTONIC SETTING: No faults are known to traversethe subject site but it should be noted that
much of Southern California, including the San Diego area, is characterized by a series of Quaternary-age
fault zones which consist of several individual, en echelon faults that generally strike in a northerly to
northwesterly direction. Some of these fault zones (and the individual faults within the zone) are classified
as active while others are classified as only potentially active according to the criteria of the California
Division of Mines and Geology. Active fault zones are those which have shown conclusive evidence of
faulting during the Holocene Epoch (the most recent 11,000 years) while potentially active fault zones
have demonstrated movement during the Pleistocene Epoch (11,000 to 2 million years before the present)
but no movement during Holocene time.
A review of available geologic maps indicates that the site is located approximately 4 miles east of the
Rose Canyon Fault Zone. Recent earthquake activity along faults in the southern extension of the Rose
Canyon Fault Zone and recent geologic studies have caused this zone to be classified as active. Recent
seismic events along a small portion of the Rose Canyon Fault Zone generated earthquakes of magnitude
4.7 or less. Other active fault zones that could possibly affect the site include the Coronado Bank, San
Diego Trough, and San Clemente Fault Zones to the west, the Elsinore and San Jacinto Fault Zones to
the northeast, and the Agua Blanca and San Miguel Fault Zones to the south.
GEOLOGIC HAZARDS
GENERAL: No geologic hazards of sufficient magnitude to preclude development of the site, as we
presently understand it, are known to exit.
GROUNDSIIAXING: The most likely geologic hazards to affect the site is groundshaking as a result
of movement along one of the fault zones mentioned above. The maximum bedrock accelerations that
would be attributed to a maximum probable earthquake occurring along the nearest portions of selected
fault zones that could affect the site are summarized in Table I on the following page.
Probable groundshaking levels at the site could range from slight to moderate depending on such factors
as the magnitude of the seismic event and the distance to the epicenter. It is likely that the site will
experience the effects of at least one earthquake during the life of the proposed structure. Design
accelerations are generally two-thirds of the peak bedrock accelerations.
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SCS&T 9311049 April 6, 1993 Page 5
TABLE I
Rose Coronado San San
Fault Zone Canyon Bank Elsinore Clemente Jacinto
Distance to
Subject Site 4 20 22 58 44
(Miles)
Maximum Credible
Earthquake 7.0 7.3 7.5 7.5 7.8
(Richter Magnitude)
Maximum Bedrock
Acceleration 0.58 g 0.24 g 0.25 g 0.08 g 0.14 g
from MCE
Maximum Probable
Earthquake 6.5 7.0 7.3 7.3 7.5
(Richter Magnitude)
Maximum Bedrock
Acceleration 0.52 g 0.22 g 0.23 g 0.07 g 0.12 g
from MPE
Construction in accordance with the minimum standards of the Uniform Building Code, the Structural
Engineers Association of California lateral force design requirements, and the local governing agency
should minimize potential damage due to seismic activity.
LIQUEFACTION: The loose, saturated, artificial fill and alluvial deposits are anticipated to be
potentially liquefiable. A complete liquefaction analysis was beyond the scope of this report.
FLOODING: Although the site is located adjacent to the lagoon, it does not appear that the site is
susceptible to flooding.
LANDSLIDES: The adjacent, northerly-facing fill slope appears to be relatively loose. This slope does
not appear to be an engineered slope and shallow sloughing and minor erosion was noted on the slope
face. In addition, clayey portions of the Santiago Formation are known for their relatively low shear
strength parameters and slope failures within Santiago Formation are known to occur in various parts of
northern San Diego County. However, the Santiago Formation does not appear to be exposed in the
adjacent northerly-facing slope. A slope stability analysis for the existing slopes on either. side of
Jefferson Street was beyond the scope of this report.
I SCS&T 9311049 April 6, 1993 Page 6
GROUND CRACKING AND SURFACE RUPTURE: No faults are known to exist on-site and ground
cracking caused by shaking from distant seismic sources is considered to be unlikely.
TSUNAMIS AND SEICHES: Historically, the San Diego County area has been free of tsunami related
I hazards, and tsunamis reaching the San Diego area have generally been well within the normal tidal
range. It is thought that the wide continental margin off the coast acts to diffuse and reflect the.. wave
I energy of remotely generated tsunamis. The largest tsunami to reach San Diego's coast was 4.6 feet,
generated by the 1960 earthquake.in southern,Chile.
I
No locally generated tsunamis are known to have occurred in the San Diego area. However, it is
I speculated that a major earthquake along one of the major offshore faults would have the potential of
generating a tsunami capable of inflicting damage to the San diego coastal region. In addition, seiches
I associated with the tsunami forces could cause moderate damage of the bay areas.
A lack of knowledge about the offshore fault systems makes it difficult to assess the risk due to locally
generated tsunamis. Considering the fact that a major tsunami has not occurred in 170 years of recorded
I history, the risk of such an event occurring in the near future appears nominal.
CONCLUSIONS AND RECOMMENDATIONS
GENERAL
I In general, no geotechnical conditions were encountered which would preclude the construction of the
proposed bicycle lane as presently proposed provided the recommendations presented herein are followed.
The. main geotechnical consideration for the construction of the proposed earth retaining structure to
I support the bicycle lane is the presence of loose fill and alluvial deposits underlying its proposed
alignment. The bicycle lane will be located near the top of a fill slope of questionable stability. This
condition results in foundation soils with poor bearing and lateral resistance. Since the area beyond the
I limits of the proposed bicycle lane is environmentally sensitive, remedial measures such as recompaction
of the fill slope are not possible. Therefore, a conventional retaining structure will not be feasible, since
it would rely on the existing fill for bearing and lateral support. Based on the aforementioned
considerations a system that will not rely on the existing fill for support and that will cause no impact on
the environmentally sensitive area is desired. Asheet pile earth retaining system appears to be the most
feasible alternative. The following considerations should be incorporated into the design.
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I SCS&T 9311049 April 6, 1993 Page 7
1) In order to reduce the active pressure on the retaining wall it is recommended that a reinforced
I, earth backfill be utilized. For budgeting purposes design recommendations for a conventional
soil backfill design will be provided hereinafter.
2) The minimum sheet pile depth will be dictated by the height of the slope and the existing fill
depth. It is recommended that the sheet piles extend at least five feet below the bottom of the
slope and into the alluvial soils. This minimum depth is designed to minimize settlements
behind the wall and surcharges on the. wall due to soil movement associated with a failure of the
1 fill slope. Based on our findings the minimum sheet pile depth will be 11 feet.
I 3) A conventional soil backfill may result in lateral pressures that make the required sheet pile
depth prohibitive. In this case "H" piles extending into firm natural ground may be utilized to
I resist a portion of the lateral loads.. Based on our borings, firm natural ground is located at an
average depth of 35 feet. In this case minimum sheet pile depth would be equal to the slope
I
I Based on our findings it is our opinion that the settlements resulting from the proposed fills will be minor
and not detrimental to the proposed improvements.
SITE PREPARATION
GENERAL: Site preparation should consist of the removal of all existing vegetation from the area
I behind the proposed sheet piles (between the sheet pile and the existing road). If a reinforced earth
backfill is constructed, the existing fill within six feet from the sheet pile and within four feet from finish
I grade should be removed. These minimum limits should be verified by the geogrid company. If a
conventional soil backfill is constructed the existing surface soils should be overcut to a depth of at least
I one foot from and replaced as compacted fill. The over excavated soils and imported fill should then
placed in thin layers and compacted to at least 90 percent as determined in accordance with ASTM
D1557-78, Method A or C.
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IMPORTED FILL: Imported fill should consist of nondetrimentally expansive soil (expansion index
less than 50) and have minimum shear strength values of 35 degrees internal friction and 150 psf
cohesion. Imported fill should be approved by this office prior to delivery to the site.
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SCS&T 9311049 April 6. 1993 Page 8
SHEET PILE DESIGN PARAMETERS
The following values may be assumed for-sheet pile design. Passive pressures should be assumed starting
at the toe of the existing fill slope and shduld be assumed to be developed only on alluvial soils.
Appropriate factors-of-safety should be incorporated.
Soil unit weight above water table = 128 pcf
Soil unit weight below water table = 64 pcf
Active earth coefficient, compacted backfill = 0.271
Active earth coefficient, reinforced earth = 0.1
Active earth coefficient, existing fill = 0.35
Passive earth coefficient, alluvium = 1.5
B TOP OF GROUND
t
NE
0 K -1(H + DI Ka- 7 III + 0) K.
-
?DKQ
OKp 7 (H+D)KpDKa
+ DI K0
FIGURE 2
RESULTANT EARTH PRESSURE DIAGRAM
(assume dredge line at toe of existing slope)
LATERAL PRESSURES
PASSIVE PRESSURE: For "H" piles embedded in formational soils a passive pressure of 800 pounds
per square foot per foot of depth up to a maximum of 8000 psf may be assumed. This pressure may be
increased one-third for seismic loading.
I SCS&T 9311049 April 6, 1993 Page 9
SURCHARGE LOAD: It is recommended than an additional foot of sheet pile height be assumed to
account for surcharge loads due to parked vehicles.
FACTOR OF SAFETY: The above values, do not include a factor of safety. Appropriate factors of
safety should be incorporated into the design.
LIMITATIONS
REVIEW, OBSERVATION AND TESTING
The recommendations presented in this report are contingent upon our review of final plans and
specifications. Such plans and specifications should be made available to the geotechnical engineer and
engineering geologist. so that they may review and verify their compliance with this report and with
Chapter 70 of the Uniform Building Code.
It is recommended that Southern California Soil and Testing, Inc. be retained to provide continuous soil
1 engineering, services during the earthwork operations. This is to verify compliance with the design
concepts, specifications or recommendations and to allow design changes in the event that subsurface
conditions differ from those anticipated prior to start of construction.
UNIFORMITY OF CONDITIONS
I The recommendations and opinions expressed in this report reflect our best estimate of the project
requirements based on an evaluation of the subsurface soil conditions encountered at the subsurface
I exploration locations and on the assumption that the soil conditions do not deviate appreciably from those
encountered. It should be recognized that the performance of the foundations and/or cut and fill slopes
I
may be influenced by undisclosed or unforeseen variations in the soil conditions that may occur in the
intermediate and unexplored areas. Any unusual conditions not covered in this report that may be
encountered during site development should be brought to the attention of the geotechnical engineer so
that he may make modifications if necessary.
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I SCS&T 9311049 April 6, 1993 Page 10
CHANGE IN SCOPE
This office should be advised of any changes in the project scope or proposed site grading so that we may
I
determine if the recommendations contained herein are appropriate. This should be verified in writing
or modified by a written addendum.
I TIME LIMITATIONS
The findings of this report are valid as of this date. Changes in the conditionof a property can, however,
occur with the passage of time, whether they be due to natural processes or the work of man on this or
I adjacent properties. In addition, changes in the Standards-of-Practice and/or Government Coles may
occur. Due to such changes, the findings of this report may be invalidated wholly or in part by changes
1 beyond our control. Therefore; this report should not be relied upon after a period of two years without
a review by us verifying the suitability of the conclusions and recommendations.
PROFESSIONAL STANDARD
In the performance of our professional services, we comply with that level of care and skill ordinarily
exercised by members of our profession currently practicing under similar conditions and in the same
locality. The client recognizes that subsurface conditions may vary from those encountered at the locations
I where our borings, surveys, and explorations are made, and that our data, interpretations, and
recommendations be based solely on the information obtained by us. We will be responsible for those
I data, interpretations, and recommendations, but shall not be responsible for the interpretations by others
of the information developed. Our services consist of professional consultation and observation only, and
no warranty of any kind whatsoever, express or implied, is made or intended in connection with the work
performed or to be performed by us, or by our proposal for consulting or other services, or by our
furnishing of oral or written reports or findings.
CLIENT'S RESPONSIBILITY
I
It is the responsibility of the City of Carlsbad, or their representatives to ensure that the information and
recommendations contained herein are brought to the attention of the structural engineer and architect for
the project and incorporated into the project's plans and specifications. It is further their responsibility
to take the necessary measures to insure that the contractor and their subcontractors carry Out such
recommendations during construction.
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I SCS&T 9311049 April 6, 1993 Page 11
FIELD EXPLORATIONS
I Four subsurface explorations were made at the locations indicated on the attached Plate Number I on
March 16, 1993. These explorations consisted of small diameter borings drilled utilizing a truck mounted
drill rig. The field work was conducted under the observation of our engineering geology personnel.
The explorations were carefully logged when made; These logs are presented on the following Plates
Number 3 through 8. The soils are described in accordance with the Unified Soils Classification System
as illustrated on the attached simplified chart on Plate. Number 2. In addition, a verbal textural
description, the wet color, the apparent moisture and the density or consistency are provided. The density
of granularsoils is given as either very loose, loose, medium dense, dense or very dense. The consistency
of silts or clays is given as either very soft, soft, medium stiff, stiff, very stiff, or hard.
Disturbed and "undisturbed" samples of typical and representative soils were obtained and returned to
the laboratory for testing.
LABORATORY TESTING
Laboratory tests were performed in accordance with the generally accepted American Society for Testing
and Materials (ASTM) test methods or suggested procedures; A brief description of the tests performed
is presented below:
I a) CLASSIFICATION: Field classifications were verified in the laboratory by visual
examination. The final soil classifications are in accordance with the Unified Soil
Classification System.
b) MOISTURE-DENSITY: In-place moisture contents and dry densities were determined for I representative soil samples. This information was an aid to classification and permitted
recognition of variations in material consistency with depth. The dry unit weight is
I determined in pounds per cubic foot, and the in-place moisture content is determined as a
percentage of the soil's dry weight. The results are summarized in the boring logs.
I
C) GRAIN SIZE DISTRIBUTION: The grain size distribution was determined for
I representative samples of the native soils in accordance with ASTM D422. The results of
these tests are presented on Plates Number 9 through 16.
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April 6, 1993 SCS&T 9311049 Page 12
d) DIRECT SHEAR TESTS: Direct shear tests were performed to determine the failure
envelope based on yield shear strength. The shear box was designed to accommodate a
sample having a diameter of 2.375 inches or 2.50 inches and a height of 1.0 inch. Samples
were tested at different vertical loads and a saturated moisture content. The shear stress was
applied at a constant rate of strain of approximately 0.05 inch per minute. The results of
these tests are presented on the attached Plate Number 17.
I
è). CONSOLIDATION TESTS: Single point consolidation tests were performed on selected
"undisturbed" samples. The consolidation apparatus was designed to accommodate a 1-inch
high by 2.375-inch or 2.500-inch diameter soil sample laterally, confined by a brass ring.
Porous stones were placed in contact with the top and bottom of the sample to permit the
addition or release of pore fluid during testing. Selected loads were applied to the samples
and the resulting deformations were recorded. The percent consolidation is reported as the
ratio of the amount of vertical compression to the original sample height. The test samples
were inundated to determine their behavior under the anticipated loads as soil moisture
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SOUTHERN CALIFORNIA
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>T SOIL & TESTING, INC.
JEFFERSON STREET BICYCLE LANES
BY: DBA/JTD DATE: --1993
JOB No.:931 1049 PLATE N,m 1C
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SUBSURFACE EXPLORATION LEGEND
UNIFIED SOIL CLASSIFICATION CHART
SOIL DESCRIPTION GROUP SYMBOL TYPICAL NAMES
COARSE GRAINED, more than half
of material is larger than
No. 200 sieve size.
GRAVELS CLEAN GRAVELS GW. Well graded gravels, gravel-
More tnan half of sand mixtures, little or no
coarse fraction is fines.
larger than No. 4 GP Poorly graded gravels, gravel
sieve size but sand mixtures, little or no
smaller than 3". fines.
GRAVELS WITH FINES GM Silty gravels, poorly graded
(Appreciable amount gravel-sand-silt mixtures.
of fines) GC Clayey gravels, poorly
graded gravel-sand, clay
mixtures.
SANDS CLEAN SANDS SW Well graded sand, gravelly
More than half of sands, little or no fines.
coarse fraction is SP Poorly graded sands, gravelly
smaller than No. 4 sands, little or no fines.
sieve size.
SANDS WITH FINES SM Silty sands, poorly graded
(Appreciable amount sand and silty mixtures.
of fines) Sc Clayey sands, poorly graded
sand and clay mixtures.
FINE GRAINED, more than
half of material is smaller
than No. 200 sieve size.
SILTS AND CLAYS ML Inorganic silts and very
fine sands, rock flour, sandy
silt or clayey-silt-sand
mixtures with slight plas-
ticity.
Liquid Limit CL Inorganic clays of low to
less than 50 medium plasticity, gravelly
clays, sandy clays, silty
clays, lean clays.
OL Organic silts and organic
silty clays or low plasticity.
SILTS AND CLAYS MH Inorganic silts, micaceous
or diatomaceous' fine sandy
or silty soils, elastic
silts.
Liquid Limit CH Inorganic clays of high
greater than 50 plasticity, fat clays.
OH Organic clays of medium
to high plasticity.
HIGHLY ORGANIC SOILS PT Peat and other highly
organic soils.
--'' - Water level at time of excavation CK - Undisturbed chunk sample
or as indicated BG - Bulk sample
US - Undisturbed, driven ring sample SP - Standard penetration sample
or tube sample
:1
SOUTHERN CALIFORNIA
SOIL & TESTING,INC.
JEFFERSON STREET BICYCLE LANE
BY: ' DBA I DATE: 04-06-93
JOB NUMBER: 931'1049 1Plate No. 2
-
LU 3-
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BORING NUMBER I o.
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_j DESCRIPTION 'S SS ••
n '• - - 0 0
-_ SM FILL, Light Brown SAND _SILTY Humid Loose
-
J SC-/SM. Brown CLAYEY SILTY SAND
'SP SANTIAGO FORMATION?. Hunild Dense
- US Yellow Tan SAND 48 100.1 -. 4.6
6 Medium 26 941.4 .8 .0
-
BG Dense
8 '-
10_ .-
• SAND Intrusion in
- Auger Below this Depth, Satur- Medium 44 : .104.6 22.9
-12 \ Samples not Representative ated Dense
lip
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to
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14
16_ US 57 93.2 29.8
118.. 0
20-
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S
44 96.4 27.1
j.22
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-
26 Boring Ended at 25'
Lost Hole Due t0 Sand
IntrusiOn -
b.
SOUTHERN CALIFORNIA SUBSURFACE EXPLORATION LOG
SOIL &TE'ST1NG INc. LOGGED :. JH DATE LOGGED:03_16_93
S •• , JOB-NUMBER: 9311049 Plate No. 3
S - 'OS" - -. -, S - - •0 •. - O0
1
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= BORING NUMBER 2
4
U ELEVATION
3. CL O U.
• (1)
I D E S C R IPT1ON
U- 0
SM FILL, Brown SILTY SAND
I BG
US
I 4 - • SC! CLAYEY SILTY SAND
SM
I 6
-
US ML& Pale Green CLAYEY SANDY
SM! SILT, Sample Tip Red
- SC Brown CLAYEY SILTY SAND
8-
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- 0 0
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Humid Loose
- Moist
to Very
Moist i 11 99.7 20.4
Moist Medium 11 I 107.3 I 15.3
to Very Stiff
Moist to
Stiff
I 10- ML& SANTIAGO FORMATION, Pale Satur- Stiff
11S SM Green SANDY SILT and SILTY ated and
SAND Dense
12- - - Water Table
14-
us
16 -
18-
2 0 - US
-- __ __________ U 22 Boring Ended at 21'
I -- -
SOUTHERN CALIFORNIA
I SOIL &TESTING,INC.
,1
44 1106.9 I 20.4
FA
Hard andi I I
Very I I I
Dense I
50!3" 1115.4 116.4
50!2" 1 121. 5 1 14. 5
SUBSURFACE EXPLORATION LOG
LOGGED BY: JH DATE LOGGED: 03-16-93
JOB NUMBER: 9311049 Plate No. 4
I -- - tL1 z I - U--
BORING NUMBER 3
z U
I
I W -J ELEVATION
z
=
z
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0. 0 0-z 0 0
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cc 2
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I SM FILL, Brown SILTY SAND Humid Loose
BG Moist
l us 9 105.7 11.7 I -
-
4_I —?—.
Very -
Asphalt and Base Moist
I
.US 6.. 57 115.5 14.9
SatuF
ated
8_ SM ALLUVIUM, Brown SILTY SAND Satur- Medium
- BIG ated Dense
I
10
US - Sample Not Retrieved 21
12
14
I!-
16 - US CL& Top Sample Olive Grey Medium 12
SM SANDY CLAY, Bottom Light Stiff!
1 - Grey SILTY SAND (Sand Loose
18 -
Trap Used) . to
Medium
I - Dense
20
• US SM/ Yellow Tan SLIGHTLY SILTY 23
SP SAND, Disturbed Sample -
22_
241 -
-
US —Sample Not Retrieved 31 -
1
26
- — — — Cobble to 28' 31
28-
30--_
I
SOUTHERN CALIFORNIA SUBSURFACE EXPLORATION LOG
LOGGED BY: JH DATE LoGGED:03_16_93 I SOIL &TES.TING, INC.
- JOB NUMBER: 9311049 Plate No. 5
1
I
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BORING NUMBER 4 -
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Z -
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OESCRIPTiON U U. o • .0 0- - S
-SM FILL, Brown SILTY SAND Humid_ Loose
-
Moist I 2- BG.
US ____ _._ 8 108.8 15.2. -
Moist
Water Table to Wet
H—
6- US SM/SC Grey Brown CLAYEY SILTY SAND 44 122.3' 10.7.-
-
SM: ALLUVIUM,. Yellow Tan Satur- Loose :
8-
SILTY SAND âted and Soft
to
-
• 2. . Medium :
Stiff
:p10
US OL& Dark Grey Organic CLAY
-SM : and Yellow SILTY SAND
12
SC/- Interbedded SILTY SAND SM: and CLAYEY SAND
16 - .SP CL - Greenish Grey-SANDY CLAY
-
Layer
18
QO -
22' - -• -
.
us
.1. :
I
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-
SOUTHERN CALIFORNIA
SOIL &.TESTING, INC..
I, •
3/3 977 27.8.
5
5
-
Medium 31 104.0 24.9
Dense
SI. S.UR FACE EXPLORATION LOG
LOGGED sy:. J DATE LOGGED;03_16_93
.JOB NUMBER: 9311049 P1-ateNo. 7
-
1
uJ
BORINGNUMBER4 - LUZ
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ELEVATION 0 -
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Interbedded SILTY SAND and Satur- Medium
I _SC&
SM CLAYEY SAND ated Dense
32 -
I 34
I 36
38 SM SANTIAGO FORMATION, Pale Satur- Very
• '' Green and Light Grey ated Dense -
- SILTY SAND
•
•
40._
-
,
.
.. ,
•
,
,
50/4.5" 123.5 12.6
Boring Ended at 40.5'
I • ' - r. - .
It
1=
I:
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' I SOUTHERN CALIFORNIA . SUBSURFACE. EXPLORATION LOG
LOGGED BY JH DATE LOGGED 03-16-93 I SOIL &TESTING, INC.
JOB. NUMBER: 9311049 Plate No. 8 -
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SINGLE POINT CONSOLIDATION TEST RESULT
1
SAMPLE NO. B2@3' B3@3' B3@5.5' B4@5.5'
-,INITIAL MOISTURE, % 20.4 11.7 14.9 10.7
- INITIAL DENSITY, PCF 99.7 105.7 115.5 122.3
-% CONSOLIDATION BEFORE WATER ADDED 4.6 1.2 3.2 2.0
-% CONSOLIDATION AFTER WATER ADDED 3•9•. 1.2 3.2 2.0
FINAL MOISTURE, % 22.0 17.0 14.2 11.2
-. AXIAL LOAD, KSF 2.86 2.86 2.86 2.86
SOUTHERN CALIFORNIA JEFFERSON STREET BICYCLE LANE
SOIL ,.& TESTING INC. BY: DBA DATE: 04-06-93
Plate No. 18 JOB NUMBER: 9311049