HomeMy WebLinkAboutCT 75-09B; Santa Fe Knolls; Soils Report; 1985-07-02EBERHART & STONE, INC. DAN R. EBERHART. CEG
GEOTECHNICAL CONSULTANTS GERALG L. STONE. RCE
2211 E. WlNSTONROAD.SUlTEF.ANAHEIM.CA92606*(714)991-0163 5205AVENlDAENCINAS,SUlTEC.CPIRLSBAO,CA92W6.(619)438-9416
GEOTECHNICAL INVESTIGATION
SANTA FE KNOLLS, C.T. 75-9 (6)
CARLSBAD, CALIFORNIA
W.O. 1343 July 2, 1985
Prepared For:
The Anden Group
6544 Corte Montecito
Carlsbad, California 92008
Anden w-0. 1343
TABLE OF CONTENTS
TEXT
REPORT ON INVESTIGATION
Purpose and Scope . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Page 1
Proposed Site Grading and Development . . . . . . . . . . . . . . . . . . . . . . Page 1
Site Description . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Page 2
Location
Topography
Vegetation
Drainage
Previous Land Use
Previous Grading
Investigation . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Paae 3
Research
Maooinq
Subsurface Investigation and Sampling
Geotechnical Enqineerinq Evaluation . . . . . . . . . . . . . . . . . . . . . . . . Page 3
Slope Stability
Bearing Value
Geology ,..............................,.................... Paqe 4
Setting
Surficial Units
Bedrock Units
Geologic Structure
Faulting
Ground Water
Landsliding
Seismicity . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Page 6
Ground Shaking
Liquefaction
Ground Rupture
EBERHART 8 STONE, INC.
Anden W.O. 1343
TABLE OF CONTENTS
TEXT (cont'd.)
OPINIONS AND RECOMMENDATIONS
Geology . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Page 8
Slopes
Faulting
Landsliding
Ground Water
Seismicity . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Paqe 9
Ground Rupture
Ground Shaking
Liquefaction
Seismic Design
Geotechnical Parameters for Gradinq . . . . . . . . . . . . . . . . . . . . . . . . Page 9
Shrinkaqe, Bulkinq and Subsidence
Excavation Characteristics
Canyon Subdrains
Transition Lots
Blanket Fill
Rock Area Overcut
Settlement
Slopes
Stabilization Fill Slooes
Stabilization Fill Backdrains
Grading . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Page 12
Observation and Testinq
Clearing
Selective Grading
Overexcavation
Subdrain Placement
Fill Placement
Oversized Rock Placement
Conventional Foundations . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Page 13
Bearinq Value
Exoansive Soil Guidelines,
Foundations Adjacent a Top-of-Slooe
Post-Tensioned Structural Slabs . . . . . . . ..*.................. Page 14
Sumna~y . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . . Page 15
EBERHART 0 STONE, INC.
Anden
TABLE OF CONTENTS
W.O. 1343
APPENDIX
References ................................................ A-l
Description of Laboratory Tests ........................... A-2
Location Map .............................................. Plate 1
Seismicity Maos ........................................... Plates 2a thru 2c
Seismic Parameters ........................................ Table I
Summary of Laboratory Test Data ........................... Table II
Guidelines for Residential Foundations Based on
Soil Expansion ........................................ Table III
Unified Soil Classification ............................... Plate A
Boring Logs ............................................... Plates A-l thru A-14
Standard Soecifications for Gradinq Projects .............. Pages 1 thru 6
Gradinq Details ........................................... Plates GO-1 thru GO-5
Geologic Maps (pocket enclosures) ......................... Plates 3a thru 3d
Geologic Cross-Sections (pocket enclosure) ................ Fla%e 4
EBERHART 8 STONE, INC.
Anden -I- W.O. I343
REPORT ON INVESTIGATION
PURPOSE AND SCOPE
Presented herein is a report on this firm's Geotechnical Investigation for Santa
Fe Knolls, C.T. 75-9 (91, Carlsbad, California.
The puroose of this investigation was to determine the nature of the earth
materials underlying the site in consideration of the proposed qrading and resi-
dential development. The scope of this investigation included the followinq:
* Review of the oublished and unpublished geotechnical and seismic data
within and near the site.
' Review of the previous geotechnical reoorts within and near the site.
a Review of aerial photographs.
' Review of the grading plans.
' General site reconnaissance and qeolooic msppinq.
' Exploratory drillinq.
' Selective samplinq.
' Laboratory testina.
0 Geotechnical evaluation of orooosed qradina.
0 Discussion of site seismicity.
' Preparation of this report;
PROPOSED SITE GRADING AND DEVELOPMENT
The tentative map indicates that the site will be developed for the construction
of 211 single-family residential structures, open space, and interior streets.
Grading plans for 138 (Lots 1-43 and 45-1391 of the 211 lots have been prepared
and are the base map for this investigation. Cut-and-fill grading is proposed
to create level building pads for the proposed structures. Cut and fill slopes
are proposed at a slope ratio of 2:l (horizontal to vertical) or flatter. The
maximum heights of cut and fill slopes are 25 feet and 60 feet, respectively.
The proposed structures are anticipated to be slab-on-grade, wood-framed, one-
and two- story residential dwellings, yielding light sructural loading.
EBERHART P STONE, INC.
Anden -2-
SITE DESCRIPTION
Location
The subject site is an irregular-shaped parcel of
W.O. 1343
land consisting of about 70
acres of undeveloped land in the city of Carlsbad, California. The site is
bounded on the west by Mision Estancia, by an existing residential development
on the south, and by undeveloped land on the northern and eastern sides of the
site. The site in relation to the surrounding area is shown on the accompanying
Location Map, Plate 1.
Topoqraphy
Topograohy at the site consists of northeast-southwest trendinq rollino hills
with interveninq tributary side canyons. The oroject site ascends qently to the
northeast along the ridqeline, then steepens near the northeastern prooerty
boundary. Maximum topoqraphic relief over the site is approximately 155 feet.
Natural slopes vary to a maximum slope ratio of about 2:l.
Veqetation
The site is blanketed with a liaht to moderate growth of natural qrasses and
weeds. Heavy brush and scattered large trees occup;~ the larger side canyon
swales.
Drainaqe
Onsite drainage is directed to the north and south into the major canyons
offsite.
Previous Land Use
Much of the site has
farming. No manmade
Previous Grading
been utilized in the past for cattle grazing and dry
structures were observed.
Portions of the subject site have been partially graded along the Mision
Estancia road alignment. This grading was performed by others for the major
water line construction.
EEERHART 8 STONE,INC.
Anden -3-
INVESTIGATION
W.O. 1343
Research
A review of the published and unpublished geologic and seismic data within and
near the site, and a review of previous Geotechnical Reports, was accomplished.
This included a study of aerial stereo photograohs from 1953, 1964, and 1973 for
the site and surrounding areas. Geologic data from these sources were trans-
ferred to the 50-scale grading plans and were subsequently field checked.
Mapping
Surface and subsurface qeoloaic mapping was accomplished utilizing the 50-scale
grading plans to plot geologic units, structure, and subsurface exploration.
This was accomplished by several of this firm's project oeoloqists durinq the
period of October and November 1984. These data have been plotted on the
enclosed Geologic Maps.
Subsurface Investiqation and Samolinq
Subsurface exoloration, during this firm's investigation, consisted of exca-
vating 9 bucket-auger borings, 10 feet to 50 feet deep. Bucket-auaer borings were logged by one of this firm's project oeologists and the Principal
Enqineerlng Geo!oqist during October 1984. Visual and tactile identifications
were made of the materials encountered, and their descriptions are presented on
the boring logs. Bulk and relatively undisturbed samales were obtained at
selected depths for laboratory testing.
GEOTECHNICAL ENGINEERING EVALUATION
Slope Stability
Evaluation of the gross stability of fill slopes, cut slopes, and buttressed
slopes under static and pseudo-static conditions was oerformed. Calculations
were made with the aid of a micro-computer and a program develooed by Douqlas E.
Moran, Inc., utilizinq the simplified wedqe method of analysis as described hy
Duncan and Buchignani (19751. Values for shear strenoth and unit weight were
utilized from laboratory test results. For pseudo-static evaluations, a hori-
zontal factor of 0.15 was utilized. A oseudo-static evaluatinn was not oer-
formed when evaluating stability of slopes where the failure surface was less
than 12", in accordance with the standards estahlished by Los Anqeles and Orange
Counties.
Surficial fill slope stability was evaluated in accordance with methods
established by the Orange County Slope Stability Committee.
ERERHART 8 STONE, INC.
Anden -4- W.O. 1343
Bearing Value
Calculations for recommended bearing values for the oroposed structures were
performed in accordance with the Terzaghi equations.
GEOLOGY
Setting
The site is located on gently rollinq hills along the western flank of the
Peninsular Ranqe Province. Bedrock underlying the site consists of sandstone
and claystone of the Eocene Delmar Formation and metavolcanic rocks of the
Jurassic Santiaqo Peak Volcanics. Residual soil and colluvium mantle the bedrock.
Surficial Units
Surficial units on and immediately adjacent the site consist of artificial fill
(Qaf and Qafu), residual soil (no map symbol), and colluvium (Qcol). The loca-
tions and extent of these units are indicated on the geologic map. A brief
description of each of these units follows.
Artificial Fill (Qaf): Artificial fill is oresent along Mision Estancia and
extends onto the tract. This material was placed under the observation and
testing of Southern California Soil and Testing, Inc. It consists of a mixture
of silt, sand, and clay derived from the adjacent bedrock. Fill was reoortedly
placed on firm soil and colluvium and was not placed on bedrock.
Artificial Fill (Qafu): Non-structural artificial fill was olaced on the tract
ad,jacent Mision Estancia. No testino of these materials was net-formed by
Southern California Soil and Testina, Inc.
Residual Soil (no map Symbol): Residual soil, up to three feet thick, mantles
most of the bedrock on the site. Residual soil is locallv absent in the
steeoer slonino areas of the Delmar Formation and many areas of the Santiaqo
Peak Volcanics. It consists of brown silty sand to silty clay, which is dry to
moist, loose to stiff, desiccated, and locally porous.
Colluvium (Qcol): Thick accumulations of colluvium blanket the side-slopes
and areas within the bottoms of drainaqe swales. Colluvium consists of brown to
gray-brown silty clay, whi,ch is dry to moist, soft to firm, locally desiccated,
and low in density.
EBERHART 8 STONE, INC.
-5- W.O. 1343
Bedrock Units
Bedrock units underlying the site consist of marine sediments of the Eocene
Delmar Formation unconformably overlying the metavolcanic rocks of the Jurassic
Santiago Peak Volcanics. The distribution and extent nf these units are indi-
cated on the geoloqic map. A brief description of each of these units follows.
Delmar Formation, Sandstone (Tdmss): Rocks of the sandstone unit consist predo-
minantly of sandstone with occasional thin seams of cla,y and siltstone
interlayers and interlenses. Sandstone varies in color from gray to brown, is
typically very fine to fine prained, internally massive to poorly bedded, well
consolidated and locally lightly cemented. Occasional concretionary beds 1 foot
to 2 feet thick are also present within this unit. This unit conformably
overlies the claystone unit.
Delmar Formation, Claystone (Tdmcl): Rocks of the claystone unit consist of
claystone and clayey siltstone with occasional interlayers and interlenses of
sandstone. They conformably underlie the sandstone unit and unconformably
overlie the Santiago Peak Volcanics. Claystone varies from brown to green to
gray to blue-gray in color. Bedding is typically poorly developed and discon-
tinuous. In general, the upper ten feet of this unit is highly weathered and
fractured and, consequently, has low strength parameters. These weak materials
are the result of creep, shallow surficial slumoing, and wettinq and drying
cycles. Below a depth of about ten feet, rocks are well consolidated and
lightly cemented.
Santiaoo Peak Volcanics (Jmv): Rocks of the Santiaqn Peak Volcanics are of
basaltic and andesitic comoosition. They are typically dark qray, fine grained
to micro-crystalline and very dense. The upoer portions of the volcanics are
weathered to various depths and partially altered to clay. Below the weathered
zone, very dense volcanic rock is oresent.
Geoloaic Structure -- -__
Subsequent to their deposition over the Santiago Peak Volcanics, the sediments
of the Delmar Formation have undergone only minor uplift and folding. Beddina
planes are ooorly develoned to massive. Where beddino was observed, dios of
5' to 15" were measured, striking in all directions. These variable beddinq
attitudes represent typically undulatory, cross-bedded, and discontinuous planar
features.
Geologic structure within the volcanics is typically absent; however, moderate
fracturing and high-angle joint patterns are common.
EBERHART 8 STONE, INC.
Anden -6- W.O. 1343
Faulting
Geologic literature and field exploration do not indicate the oresence of hiqh-
anqle normal or reverse faulting on or immediately adjacent the subject site.
Some evidence of beddino alane faulting was observed.
Ground Water
Minor water seepage was present within Borings B-l, B-2, and B-5 within the
claystone unit of the Delmar Formation. Natural springs and water seepage were
observed adjacent the Delmar Formation/Santiago Peak Volcanics contact in the
northern portion of the subject tract.
Landsliding
No major deep-seated landslides were observed during this firm's field explora-
tion. However, several shallow surficial failures were mapped in the vicinity of
Lots 3-7 and 30. These rotational failures apoear to involve residual soil and
highly weathered bedrock.
SEISMICITY
Ground Shakinq
The Southern California area is seismically active. Because of the ornximitv of
the site to several nearby active and ootentially active faults, moderate around
shaking could occur at the site as a result of an earthquake on any one of them.
The fault zone capable of oroducina the stronoest shakino at the site is the
Rose Canyon. The site in relation tn the active and potentiallv actitle faults
in the reoion, as well as eoicenters of orevious earthquakes, is oresented on
Plates 2b and 2c, respectively.
Ground resoonse during a seismic event may be estimated for a oarticular site on
the basis of previous ground motion studies, data from previous earthquakes,
activity of the faults influencing the site, and current state-of-the-art
understanding of seismic forces. Seismic parameters for active ano potentially
active faults within a loo-km radius of the site are oresented in Table I.
ERERHART 8 STONE, INC.
-7- W.O. 1343 Anden
The orobability of any site in California exoeriencinq seismic accelerations of
varying levels during a loo-year oeriod has been computed by Housner as follows:
Acceleration (%Q) % Probability (100 yrs)
15:o El
20.0
25.0
30.0
35.0
99
98
a7
63
37
19
a.7
Liquefaction
Since the factors generally considered to contribute to liquefaction are not
present at the site, the potential for liquefaction is considered nil.
Ground Rupture
Since no active faults lie within or adjacent the site, ground ruoture at the
site due to fault disnlacement is not anticipated.
EBERHART 8 STONE,INC.
Anden -2% W.O. 1343
OPINIONS AND RECOMMENDATIONS
Recommendations in this report are opinions based upon this firm's exoloration,
testing, and professional judgment. Opinions and recommendations are applicable
to the proposed development of the site under the purview of this reoort, and
should be incorporated into project design and construction practice.
Based on this investigation, the site may be developed for future residential
use, as indicated on the tentative map and grading plans, provided that the
recommendations and specifications presented herein are incorporated into design
and construction practice. Grading should be conducted in accordance with local
codes, this firm's standard gradinq specifications, and the recommendations
within this report.
GEOLOGY
Slopes
No cut slopes with adversely oriented planar features are anticipated that would _
require buttressinq.
Some cut slooes with locally adversely oriented planar features, hiahly frac-
tured rock, residual soil or colluvium, are anticioated and igill require
replacement with stabilization fills.
Fatiltinq I____
Geoloqic hazards due to active faulting are not present at the subject site!.
Landsliding
No deep-seated landslides were encountered on or adjacent the subject tract.
Ground Water
Adverse effects on the proposed development as a result of ground water are not
anticipated. Subdrains are recommended below all proposed canyon fill areas and
within slope stabilizations.
EBERHART 8 STONE, INC.
Anden -9- W.O. 1343
SEISMICITY
Ground Rupture
Ground ruoture due to fault displacement is not anticipated.
Ground Shaking
Moderate ground shaking could occur at the site as a result of an earthquake.
Liquefaction
In consideration of proposed grading, material types, current ground water con-
ditions, and anticipated ground shaking, the possibility of liquefaction is con-
sidered remote.
Seismic Desiprl
The oroposed structures and foundations should be designed to resist seismic
forces in accordance with the criteria contained in the 1985 Uniform Building
Code for seismic zone 4.
GEOTECHNICAL PARAXT'RS FOR SR?DI?IG - -----__
Shrinkaae, Bulkinp and Subsidence
Based on the results of laboratory testinq and evaluation of the WmW?d
aradina, the 3veraae shrinkaae and bulkina factors for each material tyne are
estimated as follow:
Material Tvog
Artificial Fill (Qaf)
Artificial Fill (Qafu)
Residual Soil
Colluvium (Qcol)
Sandstone (Tdmss)
Claystone (Tdmcll
Volcanics (Jmv)
Shrinkaqe -~ Bulkinq --~
-- --
15% --
15% --
10% --
-- 5%
-- 5%
-- 5%
Since compressible alluvial deoosits are to be overexcavated from areas to
receive significant amounts of fill, subsidence is anticioated to be neqliqible.
EBERHART 8 STONE. INC.
Anden -lO- W.O. 1343
Excavation Characteristics
The following excavation characteristics of the various material types at the
site have been developed based on exploratory borings, mapping, previous
geotechnical investigations, and experience with these materials. Some blasting
is anticipated within the Santiago Pea~k Volcanics below a deoth of 5 feet.
Material Type
Easy*
Ripping
Moderatelv?*
Difficult
Rippinq
Difficult** Oversized
Ripping Materials
Artificial fill (Qaf) X -- -- --
Artificial fill (Qafu) X -- -- --
Residual Soil X -- -- --
Colluvium (Qcol)
Sandstone (Tdmss)
Claystone (Tdmcl)
X -- -- --
X X X X
X X -- --
Volcanics (Jmv) X x x X
*D-9 with double riooers
**D-9 with sinale riooer
Sa'.urated materials will likely be encountered in swales and areas of overex-
cavation overlyinq the volcanics. The depth and location of seepage or qround
water are indicated on the geoloqic map and borinq logs.
Canyon Subdrains
A subdrain system will be required beneath the proposed fills in canyon areas.
Tentative locations are indicated on the enclosed Geologic Map. Details for
canyon subdrains are presented on Plate GD-1.
Transition Lots
The proposed mass grading will create transitions of cut-to-fill within pad
areas. For this condition, the transition should be eliminated by overex-
cavation of about 3 feet of the cut portion of the pad and replacement as a
compacted fill blanket, as indicated on Plate GD-5. This is accomplished to
orovide uniform bearing conditions for foundations.
EBERHART B STONE,INC.
Anden -11- W.O. 1343
Blanket Fill
To reduce the potential for water infiltration and miqration from pads above
stabilization fills, a blanket fill will be required. These pads should be
overexcavated about three feet and replaced with a blanket of compacted fill.
Rock Area Overcut
To provide for ease of pipe trench and footing excavations, street and nad areas
exposinq volcanic rock (Jmv) should be overcut. Pad areas should be overcut 3
feet below oroposed grade and street areas should be overcut to the depth of the
deepest prooosed pipeline. Materials excavated from these areas should be
placed in the deeper fill areas. Materials from the sandstone unit (Tdmss)
should be utilized for compacted fill in overcut areas.
Settlement
Compressible artificial fill, colluvium, an d residual soil are recommended to be
overexcavated. Therefore, settlement beneath prooosed fill is not anticipated.
Settlement of the proposed compacted fill is anticipated to occur during
construction.
Slopes
Cut and fill slopes should be constructed at a ratio of 2:l (horizontal to ver-
tical) or flatter.
The proposed favorably oriented cut and fill slopes r,f up to about 25 feet and
60 feet, respectively, are considered grossl,y and su~'icial1.y stable. All cut
slopes will be reviewed by the enoineering geoloqist t!urinq grading to verify
the anticipated conditions.
Fill slopes should be keyed into firm materials. Details for fill kevs are ore-
sented on Plate GD-4.
Stabilization Fill Slopes
The following oroposed cut slopes 'are anticioated to exnose locall,y adverselv
oriented planar features, highly fractured rock, or surficial soils, and will,
therefore, require replacement with stabilization fills. Their locations and
key dimensions are indicated on the Geologic Map. Details for stabilization
fills are presented on Plate GD-3. Back-cuts for stabilization fills should be
no steeper than 2:l. Flatter back-cuts may be necessary for temporary stability
during construction.
Key Key Reference
Location Width Depth Section
Rear of Lots l-5 15' 3’ A-A'
South of Calle Acervo 15’ 3’ A-A'
Rear of Lots 7-8 20’ 3’ --
EBERHART 8 STONE. INC.
Anden -12- W.O. 1343
Stabilization Fill Backdrains
A backdrain system will be required for each stabilization fill constructed.
Details for backdrains are presented on Plate GO-2.
GRADING
Observation and Testinq
Prior to the start of gradinq, a meeting should be held at the site with the
developer, grading contractor, civil enqineer, and qeotechnical consultant to
discuss the work schedule and qeotechnical asoects of the grading. Gradinq,
includinq clearing, overexcavation, and fill placement, shall be accomplished
under the full-time observation and testing of the geotechnical consultant.
Clearinq
Vegetation, trash, and other deleterious materials should be removed within
areas to be graded and wasted from the site.
Selective Grading
In order to minimize expansive soil and rock at pad and street grades, selective
grading is recommended. Subsequent to overexcavation and subdrain placement,
the following order of excavation and fill placement is recommended.
0 excavate rock and rock area overcut from volcanics (Jmv) and place in
deep fill areas.
0 excavate claystone (Tdmcll and olace in deep fill areas.
0 excavate sandstone (Tdmssl and place in shallow fili areas, rock over-
cut areas, and upper three feet of buildinq pads and roadways.
Overexcavation
. The surficial units, consisting of artificial fill, residual soil, colluvium,
slumps, and the upper portions of weathered bedrock, are considered unsuitable in
their present state for support of the oroposed fill and/or structures.
Therefore, overexcavation of these materials to firm underlyinq bedrock will be
required prior to fill placement. The location, extent and estimated depth of
overexcavation of these materials are indicated on the Geologic Map. Actual
depth and extent of overexcavation will be determined by the goetechnical con-
sultant during grading. Overexcavated soil, free of veqetation or other dele- terious materials, may be reused as compacted fill.
Prior to fill placement, overexcavated areas should be scarified to a depth of
six inches, moisture-conditioned to near optimum, and compacted to 90% or more
of the laboratory maximum density.
EBERHART 8 STONE, INC.
Anden -13- W.O. 1343
Subdrain Placement
Subsequent to overexcavation, the canyon subdrain systems should be constructed.
Tentative locations are indicated on the Geologic Map. Details for canyon
subdrains are presented on Plate GO-l. The final locations of the subdrain
systems will be determined by the geotechnical consultant during grading.
Fill Placement
Subsequent to overexcavation and subdrain construction, fill placement may
proceed. Fill should be placed in loose lifts restricted to about six inches in
thickness. Each lift should be moisture-conditioned as needed to obtain near-
optimum conditions, then compacted to 90% or more of the 1aborator.y maximum den-
sity. Each lift should be treated in a like manner until the desired rough
grades are achieved.
Oversized Rock Placement
Oversized rock, greater than 12 inches, ma.v be qenerated during qradina from
excavations within the sandstone (Tdmss) and volcanic (Jmv) units. Oversized
rocks greater than 12 inches, but less than 3 feet, may be olaced in the deeper
fill areas in accordance with Plate 60-6. Rocks larqer than 3 feet should be
reduced in size or removed from the site.
CONVENTIONAL FOUNDATIONS
The followino preliminary recommendations have been develooed for one- and/or
two-story residential structures. Wood-framed, slab-on-grade construction
yielding light structural loading is anticipated. These recommendations are for
planninq and estimating purposes onl:v and are subject to revision based on as-
graded conditions.
Based on the proposed gradinq and anticipated light structural loading, post-
construction settlement should be within generally accepted tolerable limits.
Foundations for an individual structure should be embedded within the same
bearing material, such as entirely within bedrock or entirely within compacted
fill.
Based on soluble sulfate content of the onsite materials, Type II or Type V
cement should be utilized in concrete for foundations.
EBERHART B STONE, INC.
Anden -14- W.O. 1343
Bearing Value
For preliminary design purposes, an allowable bearing value of 2000 pounds per
square foot, based on an embedment of 12 inches into compacted fill or bedrock,
may be used for continuous footings or square pad foundations. This value is
for dead load plus live load conditions and may be increased by one-third in
consideration of wind or seismic loadings of short duration.
In designing to resist horizontal soil loadinqs, a lateral bearinq resistance of
200 pounds per square foot, per foot of embedment, and a friction factor of 0.3
may be utilized for foundations embedded in compacted fill or bedrock.
Expansive Soil Guidelines
The potential expansion of the onsite~soil tyoes ranqes from Low to Very Hiqh.
General guidelines for residential foundations based on soil expansion are ore-
sented in Table III. Upon completion of rough oad grades, a lot-by-lot eva-
luation of foundation bearing materials will be made, at which time specific
recommendations for construction will be oresented.
Foundations Adjacent a Too-of-Slope
The bottom outer edge of foundations adjacent a top-of-slope should be set back
from the slope surface a horizontal distance of one-half the slope height under
consideration. The horizontal distance should not be less than five Feet and
may be limited to ten feet.
POST-TEN_SIONEO STRUCTURAL SLABS -
As' an alternative to conventional concrete foundations, post-tensioned structural
slab systems may be utilized.
Post-tensioned structural slab foundation systems should be designed by a struc-
tural engineer to resist expansive soil and orovide relatively uniform bearinq
over the slab area. Allowable bearing should be limited to a value of about
1000 pounds per square foot. A cut-off footing should be provided along the
perimeter of post-tensioned slabs, with an embedment of about 12 inches below
lowest adjacent grade.
Though presaturation of slab subgrade is not a requirement, optimum moisture
conditions should be maintained or reestablished just prior to the placement of
slab concrete.
A visqueen-type moisture barrier should be olaced at grade below concrete slabs
and be overlain by one inch of protective sand cover. This moisture barrier
should be heavily overlapped or sealed at splices.
EBERHART B STONE, INC.
Anden -15- W.O. 1343
SUMMARY
The ooinions and recommendations presented in this reoort are based upon site
conditions as the.y existed at the time of this firm's investiqations, and
further assume that exploratory borinqs are representative of subsurface con-
ditions throughout the site. Although not anticipated, materials adjacent
and/or beneath those observed may have different characteristics. This firm's
opinions and recommendations are further based upon laboratory testinq,
experience with similar projects, and professional judqment, No warranty is
expressed nor implied.
This report is subject to review by the controlling governmental body.
Respectfully submitted,
Robert J. Fulton
Project Geologist
Dan R. Eberhart
President
CEG 965
and
RJF:DRE:GCS:mab (5)
d@-@f Gerald L. Stone
Vice President
?CE 32233
EBERHART 8 STONE, INC.
Anden
EBERHART L STONE, INC.
W.O. 1343
APPENDIX
Anden
A-l
REFERENCES
W.O. 1343
Publications
Greensfelder, R.W., 1974, Maximum Credible Rock Accelerations from Earthquakes
in California, C.D.M.G., MS-23.
Hayes, Walter, W., 1980, Procedures for Estimating Earthquake Ground Motions,
U.S.G.S., Professional Paper 1114.
Housner, G.W., 1970, Strong Ground Motion, Earthquake Engineering, edited by
R.W. Wiegel.
Hutton, L. Katherine, Allen, Clarence R. and others, Southern California Array
for Research on Local Earthquakes and Teleseims (SCARLET), Preliminary
Epicenters for 1975 through 1984, CalTech - U.S.G.S.
Jennings, Charles W., 1975, Fault Mao of California, C.D.M.G., Map No. 1.
Kennedy, M.P. et al., 198C, Recency and character of faultino Offshore
MetroDOlitan San Dieqo, California, C.D.M.G., MS-40,31,42.
Moran, D.E., Slosson, J.E., Stone, R.O., Yelverton, C.A., 1973 Geology
Seismicity and Environmental Imoact, A.E.G., Special Publication.
Moyle, W.R. Jr., 1974, Geohydroloqic Map of Southern California, U.S.G.S., Water
Resources Investigations 48-73 ooen file.
Ploesel, M.R., and Slosson, J.E., 1974, Repeatable High Ground Accelerations
from Earthquakes, California Geology.
Real, C.R., Toppozada, T.R., and Parke, D.L., 1978, Earthquake Epicenter Map of
California, C.D.M.G., MS-39.
Rogers, T.H., 1965, Geologic Map of California, Santa Ana Sheet, C.D.M.G.
Schnabel, P.B. and Seed, H.B., 1973, Accelerations in Rock for Earthquakes in
Western United States, S.S.A., Vol. 63, No. 2.
Seed, H.B., Idriss, I.M. and Kiefer, F.W., 1968, Characteristics of Rock Motions
During Earthquakes, E.E.R.C., 68-5.
Previous Reports
Preliminary Soils Investigation, La Costa far south, easterly area, Ranch0 La
Costa, Carlsbad, California, by Benton Engineering, Inc., dated February 28,
1975 (75-I-2OBC).
EBERHART 8 STONE, INC.
Anden W.O. 1343
A-l (cont'd)
Supplemental Soils Investigation, La Costa far south, easterly area, Ranch0 La
Costa, Carlsbad, California, by Benton Engineering, Inc., dated November 11, 1975
(75-lo-9BC).
Review of Tentative Map, CT 75-9, Santa Fe Knolls, Ranch0 La Costa, California,
by Benton Engineering, Inc., dated April 20, 1976 (75-lo-9BC).
Supplemental Soils Investigation, two areas adjacent to Santa Fe Knolls, Ranch0
La Costa, Carlsbad, California, by Benton Engineerinq, Inc., dated July 7, I976
(75-l-2OBC1.
Review of offsite improvement plans, CT 75-9, Santa Fe Knolls, Carlsbad,
California, by Benton Engineering, Inc., dated January 17, 1977 (76-3-18F ).
ia, by Earthwork quantity estimates, Santa Fe Knolls, Unit 1, Carlsbad, Californ
Benton Engineering, Inc., dated March 21, 1979 (79-2-8F).
Preliminary Geotechnical Investigation, southeast area water line, Ranch0 Santa
Fe Road and Mision Estancia, Carlsbad, California, by Southern California Soil
and Testing, Inc., dated February 14; 1984 (25028, No. 1).
Buttress Recommendations, southeast area water line oro~ject, Mision Estancia,
Carlsbad, California, by Southern California Soil and Testinq, Inc., dated March
1, 1984 (25028, No. 2).
Report of field observation and relative compaction tests, orooosed southeast
area !#ater line, Ranch0 Santa Fe Road and La Costa Avenue, Carlsbad, California,
by Southern California Soil and Testinq, Inc., dated May 18, 1984 (25026, No. 4).
AERIAL PHOTOS
Agency
USDA 4-11-53 AXN-8M 16,17,18
USDA 4-09-64 AXN-4DD 5,6,7,8
USDA 4-09-64 AXN-4DD 80,81,82
San Diego County 10-31-73 73/20 21,22
Date Fliqht No. Photo No.
EBERHART 8 STONE. INC.
Anden W.O. 1343
A-2
DESCRIPTION OF LABORATORY TESTS
Classification
Field classifications were verified in the laboratory by visual and tactile
identification. Soils have been classified in accordance with the Unified Soil
Classification System.
Moisture-Density
Moisture-density determinations were conducted on relatively undisturbed
samples. The results are presented on the boring logs.
Maximum dry density and optimum moisture were determined in accordance with ASTM
D1557-70 and are oresented in Table II.
Potential Expansion
Determinations of ootential soil expansion were made on representative samples
in accol,dance with ASCE Exnansion Index Test (IJBC Standard 29-2). The results
are oresen%ed in Table II.
Sulfate Content
Determinations of soluble sulfate content were made on reoresentative samples,
by Soil and Plant Laboratorv, Inc., in accordance with California Method of Test
No; 417A. The results are presented in Table II.
Direct Shear
Direct shear tests were conducted on remolded samples. The samples were tested
in brass rings with 2.5-inch inside diameters. The rate of strain used was 0.05
in./min. The specimens were inundated for approximately 24 hours under normal
loads and during shearing. The results are presented in Table II.
EBERHART B STONE, INC.
LOCATION MAP - ____ -_- ---_--
scale From: Ranch0 Santa Fe, Ca.
7.5’ Quadrangle, USGS
Anden - Santa Fe Knolls
I EBERNART 8 STONE INC.
GEOTECHNICAi CONSULTANTS ?,,I FM, WNSTON RoAO,S”ITt F.ANA”EIM, CAILIFORNI/\92eca
W.O. 5343 1 DATE: 7-2-85
SITE LOCATION 1 PLATE: I
EXPLANATION OF SYMBOLS
FOR SEISMICITY MAPS
FAULT MAP, PLATE: 2-b
ACTIVE AND POTENTIALLY ACTIVE FAULTS
. . . . . .
/I”
TOTAL LENQTH OF FAULT ZONE THAT BREAKS QUATERNARY
DEPOSITS OR THAT HAS HAD SEISMIC ACTIVITY
FAULT SEQMENT WITH SURFACE RUPTURE DURING A HISTORIC
EARTHQUAKE, OR WITH ASEISMIC FAULT CREEP.
(From A.E.G. Recently Active Faults in So. Callf. Region Ma l’ 1973 a C.O.M.G. Fault-Rupture Hazard Zones in Calif. htop, IS 0)
1 EPICENTER MAP, PLATE:2-c
APPROXIMATE EPICENTER LOCATl9NS IN THE SOUTHERN CALIFORNIA
REGION WITH : A&.IGNEO MAGNITUDES GREATER THAN 5.0
A 7.0 - 7.9
0 El.0 or Greater
(From U.S.G.S. Earthquake Eplcantar Map of Calltarnlo,l978 B
CalTech-U.S.G.S. Prsllmlna~ry Epicenters for l-75 thrU 5-84)
ppROXIMATE SITE LOCATION
/
&l_F
-_-A--- --- -GC;
A- 100 KILOME TE
S I D
Y “.\.. ,-
b Y-y------’ Sea ‘**-.
,z...’ g%$$
4+*+
f rJ
/.---4*A
/ i’
OF
CALIF:
-0
9
0
-n
0
R I A I.
a w I
+-
Cl
100 km radius
\
cl
;i
00
q 0 N q i
i \
i
c .--,
T
;J’ be-) ---7
i
L
,I-, “J?lZ ON
I
SO&id &A
q Cl o- -&-
\ b
I
n Bh
The Anden Croup
POTENTIAL
C&“S*TI”E
FAULT
San Jacinto 46NE
Newport/
lnglewood
\1~L:*.:~“, . . . . ..-. ,
Elsinore
Agua Blancai
Coronado Bar
Rose Canyon
IISTANCE
‘+m SlTl
‘0 F*“LT
kn,,.*l
28NiV
23NE
ENOTH
OF
‘A”LT
“0,. I,
30-24;
35-17c
SO-85
RICHTER
MAONIT”
OF
HlSTORlCAL
iARTHWAI(E
3r*.,w than 5
6.20 (19543
6.40 (1958)
6.50 (1968)
5.50 (1980)
6.10 (1980)
6.30 (1922)
5.40 (1941)
6.00 (1910) 5.00 (1920)
5.10 (19401
6.30 (1954)
5.20 (1967)
Uo known
xistorical
earthquake!
PPPROXlMATE
AGE OF
OST RECEN,
SURFACE
SPLACEHENT
-ound failure
rt no definitf
wwn rupturt
axene
1,,000 yr.5
raternary
2 million yrs
mternary
2 million yrs
TABLE 1
SEISMIC PARAMETERS
HAXlY”M CREDlELE
EARTHOUAKE
7.50 .I1 7.00 .06
7.60.
.15
.23
.23
W.O. 1343
6.30
6.35
6.40
CH
PEAK
.08
31
1EPEnJABLE
. .08
.I3
.12
.18
.28 16
.28 17
.28 17
.25 12
M I S..d. km** end Kll,,r.. ,969
e, NW Hownr,1070,a Bolt OS,,>
'REDOMININT D”RP.TION
PLRlOD )F STRON(I
AT SITE HM,NO A
tS.esnd*l ITE ts.cm**
(NC.,. 5) (NO,. 6)
.32 24
Anden W.O. 1343
i
BORING DEPTH
NUMBER (ft.) uses
B-l s-10 SM
B-l 17-22 CL
B-l 25-34 CL
B-l 34-43 CL
B-4 2-10 ML
TABLE II
SUMMARY OF LABORATORY TEST DATA
ANGLE OF
MAX.DRY OPTIMUM INTERNAL SOL. DENSITY MOISTURE COHESION FRICTION EXPANSION SULF.
(PCf) (%) c (psf) # (degr) INDEX (%)
116 13 280 2? 3e .!vn *J
111 17 340 21 96 .120
117 14 300 20 a7 .024
115 15 280 21 68 .053
116 14 300 24 105 .725
I , / \ , /
Anden TABLE III W.O. 1343
Clllnrl ,.,e.z mn m,,*lnlTlnrlT mAPcr. n., cnm, C”r3ILIClnLr
c
I
i;“I”CLII~C3 r”R r”~~~?uI-.I ,“,.J.DA3C” y!. J&#,L LArN*a,“,-, _- ~,
POTENTIAL FOOTINGS . . SLABS
fXPANSlON
(UBC 29-21 EMBEDMENT REINFORCEMENT THICK. REINFORCEMENT PRESAT. BASE
1 STORY 2 STORY 3 STORY COURSE
Very Low Very Low 12” perimeter 18” perimeter 24” perimeter 12” perimeter 18” perimeter 24” perimeter
(O-20) (O-20) 12” interior 12” interior 18” interior 18” interior 24” interior 24” interior
i / \ / \/
Low 12” perimeter 18” per/meter 24” perimeter 2 No. 4 bars: 4” nom. 6”xti”. #lOx#lO
(21-50) 12” interior 18” interior 24” interior 1 top, 1 bottom W.W.F. moisture
Medium
(51-90)
18” perimeter 18” perimeter 24” perimeter 2 No. 4 bars: 4” net 6”x6”, #6x#6 120% of 4” 12” interior 18” interior 24” interior 1 top, 1 bottom W.W.F. optimum
0; moisture -
No. 3 bars @ 24”
O.C. each way
High 24” perimeter 24” perimeter 24” perimeter 4 No. 4 bars: 4” net 6”X6”, #6x#6 120% of ,,,
(91-130) 12” interior 18” interior 24” interior 2 top, 2 bottom W.W.F. optimum
or or moisture -
2 No. 6 bars: No. 3 bars @ 18”
1 top, 1 bottom O.C. each way
Very High 24” perimeter 24” perimeter 24” perimeter 4 No. 5 bars: 6” net No. 4 bars I? 18” 120% of 6”
(7 138) 12” interior 18” interior 24” interior 2 top, 2 bottom O.C. each way optimum
or or moisture - -
2 No. 8 bars: No. 3 bars 4 12”
1 top, 1 bottom O.C. each way
Notes on the following page are considered part of this table.
Anden
/ t
NOTES TO TABLE III W.O. 1343
11 These guidelines are based on site soil expansion and should not preclude more restrictive structural
or agency requirements. As an alternative to conventionally reinforced concrete foundations, post-
tensioned structural slab systems, designed by a structural engineer, may be utilized.
21 Footing embedments should be measured below lowest adjacent grade. At the time of concrete placement,
footing excavations should be moist and free of desiccation cracks.
3) A reinforced concrete grade beam should be constructed across garage entrances, with similar depth
and reinforcement as adjacent perimeter footings.
4) For soil with a potential expansion greater than “Low”, interior isolated spread footings and/or partial
length footings are not recommended. i
51 Where presaturation is recommended beneath interior slabs, the recommended moisture should penetrate
to the depth of the perimeter footings. The moisture content should be tested by the geotechnical
consultant 24 hours prior to the placement of concrete. Though presaturation of slab subgrade is not
a requirement for Very Low and Low expansion potentials, optimum moisture conditions should be maintained
or reestablished just prior to the placement of slab concrete.
6) Below proposed slabs-on-grade in areas to be tiled or carpeted, a visqueen-type moisture barrier should
be placed at grade and be overlain by one inch of protective sand cover. This moisture barrier should
be heavily overlapped or sealed at splices.
7) Where a base course is recommended beneath interior slabs, it should consist of pea gravel, clean sand,
or other granular material acceptable to the geotechnical consultant. The above moisture barrier/sand
cover requirement may be included as part of the recommended base course thickness.
8) Slab reinforcement should be supported at mid-slab height.
9) Garage slabs should be placed separate from footings. Garage slab reinforcement may be omitted if slab
cracking can be tolerated, provided that the slabs are saw cut or jointed for crack control.
101 For soil with a potential expansion greater than “Low”, slabs should be free-floated or structurally tied
to perimeter footings. Structural ties could be provided by the placement of No. 3 bars @ 24” O.C.,
bent from’perimeter footings about three feet into the slab.
Unified Soil Classification
(Including Identification and Description)
. = 51
E .g
!
z
i
7 .I
I ii
,I:
8 n
; .- ? ‘i r .f
w
i
5
: C
: I 0” Or+r da,. ,I mrdiun lo bllb PIas. .v4i- ~ bilb r44; la “11, Sli.hl to ~CiW, o~.:inic ,ill. medium
For .ilnlpl. cw.cc. w.llvrdrd Ir~..l..and mixtar. rdl da, Ibindrr. ,a All me”* ,i*a on Ibi. cllan an “. 5. sundad.
CONSISTENCY CLASSIFICATION
Co$e~ive Bedrock Moisture Condition SP - %+d,a;d Penetration
R - Relatively Undisturbed sample
B - ~Bulk Sample
J-- Stabillred Groundwater
p- Groundwater Seepage
d (I - Blow count for 6”
7 intervals
12 - Blow count for 12”
interval
Loose Soft Soft
Medium Dense Firm Moderately Hat-c
Dense Stiff ‘Hard
Hard Very Hard
Dry
Damp
Moist
Very Moist
Wet
EBERHART 8 STONE INC.
GEOTECHNICAL CONSULTANTS 2711 EAST WNSTON ROAD. SUITE f .ANAWEIH. CALIFDRNU 92808
1.0. 1343 1 DATE: 7-2-85
1 PLATE A
BORING LOS No. I
Aok ,/kg,,fu I-G/ W.Q. 1343
ulentnt/ Project: J%J/, Date: I0 ,/2 y/p4
Locatlon: La, /J- 6 Qd Sheet:/ot 2
Est. Surface Elev: 2 f 0 2 Total Depth: 46-j Rig Type: 2 Y*flu,k, f A*,er
96: IV
jl6) (3)
4r II
/07 r Tdw ---
/06 Zl
pr> Q7)
/If- /L
FIELD DESCRIPTION
E .y m
.’ ,,, Surface Cond~tlons: J,3hl y ,,*,-:~ By:
Notre: PVii/8~0 b&;qb f ’ ‘id,, !-earn , 4ed4F,./i, ,:/jfjr
O- z~- ‘; 2,500 * \ 73 JLe e:cf
ZIrn-4 i- *: /:Iga e
t; LA* CL<‘/Jd.‘,
/I’; &eJd*,
5-c ieav J
EBERHART & STONE, INC. ’ PlateA-/
BORING LOG No./
w.0. /3Y3
Client/ Project: /&A / rqa fq Fe /v&/lr Date: /o/z p/ f Y
Locatlan: CA ,!r 62 _ Sheet:zof 2
Eet. Surface Elev: 2 go+ Total Depth: 46’ Rig Type: 254" fiurhf/4rQer
f17)(
17 It3 17
t /.5-f
20 Jdj
c
$0 126
gy-pz&“e: F’ELD DESCR’PTloN BY: fl JF
i/ ~~
EBERHART & STONE, INC.
Cm/ ProJect:
Location:
Est. Surface Elev:
BORING LOS No. 2
e h /I/r mu
Sheet/of 2
Rig Type:, 2 ‘/ ~? / ’ 1, Total Depth: LICh Y??<V
-
-
J-
‘6
-
Is $5 is ;{ -
-
-
oi
26
-
-
%i e% 1 .ij
z= az $0 -
-
-
16
13
-
- 3i -I $
$ -
-
Yh
-
FIELD DESCRIPTION BY: flJF 1
Notes: ~;IJ;~ q Weiyb t O%idof;*a Jf~,ti~.~‘* 5: rhe-,fl J a -2s- ‘: ”
Zs-dO* e/4; r: mol,r6eB I; fr;hJLIJ.
2 r-30’ : /I-o0 Jt
fi : be&y
hd t Con tf.k-7 u0w.1 drOtiud help,
-
EBERHART & STONE, INC. Plate-A
BORING LOG No. 2
/&LA% /.J4* 7% w.0. /? 4-s
CAent / ProJect: f% [fww/h- Date: /a/Z s/ru
Locatlon: 6fv.r a lbd z Sheetzzof
Est. Surface Elev: 217t Total Depth: .3 ! ’ Rig Typo: 2 9 ” flw c bt? r A 4 9 + - 8, u ;i -
#2.! =
FIELD DESCRIPTION By: AJF
iurface Cond’titms:
iubsurface Cx?dltlons: Classlflcation, color, moisture
tightness; etc.
I--
Remarks
Notes:
-
EBERHART & STONE, INC. Plate&
Est. Surface Elev: _
BORING LOG No. 3
$ g
f!j
0 --
QiJ
‘0 - iJ
--
Ir-
!O-
-g
‘r-
f 3
3
i
T- 1
-
,
-
‘W
=
-
-
z !; ;i , ‘5 i= !g ig -
!r
-
L?
-
16
=
-
- >
c G
-
-
z
= -
E n
n
g
L
-
.L
7
-
W.O. /3Y3
Date: /O./z 9/1$ Y
_ Sheet:Lof /
Total Depth: Rig Type:A’f” d*c kc f /Awqer 23 ’ v
FIELD DESCRIPTION BY: /f JF --
EBERHART & STONE, INC. No CaVib33 Plate /4-S
BORING LOG No.2
Est. Surface Elev:
I-
- 8s 2.5 ce si - -
b
I/L
-
‘i L e; 1 .a z= “2 E 0 -
-
$
18
- Y G f L-z-
-3 -
-
7 in4
Surface Conditlhns: /,3 k fyvq2,3
Subsurface CGdltlons: Classlficatlon, color. molsture
118
-
4
- -
W.O. 1343
Date: / o/J O/BY
FIELD DESCRIPTION BY: h'.JF I
Notes: o)yYViv,c. Iy/e;~+/fr
D -z?' : ZSOO~
c 20’. /2" fh,LLq J-a,JJtiiae. x I'lJlflf
-- 4O"/FdO~
I,?4 CyeAu- ii tiaflre c~v-~,M(~/ 8:"hedJ3
Ora "cge,, hoi, 7. Qrcdafiple /
IAQ.~.X- c oyI ta, eshavti tawv ce&t-
EBERHART -5 STONE, INC.
"
BORING LOG No..dE-
Client / Project: ALZ
Locatlon: Cc7Y /c A,,,
30 b R
1 4
jr-
Yo -R
Yf-
‘zi
17 =
'0
‘0 =
-4 =
-I-
,
c. I 4
I
‘a, d -e
-~ She&-&of t
Total Depth: Rlg Type:, 2v If 8~ c kr f RYGV .+- q/ ’ /
-
‘{ :I,
,” ) ,, (j
-4 ^.^. =
FIELD DESCRIPTION BY: A7 ?-/= I
surface Conditlans:
subsurface Condltlons: Classlflcatlon. colar. moisture
tlghtness, etc. Remarks
fiehfcr
b; c.3 b 3cw rdf f -: c I.+ It dAyIci
__ /l/a a 6 rluT>wajeTe 7i I- / ,J?%Y w f f-
Notes:
-
EBERHART & STONE, INC.
-
PlateA-
BORING LOG No. J-
Went / Project: Ati Jew /IQyI -rl, F& //fvlo //,
Locatlon: La/ h 6064
iYZ*
ShfM~ / of 1
Est. Surface Elev: _ - -
P-s “$ 1
~ i
6: : -
-
-
)Y
-
IIY
-
-
. - - ‘i; $2 !a: 2 r$ % 0 -
-
-
I2
-
w
-
-
2 - - \ 4 6
2 - -
ii
-
-
Total Depth: Rig Type: 5-O ’
Notes: 4ro4-- fee@. da*.4 ii hoi/f; 1: jO/Mf
d- ZZ’: J zrcro~ 1
v I 3 r Lto,J h vevtf LINU/, hfclqr s7 Fhkedfl 2J”S-o’ :/J-40* \ 0 rrJPtf*Y I r-f 4l’nr’na,13,iC‘lr.%ur A: heo/Ji / c :corrtac7 -
EBERHART & STONE, INC. P1ate.Jf-S
BORING LOG No. J--
-
; e! ; /7 za “2 2s -
IY
-
‘J
- -
Cilmt / Project:
Locatlon:
Est. Surface Elev:
Notes \ C L/o.c-‘. 2”-3” t4vr.ck Clrn~ Jeuw.
\ I I , k qi, t. 5-D 79 C‘J- f/@ur*$ Ved,
.75?5a &An J-0 fecf
f 39 feef
EBERHART & STONE, INC. Plate,-
CnsJlt / Pro)ect:
Location:
Est. Surface Elw:
BORING LOG No. b
& KID /lr
She&/of /
Total Depth: Rig Type-2 v “8~ /?C f Rci ~FY 2 i ’
I y* 6”
20 l2Z
- -ii F% 1z z= EC s 0 -
-
-
9
7~
=
-
5 2 e- 8 5 -
-
-
&v
=
-
I
FIELD DESCRIPTION By: JF*
4”
Surface Condltlons:
t--- l I 1 . -: mw C 2 3 '.-veti\, k CI~ ri /I c f e31.j e-4 / ? ? Stpfifld 'd,,-/I;, 4 , ve fuSa/
Nofer: Yifivlq &iQI?I % fG / 8&h ti fee t J a-2J': z&3* iv0 trynuHJw-tet-.
l?: 6edJy
%:J~,nfe Jirfqtbed /VO Lavifi 4
EBERHART & STONE, INC. PW*A-lO
BORING LOG No. 7
Ada4 / alent / Prolect: s*Jta Fe kflo//r
Locatlon: &?1,/J-Lac
w.0. 1393
Date: /D/?/ /ff79
Est. Surface Elev: _ L -
2 !: 2 #Z i= ;i
[;
e
; ’ , 1
i ! -
4
,
L / Sheet:- of 2
-t Total Depth: Rig Type:2 Y ” & 3 / ’ uckef Av qer
FIELD DESCRIPTION BY: /p + -
‘tlm: ;;Th;-. Jay jig hted CO~MYOL)
I
‘05
‘01
-
foe
‘//
‘Y
‘A-
‘5
‘Y
-
Classlflcation, color. moisture tightness; etc. Remarks
I -
IE
eveeh. h~i.flY F;VM
ec ’ %fv’
Notes: vi ViUrCj wQ;o/
(-J -“zr’ : ‘/&-cy* -
: edd. ‘7
U-30 ; /J--00* -
EBERHART & STONE, INC.
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Plate A-N
BORING LOG No.-iifw
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Locatlon: Sheet-&of z
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Total Depth: 31 ’ Rig Type: 2y”Euckef Awe J I FIELD DESCRIPTION By: AJf ] ‘i; !?i ;i , s
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iurfaca Conditions:
iubsurface CondItiona: Classiflcatlon, color. moisture
tightness; etc.
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Remarks
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EBERHART & STONE. INC. PlateJILL
BORING LOG No. 8
AMdew //a,~% Fe W.O. 134 3
Ulm / Proiect: IfI- 0 //J- Date: /Q/J/h
Locatlon: fav/s-6ad I ~ Sheet: / of /
72 Total Depth: 2 r) ” /o ’ Rlg Type:
FIELD DESCRIPTION BY: oP,TS I -
R. Surf0
s” Surface Condbi~)ns: ; , 8 I 1 r
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Subsurface C,ndltlons: Closslflcatlon. color. moisture tightness, etc. Remorks
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EBERHART & STONE, INC.
BORING LOS No. 7
Client / ProJect: Ac7h /.Gnj/ Fe- fbo/~
Location: Lwl~&d Sheet: / of /
3Oki Total &pth:yRipTypa: Bgckcf- /!uzer Est. Surface Elev: _
I FIELD DESCRIPTION By:
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Subsurface Conditions: Closslficotlon. color. moisture
tightness, etc. Remarks
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EBERHART & STONE, INC. Plate.&&?
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STANDARD GRADINJ SPECIFICATIONS
1.0
2.0
2.1
2.2
2.3
2.4
2.5
2.6
2.7
2.8
2.9
The specifications contained herein and the standard details attached
hereto represent minimum requirements for grading operations on
construction projects. Variance from these specifications will not be
permitted unless specifically approved by the soil engineer. These
reconendations should not be considered to preclude more restrictive
requirements of the regulating agencies.
DEFINITION OF TERMS
BEDROCK - a relatively solid undisturbed or in-place rock existing at
either the ground surface or beneath surficial deposits of soil.
Bedrock will be identified in the field by the project engineering
geologist.
ENGINEERED FILL - a fill of which the soil engineer or his represen-
tative during grading has made sufficient observations and taken suf-
ficient tests to enable him to conclude that the fill has been placed
in substantial compliance with the governing specifications.
ENGINEERING GEOLOGIST - a geologist holding a valid certificate of
registration i.p the specialty of engineering geology.
FILL - any deposits of soil, rock, soil-rock blends ,or other similar
materials placed by man.
GOETECHNICAL CONSULTANT - the soil engineering and engineering geology
consulting firm(s) retained to provide technical services for the pro-
ject. For the purpose of these specifications. observations by the soil
engineer and engineering geologist include those performed by persons
employed by and responsible to the geotechnical consultant.
GRADING - any operation consisting of excavation, filling or combinations
thereof.
IMPORTED OR BORROW MATERIAL - any fill material hauled to the project
site from off-site areas.
RELATIVE COMPACTION - the degree of compaction (expressed as a percen-
tage) of dry density of a material as compared to the maximum dry den-
sity of the material. Unless otherwise specified, the maximum dry
density shall be determined in accordance with ASTM method of test 01557-70.
SOIL ENGINEER - a licensed civil engineer experienced in soil mechanics.
3.0
3.1
3.2
3.3
3.4
4.0
4.la
4.lb
4.2a
4.2b
4.3a
SITE PREPARATION
Clearing and grubbing shall consist of the removing of all vegetation
such as brush, grass, woods, stumps, trees, roots of trees and all
otherwise deleterious natural materials from the areas to be graded.
Clearing and grubbing shall extend to the outside of all proposed
excavation and fill areas.
Demolition shall include removal of all buildings, structures, utilities
and all other manmade surface and subsurface improvements from the areas
to be graded.
Trees, plants or manmade improvements not planned to be removed or demo-
lished shall be protected by the contractor from damage or injury.
All deleterious material generated during clearing, grubbing and demoli-
tion operations shall be wasted from areas to be graded. All clearing,
grubbing and demolition operations shall be performed under the
observation opthe soil engineer.
EXCAVATIONS
Unsuitable Materials: Material which is unsuitable shall be excavated
as directed by the soil engineer. Unsuitable materials include, but may not be limited to dry, loose, soft, wet, compressible and non-engineered
or otherwise non-approved fill materials.
Material identified by the soil engineer as unsatisfactory due to its
moisture conditions shall be overexcavated, watered or dried as needed
and thoroughly blended to a uniform near-optimum moisture condition
prior to placement as compacted fill.
Site Protection: The contractor shall be responsible for the stability
of all temporary excavations. Recommendations by the soil engineer shall
not be considered to preclude those requirements of the regulating
agencies.
Precautions shall be taken during the performance of all site clearing
earthwork, excavations and grading to protect the work site from
flooding, ponding or inundation by poor or improper surface drainage.
Temporary provisions should be made during the rainy season to ade-
quately direct surface drainage from all sources away from and off the
work site.
Slopes: Unless otherwise reconnnended by the geotechnical consultant and
approved by the regulating agencies, permanent cut slopes shall not be
steeper than 2:l (horizontal to vertical).
-3-
4.3b If excavations for cut slopes ExJose loose, significantly fractured or
otherwise unsuitable material, o,erexcavation and replacement of the
unsuitable materials with a compacted stabilization fill will be
required as directed,by the soil engineer or engineering geologist.
Unless otherwise specified by the soil engineer, stabilization fill
construction shall conform to the requirements of Grading Detail GO-3:
4.3c All lot pad areas, including side-yard terraces, above stabilization
fills or buttresses shall be overexcavated to provide for a minimum of
three feet of compacted fill over the entire pad area. Pad areas with
both fill and cut materials exposed and pad areas containing both very
shallow (less than three feet) and deeper fill shall be overexcavated to
provide for a uniform compacted fill blanket a minimum of three feet in
thickness. Cut areas exposing significantly varying material types
shall also be overexcavated to provide for a minimum three-foot thick
compacted fill-blanket.
4.3d For cut slopes made in the direction of the prevailing drainage above
the cut, a diversion swale (brow ditch) should be provided at the top of cut. The diversion swale configuration should conform to the applicable
code requirements and should be ,-eviewed by the soil engineer prior to
installation.
4.3e For pad areas created above cut l)r natural slopes, positive drainage
shall be established away from the top of slope. This may be accomplished utilizing a berm and/or an appropriate pad gradient.
5.0 COMPACTED FILL
5.1 Compaction: All fill materials shall be compacted as specified below or
by other 'methods specifically approved by the soil engineer. Unless
otherwise specified, the minimum degree of compaction (relative compac-
tion) shall be 90% of the laboratory maximum density.
5.2a Placement: Prior to placement of compacted fill, the ground surface
approved by the soil engineer shall be scarified, watered or dried as
needed, thoroughly blended to achieve near-optimum moisture conditions,
then thoroughly compacted to a minimum of 90% of the laboratory maximum
dry density.
5.2b Compacted fill shall be placed in thin horizontal lifts not exceeding
eight inches in thickness prior to compaction. Each lift shall be
watered or dried as needed, thoroughly blended to achieve near-optimum
moisture conditions, then thoroughly compacted by mechanical methods tc
a minimum of 90% of the laboratory maximum dry density. Each lift shal
be treated in a like manner until the desired finished grades are
achieved.
-4-
5.2~ When placing fill in horizontal lifts adjacent to areas sloping steeper
than 5:l (horizontal to vertical), horizontal keys and vertical benches
shall be excavated into the adjacent slope area. Keying and benching
shall be sufficient to provide a minimum of three feet of vertical bench
height within firm natural ground or approved compacted fill. All keys
and benches shall be approved by the soil engineer or engineering geolo-
gist at the time of grading. No compacted fill shall be placed in an
area subsequent to keying and benching until the area has been approved
by the soil engineer or engineering geologist. Typical keying and
benching details have been included on the accompanying Grading Details-
GO-3, GO-4, and GO-5.
5.2d Within a single fill area where grading procedures dictate two or more
separate fills, temporary slopes (false slopes) will be created. When
placing fill adjacent to a false slope, benching shall be conducted in
the same manner as the above described. A minimum three-foot vertical
bench shall be established within the adjacent approved compacted fill
(i.e., the material underlying the surface loose material) prior to
placement of additional fill. Benching shall proceed in approximately
three-foot increments until the desired finished grades are achieved.
5.3a For field control purposes, "near-optimum" moisture shall be considered
to mean optimum plus-or-minus two percent unless otherwise approved by
the soil engineer at the time of grading.
5.3b Prior to placement of additional compacted fill following an overnight
or other grading delay, the exposed surface of previously compacted fill
shall be processed by scarification, watered or dried as needed,
thoroughly blended to near-optimum moisture conditions, then recompacted
to a minimum of 90% of the laboratory maximum dry density.
5.3c Following a period of flooding, rainfall or overwatering by other means,
no additional fill shall be placed until the existing ground surface is
thoroughly scarified, aerated, overexcavated if directed by the soil
engineer, blended to achieve near-optimum moisture conditions, then
thoroughly compacted to a minimum of 90% of the laboratory maximum dry density.
5.4a Fill Material: Excavated onsite materials which are approved by the
soil engineer may be utilized as compacted fill provided all trash,
vegetation and other deleterious materials are removed prior to
placement.
5.4b Where import materials are required for use onsite, the soil engineer
shall be notified at least 72 hours in advance of importing in order to
sample, test and approve or disapprove materials from proposed borrow
sites. No import materials shall be delivered for use onsite without
prior approval of the soil engineer.
5.4c Rocks 12 inches in maximum dimension and smaller may be utilized within
the compacted fill, provided they are placed in such a manner that
nesting of the rock is avoided. Fill shall be placed and thoroughly
compacted to the minimum requirement over and around all rock.
5.4d Rocks greater than 12 inches, but less than 3 feet, maximum Dimensions
(oversized rock) require special placement procedures if they are to be
utilized within compacted fills.
5.4e Rocks greater-than 3 feet should be broken down or disposed of offsite.
Oversized rock should not be placed within the upper 10 feet of any fill
and no closer than 15 feet to any slope face. Where practical, over- sized material should not be placed below areas where structures or deep
utilities are proposed. Oversized material should be placed in windrows
on a clean, overexcavated or unyielding compacted fill or firm natural
ground surface. Select native or imported granular soil (S.E.=30 or
better) should be placed and/or thoroughly flooded over and around all
windrowed rock, such that no voids remain. Windrows of oversized
material should be staggered so that successive strata of oversized
material are not in the same vertical plane. Details for oversized rock
placement are presented on Grading Detail GO-6.
5.5a Slopes: Unless otherwise recoInmended by the soil engineer and approved
by the regulating agency, compacted fill slopes shall be limited to a slope ratio of no steeper than 2:l (horizontal to vertical).
5.5b All compacted fill slopes shall be overbuilt and cut back to grade
exposing the firm compacted fill innercore. Th,e actual amount of over-
building may vary as field conditions dictate. If the desired results
are not achieved, the existing slopes should be overexcavated and
reconstructed. The degree of overbuilding shall be increased until the
desired compacted slope surface condition is achieved. Care should be
taken by the contractor to provide thorough mechanical compaction to the
outer edge of the overbuilt slope surface. As fill slope construction
proceeds, the slope surface shall be thoroughly backrolled with a sheepsfoot roller at vertical height intervals not exceeding four feet.
5.5c Following the attainment of the desired slope height, the outer surface
of overbuilt slopes should be cut back to a desired finished surface
contour. Care should be taken by the contractor not to excavate beyond
the desired finished slope surface.
5.5d In lieu of overbuilding and cutting back, alternative construction pro-
cedures may be attempted where specifically approved by the soil
engineer prior to grading. Prior to such approval, the contractor shall
submit to the soil engineer a detailed written descriptionof the proce-
dure he proposes to utilize. Within such a description, the followihg
guidelines may be included: Unless slopes are overfilled and cut back
to grade, the outer faces of all fill slopes shall be backrolled uti-
lizing a sheepsfoot roller at intervals not exceeding four feet of ver-
tical slope height. Vibratory methods may be required.
-6-
During construction of the fill slopes, care should be taken to maintain
near-optimum moisture conditiors over the entire slope height. Following achievement of the desired slope height, the entire slope face should be
thoroughly compacted utilizing a vibratory sheepsfoot roller. Upon
completion of the above procedures, the faces of all fill slopes should
be grid-rolled"over the entire slope height with standard grid-rolling
type of equipment. Prior to grid-rolling, care should be taken to main-
tain near-optimum moisture conditions.
5.5e Following slope construction in the manner described above, if the
required uniformly compacted fill slope condition is not achieved, over-
filling and cutting back should be adopted. Completed slopes not
approved by the soil engineer should be overexcavated a minimum of 12
feet (horizontal) and replaced by the overfilling and cutting back pro- '
cedure described above.
5.5f Where placement of fill above a natural slope or above a cut slope is
proposed, the fill slope configuration should conform to the applicable
requirements as indicated on Grading Detail GD-4.
5.59 For pad areas above fill slopes, positive drainage shall be established
away from the top of slope. This may be accomplished ntilizing a berm
and/or an appropriate pad gradient.
TYPICAL CAN’YON SUBDRAIN,
CANYON PROFILE --
C-v/u ANO :,~~ ALLuLWAL RS+~OVAL.
ALTERNATIVE A- PREFERRED ALTERNATIVE C
BACKHOE TRENCH DOZER V TRENCH
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6 /NC” LUA..,~XR .-an#vaNrLn P#a- EBERHART BI STONE INC.
GEOTECHNICAL CONSULTANTS 111, EAST WMTON ROAO. SUITE F . ANI”EIY. CALIFORNIA emu
STANDARD GRADING SPECIFICATIONS
TYPICAL SUBDRAIN FOR BUTTRESS, STABILIZATION
OR SIDEHILL FILL MASSES
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GRADING DETAIL
EBERHART & STONE INC.
GEOTECHNYAL CONSULTANTS
111, E*SI WINSTOW RclAO.S”IT~ F .ANA”EIY.CALlFORNIA 91808
STANDARD GRADING SPECIFICATIONS
IPlATE GO-2
TYPICAL STABILIZATION FILL
FIG. I
1111 EAST WINsrON ROAO.S”ITE F .~NIHelH,C~LIFORNILI9~ 06
STANDARD GRADING SPECIFICATIONS
L
TYPICAL BUTTRESS FILL
FIG 2
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GRADING DETAIL
EBERHART 8 STONE INC. --
GEOTECHNICAL CONSUlTANTS
TYPICAL FILL WER NATURAL SLOPE
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TYPICAL FILL OVER CUT SLOPE
WD OM “NW- .+TLANY
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GRADING DETAIL
EBERHART & STONE INC.
GEOTE~HNICAL CONSULTANTS 2211 LAST WlNSTcJN mm SUITE F . INIWEIM. CALIFORNI.4 92806
STANDARD GRADING SPECIFICATIONS
IPLATE CD-U
TYPICAL REMOVAL OF TRANSITION LOTS
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GRADING DETAIL
EBERHART 8 STONE INC.
GEOTECHNICAL CONSULTANTS
211 I EAST WINSTON ROAD: SUITE F ANAHLIU. CAIJFORIIIA wR?i
STANDARD GRADING SPECIFICATIONS
PLATE CD-5
TYPICAL ROCK WINDROW
PROPDIID .=m@a”aD 04.PI
TYPICAL WINDROW DETAIL (ledge view)
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PROFILE VIEW
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NOTES:
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:2-a dc -- H/,~~-- STANDARD GRADING SPECIFICATIONS
IPLATE CO-6