HomeMy WebLinkAboutTract Map 3883 Lot 368 Preliminary Geotechnical Investigation
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F1REUMINARY GEOTECHNICAL INVESTIGATION
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r\ngle - Lot ,Residential Development
Lot 368, Tra~0910 Avenida Del Reposo, Meadow View Estates
Temecula, Riverside County, California
,
December 7, 1993
PROJECT NO. 9319N)1
'.
PREPARED FOR:
Ruhl & Thelma Wolford
c/o TEC
30903 Avenida Del Reposo
Temecula, California 92591
I
Ea.rth Technics 29645".Va.lle Olvera, ,'f:llmecula, California. 92591 (909) 699-5451
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:December 7, 1993
Project No. 93197-01
.
INTRODUCTION
At your request, we have performed a Preliminary Geotechnical
Investigation for the above referenced site. The purpose of our
investigation was to evaluate the underlying soil conditions with
Irespect to the proposed development and to assess the geologic and
,engineering constraints that might exist considering this
. development.
The 20-Scale Precise Grading Plan prepared by TEC., Temecula dated
November 22, 1992, was used to direct our field work. We examined
!the site in the field accompanied by Mr. Dennis Jackson of TEC and
discussed the proposed development. Plate 1 presents our
Geotechnical data obtained during our field investigation.
IACCOMPANYING MAPS. ILLUSTRATIONS AND APPENDICES
Index Map - (2000-scale) - Page 2
Geotechnical Map - (20-scale) - Plate 1
"
Regional Fault Map - (1" = 20 miles) - Plate 2
'Appendix A - Geotechnical Trench Logs
Appendix B - Summary of Laboratory Test Results
Appendix C - General Earthwork and Grading Specifications
Appendix D - Slope Stability
Appendix E - References
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INDEX. MAP
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INDEX MAP
OF
LOT 368, TRACT 3883, AVENIDA DEL REPOSO, MEADOWVIEW
TEMECULA, RIVERSIDE COUNTY, CALIFORNIA
SOURCE: U.S.G.S. 7~ MIN. QUAD BACHELOR MIN. 1953 (PR 1973)
.3
93197-01
Page 3
SITE LOCATION/CONDITIONS
~
The roughly rectangular 0.61+/- acre property is located north of
,Avenida Del Reposo in the Meadow View Estates development of
southern Riverside County. The site is bounded by Avenida Del
iReposo on the south, vacant land to the east and north, and an
,existing residence to the west. The Index Map (Page 2) presents the
Itopographic and geographic relationships of the property to
'surrounding areas.
Topographically, the site is variable from 3-10 degrees descending
~to the west along Avenida Del Reposo at the front of the
lot, steepening at the rear to over 20 degrees in the vicinity of
:the proposed disposal system. The area of the house is moderately
Iflat to 8 degrees.
No permanent improvements were noted on site, but several dirt
piles had been stockpiled on the front of the lot.
:At the time of our field work the lot corners had been surveyed and
.staked.
No bedrock outcrops were located on site. Vegetation consisted of
,light growths of grass and low weeds.
PROPOSED DEVELOPMENT
,
We understand that the site will be utilized for a 1 & 2-story
,single family residence of 3 bedrooms. The sewage disposal is
proposed by use of the septic tank/leach line method in an area
which is to remain natural ground. According to the referenced
grading plan, cuts at 2:1 (horizontal to vertical) to a maximum
height of 8 feet will be constructed on the southeast, and fill at
2: 1 to a maximum height of 20 feet will be constructed on the
northeastt. Several retaining walls varying in height from 5-8 feet
,will be constructed along the northwest pad area, and eastern
property line.
;
SCOPE OF SERVICES
.The scope of our investigation included the following:
,1. A review of available data pertinent to the site, both
pUblished and in-house unpublished data.
.:\
93197-01
Page 4
.2.
Subsurface exploration of the site utilizing 3 shallow
exploratory backhoe trenches to depths as great as 15.2 feet.
The trenches were logged, and these logs appear in Appendix A
of this report. The trenches were tested for in-place density
utilizing the Drive Cylinder Method (ASTM D2937-71).
Representative bulk samples were obtained for testing.
,
3.
Laboratory testing of representative
develop soil engineering parameters
development.
earth
for
materials to
the proposed
4. Preparation of this report presenting our findings,
conclusions and recommendations concernlng site development
based upon an engineering analysis of geologic and
geotechnical properties of the subsoils as determined by field
and laboratory evaluation.
LABORATORY TESTING
The following tests were performed for this project in our
laboratory in accordance with the American Society for Testing and
'Materials, the state of California Standard Specifications or
contemporary practices of the soil engineering profession.
:Maximum Density - optimum Moisture Determinations
!This test determines the density that a soil can be compacted to at
various contents. For each soil moisture, there is a maximum dry
density obtained and the associated optimum moisture content. The
'results are used to evaluate the natural compaction, control of the
. grading process and as an aid in developing the soil bearing
capacity. This is based on ASTM Standard D1557-78 (five layer
'method) .
:In-situ Moisture and Density
:These tests consisted of weighing and measuring the Drive Cylinder
,samples (ASTM D2937-71) in the trenches to determine in-place
moisture and density. The resul ts are used to analyze the
consistency of the subsoils and aid in determining the necessary
grading to prepare the pad area.
-:5-
, 93137-01
,Page 5
;Sieve Analvsis
.
This test determines
iparticle sizes and
.classification.
the material
is used in
grading of
generating
the individual
an engineering
;Sand Equivalent Testinq
:This is a test for the rapid determination of the relative portions
:of fine silt and clay materials within the soil samples, and is
,used for a relative comparison of soils in the determination of the
'adequate paving sections for driveways, etc.
!Expansion Testinq
.The expansion index of the soils are determined by the U.B.C.
'Method 29-2 and is used to design foundations for anticipated
expansion forces.
,Direct Shear
'A direct shear strength test was performed on a representative
sample of the on-site soils remolded to 90% relative compaction.
:To simulate possible adverse field conditions, the sample was
,saturated prior to shearing. A saturating device was used which
,permitted the samples to absorb moisture while preventing volume
change. This test is used to determine soil strengths for slope
> stability evaluations and for foundation bearing capacity.
SUBSURFACE CONDITIONS
!The site is underlain by a thick colluvial/soil deposit of silty
sand with a trace of clay. Maximum thickness is about 3.5 feet on
.the northeast with low moistures and low densities. In-place
densities for the colluvium was measured at 94.3 pcf (74.4%
:relative compaction) in T-1 at 1. 5-2.0 feet and 9.7% moisture.
Beneath the colluvium at depths as shallow as 2.8 feet (Trench T-2)
:is the sedimentary bedrock of the pauba Formation. This unit
'consists of a sequence of interbedded siltstones, sandstones and
gravelly sandstones-all with varying percentages of clay.
"
, 9:3197-01
Page 6
In-place densities for the Paulba formation were moderately high
from 119.8pcf (91.3%) at 5-5.5 feet in Trench T-l, to 120.2 pcf
(91.6%) at 3.4-4.0 feet in T-2.
,
The orientation of the bedrock is very low angle at less than 6
:degrees to the southeast. No evidence of down slope movement is
,apparent in any of the surrounding natural slopes. (See also Slope
:Stability Section).
GROUND WATER
Ground water was not encountered to a depth of 15.2 feet at the
. lowest portion of the lot, nor was it encountered during a previous
:percolation test at the rear of the lot. Our field investigation
.displayed no evidence, such as mottling, to indicate that perching
:of ground water occurs at the soil/bedrock contact beneath the
:site. No evidence of seepage was seen in the natural slope faces.
Water has never been encountered in this area at depths less than
,25-30 feet below the ground surface, except seasonally within the
'stream channels.
FLOODING
,According to the Federal Emergency Management Agency and the County
of Riverside, the site is not located within the boundaries of a
lOa-year flood plain. The large swale located 300 feet north of
:the rear portion of the site would not impact the site, but is
included in the 100-year flood plain.
GEOLOGY
:The entire site is underlain by the Pauba Formation a sedimentary
,bedrock of early Quaternary age. The formation represents a series
:of terrestrial stream bed deposits which varies rapidly from silts
:to sands and clean gravelly sands. Portions of the formation
'including at the site can be very sandy. The vague bedding exposed
'in T-1 and T-3 had an orientation across the site of N 20 - 40 E
and 2-6 degrees south. No evidence of slope instability exists at
the site.
M.P. Kennedy (1976) shows no lineaments or other possible fault-
related geomorphic features crossing the site.
I
93197-01
'Page 7
SEISMIC SETTING/GROUND MOTION PARAMETERS
.
The regional seismic setting is shown on Plate 2. The nearest
active or potentially active faults to the site includes the
IElsinore (1.8 miles southwest) , and the San Jacinto (15.4 miles
Inortheast) .
The Elsinore (Wildomar) Fault because of its proximity to the site
,is the design fault when evaluating the site seismic parameters.
TABLE 1
COMPARISON OF SEISMIC PARAMETERS
.Paul t
Maximum Peak Ground
Probable Acceleration
Distance to site Earthquake (M) At site (q)
1.4 Miles SW 6.8 0.40
15.4 Miles NE 7.2 0.15
.Elsinore
,San Jacinto
HISTORIC SEISMICITY
As shown in Table 2, during the last 100 years in the San
Bernardino/Riverside area, the greatest number of moderate to large
earthquakes (greater than 6.0 M) have occurred along the San
Jacinto Fault (Hileman, Allen and Nordquist, 1974). The most
significant earthquake epicenter on the Elsinore occurred 10 miles
northwest at Lake Elsinore in 1910 estimated as a 6.0 magnitude
.event.
s
93197-01
Page 8
TABLE 2
EARTHOUAKE EPICENTERS GREATER THAN 6.0 M WITHIN 65 MILES
Richter Approx. Distance to
,Date Maqnitude site form Epicenter Fault
,
1857 8.2 88 miles NW San Andreas
1899 7.1 25 miles SE San Jacinto
1910 6.0 5 miles SW Elsinore
.1918 6.8 37 miles NE San Jacinto
1948 6.5 43 miles NE MissionCreek
1972 6.2 54 miles NW San Fernando
1986 6.2 57 miles SE San Andreas
,We have utilized the computer program titled EQ
(1989) to assess historic activity at the site.
analysis, the maximum ground acceleration at the
:period of 1800 to present is 0.24g.
SEARCH (Blake
Based on this
site from the
SEISMIC EXPOSURE
:Although no precise method has been developed to evaluate the
seismic potential of a specific fault, the available information on
historic activity may be projected to estimate the future activity
.of the fault. This is usually done by plotting the historic
:activity in terms on number of events in a given time interval
versus magnitude of the event. Based on such plots, recurrence
intervals for earthquakes of given magnitudes may be estimated.
The other method of determining maximum probable capability of the
!fault is by evaluating the accumulated stress and determining the
subsequent release of this stress in the form of an earthquake over
a given interval of time.
We have utilized strain rates of 0.8 em/year for the Elsinore fault
as suggested by Clark, Harms, et al (1984) to estimate the
maximum probable earthquake. For this project the maximum probable
or "design earthquake" is defined by CDMG Note 43 at the maximum
historical event with a recurrence period of 100 years. We
'estimate the maximum probable or "design earthquake" for the
,Elsinore fault to be 6.8 magnitude. This is in agreement with the
deterministic model by Blake, (1989).
9
93197-01
Page 9
Based on data presented by Greensfelder (1974), we estimate the
maximum credible event for the Elsinore Fault in this region would
be an event of 7.0 magnitude. The maximum credible event is the
,greatest event that the fault appears capable of theoretically
producing without a consideration of time interval based upon the
'present tectonic framework.
GROUND MOTION CHARACTERISTICS
. The ground motion characteristics which could affect the site
'during the postulated maximum probable earthquake of 6.8 magnitude
'on the Elsinore Fault were estimated. Available information in the
literature about maximum peak bedrock acceleration and its
attenuation with distance (Schnabel & Seed, 1973), the effects of
:site-soil conditions on surface ground motion parameters (Seed &
Idress, 1982), and site response criteria (Hays, 1980) were
,utilized.
This information indicates that maximum peak rock acceleration on
'the order of 0.40 g may be anticipated at the site. Maximum ground
surface acceleration is expected to be dampened by the thick (1200
feet) sedimentary sequence to about 0.28g.
iRepeatable ground acceleration can be estimated at 65 percent of
ipeak ground acceleration for design purposes (Ploessel & Slosson,
.1974) with a value of about O.16g. The predominant period of
,bedrock acceleration is expected to be 0.30 seconds with 24 seconds
:of strong ground shaking (Bolt, 1973).
SECONDARY SEISMIC HAZARDS
.
The dense nature of the underlying sedimentary bedrock coupled with
:the depth to groundwater of over 25 feet precludes such secondary
seismic hazards as liquefaction, lateral spreading or settlement at
:the site. No rockfall or landslide hazard exists at the site. The
potential for seismically-triggered landslides is discussed in
,detail under the slope stability section.
:According to the County Maps and Alquist-Priolo Special Studies
Zone Map, the site is not included in the Special Studies Zone for
'any active or potentially active faults.
\0
9.3197-01
Page 10
CONCLUSIONS AND RECOMMENDATIONS
: Foundation :Desiqn
,
,A strip and spread footing foundation system should provide an
;adequate foundation for one and two-story buildings in this site.
,All exterior footings should be founded a minimum of 18 inches
Ibelow adjacent finished grade for two-story buildings, and 12
inches for one-story buildings. Interior footings may be founded
'a minimum of 12 inches below finished grade. When the footings are
founded in a minimum of 2 feet of properly compacted fill or dense
,bedrock, an allowable bearing capacity of 1800 psf for 12 inch wide
footings is acceptable for dead plus live load. This value may be
,increased by one-third for short term wind and seismic loading
conditions.
When foundations are placed in natural soils, no cobbles over 6
inches should be left within the base of the foundation. A typical
!foundation design is included in Appendix C. One No.4 bar top and
,bottom is recommended as a minimum design.
;sett1ement
Our subsurface investigation revealed that the natural soils below
a depth of 2.0 to 3.0 feet are dense. When the upper 2-3 feet of
!fill is prepared in accordance with the "Foundation Design" and
compacted fill requirements, footings should experience less than
;1-inch settlement with less than 1/2 inch differential settlements
'between adjacent footings of similar sizes and loads. This
settlement is based upon grading of up to 30+ feet of fill. If
'thicker fills are proposed, settlement could be greater and should
be evaluated prior to placement.
:Concrete Slabs-On-Grade
Sufficient fine-grained materials exists within near surface earth
:materials to possible create moisture problems. Therefore, we
recommend that a moisture barrier be placed under any concrete
,slabs that might receive a moisture-sensitive floor covering. This
moisture barrier should consist of a 10-mil polyethylene vapor
\I
'93197-01
. Page 11
ibarrier sandwiched between a 1-inch layer of sand, top and bottom,
'to prevent puncture of the barrier and enhance curing of the
,concrete. Nominal reinforcement of the slabs with light 6 inch by
,6 inch, 10 gauge/ 10 gauge welded wire fabric is advisable. The
,subgrade below the slab should be moisture conditioned and properly
,compacted prior to placement of concrete.
IEXtlansive Soils
;Expansion testing of near-surface soils (T-1 ; 0-3 feet) indicate
'the near surface soils have a low expansion potential.
!Earthwork Shrinkaqe and Subsidence
,When the 2 feet of overexcavated soils are regraded to compacted
'fill standards, earthwork shrinkage would be in the range of 5 to
,20 percent with a recommended average of approximately 9 percent.
i Earthwork operations should cause only a nominal subsidence of
approximately 0.1 foot or less.
IRetaininq Wall Desiqn
:Retaining walls should be designed using the following parameters:
.0
:0
o
Active pressure
Active pressure
Active pressure
(level backfill)
(2: 1 backfill)
(1 1/2:1 backfill)
50 lb/ft /ft
57 lb/ft /ft
66 lb/ft/ft
IFor purpose of lateral resistance, a value of 0.30 may be used for
:frictional resistance. A value of 275 lb/ft /ft may be used
~ :for passive resistance for footings placed into properly compacted
:fill. Frictional and passive resistance may be combined, provided
:the later is reduced by one-third.
Special loads for dead plus actual loads whould be considered in
,the driveway/parking area that is retained.
!Lateral Loads
Lateral loads in the near-surface soils are:
'Acti ve
'At Rest
,passi ve
- 42 pounds per square foot of soil depth (psf/ft)
- 62 psf/ft
- 275 psf/ft (for wood shoring)
350 psf/ft (for concrete footings)
1Z.
'93197-01
:Page 12
,Active means movement of the structure away from the soil; at rest
,means the structure does not move relative to the soil (Such as a
loading dock); and Passive means the structure moves into the soil.
The coefficient of friction between the bottom of the footings and
'the native 'soil may be taken as 0.30.
'Trench Stability
The near-surface soil to a depth of 5 feet should stand vertically
,when excavated, however, trenches in excess of 5 feet in depth
,should have the sides laid back at 1: 1 in accordance with OSHA
,requirements.
;Slope Stability
The current grading, including slopes and finished face
inclinations, indicates the maximum slope height is 20 feet or
less. The moderately high strength values allow 2:1 (horizontal to
vertical) slopes up to 25 feet without gross instability.
Selection of Shear Strenqth Parameters
The following shear strength parameter utilized for our slope
stability analysis was determined by our laboratory test results as
presented below:
Material
(Cut or Fill)
Friction Angle
(Deqree)
Cohesion
lb/ft2
'Anticipated On-Site Fill
32
375
o
,We have utilized values of 32 degrees and 375 lbjft2 for bedrock cut
,slopes although it represents a conservative number, determined
;from a remolded saturated sample. Bedrock is expected to be 20% +
stronger (Coduto, 1989).
'Even more critical to overall cut slope performance is the
orientation of joints, fractures and bedding. Plate 1 presents our
'f ield measurements of the vague bedding, and as can be seen on
Plate 1, no adverse out-of-slope components are present to initiate
"block" or "wedge" type failures.
\3
93197-01
,Page 13
!Drainage and terracing should be in accordance with Uniform
!Building Code Chapter 70 requirements. At no time should water be
'diverted onto the slope face in an uncontrolled and erosive
. fashion. Rapid erosion and rutting of the fill slopes is possible
land they should be planted with drought resistant landscaping as
,soon as possible.
GENERAL SITE GRADING
1. Clearinq and Grubbinq
,The vegetation will require clearing and removal off-site. Any
!boulders larger than 12 inches should not be placed in any
structural 'fill.
;2. Preparation of Buildinq Pad Areas
The proposed building pad is shown in transition and will require
an overexcavation from rough grade to eliminate the exposed cut and
Ifill transition contact. A typical detail is shown in Appendix C.
;3. Preparation of Surface to Receive Compacted Fill
:All sufficiently dense (85 percent relative compaction) surfaces
,which are to receive compacted fill should be scarified to a depth
'of 6 inches, brought to near optimum moisture content and compacted
:to 90 percent relative compaction. other softer areas must be
:overexcavated to sufficiently dense material and recompacted. This
,would include raising existing fill grades. Typical overexcavation
depths based on our field testing would be 2-3 feet. Actual depth
of removal should be determined at the time of grading by testing.
:4. Placement of Compacted Fill
Compacted fill is defined as that material which will be replaced
in the areas of removal due to root removal, the placement of
!footings and paving, and also wherever their grade is to be raised.
'All fill should be compacted to a minimum of 90 percent based upon
:the maximum density obtained in accordance with ASTM D 1557-78
\~
9:3197-01
Page 14
procedure. The area to be filled will be prepared in accordance
'with the preceding section. The recompaction of the cut material
may be waived if field density tests indicate densities in excess
,of compacted fill standards.
Fills placed on natural slopes of 5:1 (horizontal to vertical) or
,steeper will require a key and benching as shown in Appendix c.
S. Pre-Job Conference
'Prior to the commencement of grading, a pre-job conference should
be held with representatives of the owner, developer, contractor,
architect and/or engineer in attendance. The purpose of this
:meeting shall be to clarify any questions relating to the intent of
'bhe grading recommendations and to verify that the project
,specifications comply with recommendations of this report.
'6. Testinq and Inspection
,During grading, density testing should be performed by a
representative of the soil engineer in order to determine the
degree of .compaction being obtained. Where testing indicates
insufficient density, additional compactive effort shall be applied
,with the adjustment of moisture content where necessary, until 90
Ipercent relative compaction is obtained.
Inspection of critical grading control procedures such as keys,
installation or need for subdrains should be made by a qualified
soils engineer or engineering geologist.
,
'7. Development Impact
,Provided the recommendations of this report are incorporated into
'the design and construction of the residential project, both the
proposed development and off-site areas will be safe from geologic
hazards.
15'
93197-01
Page 15
GENERAL
,All grading should, at a minimum, follow the "Standard Grading and
Earthwork Specifications" as outlined in Appendix C, unless
otherwise modified in the text of this report. The recommendations
lof this report are based on the assumptions that all footings will
,be founded in dense, native, undisturbed soil or properly compacted
fill soil. All footing excavations should be inspected prior to
,the placement of concrete in order to verify that footings are
'founded on satisfactory soils and are free of loose and disturbed
,materials and fill. All grading and fill placement should be
Iperformed under the testing and inspection of a representative of
'the soil engineer.
The findings and recommendations of this report were prepared in
accordance with contemporary engineering principles and practice.
,We make no warranty , either express or implied. Our
,recommendations are based on an interpolation of soil conditions
,between trench locations. Should conditions be encountered during
grading, that appear to be different that those indicated by this
,report, this office should be notified.
(4) Addressee
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EXPLANATION
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~ EXPLORATORY TRENCH by EARTH TECHNICS
SYSTEM DESIGN
'.
* 3-BEDROOM HOUSE REQUIRES,1000-GALt.ON SEPTIC TANK
* RECOMMENDED APPLICATION RATE OF 30 SQUARE FEET IS
300 ,SQUARE FEET OF ABSORPTION AREA
* 30% SLOPE REQUIRES 1.3. COVER FACTOR OR 390'SQUARE FEET
OF ABSORPTION AREA
. ..:.* UTILIZING 1 FOOT' OF GRAVEL 130 LINEAR FEET OF 3-FOOT,
WIDE LEACH tINE IS REQUIRED
. .' ~.-
* NO. PORTION OF ABSO;u'TION SYSTEM UNDER DRIVEWAYS. HORS,E<;:ORRALS
. PORCHES. . .
'.........
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BEDDING ATTITUDE
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EXPLORATORY TRENCH by Calif. Gee Tek
3/22/84
YTP'4
PERCO~TION TEST by Calif. Gee Tek
3/22/84
'.
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PRIMARY &
* SEPTIC TANK BENEATH CONCRETE lHLL REQUIRE ACCESS COVER .
r--,
~"_ _ 100% LEACH LINES
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PLATE 1
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MAJOR EARTHQUAKES Bnd RECENnv ACTIVE FAUlTS h
SOUTHERN CALIFORNIA REGION
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SUMMARY OF FIELD DENSITY TESTING
Moisture
'Test Test Depth Dry Density Content soil Relative
No. (Feetl (pcfl (%l Tvpe Compaction
R-l 1.5 -2.0 94.3 9.7 A 74.4
R-2 5.0 -5.6 119.8 7.8 B 91.3
R-3 3.3 -4.0 120.2 8.2 B 91.6
MAXIMUM DENSITY - OPTIMUM MOISTURE DETERMINATION
The maximum density was determined in accordance with ASTM standard
:D1557-78. The result by full laboratory curve is :
Sample
; Location
Depth
(Feet) Soil Description
Maximum
Drv Densitv
Optimum
Moisture
T-1
4-6
(Soil Type B) Pauba fm 131.3
+ sandstone bedrock
Light yellow brown
to brown gray silty
sand with gravel &
trace of clay
11. 4
SUMMARY OF EXPANSION TESTING
U.B.C. METHOD 29-2
;Sample Location
Depth
Expansion Index Expansion Potential
T-1
4-6'
26 Low
SAND EOUIVALENT TESTING
,Sample Location
Depth
Sand Equivalent
T-1
4-6'
18
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PER CENT FINER BY WEIGHT
GRAIN SIZE DISTRIBUTION
By:iwLS Oat.: l'l-/~?
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Earth Tech,o,ics
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EXCAVATION NO. T-1 DEPTH: 4 -6'
SATURATED TEST IN SITU MOISTURE TEST
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DIRECT SHEAR TEST DATA
'.'
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Earth Technics
EXHIBIT
t6,. .
JoeNo"0!l1~1~of DATE: IU9?J
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APPENDIXC
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. . .
STANDARDGRAD1NG AND EARTHWORK SPECIFICATIONS
These specifications present Earth Technics Inc., standard
recommendations for grading and earthwork.
No deviation from these specifications should be permitted unless
specifically superseded in the geotechnical report of the project
or by written communication signed by the Geotechnical
Consultant. Evaluations performed by the Geotechnical Consultant
during the course of grading may result in subsequent
recommendations which could supersede these specifications or the
recommendations of the geotechnical report.
1.0 GENERAL
,1.1 The Geotechnical Consultant is the Owner's or
Developer's representative on the project. For the
purpose of these specifications, observations by the
Geotechnical Consultant include observations by the
Soils Engineer, Geotechnical Engineer, Engineering
Geologist, and those performed by persons employed by
and responsible to the Geotechnical Consultant.
1.2 All clearing, site preparation, or earthwork performed
on the project shall be conducted and directed by the
.Contractor under the supervision of the Geotechnical
,Consul tant. . .
1.3 .The Contractor should be responsible for the safety of
the project and satisfactory completion of all grading.
:During grading, the Contractor shall remain accessible.
,
'-
1.4 .Prior to the commencement of grading, the Geotechnical
Consultant shall be employed for the purpose of
;providing field, laboratory, and office services for
:conformance with the recommendations of the
:geotechnical report and these specifications. It will
,be necessary that the Geotechnical Consultant provide
adequate testing and observations so that he may
determine that the work was accomplished as specified.
'It shall be the responsibility of the Contractor to
assist the Geotechnical Consultant and keep him
apprised of work schedules and changes so that he may
schedule his personnel accordingly.
1.5 It shall be the sole responsibility of the Contractor
to provide adequate equipment and methods to accomplish
the work in accordance with applicable grading codes,
agency ordinances, these specifications, and the
approved grading plans. If, in the opinion of the
Geotechnical Consultant, unsatisfactory conditions,
such as questionable soil, poor moisture condition,
inadequate compaction, adverse weather, etc., are
I
.
I
.{;~
Standard Grading and' Earthwork Specifications.
Page Two
resulting in a quality of work less than required in
these specifications, the Geotechnical Consultant will
be empowered to reject the work and recommend that
construction be stopped until the conditions are
rectified. .
1.6 It is the Contractor's responsibility to provide access
to the Geotechnical Consultant for testing and/or
grading observation purposes. This may require the
excavation of test pits and/or the relocation of
,grading equipment. ''''
1.7 A final report shall be issued by the Geotechnical
:Consultant attesting to the Contractor's conformance
Mith these specifications.
2.0 SITE :PREPARATION
.'
2.1 All vegetation and deleterious material shall be
disposed of off-site. This removal shall be observed
:by the Geotechnical Consultant and concluded prior to
.fill placement. .. ,.
2.2 soil, alluvium, or bedrock materials determined by the
-Geotechnical Consultant as being unsuitable for
placement in compacted fills shall be removed from the
site or used in open areas as determined by the
Geotechnical Consultant. Any material incorporated as
a part of a compacted fin must be approved by the
Geotechnical Consultant prior to.fill placement.
2.3 After the ground surface to receive fill has been
cleared, it shall be scarified, disced,or bladed by
r the Contractor until it is uniform and' free from ruts,
hollows, hummocks, or other uneven features which may
prevent uniform compaction. .
. The scarified ground surface shall. then-- be'brought to
optimum moisture, mixed as required, ,and~compactedas
specified. If the scarified zone is greater than
twelve inches in depth, the excess shalt,be removed and
placed in lifts not to exceed six inchesor less.
.
Prior to placing fill, the ground surface to
fill shall be observed, tested, and approved
Geotechnical Consultant.
receive
by the
-./.,,..'.'",'
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standard Grading and .Earthwork specifications
Pll.ge 'rhree
2.4 Any underground structures or cavities such as
cesspools, cisterns, mining shafts, tunnels, septic
tanks, wells, pipe lines, or others are to be removed
or treated in a manner prescribed by the Geotechnical
Consultant.
2.5 In cut-fill transition lots and where cut lots are
partially in soil, colluvium or unweathered bedrock
materials, in order to provide uniform bearing
conditions, the bedrock portion of the lot extending a
minimum of 5 feet outside of building lines shall be
overexcavated a minimum of 3 feet and replaced with
compacted fill. Greater overexcavation couldbe
required as determined by Geotechnical Consultant where
deep fill of 20+ feet transitions to bedrock over a
short distance. 'rypical details are given on Figure D-
1.
:3.0 COMPACTED FILLS
3.1 Material to be placed as fill shall be free of organic
matter and other deleterious substances, and shall be
ll.pproved by the Geotechnical Consultant. Soils of poor
gradation, expansion, or strength characteristics shall
be placed in areas designated by Geotechnical
Consultant or shall be mixed with other soils to serve
as satisfactory fill material, as directed by the
Geotechnical Consultant.
3.2 Rock fragments less than twelve inches in diameter may
be utilized in the fill, provided:
1.
They are not placed in concentrated pockets.
I
.
I
2. There is a minimum of 75% overall of fine grained
material to surround the rocks.
3. The distribution of rocks is supervised by the
Geotechnical Consultant.
3.3 Rocks greater than twelve inches in diameter shall be
taken Off-site, or placed in accordance with the
recommendations of the Geotechnical Consultant in areas
designated as suitable for rock disposal. (A typical
detail for Rock Disposal is given in Figure 0-2.
-:P
. Standard Grading and Earthwork Specifications
Page. Four ..
'.
3.4 .' Material that is spongy, subject to decay ,or otherwise
considered unsuitable shall not be used in the
compacted fill.
3.5 Representative samples of materials to be utilized as
compacted fill shall be analyzed by the laboratory of
the Geotechnical Consultant to determine their physical
properties. If any material other than that previously
tested is encountered during grading, the appropriate
analysis of this material shall be conducted by the
Geotechnical Consultant as soon as possible.
3.6 Material used in the compacting process shall be evenly
spread, watered, processed, and compacted in thin lifts
not to exceed six inches in thickness to obtain a
uniformly dense layer. The fill shall be placed and
compacted on a horizontal plane, unless otherwise
approved by the Geotechnical Consultant.
3.7 If the moisture content or relative. compaction varies
:from that required by the Geotechnical-Consultant, the
:Contractor shall rework .the fill until' it is approved
by the Geotechnical Consultant.' .'
.
3.8 ~Each layer shall be compacted to 90 percent of the
.maximum density in compliance with the testing method
!specified by the controlling governmental agency or
ASTM 1557-70, whichever applies.
:If compaction to a lesser percentage is authorized by
,the controlling governmental agency because of a
:specific land use or expansive soil condition, the area
'to receive fill compacted to less than 90 percent shall
either be delineated on the grading plan or appropriate
,Lef~~ence made to the area in the geotechnical report.
.
I
3.9 :All fills shall be keyed and benched through all
topsoil, colluvium alluvium, or 'creep material, into
sound bedrock or firm material where the-slope
receiving fill exceeds a ratio of' five horizontal to
one vertical, in accordance with the recommendations of
the Geotechnical Consultant. " .'
,
.-:='-.
3.10 The key for side hill fills shall be a minimum width of
15 feet within bedrock or firm materials,'unless
. otherwise specified in the geotechnical report. (See ,
detail ,on Figure 0-3.) . ., .-. .
'-.,.
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" "
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, ".
.'.C.
.Standard Grading and'Earthwork Specifications
Page Five
3.11 Subdrainage devices shall be constructed in compliance
with the ordinances of the controlling governmental
agency, or with the recommendations of the Geotechnical
Consultant. (Typical Canyon Subdrain details are given
in Figure 0-4.)
3.12 The contractor will be required to obtain a minimum
relative compaction of 90 percent out to the finish
slope face of fill slopes, buttresses, and
stabilization fills. This may be achieved by either
over building the slope and cutting back.to the
compacted core, or by direct compaction of. the slope
face with suitable equipment, or by any other procedure
which produces the required compaction approved by the
Geotechnical Consultant.
3.13 All fill slopes should be planted or protected from
erosion by other methods specified in ~he Geotechnical
report.
3.14 Fill-over-cut slopes shall be properly. keyed through
topsoil, colluvium or creep material into rock or firm
materials, and the transition shall be, stripped of all
soil prior to placing fill. (See detail on Figure 0-
'3. )
4.0 CUT SLOPES
4.1 The Geotechnical Consultant shall inspect all cut
slopes at vertical intervals not exceeding ten feet.
4.2 If any conditions not anticipated in the geotechnical
repor-l:; such as perched water, seepage, lenticular or
confined strata of a potentially adverse' nature, ..
unfavorably inclined bedding, joints or fault planes
encountered during grading, these conditions shall be
analyzed by the Geotechnical Consultant, 'and
recommendations shall be made to mitigate these
. problems. (Typical details for stabilization of a
portion pf a cut slope are given in Figures D-3a and D-
5. )
I
r
4.3 ,cut slopes that face in the same direction as the
prevailing drainage shall be protected from slope wash
by a non-erodible interceptor swale placed at the tope
:of the slope.
", .
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,." :'
'. :Standard Grading and Earthwork Specifications
jPage Six
4.4 Unless otherwise specified in the geotechnical report,
no cut slopes shall be excavated higher or steeper than
that allowed by the ordinances of controlling
'governmental agencies.
4.5 Drainage terraces shall be constructed incompliance
with the ordinances of controlling governmental
agencies, or with the recommendations of the
Geotechnical Consultant.
5.0}'TRENCH BACKFILLS
5.1 Trench excavations for utility pipes shall be
backfilled under the supervision of the Geotechnical
Consultant.
5.2 After the utility pipe has been laid, the space under
and around the pipe shall be backfilled with clean sand
'or approved granular soil to a depth of at least one
foot over the top of the pipe. The sand backfill shall
be uniformly jetted into place before the controlled
backfill is ,placed over the sand. .... _"
5.3 The on-site materials, or other soils'~pproved by the
-Geotechnical Consultant shall be watered and mixed as
necessary prior to placement in lifts over the sand
backfill.
5.4 The controlled backfill shall be compacted to at least
90 percent of the maximum laboratory density as
determined by the ASTI 01557-70 or the controlling
governmental agency.
5.5 Field density tests and inspection of the' backfill .
procedures shall be made by the Geotechnical Consultant
during backfilling to see that proper moisture content
and uniform compaction is being maintained. The.
contractor shall provide test holes and exploratory
pits as required by the Geotechnical Con~u1tant to
.enable . sampling and testing.
6.0. GRADJ:NG CONTROL
I
r
6.1
:Inspection of ,the fill placement shall be~ provided by
.'the .Geotechnical Consultant during the progress of
:grading.
. .~,,:~~:,~>;~, .
, .
,.:-;;:......,..,........
,?/!/
," i:.
standard'Grading and'Earthwork Specifications
Page Seven
6.2 In general, density tests should be made at intervals
not exceeding two feet of fill height or every 500
cubic yards of fill placed. This criteria will vary
depending on soil conditions and the size of the-job.
In any event, an adequate number of field density tests
shall be made to verify that the required compaction is
being achieved.
6.3 Density tests should also be made on the surface
material to receive fill as required by the
Geotechnical Consultant. .
6.4 All cleanout, processed ground to receive fill, key
excavations, subdrains, and rock disposals should be
inspected and approved by the Geotechnical Consultant
prior to placing any fill. It shall be the
Contractor's responsibility to notify the Geotechnical
Consultant when such areas are ready for inspection.
7.0 CONSTRUCTION CONSIDERATIONS
7.1 Erosion control measures, when necessary, shall be
provided by the Contractor during grading and prior to
the completion and construction of permanent drainage
':controls.
7.2 Upon completion of grading and termination of
,inspections by the Geotechnical Consultant, no further
filling or excavating, including that necessary for
:footings foundations, large tree.wells, retaining
,walls, or other features shall be performed without the
approval of the Geotechnical Consultant.
7.3 Care shall be taken by the Contractordurinq final
grading to preserve any berms, drainage terraces,
interceptor swales, or other devices of permanent
nature on or adjacent to the property.
I
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I
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TRANSITION LOT DETAILS
CUT-FILL LOT
.. NATURAL GROUND
l~
-
-
-- -
- --
-- 5' I-
_ _-- _--- MIN. ~ .
:cOMiA~fED ::FILi.:-:-:02-::;--I;.'Wh~-~ ~ ~-:-:--f::----_:::=-:::=: 30" MIN.
,_________________.~I\..... ___>- ,'" "\' ". --r-.
.___________.......e-___..._..J.,.:r:__......-_ T
--::~:~~?~~\i~S~~~-:-:-: OVEREXCAVATEAND RECOMPACT
,- -.,.-.,.- -:.o":\}~_:"'-- "'-"'^ '
.=-_- -;''ij\O'J ~--: .,,;:;.:::"'---
-::.?-"" --.:.-----
,.
UNWEATHERED BEDROCK OR 1
r- MATERIAL APPROVED BY . -----I
1 THE GEOTECHNICAL CO.NSULTANT
CUT LOT
NATURAL. GROUND
1-
--
--
-.
--- ..... -- -- .----
--- --- .".. ---
~--- .""..""'"
...-.- ,,---- " - -..:- REMOVE - -. h
_~ _ _ - - --'1:l~;~~:;~tE~~'~ ...... -~r~.
~----------------------~--.~------------------------~
--------------------~~~~------~------------
---_-:....--=---...:-_--....:-_-- -- ------ -- -- ~ -----
.-;CciMPACTEO==------...;:~-: ~"
:...:~~~~ OVER EXCAVATE AND RE~OMPACT
f
r
UNWEATHERED BEDROCK OR co.. ,-
MATERIAL APPROVED BY '.C"
r THE GEOTECHNICAL CONSULTANT '. <t.'
. ... ," .
.NOTE: . '. ' '. ';:':':.'.
. . . Deeper overexeovation and recomoadion shall be p~~f~~~d
"if determined '0 be neeesscry by the geotechnical consultant.
"
.
'-'::':?:';;~"'.
.h:-..'~!~.,;r,:19:-;,.,-, "
..,....
?:;?
'-
"'-.-;:~":.:.--:"
BENCHING DETAILS
PROJECTED PLANE
I to I maximum from toe
- - ------.
----:-:-:.COMPACTeD -:-:-:-:-:.
__~-:-:-:-:"';--=_:':;FILL ::-.::-::~-:~
---------------------
-----------~---_---.-----_-:..---:;~_-:-_-~
_--: _::-~::-:~:;-:i"-:-=E"~-:;;.=-~
___-..:_..:_ .:_-_-_-..:_.:_-::_ _ .:_~- - --- - - -::1'
_-_-_-_-_-_-_-_-:..~~----;- I,,~r^' .
-------------- --
------------- -- - .
_____-_-_-_-;r_-___-_-;,- \~/
of slope to approved ground ..:_:-:-::-::_2~-_-:-::_-;~.:.: . . \ .
__________... ! .. REMOVE
.:;2".--'=::-::-----:::-::- UNSUIT ABU:
__-------:7-:""--- MATERIAL
_ _ -::_~:j:~C~;. M1N ~.~-
/4 ~ -_-;..---_~-------- BENCH' BENCH'
^ 1 -r-_-;;~------.:.:..:---.: I HEIGHT
--I- ----------- (' I)
__-_-..=2% MIN.:"'-':: typlCO VARIES
-----~----
T ~^"" -; :v-
2' MIN.l 15' MIN. I
KEY t"LOWEST BENCH ..,
DePTH (KEY)
I FILL SLOPE
V'
NATURAL
GROUND \
-
------------
_-: caMP ACTeD =-:-:-~
FILL OVER' CUT SLOPE __-:-=:-JFILL%~:-7
---------~----
-=----- ---------~-------=;. ~ ./
-------~~---~---
----------------- - -
____........c_____ 6 ~ ""'"
_-:__...:::...-::::c_-_-____;~-_ I
--..........-- ------ - ...
REMove. NATURAL . .z::-::_~ -...?"'_"'5. ,,.,,,-\
UNSUITABLE GROUND -:------...:.:::;-----~. ~
MATERIAL ~ '\... - ..:_::::--~- ...., r4' MIN. BENCH
_ _ - _-..:-~~-_-- BENC HEIGHT ~
....._., _ _ .,.. ":;~~2a;M-'I-N =- . ... . (typicolll VARIES I
__ __ 10 __ . -.-'~ .
______ _ _ T - .
---- ..",.-~ ~ ~ .
, - ~15t MIN.~
_ ' LOWEST BENCH I
-'
'--
CUT
FACE
To be constructed prior
to fill placement
,". "_._"'--<W,.
"-'-:' :;:;.J'_.
. ..' ,;"",- .
. .
....,'
NOliES: . . .
LOWEST BENCH: Depth and width subject to field change
.' based ~ consultant's inspection. ..... .
S~20RAI:JAGE:. e:,~k e,.;.:.,s mer be required at the'
:liscret Ion or the geotechnical consultant'. .
.~
.~,." .
FOUNDATION AND SLAB RECOMMENDATIONS',
FOR EXPANSIVE SOilS
,
(ONE AND TWO-STORY RESIDENTIAL BUILDINGS)
t-IITOfIIY FOOTINQI!I
EXPANSION INDEX EXPANSION INDEX EXPANSION INDEX EXPANSION INDEX
0-20 2t - 150 151 - 10 " - 130
VERY LOW EXPANSION LOW EXPANSION . MEDIUM EXPANSION HIGH EXPANSION
ALL "OOTINOI '2 INCHE. ALL FoonNOS 11 INC~EI EXTnIO.. FOOTINOS " EXTlRIOfIl FOOTINGI 14 IHCHEI
DEE~. FOOTUln~ DEi,el'. 'OOTI~a3 INCHES DEEP. INTERIOR DEEP, INTERIOR FOOTINOS 12
CONTIt!UOU!. r:o Cn::r:l CONTll'fUOue. H!O." I/.n FOOTI"GI 12 INCHES DEE". INCHEI DEEP. '.HO. . IAII TOP
REQumED FOil ur;.rfS\Oii TOP AND BOTTOM. '-NO. .. IAII TOP AND . AND lonOM.
FOlleEl. lOTTO...
,
I.LL FOOTIHI)8 " INCH~tI AU FoonNa!','(Ii INCHEe Al.L FOOTINOS 18 INCHES EXTERIOR FOOTINGS 14 INCHEI
DEEr. FOOTIIlO: DEE:I., FOOTI>:3$ DEEP. FOOTING8 DEE'. INTERIOR FOOTINGS ,.
C.(:;;TI!{UO:J::. i;O erE;;!. co;m~UOUG. HiO. 4 BAR CONTINUOUS. '~"O. 4 eAR INCHES DEEP. 1-NO. II IAR TOfI'
,REQUIRED FOR EXPANSION TOfl AND IOTTOM. TOfl AND 10TTOM. AND 'OTTOM.
FORCIl..
.NOT REQUIRED. 12 IHCI:':':t1 DE;:,.. t-tlO. "' CAR 18 INCHES DEEP. 1-NO. 4 DA." 24 INCHES DEEP. 1-NO. . 'A"
TOP A.ND 'OTTOM. TOfl AND 'OTTOM. TOfl AND 'OTTOM.
'-'TORY P'OOTJNOI
~""AaE DOOR (JRMIE
'EA"
LlVINO- AREA FLOOR ILAIS a 112 I"C~ES THICK. NO MESH 8 112 INCHES THICK. . 112 ItCHES THICK. 4 INCHES THICK. I X 1-1/1
'MOORED FOR EXPANSION e x 8-10/tO WI"E MESH AT 8 X 1-10110 WIRE MESH AT WIRE MESH AT MID-HEIGHT.
FORCES. NO "eASE REQUIRED. MID-HEIGHT. I INCHES MID-HEIQHT. .e INCHES NO. a DOWELLS FROM FOOTING
. MIL VISQUEEN MOISTURE GRAVEL OR SAND lASE. e GRAVEL OR SAND lASE. . TO SLAI AT S8 INCHES ON
IAP.RIER PLUS t INCH BAND. . MIL VISQUEEN MOISTURE MIL VISQUEEN MOISTURE ceNTER. 4 INCHES GRAVEL OR
BARRIER 'pLUS 1 INCH SAND. IARRIER 'LUS tlNCH SAND. BAND lASE. e MIL via QUEEN
MOISTURE IARRIER 'Lua t
INCH lAND.
QARAQE FLOOR SLABS 8112 INCHES THICK. NO MESH S 1/2 INCHES THICK. 8 112 INCHES THICK. 4 INCHES THICK. II X 1I.1I1t
REQUIRED FOR EXPANSION II X 1-10110 WIRE MESH OR II X 1-101t0 WIRE MESH OR WaRE MESH OR QUARTER
FORCES. NO BASE REQUIRED. QUARTER ILASS. ISOLATE QUARTER ILABS. ISOLATE aLABS. ISOLATE FROM STEM
NO MOISTURE BARRIER FROM STEM WALL FOOTINGS. FROM lITEM WALL FOOTINGS. WALL FOOTINGS. 4 INCHES
,REQUIRED. 2 INCHES ROCK. GRAVEL OR 4 INCHES ROCK, GRAVEL OR ROCK, QRAVEL OR lAND .ASE.
lAND IAaE. NO MOISTURE lAND lASE. NO MOISTURE NO MOISTURE IARRfER
IARRIER REQUIRED. 'ARAER REQUIRED. REOUIRED.
"RE-SOAII:ING OF LIVING ,NOT REQUIRED. MOISTEN SOAK TO 12 INCHES DEPTH SOAK TO 11 IfCHES DEPTH aDAK TO 24 INCHES DEPTH TO
A"fA AND GARAGE SLAa 'PRIOR TO POURING TO 4'1 AaOVE OPTIMUM TO a'l AaOVE OPTlUUU 15'll ABOVE OPTIMW MOISTURE
IOIU ,CONCRETE. MOISTURE CONTENT. MOISTURE CONTENT. CONTENT.
NOTEn: U ALL DI:PTHS ARE RELATIVE'TO SL.... IUIGRADE.
2) SPECIAL DESIGN UI REQUlRED FOR VERY HIGHLY EXPANSIVE 10lLI.
FOUNDATION AND SLAB DETAil
(NOT TO SCALE)
DOWEL. (WHEN REQUIRED)
YI80UEEN
ORAVEL OR lAND ....IE (WHEN REQUIRED)
DEPTH OF
HlE-IO"'IlED
lOlL .;
l~____~~~~_.:..-_~_
?;~
FOUNDATION AND SLAB RECOMMENDATIONS
JOB NO.:
DATE:
FIGURE NO.:
...\.(
~.W:EARTH'TECHNICS .,oJ
.~ ~'. . '."'-.'..~-,
_-.i!:C
APPENDIX D
?J:>
SURFICIAL SLOPE STABILITY
--------
,
S.F. = H (If B) cos2o<tan ~ + C
~s H Sin<><- coso<.
0.;.,
zone of '
saturation
("A, ,( o. B94~)
~'n (0,44b'l.-)
H = Depth of saturation zone
~B = Bouyant wei ght of soil ~ 7 tp .7
.
2l's = Total wet weight of soil = Uf(.o
0= Angle of internal friction = 3'2..
C= Cohesion = ~7'O
S.F.=
= ~.
H' S.F.
1- 4.D I
4 2. ~4
k. 1.1~
,
r\ hl:,.7)(' 8oo8)(O.'?40)....~15
H Q41.D)(O.44(,2)(o.e~4g)
-=- 11(?8.?g);-~7S
rI (0i., ~)
Project No.:
Calc. by:
Chk. by:
Date:
~
,.
~310J7-0 \
WL.S'
cSS
{2Ibl'?~.
?J~
.
APPENDIX E
.
t{J
-
REFERENCES
.
,Blake, Thomas, F.,' Computer' Services and Software, .1989, A
computer Program for the Deterministic Prediction of Peak
Horizontal Acceleration From Digitized California.Faults,
Eqfault, :July. 1989!
,Blake, Thomas F., Computer Services ahd'Software, 1986, A Computer
Proqramfor the Empirical Prediction of Earthquake-Induced
Liquefaction Potential, LIQEFY2, 1986; .. '. ,
,Blake, Thomas 'F., Computer Services and Software, 1989, A' computer
Program to Determine Historical Seismicity from' Digit.ize9-
. Faults in Southern California, EQSEARCH, July 1989;. ,
,Department 'of Water Resources, 1971, Water Wells and Springs in tl1e
Western Part of the Upper Santa Ana Margarita River Watershed, .
Bulletin:No. 91-20, August, 1971;
c
English, W.A., 1926, Geology and oil 'Resources
Hills Re,gion, Southern California: U.S.
Bulletin 768, 110 pp.;
of the Puente
Geology Survey
. Federal Emergency Management Agency, 1988, Flood Insurance Rate
-Map, Community Panel No. 060245 2740 B, Map Revised, September
30, 1988;
Given,D.D., ,:,1981 "seismicity of the San Jacinto Fault Zone",
South Coast Geological Society, Annual Field Trip Guidebook'
No.9; ," .... .
'"". .'
Hart, E.W., i985, "FaUlt-Rupture Hazard Zones in california",
California Division ,of Mines and Geology Special Publication
42; ~~; . '
. -.' . . ~'.' . ,....:. .
Jennings, C.W., 1975, Fault Map of California, California'
Division, 'of Mines and Geology, Geologic Data Map No.1;
,. Kennedy, M.P., 1977, "Recency and Character of Faulting Along the
Elsinore:Fault Zone in Southern Riverside County, California" ,
Special Report 131; .
, LeiC!]hton"and ;Associates, 1985, Geotechnical Investigation, Four
. Parcels'(20;!: acres), Jefferson Avenue and Lemon >. Street,
Tentative Parcel Map No. 21068,. Murrieta, 'Riverside County,
california, Project No. 6851516-01, dated November;,4't'. 1985; .
. . '-:.oj,
,Mann, John F., 1955,' Geology. of a Portion' of the Elsin'ore ' Fault
Zone,.; Special. Report 43, California Division. of'iMines and
"'Geology, October 1955;".,.:;G/:"
o
.- ,
.' ,':tr,7:.::',"
" .~....
" ,.'.
: '.';<::;,~~7;::::; :,.
. '. ~"-";' .'. .,
.~ l.. . ""~,.'
-.......-. .
".-.'.. .
(,
A\
r
,
,
, .
..,;:t....'
..-.....
~.
,.
REFERENCES (CONTINUED)
.
McGoldrick, James P., Consulting Engineers, 1979,. Geologic and
'Seismic Hazards Investigation of Approximately 44 acre Parcel
IMap 13648, SEC of Lemon Street and Jefferson Avenue, Murrieta,
:California, dated December 14, 1979~
f
Ploessel, M.R., Slosson, J .E.,. September, 1974, Repeatable High
I Ground Accelerations from Earthquakes, California Geology~
RANPAC Soils, Inc., 1989, Fault Hazard and Preliminary Geotechnical
. Investigation, Murrieta Gateway Plaza, Tract No.' 21'335, KalmiC!
I Street and 1-15, Murrieta, California, Work Order No.. 900-03,
,dated November 8, 1989 ~
Rassmusen Associates, 1979 , Preliminary Geology Investigation;
: Parcel Map 13648, 'East Corner of Lemon' Street and Jefferson
,Avenue, Murrieta, California, Project No. 1467, dated March'.
23, 1979~ '
Real,' C.R., et. al., 1978, Earthquake Epicenter Map of California
1900-1974~ California Division of Mines and Geology Map Sheet
39~
"\----.-.......
.
Rockwell,T.X., Millman,' D.E., McElwain, R.S., and Lamar, D.L.,
1985, Study of Seismic Activity by TrenChing Along the Glen
Ivy North,.;Fault, Elsinore Fault Zone, Southern California,
Lamar-Merifield Technical Report 85-1~'
Rockwell, T.X:, "&Larmar, D.L., 1986, Neotectonics of the Elsinore
Fault, Southern California, In Neotectonics and Faulting in
Southern C~lifornia,pg 149, GSA Cordilleran Section, March
25-28, 1986~ '
,
'.
,Schnabel, P.B., and Seed, H.B., 1973, "Accelerations in Rock for
Earthquakes in the Western United States", Bull. of the
,. Seismol. Soc. of 'Am., Vol. 63, NO.2, pp 501-516~
"
'seed, H.B., Idriss, I.M., 1982, Ground Motion . and Soil
Liquefaction During Earthquakes,' Earthquake Engineering
Research Institute~
,'.'f-""
Soil Tech, Inc., 1986, Geologic and Seismic Hazards Investigation,
'Tentative Parcel,Map 21759, 'NE of Adams and'Ivy.;.street,
Murrieta, California,. dated July 1986~' . ~':,,: .'
. ~i',(:.
,Weber, .F.H., :Jr., 1977, Seismic Hazards Related to\'~Geologic
Factors, Elsinore and Chino Fault Zones, Northwestern
Riverside County, California, V.G.S. Open.File 'Report, 77-4
L.A. ,.,96 pages.
,;".,;';'" ....'.~;
, .. -I~. . ,
'-':;;'''.,
", 't.
~'V
I. .
'.'
,