HomeMy WebLinkAboutCT 81-18; G.R. CAPITAL N/S UNICORNIO DR.; SOIL INVESTIGATION; 1981-11-06r ..... .. . .,
REPORT OF SOil INVESTIGATICN
La Costa Condominiums
Lots 515, 516, 517, Map 7076,
La Costa M~adows, Unit #3
La Costa area, Carlsbad, California
JOB NO. 81-1968
06 November 1981
prepared for
1'.\.4 ..... ,~, '.-
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,-----------------------, .. __ ._-------------------------'-G & R CAPITOl. CORPORAT,a-{ p
prepared by
GEOTECI*4ICAL EXPlORATlaf, INC.
8145 Ronson Road, Suite H
San Diego, CA 92111
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GEOTECHNICAL EXPLORATION, INC.
SOIL &: FOUNDATION ENGINEERING
GROUNDWATER • GEOPHYSICS • ENGINEERING GEOLOGY
-06 November 1981
G & R CAPITOL CORPORATION
359 San Miguel, Suite 102
Newport Beach, CA 92660
Subject: REPORT OF SOil INVmlCATl<JIf
La Costa Condominiums
Lots 515, 516, 517, Map 7076
JOB NO. 81-1968-
,---La-Co.sta-Meadows,-Unit.,jf3.;)..-------------__
La Costa area, Carlsbad, California
Gentlemen:
In accordance with your request, Geotechnical 'Exploration, fnc. hereby submits the
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following report summarizing, OUT work and test results, as well as our conclusions and
recommendations concerning t~ subject project. It is our understanding the existing
fill soils located on the subject site were placed under the supervision-and testing of
, -Benton Engineering, Inc., during a previous grading operation. Our firm placed random
test pits in the existing fill S9ils, after the grading operation was completed, in order
to verify that the soil conditions were not modified after the controlled grading
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operation' was completed and to determine the depth to and con'ditlon of the
underrying natural ground soils. Our field work was performed on October 29,.1981.
SCO~ ()F WORK
It is our understanding that the s'ite is beinlJ developed to receive a 28-unit
condominium complex. The p~oposed structures are to be a maximum of tWQ stories
in height and. will be-constructed of standard-type building materials, utilizing
conventional, continuous foundations or spread footings. A Plot Pian, illustrating the
approximate location of all fill materials and cut and fill slopes, is enclosed as Figure
No. I. With the above in mind, the Scope of Work is briefly outlined as follows:..
. 1. Identify and classify the surface and subsurface soils to depths, in conformance
.with the Unified Soil Classification System (refer to Appendix A).
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La Costa Condominiums
(X) November 1981
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Job No. 81-1968
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2. Determine the allowable bearing pressures for the natural ground and the soils
to. be used 'in compacted fill, based on their shear-strength characteristics and
our experience with the soils.
3. Recommend treatment for any expansive soils that could cause detrimental
damages to the proposed structures.
4. Determine the extent, d~pth and condition of existing fill soils on the site.
5. Predict the settlement of the natural-ground. soils, as well as existing compacted
fill soils under the proposed structural, loads.
SITE
The. site,. consisting of approximately one acre, is located approximately 150 feet east
of Cacatua S~reet, on the north side of Unicornio Street in the La Costa area of the'
City of ·Carlsbad. The property is bo rae red' ort the west and north bY. residential·
properties and on the east by a graded, vacant lot. ---.~----., _. --~ -
At the time of our inspection',' a previous grading operation on the site generated a
relatively level building pad with drainage to the south. The site; prior to grading,
appears to have consisted of moderately to steeply sloping hillside (sloping to the
north) terrain. Prior to grading, on'""site vegetation appears to have consisted of a
moderate growth of grasses and weeds.
A combination tut-and-fill slope, a maxi~um of 60 fe~t in height, has been placed at
the 'north end of the subject property. This slope possesses a slope ratio of 1.5
horizontal to 1.0 vertical (as' referenced by an undated Site Plan by HenrY Warley
Associates and identified as their Job No. 81-59) and dips to the north-nortnwest.
Surficial slipp~ge and erosional rills were obserV~d on the· face of the slope (this
p'roblem is specifically addressed in Reconwnendation ,15h
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[a Costa Condominiums
06 November 1981
FIELD
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Job No. 81-1968
Page 3
Six test trenches well! placed on the site to determine the overall depths and the'
extent Of the existing fill soils, and the condition of the bearing soils. The
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excavations were located in the field by referring to a. Site Plan, prepared by Henry
Worley Associates~ undated. The excav~tions were visually inspected by our Field
Engineer, and samples were taken of the. predominant soils throughout the field
operation. Test' tre"-~h logs. have been prepared on the basis of our inspection and
the results have been summarized on Figure No. II. The predominant soils have been
--------'-€las5ified-i~€onfoFmafl€e_with_th~ Unified-SOiI-Clas-sUi«::ation-Sy.stem-{refer-tO-Appendix--------~-.. -
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A).
SOILS
The fill soils encountered primarily ranged from less than 1.0 feet in thickness at the
south end of the site to 5.0 feet in thickness at the north end. The fill soils consist
primarily of greenish-gray, sandy, silty clays and clayey, silty sands. The uppermost
0.5 feet of fill is relatively loose., However, fiel.d dens{ty tests taken of fill 'soils
beneath this uppermost layer indicate they are moderately to well compacted.. The filt
soits possess highly to critically expansive characteristics as' tneasliredby the County
of San DiegoTest for Expansive Soils. The fill soils well! found to be under'hlin with,
formational materials consisting of medium dense to dense, brown~ non-'expansive, fine
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to medium sands with-a heavy day binder and gray-green, fractured claystones. The
claystones were tested and found to be highly to critically expansive.
All natural ground topsoils appear to have been removed from the site ~uring the
previ<?us grading oper.ation.
GROLNOWATERj
Nogrot,lndwater problems were encountered during the course of our field investi-, .
gation and we do not expect significant problems to develop in the future--if the
property is developed as presently designed. It. should be kept in mind, however, that
CIJly required grading operations may change surface drainage patterns and/or reduce
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La Costa Condominiums
~ November 1981
Job No. 81.,.1968
Page 4
permeabilities due to the densifjcation of-compacted soils. Such changes of surface
and subsurface hydrologic conditions, plus irrigation of 'landscaping or significant
increases in rainfall, may result in the appearance of minor amol,lnts of surface or
near-surface water at locations where nOl)e existed previously. The damage f.rom such
water is expected to.be minor and cosmetic in nature, if good positive drainage is im-
plemented at the completion of construction. Corrective action should be taken on a
site-specific basis if, and when, it becomes necessary.
lABORATORY TESTS -------._----.-_.
L~boratory tests were performed on the disturbed and undisturbed soLI samples in
order to determine their physical and mechanical properties and their ability to sup-
port the proposed structures. The following tests were conducted on the sampled
soils:
1. Moisture Content
2. Density Determinations
3. Mechanical Analysis
4. Expansion Tests
5. Oirect Shear Tests
6. Consolidation Tests
The moisture and. density_ determination relationship on undisturbed soil samples gives
qualitative information regarding the soil strength characteristics and soil conditions to
be anticipated .during the future grading operation.
The mechanical analysis was performed on selected soils according' to A.S. T .M~
422-52T. The mechanical analysis was used to aid in the classification of die soils
according to the Unified Soil Classification System •
Expansion-tests were determined from the County of San Diego -Test Method for
Expansive Soils. Expansive soils are classified as follows:
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La. Costa Condominiums
(» NO\'ember 1981
o to 3 percent
3 to 6 percent
6 to 12 percent
Above 12 percent
Job No. 81-1968
Page 5
low or Considered "Nqnexpansive".
Medium
High
Very High
According to the County of San Diego Test for Expansive Soils, swells of less than 3
percent are classified as nonexpansive soils.
Direct shear tests. were performed upon undisturbed-:-and remoldedbuik s~mples in
order to determine the soil stren.gth and supporting capacity for the natural-ground
soils and these same soils to be used in the. compacted fill. The shear. tests were
made with a constant strain direct shear machine. Specimens to be tested were
saturated and then sheared under various normal loads without appreciable drainag~ of
the samples •
. Consolidation Tests were performed on lmdisturbed natural-ground soils and' remolded
soils expected to be used in the compacted fills. The soils are containect: in 1-inch
high brass rings and loaded into a consolidometer.. The specimens are subjected to
increased loads and the resulting consolidations noted. The consolidation tests aid in
determining anticipated settlements of the natura' ground under the proposed building
loads.
Field density tests were performed in accordance with A.S. T .M. 0-1556. Maximum
density determinations were performed in accordance. with A.S.T.M. 1>-1557. The
relative .~ompaction results, as summarized on Figure No. II; are the ratios of the field
densities to the laboratory Maximum Dry DenSities, expressed as percentages.
CO«:lUSla-IS AND RECOMM~o"'tl~S
The following conclusions and recommendations are based upon too" practical field.
investigations conducted by our firm, and resulting laboratory tests, in conjunction
with our knowledge and experience with the soils occuring on the subject site.
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,La Costa, Condominiums
06 November 1981
Job No. 81-1968
Page 6
1. The site was found to be overlain with 0.5 to 5.0 feet of compacted fill soils.
T~e filts co!"sist of green-gr~y, silty, sandY clays. The clays were tested and
found to possess up to 12.0 percent swell, as ~asured by the County of San
Diego Test for Expansive Soils. The fill,s are underlain by good bearing,
formational materials consi'sting of bedded, 'gray-green claystones and brown,
'non-expansive, fine to medium sands. ""(he formational claystones also possess
up to 12.0 p~rcent swell as measured by the County of San Diego Test for
Expansive Soils. -
lesU-oJtne:--lrFpJace-fillsolts-yietc:tecr fiel<:.r--densitles-of-Slpercenr--anq89,
percent of Maximum Dry Density. Although fill soils must, in general, be
compacted to 90 percent of Ma}(imum Dry Density to be considered as accept-
able, we feel that the filt soils tested are in a sliitabre condition-due to their
criti~ally expansive nature. This density condition can actually prove to, be
beneficial in regard to minimization of potential distress and cosmetic damage
resulting from expansion of the clayey SoUSa Be assured that the in-place
density of the fill soils was taken into account by this firm jn recommending
design bearing capacities and predicti'ng future settlement of the proposed
structures.
2. Unless properly dealt with, the highly to critically expansive ,characteristics of'
the on-site ,soils described previously' can cause significant damage to the
structures an4 associated improvementS' (such as those planned for the subject
property). ,In ~rder to reduce significantly the potential for such damage, on~
of the recommendations herein must be followed:
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2.1, If the planned, structures and improvements are to be constructed using,
standard, nonexpansive-soils, design. criteriiil, ,the site shall be prepared as
follows:
2.1.1 The highly to critically expansive soils s,hall be rerooved from
aU structl,lral areas to a minimum distance of five feet outside perimeter
footings. The clay soils shall be rerooved to a minimum depth of 3 feet
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below the proposed, rough, finish-grade elevation~.
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e " La Costa Condominiums
06 November 1981-
Job No: 81-1968
Page 7
2.2
1.1.2 Excavated areas shall be backfilled with nonexpansive soils
(such as on-site, brown, fine to medium sands or soils obtained from an
approved off-site borrow pit). The nonexpansive select materials must
be placed and compacted to at least 90 percent of Maximum Dry Density;
in accordance with the requirements of the City of Carlsbad Grading
Ordinance. Upon sati~factory completion of the backfilling operation,
continuous ,and spread footings, may be designed, in accordance with the
soil-bearing value assigned to the compa~ted nonexpansiw fill materials.
The continuous and spread footings shall have a minimum width of 12
inches and extend, a minimum depth of 12 inches into the compacted fill
soiJs-Ht-is-re£ommended-two~story-struetures-be-,founded-;-on-18-inehf---,-----
deep footings).
2.1'.3' Areas receiving-improvements, such' as patios; sidewalks,
A.C. pavement (parking areas), et cetera,shall be underlain by at least
six inches of non-expansive fill materials, and be reinforced with 6 x 6 -
10/10' steel wire me'sh.
If it is intended to construct the proposed structures and improvements
on the expansive clay soils without preparation of the site (as ,described
in' Recommendatfon No. ,~.1)~ the-following' recommendations . become'
applicable:
2.2.1 The continuous foundations and spread footings s'hall
", extend a minimum depth of 2,4 inches into fhe firm natural, ground or
compacted fill. The continuous foundations shaU, be reinforced with
four No. 4 steel bars (or ~uivalent); two bars shall be located near the
top of the foundations and two bars near the bottom~ Continuous
foundations must be carried across garage entranc~s.
2.2.2 Concrete floor slabs, if used, shaft be founded on at ,least
six (6) inches of sand or decomposed granite, overlying visqu,een. The
slabs shaH be reinforced with No.3 steel bars placed on 24-.inch centers
(both ways). It is suggested suspended wooden ,floors be utilized where
possible.
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La Costa Condominiums
~ November 1981
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Job No. 81:'1968,
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2.2.3 Prior to pouring footings and foundation$, and prior to
placement of .floor slab base sections, the clayey soils shall be thoroughly
watered such that tht."Y possess a moisture content of 2 percent above .
optimum moisture content (or more) at a depth of 1-2 inches &elow the
. footing grade.
2.i.4 It is recommended that all noristrlictural concrete slabs
(such as patios, driveways, sidewalks, et cetera),and all parking areas, be
founded on at least six inches of nonexpansive soils and be reinforced ._---_.
with 6 x 6 -10/10 steel wire mesh.
2.2.5 The use of isolated interior piers should be avoided.
2.2.6 Garage slabs should be deSigned as free-floating, to allow
independent movement of the slabs and perimeter footings.
2~2.7 Provide positive drainage aWay from all peri~ter footings
with (}-vertical fall of at least six .inches· in horizontal distanCe of s,ix: feet
outside house walls...
3. Utilizing an Angle of Internal Friction of at least 21 degrees, and a cohesion of
4CX). pounds per square foot (with the appropriate Terzaghi Equation), the
maximl,.lm safe soil-bearing value (at a depth of 12 inches into' the n~tural
materials or compacted fill soils on this site) is at least 2,000 pounds per square
foot.. This SOil-bearing value may be utilized in the design of continuous
foundations and spread footings when founded a minimum of 12 inches into the
firm natural ground OF compacted fill. It 'is recortnnended' that two-story
structures, be founded on 18-inch reep footings. Foundations embedded in the
highly expansive soils must be 24 inches deep. Thiss,!if-bearing value may ,be
increas~d one':'third for design loads that include wind or seismic analysis. If
imported soils are required, the il11port soils shall be non-expansiVe and' shall be
obtained from an approved borrow area.
La Costa C0!1d0n:tiniums •
~ November 1981
Job No. 81 :-"1968
Page 9
A soil-bearing value for imported soils, should they be utilized on the site, can'"
not be given until the materials source is known. It is anticipated, however,
that a valu~ of at least 2,{XX) pounds per square foot will be obtained for
footing depths of 12 inches.
4. Based on our lahoratory test results and our experience with the soil types on
the subject site, the soils will experience settlement in the magnitude of less
than 0.5 inches under a structural load of2,{XX) pounds per square foot.
5; The acti¥!! earth pressure when 'retaining the green-gray clayey soils (to be
utilized in the design of walls, et cetera), shall be based on an Equivalent Fluid
Pressure of 70 pounds per sqlJare foot.
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The ac:tiw earth pressure to be utilized when retaining the brown, fine to
medium sands shall be based on an Equivalent Fluid Pressure .of 35 pounds per
cubic· foot.
The passive' earth pressure of the green-gray; dayey . soils (to be used for design
. _ _ ___ of buUdi,ng foundations and footings to. resist the lateraL forces) shall be based,
on an Equivalent Fluid Pressure of 2O(J pounds ,per cubic' foot (at any depth).
An Equivalent Fluid Pressure of 300 pounds per cubic foot may be utilized when
. founded in the brown; fine to medi!Jm sands.
7., A Coefficient of Friction of 0.3 times the dead load may be used between the
bearing soils and, concrete wall foundations or structure foundations and. floor
slabs when founded on the· green'-gray, claystones and fills. A Coefficient ·of
Friction of 0.4 may be utilized when founded on the brown, fine to medium
sands.
8. The compacted fill soils that occur withIn 5 feet 'of the 'face of the fill slopes
will possess poor lateral . stability, even though they have been compacted.
Proposed structures and other improvements (such as walls, fences, patios, side-
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La Costa Condominiums
06 November 1981 '
Job No~ 81-1968
Page 10
walks, swimming pools, driveways, asphalt paving, et ce~era), that' are located
within .5 feet cif the face of compacted fill slopes, could suffer differential
movement as a result of the poor lateral stabilitY of these soils.
Foundations and footings of proposed structures" walls, et cetera, when found-
ed 5 feet and further away from the top of compacted fill slopes, may be of
staridar~ design in conformance with the, recommended· soil-bearing value. If
the proposed foundations and footings are located closer than 5 feet Insi'de the,
top of compacted fill slopes, they shall be deepened to 1 foot below a lin~
beginning-ar-a-p~int-5-feer horirontalty-inside-the-fitrsloper Cfrtd-projecte<t;-----·-----,-
outward and downward, parallel to the face of the fill slope (see Figure No. V).
9'. It 15 recommended existing compacted fill slopes and natural cut slopes' be
planted with an erosion-resistant plant suitable to soils prone to shrinkage
cracking, in conformance with the requirements of the County of San Diego.
10. Planter areas and planter boxes shall be sloped to drain away from the founda-
tions, 'footings and floor slabs. Planter boxes shall be constructed with a s,ub-..
surface drain, installed in gravel, with the direction of, subsurface and surface
'flow away from' the foundations, footings and floor slabs, to an adequate drain-'
age facility.
11. T~e existi'ng debris and vegetation observed on the site must be removed prior
to the preparation of building pads and/or areas to receive structural improve-
ments.
12. Any backfill ;oils placed in util.ity trenches, .or behind retair:ting walls, which
support structures and other improvements (such as patios, sidewalks, drive-
ways,' pavements, et cetera), other than. landscaping; shall be compacted to at
,teast 90 percent of Maximum Dry Density •
13.'. It is our opinion that natural-ground cut slopes of maximum inclinations of 1.5
horizontal to 1.0 vertical shall be stable and free from deep-s7ated failures. for
,~ slopes not exceeding 60 feet in height.
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La Costa Condominiums
(X) November 1981
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Job No. 81-1968
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14. It is our opinion that compacted fill soils of maximum .inclinations of 1.5
horizontal to 1.0 vertical shall be stable and free from deep-seated failures fOf
slopes not exceeding 10 feet in height.
15. Adequate measures shall be taken to properly finish-grade the site after the
structures and other improvements are in. place. prainage waters from this site
and adjacent properti~s are to be directed away from tops of slopes, founda-
tions,floor slabs and footings, onto the natural drainage direction for this area
or into properly designed and approved drainage facilities. Proper sub$urface
and s'urface drainage will ensure that no waters will seek the level of the bearing
---'-----501 trurnter th'e' fOlffntati'Onr, f(5ot'lngr~m<t fto~)r-s labs-;;-Failure"" to-observe-thl5---' ----
recommendation could result in uplift or undermining and differential settlement
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of the structures or other improvements on the site.
The observed surficial slippage and erosional rills on the face of the existing
cut-and-fill slope indicate that surface waters have, in the past, been al,lowed to
E;xit the site over the slope face~ Particular care should be taken to direct
. future· drainage waters away from the slope, in order to minimize the potential
of future failures.
Geotechnical Exploration, Inc. will assume no liability for damage' to structures
w~ich is attributable to poor drainage.
16. ' No swimming pools· or 'subsurface. struct,ures shall be placed in the: highly
expansive soils' without being properly designed by a structural engineer arid/or
sojfs engineer.
GRADING NOtEs
Any additional' required grading operations shall be perfor~ iilaccordan<;e with the
general requirements of the City of Carlsbad Grading Ordinance, under the supervision
of a qualified soils engineer or supervised field' soils technician.
It is the responsibility of the Owner and/or Developer to ensure that' the recommenda-
ttons summarized in this report are carried out in the field operations.
La Costa Condominiums
~ Novemb.er 1981
l.lMITATIa..S
Job No. 81-1968
Page 12
Our conclusions and recommenda~ions have been based on all available data obtained
from our field investigation and laboratory analysis, as well as our experience with the
soils and formational materials located in this portion of the La Costa area.
Of necessity,' we must assume a certain degree of continuity between exploratory
excavations and/or natural exposures. It is, therefore, necessary that all observations,
-~----GonGlusion-s-and-reGommendatiens-be-verified-at-th~ ~ime-additional-grading... operations-----
begin, or when· footing excavations are placed. In the event discrepancies are noted,
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we should be notified immediately so that an inspection can be made and. additional
recommendations issued;. if required •.
Compaction tests were taken in randomly placed trenches and indicate the existing
soils were property pr~pared and compacted. However, our firm cannot assume
liability for' the integrity ~f the entire fill pad since our firm was not. present during
the actual·grad.ing operation. The fiJI soils on the subject site . were previously tested
(during the grading. operation) by Benton Engineering, Inc. The test results are
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summarizecF irftheir report-entitled ·Final' Report of Compaction Filled GrolJOO ~nd
Classification of Soil Condtions·, lots 413 to 584, inclusive, and certain street areas, La
Costa Meadows Unit No.3, and dated October 19, 1972.
This report should be co~sidered valid for a period of three (3) years, and is subject to
review by our firm following that time. If significant modifications are made to the
building and/or grading plans, esp,ecially with respect to the height and location of cut'
and fill slopes and the height and location of proposed structures, this report must be.
presented to US for immediate review and possible revision.
The firm of GeotechniCal Exploration, Inc. shall not be held responsible for changes to
the physical condition of the prop~rty, such as addition' of fill solis or changing
drainage patterns, which occur subsequent to issuance of this report.
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La Costa Condominiums
~ November 1981
Job No. 81-1%8
Page 13
Once again, should any questions arise concerning this report, please do not hesitate
to contact us. Reference to our Job No. 81-1968 will expedite response to your
inquiries.
Respectfully submitted,
GEOTECI-fIIICAL EXPlORATIO'of, INC.
JBR/CWl/pj
Enclosures·
".
• REFERENCE: This Plot Plan
was prepared from an undated
Site Plan by Henry Warley
Associates, identlfied as
their jo~INo. 81-59.
LEG END
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,11:'# I
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"'-,... --
'II
Property
Line
Pr9posed
Structures
Existing
Brow Ditches
Test Trench
Locations
Existing
Cut Slope
.D~iY 1 i ght Li ne
Existing
fill . slope
, c ,... ... ~~ ___ ........... _ ...... ~ ,-_~--.....-.. ,-". .--~ .....
TEi Thia Plot "-' .. nat 10 be ~ lot Ieg8I ~ ~ MCldImtnIIionI"'IIP9WII~. !Nto AduII6 p(Op«'ty ......... and'locMiona .
I ~ lNIY'be ob&airwci !roM. the ~.
yiIdIng ~,~ ~ .~8uiIr GradinfJ·P\MS.., ._ .... _ ..... _ .. _~_r ___ ~.---._ ... __ .. _ .....
.... ...... .... ....
PLOT
-------
1.5: I
PLAN
-......
--~
-....-----~ ---'.-~--
/
'X T-2
I T-6 rhO
.~.
.1
i
'PMK\N~'
T..,l
...... '---
.-,
-----, ----. "-
-..:~;;::::=::..:-~=:;::-.. ;..:-.:::::;;:.::'=-.:::::; =-':.==::~-:;::::-.= -.'.:':'.::.::~.-:-+--.-... _----.,
(J"l r rrYf""')1\I'O . I \, I ( • \ )'-\ • 'v i
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SCALE;
1-11 := 40 1
1.5: ,
,. --
'------~ -~---
1f 1T-3
PARKINq
!T-5
!T-4
~~.:::-.=:~u~.:;.,_;.; _._
I~h 1Jf'\ A 1 -lqf,R
,
Log of Test Trenches
-.~ CI ~ 0 ,
II. ..I .
C u 5611 Description -:E .&: (Unified Soli Classification) -Q.
Q. ftI
IJ ..
0 "
Trench No. 1 ---~~--~ i' ,,'. Loose to medTUiTl.;aen-se-, 5 ffglit ry a'amp, green, gray
:'.. " ,-', and brown si ltv' sandy clay (SC-CH) FILL
I~ 'I ,I:-l
2-',1 ~l',', Medium-dense? slightly da~p, greenish-gray, ~ighlytl'Ci" ,fractured, clayey $andy SIltstone
, ~. (SM-ML)
4 1:(1'1:1 FORMAT ION,
118.7 11.0 +1.0
Trenclr No. 2--O~M~{~~~~tr-------------~,·------------~,~-----------'----~--~~~~~ !\ ' ,-: , Loose to med i urn-dense, slight ly damp, green, gray and
",", ~ brown, silty sandy clay
0-"'~ 10: \' " 2<~Q),: "" "i\ '.! >-",. ~
(SC-CH)
FILL
~" .. " ~ ~1(Qi: Medium-dense, damp~ green-gr(tH silty sandy claystone
4 "<::.{ .,) . FORMATION
~!5~ Dense, mottled tan, green, gray and brown, fine-to ~:':,}.:\I~edium-grained sandstone with abundant mai-inefossils ::;'.: ~::. 6-:?@::: Medi,um-dense to dense, damp, light-brown, fi'rie 'tq
::,\:/:~;: medium sand with a, few marirTstfssils FORMATION
o Bag Sample o Undisturbed. Sampla
*In-Place Density
"In-Place Moisture·
26.0 8.4 , .
., .1. I
Job No. 81-1968
. figure No.-~ I a-
+11.2
l ..
c -.c
Q. GI :0
Trench No_. ~
Log of Test Trenches
_ Soli Des,erlptlon
(Unified Soli Clalilfleallon)
----~·I·o-,,"y ------_.. -_.. --_._ ... --------------
~-":--~f\ Loose, dry, gray to green-brown, silty sandy -
.j" , \ clay (SC-CH)
2 ~"G):. \.. ---becomes med i um-. r:-.~': . dense, FILL
....... '.
-Medium-dense to dense, damp, mottled brown and
gray-brown fine to medium sand with heavy clay
bi.nder, and containing o~caS'ioral marine-fossi.1s
(Sp-SC)
FORMATION
Trench No. 4
o ... ; i:" '::>' ,', Loose to medium-dense-, sl ightly damp, green, gray E(~~ and brown s i 1 tv sandv c lav (SC-CH)F I LL 2'-r,91-f Medium-dense, dry. gray siltstone; highly fractured
T Ifill and laminated (MH)
1 I d L-----------------,!!e.~!.1les less fq~lc~t~u..!..re~d!:!-._!...:FO~R.!!.M.!!'A!;!T..!I:.:::O.!.!N~ 4-~ :~'8
1(\ t,;
6 ~<.-'~: Dense, slightly damp, green-gray silty sandy
, .~ ~ claystone (CL-CH}
, :-..... ,.
o 8.g S.m,pla o Undllturbed Sample
·In-Place Denllty
··In-Plaee Moisturec
FORMATION
~_ p",.. J. •
:J! o -
1.20.0 10.1 -+5.0
+9.2
_ J I
Jo~ No. 81-1968
Flgqre No. . I I b
•
.. ~ (--._-
.-
i u..
c -.r: -Q.
" o
Log of Test Trenches
5011 Description
, (Unified Soli Clllllflcitlon)
0.-Trench No.5 ,:.7~::.~·.~ Loose'to'mecff um:'de~s-e ,"s 1 ight 1 y' damp;' green', "g'ray' '
"' . ''' .. ' and brown 5 i 1 ty sandy clay (SC-CH) FILL
. ,
2 ~~'~'~~--~~~~--~'~--~--------~~'~----------~--~ ::~'cB:~: .
.,: .. ""
4 -~.: :::":: :
" "" ,.'. .", ,; ~
6 -. ':.: ' ," '/ ,'. . .. ,
Medium-dense to den~e, damp, light-brown
medium sand with slight clay binder
(Sp-SC)
fine 1;0
FORMATI,ON
Medium-dense, dry to damp, slightly f~actured
green-gray silty sandy clqyston~
. tCL-CH) FORMAT I ON
Trench No. 6
c
" 0 :. .-.---,u .;[
a:: E o (J
.. -01 --+, c:
-0 c:
.2 -3 .. ,.-c-tt O
0.111 )(c
",,0 (J
O'~~~----------~--------~--------------------------~----~--~--~--~ ' .. " ::.::: Loose to medium-dense, s light I y damp, green, gray (Q).' and brS/wn si lty sandy clay (SC-CH) FILL
... :. " " 2~:~,.-.~~;.~.~--------------~--·-----------------~-----------4
:. ' .. ,:" :.: ~.~.
.~"~.~'
4 .::,;\)./
Medium-dense to dense, damp, golden brown, fine to
medium sand with occasion~l marine fossil layers (SP) FORMATION --... -.. --.-.--~.-,----.--.........,.---~-----------_4
Very dense. mottled tan,green, gray and brown, fine-
to medium-grained sandstqne)containing abundant
marine fossi Is ~SP , FORMATlO~: ,
Medium-de'nse to dense, d~mp, gray-green fine to
'med i urn sand wi th heavy clay binder·
(SC-CH)
FORMATION
o Bag Simple *In-Place Density
uln-Place Moisture o Undisturbed Simple
·..Lt
Job No. 81-1968
F!gure No. I Ie
140
130
120
Ho-
100
!O
\ ~ .
'\ ~
\ , 1
\ " " \ ~.
1\\ \
\ \
\ \
\
~
V ~
I !J -'ti ~ '(j
I-:x:: (!)
W'
~
!: -z
.::J
)0-cr a . ,
MAXIMUM DRY
DENSI TV (pet)
FILL SUITABILITY TESTS
\
\
,~ ~--3 k"~ ~\···"1
~ ~\ \
\~\ \
'\ \ " , .\
\ \ 1\' \
and 2
DIRECT St£AR· TEST DATA I 2
APPARENT COHE SION fplf)
APPAR£.NT FRier ION ANGLE
100
80
60
MECHANICAL ANALYSIS
.3 714 4 10 40 200
---------~--------,--
~,
\ 40
1\ i\ ~.~ 1\.' 20
\\ \ 0
410
28
\ \ \ 1000 100 10 1.0 0,1 0.01 0.001
\ G \. ~OB \ \ \. !'\ r\\.
RAIN SIZE IN MILLIt-1ETEAS . .
I .2 '3 ~r"2.70 .
118.7 118.5 120.0 SPECIFIC GRAVity
OPTIMUM MOISTURE , 11.0 11 .-4 , 10.1 . ~R~·60
~~C2.50 'CONTENT (%r'-. , .~ ZERO AIR VOIDS CURVES
M·OISTURE CON·TENT % &1
eo 0 _ 10 . 20 30 40
LABORATORY COMPACTI.ON TEST
SOIL
TYPE SOIL CLASSIFICATION
I Gray-green, clayey sandy silt
2 ~ray-green, silty sandy clay
3 Brown, clayey flne to medium sand
SWELL TEST DATA . I 2
INITIAL DRY DEN SIT Y (pc f) 104.5 106
INITIAL WAT ER CONt EN T (%). 10.5 10.0
LOAO (~..! f) 144 144
PERCENT SWELL 1.0 11.2
B~ING, TRENCH· DEPTH
NO. NO.
3
108
9.4
144
5.0
3.0'
3' 2.0'
.3 6.0'
JOB NO.: 8.1-1968
'. FIGURE NO: HI
. r
:>
u
L.I..I
ex:
:::I
Vl
V"I
L.I..I
ex:
a..
Z
0 -
I-
~
0
.-
...J
0
Vl
Z.
0
U
•
•
-------~---~----------.~-----~--o
. OOO'OL~~--~~--~~~~4--4--1 ~~~~~~~--+--+--+-~--~~~~~
~ u..
0"
V"I ......
I/)
..0
....J
QJ
S-
:::S'.
Ill,
I/)
QJ
S-
'0..
,...
to
E S-
O
Z
-= 1=-.. _ ~.I----
OOOE I +---~--.~--v----~--
0002 I I V .. J'
-------------.... ---'
000 L -----'" -r/~ ----/-f-- - -f-"
. "
- -.... ---.. - -----
I I
--:....-11-1--~-.;...I--:-~--I-----~-~-----
005 J OOV~+-~~~Ul~~~~-+~--~+-~-+~~+-~~~----~+-~~
OOE I'l~~~~~-+~~~--r-~~~~~--~-+--~~--~~'.
o N :t: OOZ~~~J~~~~~~~~~~~~~~~~~~~
I
-----~---------~-~---~~--------
Job No.81·-1968
.F1gu.re .No. IV
Propoeed Structure
, Concrete Floor Slab
5' 011
•
........
Top of Compacted Fi 11 Slopp.
/'
Compqcted. Fill Slope
(MaximUm Inc linaticn 1. 5 : 1.0)· -' h!inf~r::enta--nod~F-loo:'r~ _ : I ;
Foundations
Slabs fo llowi'ng the Rp.c-"
-.-
Footing
0"!'11P. nda t;tofrg;-'crf-the Ar~hite-ct;"--
or Structuralqinecr.
---=~-------~ --:--------ConcretE! Foundation -"';;'-'-~ . . -: ---'-~~ ...,...
-
. ' --:----. .:.=-
. --~. ---
. __ .. _----_. -
Compacted F'i: n
~ ---'5' 0"---'-
.:--'--
T Y PIC A L SSCTIQN
. (Showing Proposed Foundation Located Within Five Feet of Top of Compactt:d 'Fill Slq;e)
PISTANC ~ FRO~
• TOP (W SLOPF.:
0
I 1
I 2
I
J
1.'
1.5 . 1.0 .
5211
44"
36/1
28"
20"
TOT AJ. DEPTH OF FOOTING
Fill Slc;>pe 2.0 : 1.0
42"
36 11
30"
24"
-18"
Fill Slope
Job No. 81-1968-
Figure No.·V
• • =<
APPENDIX A
UNIFI'ED SOIL CLASS'IFICATION CHART,
SOIL DESCRIPTION
COARSE-GRAINED
More than half of material I. larger than a No. 200 sieve'
GRAVELS, CLEAN GRAVELS
More than half of coarse fraction is larger than GW Well-graded gravels,gravel and s~nd mix-
NO.4 sieve size, but smaller ,than 3" tures, little or no' fines.
GP Poorly graded gravels, gravel and sahd mix-
tures, little or no fi,nes.
GM Silty gravels, poorly grad~d gravel"sand-silt GRAVELS WITH FINES
,,-----(appreeiable-ameunt)--,----mixtures.----
SANDS, CLEAN SANDS
More than half of coarse fraction is smaller than a
NO.4 sieve.
SANDS WI1:H FINES
(appreciable amount)
FINE·GRAINED
'GC Clay gravels, poorly graded gravel-s~nd-silt
mixtures.
SW Well-graded sand, gravelly sands, little orno
no fines.
SP Poorly graded sands, gravelly sands, littie or
no fines.
SM Silty sands, poorly graded'sand and silty
mixtures:
SC Clayey sands, poorly gra,ded sane! and clay
mixtures.
More than half of material I. smaller than a No. 200 sieve
SILTS AND CLAYS
Liquid Limit Less Than 50
• Liquid Limit Greater Than ,50
HIGHLY ORGANIC SOILS
'.
ML Inorganic silts and very fine sands, rock flour,
sandy silt and clayey-silt sand mixtures with
a slight plastiCity.
CL InorganiC ,clays of low to medium plasticity,
gravelly clays, sandy clays, silty clays, clean
clays.
OL OrganiC silts and organiC silty cfays of low
plasticity. '
MH InorganiC Silts, micaceous or diatomaceous
fine'sandy or silty soils. elastic silts.
CH Inorganic clays of high plasticity. fat clays, , '
OH OrganiC clays of medium to"high plasticity.
PT Peat and other hiQhly organic soils.