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References : 1) Evaluation of Faulting and Liquefaction Po- tential, Portion of Wolf Valley Project, Rancho California, County of Riverside, California; report by Earth Research Associates, Inc. , dated November 20, 1987. 1 2) Preliminary Soils Engineering and Engineering Geologic Investigation, Redhawk Project, Rancho 1 California; report by Earth Research Associates, Inc. , dated February 2, 1988 . 1 3 ) Removal Requirements for Structural Fills Adjacent to Golf Course Fairway Numbers 1, 2 , 3 , 4 , 8 and 18, Redhawk Project, Rancho California, County of Riverside, California; report by Earth 1 Research Associates, Inc. , dated January 18 , 1988 . 4) Supplemental Soils Engineering and Engineering 1 Geologic Investigation, Portion of Redhawk Project, Phase I , Vesting Tentative Tract Map No. 23063 , Rancho California, County of Riverside, California; report by Petra Geotechnical, Inc. , dated November 1 17, 1988 . 5) Supplemental Evaluation of Faulting, Southwest 1 Portion of Redhawk Project, Rancho California Area, County of Riverside, California; report by Petra Geotechnical, Inc. , dated March 1, 1989. 1 1R 4 77354 PETRA GEOTECHNICAL, INC. 41640 Corning Place . Suite 107 • Murrieta • CA 92562 • Tel: (909) 600-9271 • Fax:(909) 600-9215 1 GREAT AMERICAN DEVELOPMENT COMPANY May 8, 1989 ' J.N. 298-87 Page Two Gentlemen: ' This report presents the results of our "Supplemental Soils Engineering and Engineering Geologic Investigation" for Tenta- tive Tracts 23064, 23065 , 23066 and 23067 . The purpose of ' this supplemental investigation was to obtain more detailed information concerning subsurface soil and geologic conditions, and then provide specific conclusions and recommendations per- taining to general site grading, remedial grading requirements, potential for hydro-consolidation and liquefaction, shrinkage and subsidence, and foundation construction. Our conclusions and recommendations are based on proposed grading as indicated ' on the enclosed 100-scale plans prepared by Rancho Pacific Engineering ( 11 sheets) . REFERENCED REPORTS References 1, 2 and 3 were prepared by Earth Research Asso- ciates, Inc. , the predecessor firm to Petra Geotechnical, Inc. This name change is a result of corporate restructuring which became effective on April 1, 1988 . LOCATION AND SITE DESCRIPTION ' Encompassing a combined area of 910+ acres, the subject tentative tracts occupy the southerly and northeasterly portions of the approximately 1300-acre Redhawk Project, Rancho California. Topography is characterized by numerous ridges and low rounded hills with intervening valleys, canyons, and gullies. Natural ' slopes vary from flat on ridge tops to near vertical at the con- tact with adjoining lower canyons and valleys. Maximum topogra- phic relief throughout the 4 tracts is approximately 250 feet with ground surface elevations ranging from 1100 to 1350 feet. Drainage is multi-directional, and is generally derived from natural precipitation and consequent runoff. There were no springs or seeps observed with the tracts during the course of ' this supplemental investigation. Ponded water, however, exists within a small artificial fill reservoir dam located within Tract 23064. • 3 1 GREAT AMERICAN DEVELOPMENT COMPANY May 8, 1989 ' J.N. 298-87 Page Three With the exception of barbed wire fences and two artificial fill reservoir dams , there are no other man-made structures present ' within the subject tracts . Valley and canyon bottom areas are typically covered with a moderate to heavy growth of weeds and grasses , and occasional scrub brush and trees. Ridges and adjacent natural slopes are generally covered with a moderate to heavy growth of scrub brush. PROPOSED DEVELOPMENT The accompanying 100-scale plans indicate a total of 1916 single- ' family lots, ten ( 10) multi-family residential sites, two ( 2 ) school sites, two ( 2) commercial sites , and four ( 4 ) parks are proposed throughout the subject tracts . Mass cut and fill grading is planned for physical development of the above building areas as well as associated access streets . Maximum vertical depths of planned cut and fill are approximately 1 100 feet and 50 feet, respectively. All graded slopes, cut and fill, are planned at a ratio of 2: 1, horizontal to vertical, and to heights of up to approximately 60 feet (both cut and fill) . ' Several daylight cut lots bordered by descending natural slopes are also proposed within the development. ' Tracts 23064 , 23065 and 23066 are golf course oriented residen- tial developments. Golf course fairways, which occupy several major adjoining canyon and valley areas, are presently in the grading and construction stages of development. FIELD INVESTIGATION ' To supplement our previous findings and recommendations presented in the referenced reports, an additional 133 backhoe test pits ' (Test Pits 117-249 ) and 42 borings (Borings 37-78 ) were excava- ted within selected areas. The primary objective of the addi- tional test pits and borings was to determine removal require- ments in alluvial areas, and to evaluate hydro-consolidation and ' liquefaction potential. Logs of all previous and new test pits and borings are presented in Table I and on Plates B-1 to B-107 . • 9 1 GREAT AMERICAN DEVELOPMENT COMPANY May 8 , 1989 ' J.N. 298-87 Page Four Approximate locations of the test pits are borings are shown on the accompanying plans. Available logs of previous borings by other consultants are also given in Appendix B. ' LABORATORY TESTING Associated with the subsurface exploration was the collection of disturbed and relatively undisturbed samples of earth materials from the test pits and borings for laboratory testing. Maximum dry density, expansion potential, shear strength, soluble sul- fate content, and consolidation tests were performed on selected ' samples considered representative of those encountered. In situ moisture and density of in place earth materials were also deter- mined in representative strata. A description of laboratory test ' criteria is given in Appendix A, and all test data are summarized on Plates A-1 through A-53 , and on the Boring Logs, Plates B-1 through B-107 . An engineering evaluation of the test data is re- flected throughout the "Conclusions and Recommendations" section of this report. ' EARTH MATERIALS The subject tracts are underlain with surficial deposits of ' compacted fill, uncompacted fill, residual soil, alluvium, col- luvium, slope wash, and terrace deposits. These materials, in turn, are underlain with late Pleistocene sedimentary deposits belonging to the Pauba Formation. General descriptions of each ' of these earth units are given in the following paragraphs. more detailed descriptions are presented in the appended test pit and boring logs. ' Uncompacted Fill (Map Symbol afl) ' Fill materials associated with the two existing reservoir dams located within Tracts 23064 and 23065 are composed of locally derived soil and/or Pauba Formation bedrock materials . The ' maximum thickness of the artificial fill deposits is estimated at between 10 to 20 feet. Unmapped spoil fill also occurs in relatively minor amounts on the downslope portions of numerous dirt roads traversing the four tracts. • 3 I GREAT AMERICAN DEVELOPMENT COMPANY May 8, 1989 ' J.N. 298-87 Page Five Compacted Fill (Map Symbol afc) Structural fills have been placed along the edges of several golf course fairways where ascending fill slopes are ultimately planned in adjacent residential areas . Structural fills have also been placed across some fairways in future roadway areas. All structural fills have been placed under the purview of our firm. This earthwork began in early 1988 and is still in progress in other golf course areas. Alluvium (Map Symbol Qal) Recent alluvial deposits are composed primarily of fine to medium grained silty and clayey sand, and subordinate coarse sand with ' occasional gravel and cobble lenses. Typically, alluvial depos- its were found to vary from dry to moist, loose to medium dense and porous, and to be subject to varying degrees of hydro-consol- idation. The thickness of alluvial materials is highly variable and ranges from 3+ feet in narrow tributary gully areas to grea- ter than 50 feet in broad valleys. On the basis of laboratory consolidation tests, the thick deposits of alluvial materials ' underlying broad valley and canyon areas were found to be sub- ject to a relatively high degree of hydro-consolidation to depth of up to approximately 20 to 25 feet. Colluvium (No Map Symbol) Colluvial deposits composed of loose to dense silty sand and clayey sand occupy small tributary canyon areas and typically coalesce with alluvial materials. These materials generally ' exhibit similar in place characteristics as alluvial deposits but generally become dense at relatively shallow depths (e.g. , becoming dense below depths of approximately 3 to 10+ feet) . For ease of mapping, these materials have been combined with alluvial deposits. ' Slope Wash (Map Symbol Qsw) Slope wash deposits composed of loose to medium dense silty sand ' and clayey sand also coalesce with alluvial materials in major canyon and tributary areas. Therefore, for purposes of mapping, these materials have also been combined with alluvial deposits • I GREAT AMERICAN DEVELOPMENT COMPANY May 8, 1989 ' J.N. 298-87 Page Six for most areas of the subject tracts. However, a relatively large accumulation of slope wash materials have been mapped on lower gently sloping areas within a portion of Tract 23067 (see Plate 23067-3 ) . In this area, slope wash materials were found to be dense at depths below approximately 5 . 5 to 9 . 0 feet. Terrace Deposits (Map Symbol Qt) ' Terrace deposit materials consisting of reworked Pauba Formation occupy two ridge tops , one each within Tracts 23065 and 23066 . Terrace deposit materials were found to be dense to very dense . 1 Residual Soil (No Map Symbol) ' Gravelly silty sand and clayey sand residual soil materials have developed over Pauba Formation materials in thicknesses ranging from 1 to 3+ feet. Thicker accumulations, however, occur within 111 gentle swale areas in thicknesses of approximately 3 to 6 feet. Typically, residual soil materials were found to be dry to damp, and loose to medium dense. 1 Pauba Formation (Map Symbol Qps) 1 Hillside areas of all four tracts are underlain by late Pleisto- cene sedimentary deposits belonging to the Pauba Formation. This formation is composed primarily of reddish-brown to light brown, ' fine to coarse grained sandstones and silty sandstones with occasional gravel and silt beds. Typically, in place materials vary from damp to moist, and dense to locally very dense. ' Geology Geologic Settling As noted above, the subject tracts are underlain with sandstones and silty sandstones of the Pauba Formation, and are bordered on the north and west by alluvial plains of Temecula Creek and Wolf Valley, respectively. Bedding within the Pauba Formation is gen- erally massive with gradational and indistinct contacts. Where observed, bedding was found to dip at low to moderate angles with no discernible preferred orientation. • 7 1 1 GREAT AMERICAN DEVELOPMENT COMPANY May 8, 1989 ' J.N. 298-87 Page Seven Faulting and Seismicity ' Faulting and seismicity are discussed in detail in References 1, 2 and 5 . iGroundwater Shallow groundwater conditions were not encountered in the majority of the borings and test pits excavated within alluvial areas . Groundwater was only encountered in Borings 7 , 13 , 60 , and 65 at respective depths of 13 . 0, 47 . 0, 12. 5 and 21. 0 feet. 1 Boring 60 was drilled within the flood plain area of Temecula Creek, Tract No. 23067 . ' CONCLUSIONS AND RECOMMENDATIONS General Based on the results of this supplemental investigation, combined with our previous findings, we conclude from a soils engineering ' and engineering geologic viewpoint that development of Tentative Tracts 23064, 23065 , 23066 and 23067 is feasible provided the following conclusions and recommendations are incorporated into __ the design criteria and project specifications. Earthwork All earthwork should conform to the Grading Code of the County of Riverside, the enclosed "Standard Grading Specifications" ' (Appendix C) , and in accordance with the following recommenda- tions. Site Clearing All weeds, grasses , scrub brush, trees , and similar vegetation should be stripped from areas to be graded and hauled offsite. I I 1 t \/ 1 1 GREAT AMERICAN DEVELOPMENT COMPANY May 8 , 1989 1 J.N. 298-87 Page Eight Excavation Characteristics t Based on our subsurface boring and test pit data, and on our experience with similar earth materials, onsite soil, and Pauba Formation bedrock materials will be excavatable with conventional earthmoving equipment requiring little to moderate prior ripping. 1 Removals and Canyon Cleanouts Owing to the typically poorly consolidated and porous nature of near surface alluvial, colluvial, and slope wash deposits, as 1 well as to their susceptibility to hydro-consolidation, removal of unsuitable surface materials and replacement as compacted fill will be required in all canyons, valleys and gullies to receive 1 structural fills. Estimated depths of removal that will be required are indicated on the accompanying plans. The indicated depths range from 3 to 25 feet. Unless additional subsurface exploration (and laboratory testing) is performed within major canyon and valley areas which may indicate shallower removal depths in local areas may be feasible, the indicated depths as shown on the accompanying plans should be considered as minimums. 1 All uncompacted fill deposits existing within Tracts 23064 and 23065 , as well as underlying unsuitable alluvial materials, 1 will require removal and replacement as properly compacted fill. Depths of removal are anticipated to be on the order of 10 to 20 feet. Compacted fills placed against canyon walls and on natural slope surfaces inclining at 5: 1 or greater should be benched through loose residual soils and placed on a series of level benches 1 excavated into competent bearing soils or bedrock. Residual soil materials vary from 1 to 3+ feet in thickness on ridge tops and lower descending slopes, and from approximately 3 to 6 feet in gentle swale areas. Canyon Subdrains 1 Perforated plastic pipe and gravel canyon subdrains should be within all major canyons to be filled in accordance with spec- ifications given in SG-4 of the Standard Grading Specifications. Subdrains should be placed so as to outlet at the lowest practi- cal elevation. In most instances, this will involve the place- ment of fill at the mouth of the canyon prior to installation of 4 I 1 GREAT AMERICAN DEVELOPMENT COMPANY May 8 , 1989 J.N. 298-87 Page Nine the subdrain. Approximate locations of recommended subdrains are shown on the enclosed plans. Actual locations will be determined during grading. Cut/Fill Transitions Cut/fill transition zones should be eliminated from building pads where the depth of fill exceeds 18 inches. This should be accomplished by overexcavating the cut portion and replacing the materials as properly compacted fill. Recommended depths of overexcavation are given below: I Depth of Depth of Fill on "Fill" Portion Overexcavation "Cut" Portion Up to 3 . 0 feet Equal Depth ' 3 . 0 to 6 . 0 feet 3 . 0 feet Greater than 6. 0 feet 1/2 Depth of Fill to a Maximum Depth of 15 feet 1 Compacted Fill Blankets A 3 . 0 foot compacted fill blanket will be required on daylight cut pads bordered by descending natural slopes . If it is deter- mined during grading that certain cut slopes will require stabi- lization by means of a buttress or stability fill, a compacted fill blanket will also be required on all lots located above these stability fill masses. Fill Placement 1. All fill should be placed in 6 to 8 inch maximum lifts , watered or dried as necessary to achieve near optimum ' moisture conditions, and then compacted in place to a minimum relative compaction of 90 percent. 2. The laboratory maximum dry density and optimum moisture content for each change in soil type should be determined in accordance with Test Method ASTM D1557-78 . I -% d/ Ice 7 • /D 1 I GREAT AMERICAN DEVELOPMENT COMPANY May 8 , 1989 ' J.N. 298-87 Page Ten Stability Analyses and Calculations ' On the basis of stability calculations (Appendix D) , proposed cut and fill slopes will be grossly stable at the inclinations and to the heights planned. Calculations were performed for a ' 60 feet high, 2 : 1 fill slope utilizing weakest shear strength parameters determined for remolded soils. Although calculations were not performed for a similarly configured cut slope, higher ' factors of safety would result due to greater shear strength values of in place bedrock materials. ' Fill Slope Construction Fill keys excavated into competent bearing soils or bedrock as ' approved by the soils engineer should be provided at the base of all proposed fill slopes to be constructed on natural slope surfaces inclining at 5 : 1 or greater. Minimum key widths should ' equal one-half proposed fill slope heights , with a minimum width of 15 feet. Minimum key depth should be 2 feet at the toe, and the bottom of the key should be inclined a minimum of 2 percent towards the heel. ' To obtain proper compaction to the face of fill slopes, low height fill slopes should be overfilled and backrolled during ' construction, and then trimmed back to the compacted inner core. Where this procedure is not practical for higher fill slopes, final surface compaction should be obtained by back-rolling during construction to achieve proper compaction to within ' 6 to 8 inches of the finish surface, followed by rolling with a cable-lowered sheepsfoot and grid roller. Track rolling is not recommended. Fill Over Cut Slope Construction Where fill over cut slopes are proposed, a fill key excavated into competent bearing soils or bedrock should be provided at the contact. The width of the fill key should equal one-half ' the height of the slope, or a minimum of 15 feet, whichever is greater. The bottom of the key should also be tilted back into the slope at a minimum gradient of 2 percent. 1 GREAT AMERICAN DEVELOPMENT COMPANY May 8, 1989 ' J.N. 298-87 Page Eleven Cut Slope Construction t Owing to the general lack of significant adverse bedding of Pauba Formation materials , cut slopes, in general, are expec- ted to be grossly stable. All cut slopes, however, should be ' inspected by the engineering geologist to confirm geologic structure. Slope Landscaping Landscaping for graded cut and fill slopes should consist of ' plant material requiring minimal cultivation and irrigation water to thrive. An irrigation system should be installed. However, overwatering and subsequent saturation of slope ' surfaces should be avoided. Moreover, the irrigation system should consist of very shallow or above grade piping to avoid the need for deep trenching within the slope surfaces. ' All graded slopes should be landscaped as soon as practical after the completion of rough grading (whenever water is available for irrigation) . If permanent landscaping cannot ' be provided within a reasonable period of time, spray-on pro- ducts designed to seal slope surfaces should be considered as a temporary measure to inhibit surficial erosion. To inhibit surficial erosion, the tops of all cut and fill slopes should be protected from surface runoff by means of compacted earth berms and/or paved drainage catchment and ' diverter devices. ' Natural Slopes Existing natural slopes are underlain by massive, granular ' Pauba Formation materials and exhibit no evidence of insta- bility. In addition to the recommended compacted fill blanket on day- light cut lots bordered by descending natural slopes, the adjacent natural slopes should be protected from any further surface runoff by means of top-of-slope compacted earth berms and/or paved drainage catchment and diverter devices. • t2 i t GREAT AMERICAN DEVELOPMENT COMPANY May 8, 1989 ' J.N. 298-87 Page Twelve Ascending natural slopes located above daylight fill lots ' should be provided with toe-of-slope, paved interceptor swales which conduct collected water to an appropriate dispersal area. Additionally, reinforced concrete block slough walls should be provided at the toe of the natural slope to prevent the accum- ulation of mud flow debris onto the lots. As a further measure to inhibit surficial erosion, natural slopes should not be stripped of existing vegetation. Geotechnical Inspections 1. An inspection of clearing operations, removals of loose fill, canyon cleanouts, fill key excavations, cut slopes, ' and general grading procedures should be performed by the project soils engineer and engineering geologist. No fills should be placed without prior approval from the geotech- nical consultants . 2 . The project soils engineer or his qualified representative should be present onsite during all grading operations to verify proper placement and compaction of fill, as well as to verify compliance with the recommendations presented herein. Volumetric Changes Volumetric changes in earth quantities will occur when going from cut to fill. Estimated shrinkage/bulking factors for various earth materials are given below: ' Unsuitable Fill, Alluvium, Colluvium, and Slope Wash Shrinkage of 10 to 15 percent ' Bedrock and Terrace Deposits Shrinkage of 3 percent It is expected that any subsidence will be negligible in exposed ' bedrock areas approved for placement of fill . However, for the purposes of estimating earthwork quantities, we recommend a fac- tor in the approximate range of 0. 05 to 0 .10 feet be utilized. • ' eI 1 GREAT AMERICAN DEVELOPMENT COMPANY May 8 , 1989 ' J.N. 298-87 Page Thirteen ' Settlement ' Provided removal of unsuitable soil materials and placement of fill are performed as recommended herein, post grading settlement is expected to be within acceptable limits. Foundation Recommendations General Provided grading is performed as recommended herein, proposed ' residential buildings may be safely supported by conventional shallow spread and continuous footings . Likewise, the resultant grading will produce a stable site suited for future roadway ' improvements and underground utilities . Recommended allowable bearing capacities, lateral bearing, and other design parameters will depend on the character and quality of subgrade soils ex- isting within the upper several feet of finish grades . However, ' final foundation recommendations are not expected to vary signif- icantly from those presented in the remaining sections of this report. 1 Allowable Bearing Capacities An allowable bearing capacity of 1500 pounds per square foot, including dead and live loads , may be utilized for design of footings founded at a minimum depth of 12 inches below the nearest adjacent final grade. This value may be increased to 1800 pounds per square foot for footings founded at a minimum depth of 18 inches. When designing for short duration wind or seismic forces, the above values may be increased by one-third. ' Settlement of Footings Under the above bearing pressures, total settlement of footings is expected to be less than 3/4 inches , and differential settle- ment is expected to be less than 1/4 of an inch. \/ if 1 GREAT AMERICAN DEVELOPMENT COMPANY May 8, 1989 J.N. 298-87 Page Fourteen Lateral Resistance A coefficient of friction of 0. 4 times dead load forces may be used for concrete in contact with soil to resist lateral loads. In addition, a passive earth pressure increasing at a rate of 250 pounds per cubic foot per foot of depth, to a maximum value of 2000 pounds may be utilized. ' Deepened Footings Where building, block wall, or retaining wall footings are to be constructed near or on descending slopes, these footings ' should be deepened such that a minimum horizontal distance of 5 feet is maintained between the outside bottom edge of the footing and the face of the adjacent slope . Retaining Wall Parameters 1. All retaining wall footings should be carried to a mini- mum depth of 12 inches into undisturbed bedrock materials, approved competent native soils, or compacted fill. 2 . An active lateral earth pressure equivalent to a fluid hav- ing a density of 40 pounds per cubic foot should be used for design of cantilevered walls retaining a drained level back- fill. Where the backfill slopes upward at 2: 1, horizontal to vertical, the above value should be increased to 53 pounds per cubic foot. 1 3 . All retaining walls should be provided with weep holes; or with perforated pipe and gravel subdrains to prevent entrap- ment of water in the backfill. Perforated pipe should con- sist of 4-inch minimum diameter PVC Schedule 40 , or ABS SDR- 35, with a minimum of 16 perforations per foot on the bottom ' one-third of the pipe. The pipe should be embedded in 3 . 0 cubic feet per foot of 1 1/2-inch, or 3/4-inch open-graded gravel wrapped in filter fabric. Filter fabric may consist of Supac 5-P, or equal. ' 4. Onsite soil materials exhibiting a Very Low or Low Expan- sion Potential should be used for backfill behind retain- ing walls. All backfill should be placed in thin horizontal lifts , watered as necessary to achieve near optimum moisture I I GREAT AMERICAN DEVELOPMENT COMPANY May 8 , 1989 J.N. 298-87 Page Fifteen conditions, and compacted in place to a minimum relative compaction of 90 percent. Flooding or jetting of backfill materials should be avoided. Expansive Soil Considerations Initial laboratory testing indicates onsite soil and bedrock materials exhibit Very Low to Medium Expansion Potentials. There- fore, expansive soil conditions will have to be determined for individual lots during and near the completion of grading. How- ever, it is anticipated that removal and mixing of site soils, combined with proper placement schemes will result in most lots being underlain with soils near pad grade exhibiting a very low or low Expansion Potential. Depending on the final evaluation, however, the following minimum criteria will be recommended. 1. Very Low Expansion Potential (Expansion Index 0-20) I Standard depth footings may utilized with respect to floor heights (i.e. , 12 inches for one-story, and 18 inches for two-stories) . No special reinforcement of footings or floor slabs will be required. However, some reinforcement may be necessary for structural considerations as determined by the project architect or structural engineer. 1 2. Low Expansion Potential (Expansion Index 21-50) Standard depth footings may utilized with respect to floor heights (i.e. , 12 inches for one-story, and 18 inches for two-stories) . All continuous footings should be reinforced with two No. 4 bars, one top and one bottom. Spread footings should be reinforced with No. 4 bars spaced 18 inches on centers, both ways, near the bottom of the footing. Dwelling area floor slabs constructed on-grade should be reinforced with 6-inch by 6-inch, No. 10 by No. 10 welded I wire mesh; or with No. 3 bars spaced 24 inches on centers, both ways. All slab reinforcement should be supported on chairs or brick to ensure the desired placement near mid depth. •1 116 I GREAT AMERICAN DEVELOPMENT COMPANY May 8 , 1989 J.N. 298-87 Page Sixteen Reinforcement of garage floor slabs will not be necessary. However, garage floor slabs should be poured separately from ' adjacent wall footings with a positive separation maintained with felt expansion joint materials, and quartered with weak- ened plane joints. A grade beam, 12 inches by 12 inches, ' should also be provided across garage entrances. The grade beam should be reinforced with two No. 4 bars, one top and one bottom. 3 . Medium Expansion Potential (Expansion Potential 51-90) ' All footings, exterior and interior, for either one or two- story construction should be founded at a minimum depth of 18 inches below the nearest adjacent final grade. ' All continuous footings should be reinforced with two No. 4 bars, one top and one bottom. Spread footings should ' be reinforced with No. 4 bars spaced 18 inches on centers, both ways, near the bottom of the footing. Dwelling area floor slabs constructed on-grade should be ' reinforced with 6-inch by 6-inch, No. 6 by No. 6 welded wire mesh; or with No. 3 bars spaced 18 inches on centers, both ways. All slab reinforcement should be supported on ' chairs or brick to ensure the desired placement near mid depth. Garage floor slabs should be reinforced in a similar man- ner as dwelling area slabs. In addition, garage floor slabs should be poured separately from adjacent wall footings with a positive separation maintained with felt expansion joint ' materials, and quartered with weakened plane joints. A grade beam, 12 inches by 12 inches, should also be provided across garage entrances. The grade beam should be reinforced with two No. 4 bars, one top and one bottom. Prior to placing concrete, subgrade soils below all slab areas should be thoroughly wetted to achieve a moisture ' content equal to or greater than 110 percent of optimum moisture content. Minimum depth of moisture penetration should be 18 inches. 1 a (7 1 I GREAT AMERICAN DEVELOPMENT COMPANY May 8, 1989 ' J.N. 298-87 Page Seventeen The above criteria are recommended to minimize potential dis- tress to footings and floor slabs due to expansive soils. Addi- tional or heavier reinforcement may be necessary for structural considerations as determined by the project architect or struc- tural engineer. Moisture Vapor Barrier ' Where floor coverings are considered, concrete floors con- structed on-grade should be underlain with a moisture vapor barrier consisting of a polyvinyl chloride membrane such as ' 6-mil visqueen, or equal. At least one ( 1) inch of sand should be placed over the membrane to promote uniform curing of the concrete. Soluble Sulfate Analysis Site soils tested were found to contain less than one-tenth of one percent water soluble sulfates. Therefore, according to Table 26-A-6 of the Uniform Building Code, special sulfate ' resistant cement will not be necessary for concrete placed in contact with onsite soil. Additional testing, however, is recommended at the completion of grading to verify this ' condition. ' Yard Drainage Positive drainage devices such as area drains , planter drains, or drainage swales should be provided around each building. Excess water should not be allowed to collect nor pond against building foundations. Roof gutters and downspouts may be re- quired on the sides of houses where there is insufficient area to construct yard drainage devices. Multi-Family, School, and Commercial Sites When building locations are known, cut/fill transition zones created within the multi-family, school, and commercial sites ' will require elimination utilizing the procedure presented herein. Moreover, a specific site study may be necessary depending on the types of buildings to be constructed within ' these sites, and the magnitudes of their imposed loads on the underlying foundation soils. - a 973 f 1 GREAT AMERICAN DEVELOPMENT COMPANY May 8, 1989 J.N. 298-87 Page Eighteen Utility Trench Backfill 1 All utility trench backfill under slabs and within street and utility right-of-way areas should be compacted to a minimum relative compaction of 90 percent. Onsite soils cannot be den- 1 sified adequately by flooding and jetting techniques. Therefore, mechanical compaction will be required. 1 As an alternate for interior trenches ( trenches under building slabs) , and for utility trenches located in confined areas, imported sand having a Sand Equivalent value of 30 or greater may be used for backfill and flooded or jetted into place. ' No specific relative compaction will be required. However, inspection, probing, and if deemed necessary, testing should be performed. ' Where exterior and interior utility trenches are proposed parallel to building footings, the bottom of the trench should not be located within a 1: 1 plane projected downward from the ' bottom edge of the adjacent footing. ' GRADING PLAN REVIEW Definitive 40-scale grading plans, when prepared, should be ' reviewed by our firm with respect to conformance with the geo- technical recommendations presented herein. Depending on this review, modifications to these recommendations and/or addi- ' tional recommendations may be warranted. INVESTIGATION LIMITATIONS 1 This report is based on the project as described and the geo- technical data obtained from the field tests performed at the ' locations indicated on the plan. The materials encountered on the project site and utilized in our laboratory investigation are believed representative of the total area. However, soils can vary in characteristics between excavations, both laterally ' and vertically. Our firm should be notified of any pertinent change in the project plans or if subsurface conditions are encountered which differ from those described in this report, since this may require a re-evaluation of our recommendations. This report has not been prepared for use by parties or projects other than those named or described above. It may not contain sufficient information for other parties or other purposes. (Q GREAT AMERICAN DEVELOPMENT COMPANY May 8, 1989 J.N. 298-87 Page Nineteen Since our investigation is based upon the site materials ob- served, selective laboratory testing, and engineering analysis, the conclusions and recommendations presented herein are profes- sional opinions. These opinions have been derived in accordance with current standards of practice, and no warranty is expressed or implied. This opportunity to be of continued service is sincerely ap- preciated. Please call if you have any questions pertaining to this report. Respectfully submitted, PETRA GEOTECHNICAL, INC. �PE�PROF�. ORIGINAL'/�' I_��/ r0 co L SIGNED 1 No. GE 2024 A 1 Siamak Jafro : p ;* CxP,6i=boy President Principal gineer N9r�atFCHN� P* 1 Engineering Geologist G.E. 2024 '6'°; Poa" CEG 936 ' CB/AB/SJ/nls TI"S DOCUMENT WAS ISSUED PREVOI L' i;,:::: ': ' . NOT REFLECT CURRENT S TE STANDARDS OF GEOTECHNICAL PRACTICE. THE ' CONTENTS OF THE DOCUMENT SHOULD NOT BE USED OR RELIED UPON WITHOUT A REVIEW BY QUALIFIED PROFESSIONALS. ' ra. (Date) //a' a/ '�`'GEOTECHNICAL, INC. I • I I Jo 1 1 J.N. 298-87 1 1 1 ENCLOSURES 1 APPENDIX A Laboratory Test Criteria, Laboratory Test Data, Test Pit Logs, and Boring Logs 1 APPENDIX B Previous Borings by Others APPENDIX C Standard Grading Specifications 1 APPENDIX D Stability Calculations 1 1 1 1 i 1 1 1 1 1 12 J.N. 298-87 APPENDIX A TENTATIVE TRACT MAPS ( 11 Sheets) In Pocket LABORATORY TEST CRITERIA LABORATORY MAXIMUM DRY DENSITY Plates A-1 and A-2 IN-PLACE MOISTURE DENSITY/TEST DATA/TEST PITS . . . . Plates A-3 to A-7 ' EXPANSION INDEX TEST DATA Plate A-8 SOLUBLE SULFATES Plate A-9 DIRECT SHEAR Plate A-10 CONSOLIDATION PRESSURE CURVES Plates A-11 through A-53 BORING LOGS Plates B-1 through B-107 tLOGS OF TEST PITS Table I t 023 J.N. 298-87 LABORATORY TEST CRITERIA Soil Classification Soil encountered within the property were classified and described ' utilizing the visual-manual procedures of the Unified Soil Classi- fication System. ' Maximum Dry Density ' The laboratory maximum dry density and optimum moisture content were determined for selected samples of soil and bedrock mate- rials in accordance with Method A of Test Method ASTM D1557-78. Pertinent test values are given on Plates A-1 and A-2. - - In Situ Moisture and Density ' Field moisture content and dry unit weight were determined in representative strata of soil and bedrock materials during the field exploration. Dry unit weights were determined in pounds per cubic foot and the moisture content expressed as a percen- tage of the dry unit weight. Test data obtained from the test pit trenches are summarized on Plate A-3 through A-7. Test data obtained from borings are given on Plates B-1 through B-107 . tExpansion Potential Expansion Index tests were performed on selected samples in accordance with Uniform Building Code Standard Test No. 29-2 . ' Test data and expansion potentials are given on Plate A-8 . ' Soluble Sulfates Soluble sulfate contents were determined for selected samples ' by Anaheim Test Laboratory of Santa Ana, California. Results of these tests are included on Plate A-9. t e � LABORATORY TEST CRITERIA J.N. 298-87 Page Two ' Direct Shear The Coulomb shear strength parameters, angle of internal fric- tion and cohesion, were determined for remolded and undisturbed test samples. All test samples were artificially saturated, then sheared under varying normal loads at a constant rate of strain of 0 . 05 inches per minute. Test results are summarized on Plate ' A-10 . ' Consolidation Settlement predictions under anticipated loads were made on the basis of the consolidation tests. Axial loads were applied in ' several increments to a laterally restrained one-inch high sam- ple. Loads were applied in a geometric progression by doubling the previous load, and the resulting deformations were recorded at selected time intervals. Test samples were saturated at a loading of 1. 4 kips per square foot in order to evaluate the effects of a sudden increase in moisture content (e.g. , hydro- consolidation potential) . Results of consolidation tests per- formed to date are graphically presented on Plates A-11 through A-53 . Several consolidation tests were in progress at the time this report was being prepared, and a number of other samples are scheduled for testing. This additional consolidation test data will be appended to future copies of this preliminary report. 1 1 45 I IJ.N. 298-87 IEXPLORATORY BORINGS ' LABORATORY MAXIMUM DRY DENSITY Boring Depth Geologic Optimum Maximum Dry INumber (ft. ) Unit Soil Description Moisture ( %) Density (pcf) B-2 5 .0 Qps A - Clayey Sand (SC) 11. 0 124 I B-2 15 . 0 Qps B - Silty Sand w/Clay (ML) 15 . 0 117 B-2 25 . 0 Qps C - Sand w/Silt (SW/SM) 10 . 5 126 B-3 10 . 0 Qps D - Clayey Sand (Sc) 13 . 0 122 ' B-3 20 . 0 Qps E - Sand w/Clay (SW/SC) 10. 5 128 B-3 30. 0 Qps F - Sand w/Silt (SW/SM) 13 . 5 118 B-3 40 . 0 Qps G - Silty Sand w/Clay (SM/SC) 13 . 0 121 IB-5 10. 0 Qps H - Sand w/Clay (SW/SC) 10 . 5 129 B-5 20 . 0 Qps I - Sand w/Silt (SW/SM) 11 . 0 128 B-5 30 . 0 Qps J - Silty Sand w/Clay ( SM/SC) 12 . 0 125 B-5 40 . 0 Qps K - Sand w/Silt ( SW/SM) 12 . 0 125 B-38 15. 0 Qal L - Clayey Sand (SC) 8 . 0 134 IB-47 2 . 0 Qal M - Sand w/Silt (SW/SM) 10 . 5 129 IB-48 4 . 0 Qal N - Silty Sand ( SM) 10 . 0 128 B-51 12 . 0 Qal 0 - Clayey Sand (SC) 8 . 0 133 IB-53 6 . 0 Qal P - Silty Sand ( SM) 8 . 0 134 B-56 21. 0 Qal R - Silty Sand w/Clay (SM/SC) 8 . 5 131 IB-59 21. 0 Qal R - Silty Sand w/Clay (SM/sc) 8 . 0 134 IB-60 9 .0 Qal S - Sand (SW) 12 . 0 117 B-61 6 . 0 Qal T - Silty Sand w/Clay (SM/SC) 7 . 5 136 IB-74 20 .0 Qps U - Silty Sand (SM) 9 . 0 132 B-75 10 .0 Qps V - Silty Sand ( SM) 8 . 5 133 IB-76 5 .0 Qt W - Clayey Sand (SC) 8 . 0 134 I ' PLATE A-1 1 I IJ.N. 298-87 IEXPLORATORY TEST PITS LABORATORY MAXIMUM DRY DENSITY III Test Pit Depth Geologic Optimum Maximum Dry I Number (ft. ) Unit Soil Description Moisture (%) Density (pcf) TP-5 5 .0 Soil AA - Clayey Sand (SC) 11. 5 129 1 TP-14 1. 0 Qal BB - Silty Sand (SM) 11. 0 129 TP-15 5. 0 Qal CC - Silty Sand (SM) 10. 0 132 1 TP-134 3 . 0 Qal DD - Silty Sand w/Clay ( SM/SC) 8. 0 133 TP-136 4. 0 Qal EE - Silty Sand w/Clay (SM/SC) 8. 0 133 I TP-143 1. 0 Qal FF - Silty Sand (SM) 9. 0 130 TP-144 3 . 0 Qal GG - Silty Sand w/Clay ( SM/SC) 8. 0 134 TP-149 4 . 0 Qal HH - Silty Sand w/Clay ( SM/SC) 8 . 0 133 ITP-153 4 . 0 Qal II - Clayey Sand (SC) 8. 0 133 TP-162 5 . 0 Qal JJ - Silty Sand ( SM) 8. 0 134 ITP-169 9.0 Qsw KK - Silty Sand (SM) 8. 0 134 TP-194 3 . 0 Qal LL - Silty Sand (SM) 8. 5 132 I TP-196 3 . 0 Qal MM - Sand w/Silt (SW/SM) 10.0 127 TP-208 4 . 0 Qal NN - Silty Sand (SM) 7. 5 135 ITP-211 5 . 0 Qal 00 - Sand w/Silt (SW/SM) 10. 0 128 TP-222 5. 0 Qal PP - Clayey Sand (SC) 8. 5 131 I TP-224 4 . 0 Qal QQ - Clayey Sand (SC) 9. 0 131 TP-225 5 .0 Qal RR - Silty Sand w/Clay ( SM/SC) 9. 0 131 TP-228 6. 0 Qal SS - Silty Sand (SM) 8. 0 133 1 TP-232 4.0 Qal TT - Sand (SW) 12 . 0 121 ' TP-246 4 . 0 Qal UU - Clayey Sand (SC) 9. 0 129 I I PLATE A-2 1 Tedi9 23 r a7 I IJ.N. 298-87 ' EXPLORATORY TEST PITS IN PLACE MOISTURE AND DENSITY TEST DATA ' Test Pit Depth Moisture Dry Density Maximum Dry Relative Number (Ft. ) (%) (pcf) Density (pcf) Compaction ( %) ' 5 2 . 0 12 . 6 100 . 2 123 129 81 5 5. 0 4 . 2 114 . 0 88 6 3 . 0 4 . 6 105 .7 126 84 I 6 5. 0 11. 1 102 . 1 130 79 7 3 . 0 6 . 8 97. 4 136 72 7 5. 0 9 . 5 111.7 132 85 14 5. 0 7 . 1 99. 8 133 75 I 14 5. 0 7 . 1 99 . 8 133 75 15 2. 0 9 . 8 96 . 2 131 73 15 5.0 8 . 4 114. 8 132 87 I 18 3 .0 12. 1 97 . 1 122 80 18 5. 0 9 . 2 109 .7 132 83 19 2. 5 4 . 2 93 . 6 132 71 I 19 4. 5 5 .7 109 . 4 132 83 20 3 . 0 1. 9 98 . 5 128 77 20 5. 0 1. 6 103 . 1 118 87 21 2. 5 4 . 2 101. 9 128 80 I 21 5. 0 5 . 0 104 . 4 129 81 94 5 . 0 6 . 6 92. 6 125 74 95 3 . 0 5 . 6 106. 5 133 80 I 97 1. 0 5. 2 104.8 130 81 117 5 . 0 7 . 2 99. 4 130 76 119 2 . 0 9 . 8 91.6 130 70 119 5 . 0 6 .7 97 .7 130 75 I133 1. 0 17 . 2 98.8 129 77 133 3 . 0 13 .7 87 . 6 129 68 133 5 . 0 5 . 1 97 .7 129 76 I 134 3 . 0 8 . 7 113 . 4 133 85 138 4. 0 5 . 0 112. 9 130 87 141 1. 5 10 . 0 107 . 3 130 83 I 141 5. 0 3 . 9 112 . 5 133 85 142 2. 0 6 . 4 101. 6 130 78 142 4. 0 5 . 4 104. 9 133 79 143 2 . 0 7. 3 119. 5 130 92 I144 2 . 0 10. 9 108. 1 134 81 144 4 . 0 4. 4 103 . 8 134 77 145 2 .0 6. 5 100. 3 130 77 I 145 4 . 0 4. 4 103 . 8 133 78 146 2 . 0 9 . 3 105. 5 130 81 146 4 . 0 5 . 1 107 . 5 134 80 I 147 2 . 0 7 . 0 99.8 130 77 147 4 . 0 9 . 2 106 . 2 134 79 ' PLATE A-3 I Jb I I J.N. 298-87 Page Two IEXPLORATORY TEST PITS IN PLACE MOISTURE AND DENSITY TEST DATA I Test Pit Depth Moisture Dry Density Maximum Dry Relative Number ( ft. ) ( %) (pcf ) Density (pcf) Compaction (%) I 149 2. 0 10. 8 118 . 8 130 91 149 4 . 0 8. 2 120. 3 133 90 150 2 . 0 9. 5 114. 9 130 88 I 150 4 . 0 7. 0 109 . 4 122 90 151 2 . 0 4 . 6 100. 5 130 77 151 4 . 0 7 . 1 106. 8 130 82 152 2 . 0 4 . 8 128. 0 130 98 I 153 3 . 0 3 . 8 98. 5 133 74 154 2 .0 7 . 5 110. 5 130 85 155 2. 0 5 . 9 111. 2 130 86 I 155 4. 0 5 . 0 114. 4 133 86 156 2 . 0 6 . 8 111. 4 130 86 157 3 . 0 9 . 8 106. 4 130 82 I 157 5. 0 10 . 6 117 . 1 133 88 158 2 . 0 11.7 124. 5 133 94 158 4 . 0 4 . 5 101. 6 121 84 159 2 . 0 2 . 4 99. 2 121 82 I 160 2 . 0 10 . 5 108 . 1 134 81 160 4 . 0 6 . 2 101. 6 134 76 161 2 . 0 11. 3 107. 9 134 81 I 161 4 . 0 4 . 9 107. 5 134 80 162 2 . 0 11. 4 106. 4 134 79 162 4 . 0 5 . 8 110. 8 134 83 163 2 . 0 8 . 6 108 . 6 134 81 I 163 4 . 0 2 .7 104. 0 133 78 165 2 . 0 5 . 0 96. 6 130 74 165 5 .0 3 . 8 98. 8 130 76 I 167 167 2 . 0 5. 0 17 . 2 10 . 4 87 . 4 89. 8 130-- 67 -- 169 2 . 0 8 . 8 104. 2 134 78 I 169 4. 0 6 . 4 123 . 2 134 92 170 2 .0 8 . 3 110. 1 134 82 170 4. 0 5 . 9 107 . 7 134 80 171 2 . 0 8 . 6 113 . 6 134 85 I 171 5 . 0 7 . 2 117 . 5 134 88 172 2 . 0 7. 8 112. 5 134 84 172 4 . 0 7 . 5 104 . 4 134 78 I 173 2 . 0 9 . 0 109 . 4 134 82 173 4. 0 5. 2 112 . 5 134 84 174 2. 0 7 . 6 105 .7 134 79 I 174 4. 0 4 . 6 108 . 3 134 81 175 2 . 0 7 . 6 105 . 9 134 79 PLATE A-4 1 I • el? I I J.N. 298-87 Page Three IEXPLORATORY TEST PITS IN PLACE MOISTURE AND DENSITY TEST DATA I Test Pit Depth Moisture Dry Density Maximum Dry Relative Number ( ft. ) ( %) (pcf) Density (pcf) Compaction (%) I 175 4. 0 3 . 6 107. 7 134 80 176 2 . 0 10 .9 123 .0 124 99 176 4 . 0 12 . 1 118. 4 124 95 I 177 2. 0 8 . 9 100. 3 132 76 177 5. 0 7 . 1 104. 2 132 79 178 2. 0 9. 2 106 . 2 132 80 178 4. 0 8 . 0 104 .0 132 79 I 179 2 . 0 9 . 1 103 . 3 132 78 179 4. 0 6. 5 114. 2 134 85 180 2. 0 8 . 1 98 . 8 132 75 I 180 4. 0 5 . 7 111. 8 134 83 181 2 . 0 6. 8 105. 5 132 80 181 4 . 0 3 . 5 112. 9 132 86 I 182 2. 0 8 . 1 108. 1 132 82 182 4. 0 4 . 7 106. 0 132 80 183 2. 0 9. 1 107 . 5 132 81 183 4 . 0 6 .4 115. 5 134 86 I 184 2 . 0 5. 0 113 . 1 132 86 184 4. 0 4. 9 120 . 6 132 91 185 2. 0 8 . 6 104. 0 132 79 I 185 4. 0 4 . 0 103 . 1 132 78 186 2 . 0 9 . 2 104 . 6 132 79 186 4 . 0 4. 5 96. 4 132 73 187 2 . 0 10. 3 112 . 1 132 85 I 187 4 . 0 6 .7 113 . 8 132 86 188 2 . 0 9 . 4 114 . 2 132 87 188 4. 0 4. 0 124 . 0 134 93 I 189 2. 0 3 . 1 104 . 0 132 79 189 4. 0 3 . 5 100. 5 133 76 190 2 . 0 6. 2 113 . 4 132 86 I 190 4. 0 2 . 6 110. 5 132 84 191 2 . 0 4 . 8 100. 1 132 76 191 4. 0 5. 8 112 .7 134 84 192 2 . 0 11. 4 110 . 5 124 89 I 193 2 . 0 8. 4 99. 2 132 75 193 4. 0 5. 4 101. 2 132 77 194 2 . 0 8 . 6 100 . 9 132 76 I 194 4 . 0 3 . 4 108. 8 132 82 195 2 . 0 7 . 6 91. 6 132 69 195 4 . 0 7 . 8 103 . 6 132 78 I 196 2 . 0 6 . 8 103 . 1 127 127 81 196 4. 0 5 . 9 92 . 6 73 PLATE A-5 I I Jo ' I I J.N. 298-87 Page Four IEXPLORATORY TEST PITS IN PLACE MOISTURE AND DENSITY TEST DATA ' Test Pit Depth Moisture Dry Density Maximum Dry Relative Number ( ft. ) ( %) (pcf) Density (pcf) Compaction (%) I 197 2 . 0 8 . 0 95.7 132 73 208 2 . 0 8 . 1 110. 5 135 82 208 4 . 0 6 . 9 104 . 2 135 77 I 209 2 . 0 6 .9 100. 5 132 76 209 4 . 0 2 .8 110 . 3 135 82 210 2 . 0 5 . 1 98 . 5 132 75 210 4 . 0 9 . 4 88 . 3 127 70 I 211 2 . 0 6 .6 92 . 0 128 72 211 4 . 0 3 .8 102 . 0 128 80 212 2 . 0 6 . 3 100 . 5 132 76 I 212 4 . 0 5 . 7 103 . 6 127 82 213 2 . 0 13 .8 107 . 3 132 81 213 4 . 0 12 . 8 110 .7 134 83 I 214 2 . 0 6 . 5 107 . 5 132 81 214 4 . 0 4 . 8 104 . 6 132 79 215 2 . 0 5 . 0 105 . 1 132 80 215 4 . 0 3 . 5 99. 4 127 78 I 216 2 . 0 11. 1 94. 2 132 71 216 4 . 0 9. 2 99 .4 132 75 218 2 . 0 10 . 9 103 . 6 132 78 I 220 3 . 0 13 .7 109.7 132 83 222 2 . 0 11. 1 109.9 131 84 222 4 . 0 12 . 6 116 . 2 131 89 224 2 . 0 11. 0 105 . 1 131 80 224 2. 0 3 . 9 106 . 2 131 81 225 2 . 0 10 . 0 102 .7 131 78 225 4 . 0 5 . 4 113 . 8 131 87 I 225 6 . 0 10 . 9 117 . 5 131 90 226 2 . 0 10 . 4 100 . 3 132 76 226 4 . 0 6 . 3 106 . 8 131 82 I 226 6 . 0 6 . 3 113 . 8 131 87 227 2 . 0 11. 1 107 . 9 132 82 227 4 . 0 5 . 4 118 . 2 131 90 227 6 . 0 8 . 4 119 . 0 131 91 I 228 2 . 0 8 . 5 108 . 1 132 82 228 4 . 0 4 .7 102 . 5 134 76 228 6. 0 6 . 5 110 . 5 134 82 I 229 2 . 0 10 . 0 102 . 5 132 78 229 4 . 0 3 . 2 109 . 9 133 83 230 4 . 0 3 . 8 96 . 4 133 72 I 230 6 . 0 5 . 6 113 . 1 133 85 231 2 . 0 7 . 5 98 . 3 133 74 PLATE A-6 I I J.N. 298-87 Page Five IEXPLORATORY TEST PITS IN PLACE MOISTURE AND DENSITY TEST DATA ' Test Pit Depth Moisture Dry Density Maximum Dry Relative Number (ft. ) (°s) (pcf) Density (pcf ) Compaction (%) I 231 4. 0 10 . 3 105. 7 133 79 231 6. 0 8. 4 106. 2 133 80 232 2 . 0 4 . 3 96. 8 121 80 I 233 2. 0 4 . 0 97. 9 128 76 233 4. 0 5 . 3 81. 8 128 64 234 2 . 0 8 . 0 100 . 5 133 76 234 4. 0 8 . 5 97 . 4 133 73 I235 2 . 0 9 . 4 95 . 3 132 72 235 4. 0 7 . 0 102 . 9 132 78 235 6. 0 3 . 9 106 . 4 133 80 I 237 2. 0 9 .7 106 . 2 132 80 237 4 . 0 5 . 0 113 . 8 133 86 237 6 . 0 8 . 1 112 .7 133 85 I 238 2 . 0 12 . 1 95 .7 132 73 238 4 . 0 4 . 1 96 . 6 133 73 238 6 . 0 6 . 0 104 . 9 133 79 239 3 . 0 7 . 9 118 . 8 125 95 I 241 2 . 0 11. 0 93 . 3 132 71 241 5 . 0 6 . 0 97 . 9 121 81 242 2 . 0 4 . 4 113 . 4 129 88 I 243 2 . 0 15 . 5 105 .7 132 80 243 4 . 0 10 . 5 111. 8 129 87 243 6. 0 9 . 0 118 . 6 129 92 244 2 . 0 13 . 8 104 . 0 132 79 I 244 6 . 0 10 .7 120 . 1 129 93 246 2 . 0 8. 1 102 . 2 129 79 246 4 . 0 6 . 2 122 .7 129 95 I 247 2 . 0 9 . 8 106. 8 129 83 247 4 . 0 11. 2 116. 8 129 91 I I I I PLATE A-7 3 a. I I J.N. 298-87 ' EXPANSION INDEX TEST DATA* I Expansion Expansion** Soil Type Index Potential A - Clayey Sand (SC) 38 Low B - Sandy Silt w/Clay (ML) 52 Medium ' D - Clayey Sand (SC) 61 Medium J - Silty Sand w/Clay (CM/SC) 24 Low IO - Clayey Sand (SC) 26 Low IQ - Silty Sand w/Clay (SM/SC) 17 Very Low U - Silty Sand (SM) 2 Very Low IW - Clayey Sand (SC) 30 Low II - Clayey Sand (SC) 31 Low ILL - Silty Sand (SM) 3 Very Low INN - Silty Sand (SM) 9 Very Low PP - Clayey Sand (SC) 27 Low RR - Silty Sand w/Clay (SM/SC) 11 Very Low UU - Clayey Sand (SC) 18 Very Low I * Per Uniform Building Code Standard Test No. 29-2 ' ** Per Table 29-C, "Classification of Expansive Soils" , Uniform Building Code, latest edition. I I I PLATE A-8 I I 33 i ' J.N. 298-87 SOLUBLE SULFATE CONTENTS ' Sample Location and Depth Sulfate Content (%) B-2 @ 15. 0 ft. 0 . 0138 B-2 @ 25. 0 ft. 0. 0132 ' B-3 @ 10. 0 ft. 0. 0174 B-3 @ 20. 0 ft. 0. 0156 B-3 @ 30. 0 ft. 0 . 0144 B-3 @ 40. 0 ft. 0. 0138 ' B-5 @ 10. 0 ft. 0 . 0176 ' B-5 @ 20. 0 ft. 0 . 0150 B-5 @ 30. 0 ft. 0 . 0134 B-5 @ 40. 0 ft. 0 . 0128 1 1 1 1 PLATE A-9 1 541 I J.N. 298-87 IDIRECT SHEAR TEST DATA IRemolded Test Samples* I Angle of Internal Cohesion Soil Type Friction (degrees) (psf) ID - Clayey Sand ( SC) 31 380 J - Silty Sand w/Clay (SM/SC) 32 240 IU - Silty Sand (SM) 34 100 CC - Silty Sand (SM) 33 160 ' PP - Clayey Sand (SC) 30 310 I * Remolded to 90% Relative Compaction Undisturbed Test Samples IBoring Depth Angle of Internal Cohesion Number (ft. ) Friction (degrees) (psf) IB-74 20 . 0 37 620 B-75 10 . 0 36 590 IB-77 20. 0 35 640 I •I I I PLATE A-10 I I --reos 97a 41 kr I BORING NO.: 37 SAMPLE NO.: DEPTH, ft.: /p,—� MATERIAL: I MOISTURE TOTAL UNIT HEIGHT, SATURATION, SAMPLE CONDITION CONTENT, % WEIGHT, pcf VOID RATIO, inches S TYPE I INITIAL 7 ¢1 io 7, 3 /, ooco 35 FINAL /S.3 //0 9 O. 9o22 9/ I0.0 1 al I F l.. -1 1i. 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SATURATION, SAMPLE CONTENT, % WEIGHT, pcf inches t TYPE I INITIAL 6?3 //4.0 /, Oo00 47 FINAL /Q,3 /20. 7 O. 9,4e797 • 0.0 } I' j i I�{: I I _1 I} I + 41 Ir I 1 ` .._lin II1.. I!"7-1-''''''"11:-1- C 1"1 } -. I r ri C L I . ! 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I 37 I BORING NO.: 35 SAMPLE NO.: DEPTH, ft.: 9.o MATERIAL: I MOISTURE TOTAL UNIT HEIGHT, SATURATION, SAMPLE CONDITION CONTENT, % HEIGHT, pcf VOID RATIO inches Z TYPE INITIAL 6'.3 ///.¢ 1. 0000 ¢4e I FINAL /4. & /20, 7 o. FP,/ /O 0 I0.0 .. I 1 .; 1 1I •i--::--1.1 1-1I • 1 1 - I t 1 -d-.7-71 I 2.0 1 LI 1 I V_ 1 ::."1-• 1 r,. i-41,14--1,-------11------:1 1 11 rt—.11+: Ifs 7 ( I . �. ' I 11 1 -1' - 1 ' 771,11:-7- ILr�J 1 I _'i a.— 1 I —a I Lt - 7_ 1 _ — X1_ , :;II,d 1 '. �'- G - 1 �- 1 o -- 17-771717!--.-7,1,i7-7r 1 I a r- . a.. — 1 I.� L.. L S.0 _, 1 I v ,..1!!.._;;__,...„...E''':;;-..i.:t4 ' 1 . r� _ '_._.ice 7 Z 'J 1 --r 1 1 I 1 I. 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I 34 • I BORING NO.: 39 SAMPLE NO.: DEPTH, ft.: 7=5 MATERIAL: MOISTURE TOTAL UNIT HEIGHT, SATURATION, SAMPLE CONDITION CONTENT, ZIYEIGHT, pcf VOID RATIO inches Z TYPE I INITIAL /0,8 //9.8 /. 0000 72 FINAL /Z.to /25-2. 0952!0 / 00 0.0 I :1 I I _ I :114,-.'14,,i-.1-1 F-11',1I ._ t I i l.- L I } 1 } L ' I ...F ' W LI I = I '. + {II ▪ 1_ {-1 i { I.1 1 4 1 1 .-«-411 I I' . 11 .. • .4L_ ! o _ p — .1:1. 1 _—__. 1.. _ 1 I cel U F Z 1 I..f - Urx ....1._...1._.:_:..1...r:..7-11:-:.I.,-1-LL 1 ' -Ll 1... lal 10.0 !- • 1 1 ; - _1 L H:144'J 1 I, JT 1. 4 I .�..' IE r } ., f 1. 1 "c177':111.111-1.11! 1 _.,1...-- 1 I 12.0 . :. 14.0 �. „ �_. I I _.l .1.. .-. 1 - I _ I F i I 16.0 II 0.2 0.5 I.0 2.0 5.0 10.0 20 0 50.0 100.0 VERTICAL STRESS, kips per square foot ' 0 FIELD MOISTURE • INUNDATED LIQUID LIMITS = PLASTICITY INDEX = ' J.N. 298-87 CONSOLIDATION TEST RESULT Plate4-/5 Petra Geotechnical , Inc. I . 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I 65 I BORING NO.: 55 SAMPLE NO.: DEPTH, ft.: 7, o MATERIAL: I CONDITION MOISTURE 1 TOTAL UNIT VOID RATIO HEIGHT, SATURATION, SAMPLE CONTENT, % WEIGHT, pcf inches Z TYPE ' INITIAL //.3 /19. 9 /.0000 7S FINAL /2.3 /Z(o,¢ o. 9119.5" 7? ' 0.0 4 'I • 1 1, 1 I , I 1 1 1 , . I t—I 1.. { 1 7 .1,4:1,..;__ .1t I 1 1 ' I',t L i • 2.0 - ._:4_,...._-.1:j.–:t_. ! I 1:j 7 'i } Li _. • r-1 t I �I = j � 11 f 4.0 I . T f -, T = 4-' . T ' 7 1 -' j —{- er .:1;:' •14.41-:.1: 7 . } ,., I F . l I"'{ II II � I I - c 8.0 t l I , 1 �---{ 1 fi^ H. ri z LJ ' w — 1 ._i I I I i f 4 T 1} .I _ I t 1 s Cl. •: , — .,..LC —r r r I .f'-r I I r ry- ? . ,'i., i j.: 10.0 I _ _ i 1 I rl 1 � r 1 j 7_ r I {_. • 1 - : .i • 1 I -I 14.0 . .. .. ...,._....... . ..:.. : . ...:-:.. _ . '._......._.I_. • i.._ .,. ..:,. 1 ' I.. I _ i..: i i .__. 16.0 I . . 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CONSOLIDATION TEST RESULT Plate A-43- III 7e, I BORING NO.: 5-9 SAMPLE NO.: DEPTH, ft.: /5„C MATERIAL: I MOISTURE TOTAL UNIT HEIGHT, SATURATION, SAMPLE CONDITION CONTENT, % WEIGHT, pcf VOID RATIO inches Z TYPE ' INITIAL /0.0 //0.2 /. 0000 Sy FINAL 45;1) /19. 7 0.9208 99 I 0.0 d 2.0 �._ 1 � r, I � I 1.4 i 1 � � � - nr , 1 - ' l1� t' .T i_.1..:1.1:11_..11,..47411__.++4.-11- -:.“--.., 1 �� , j. - I t� 1 .T - - I z I ' 1 � I i- itt y _ f FB -I i -1- ' I L i � L { 1 ' 6,1 8.0 I {�� L i ,I �1r ly , . ,_ � _ 1--+ F ' i 1 11+1 :LIE LI ` -_ 10.0 I ' II 1 — ,"i ILt{ iI I-. ----- -- ' 12.0 ;- y - { I... 14.0 y '..: 16.0 I 0.2 0.5 1.0 2.0 5.0 10.0 20.0 50.0 100.0 VERTICAL STRESS, kips per square foot 2. FIELD MOISTURE LIQUID LIMITS = • INUNDATED PLASTICITY INDEX = I J.N. 298-87 Petra Geotechnical , Inc. CONSOLIDATION TEST RESULT P1 ate A-46 I 7/ I BORING NO.: SeJ SAMPLE NO.: DEPTH, ft.: 27 s MATERIAL: I MOISTURE TOTAL UNIT VOID RATIO HEIGHT, SATURATION, SAMPLE CONDITION CONTENT, X WEIGHT, pcf inches Z TYPE I . INITIAL 8.3 /0¢..3 /, 0000 ,g , FINAL /Q,,j //Z 9 0.9235 / 00 I 0.0i 1 1 i . .I T.H. Y t+ a1 2.0 I , -= a„ i _ 1 I -F` i _ -ii t _I '''-' 1-1-4""i I 1 ! t I r : tea , J Il , r L 1 �I I 1—;� �—I' —I— L tritt„71, - ! '--t -!-, -r 17 I Z 6.0 s . I Illi _ _ i ._..II II 04Cr _1 -t I f r �_f . -II 0 f t4 I VI u 8.0 1� 1 {-,-r rr i I` f --I , i— E f I 10.0 . 1I CC La 1 _. I i..:rl -- { -- 1 i , II I -, ................ ..L!!1...:-L,, ti- ., r , r f 4r h { 1 1 y 14.0 _ .111. . _.. ..I_. .. _... -. ' 1 — — - , y �_; 6.0 ' 0.2 0.5 1.0 2.0 5.0 10.0 20.0 50.0 100.0 VERTICAL STRESS, kips per square foot 0 FIELD MOISTURE LIQUID LIMITS I • INUNDATED PLASTICITY INDEX I J.N. 298-87 CONSOLIDATION TEST RESULT Plate/1-¢7 Petra Geotechnical , Inc. I • 07 I BORING NO.: 59 SAMPLE NO.: DEPTH, ft.:301 MATERIAL: ICONDITION MOISTURE TOTAL UNIT y01D RATIO HEIGHT, SATURATION, SAMPLE CONTENT, % WEIGHT, pcf inches S TYPE I INITIAL /2 3 /0/.5 /, 0000 SO FINAL /9.5 //0. 7 0.9/68 /0/ 0.0 1 n:; 1. I I - I II i I 1... T J. I r I :--H-7-----1--,L1--!".4:71-4--11#1 r- 1 11II I I I ,l I j }2.0 1 1I _44._1: I I ii ' H.,, i r �' 1 � ji L : ._ _ 1 " 1-_ II _ ' 1 - tJL ,1 , ' ' 4 0 tI 1 :� —t r 1 1 I• i 'I �" i7 1 ▪ _t__ 1 ` Ty'L: ,_-. 1 T� I t 1 I I I I ▪ _ 4— -' '_l.. 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