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HomeMy WebLinkAbout; Agua Hedionda Lagoon Slope Failure; Agua Hedionda Lagoon Slope Failure; 1999-03-04REPORT GEOTECHNICAL EVALUATION OF THE SLOPE FAILURE ALONG RIGHT-OF-WAY ADJACENT TO AGUA HEDIONDA LAGOON CARLSBAD, CALIFORNIA 1 1 I 1 1 I I 2 Preparedfor Engineering Department City of Carlsbad 2075 Las Palmas Avenue Carlsbad, CA 92009-1576 URSGWC Project No. 58-9911017F.OO-OEC01 March 4, 1999 URS Breinet Wo on warn Ely He 1615 Murray Canyon Road, Suite 1000 San Diego, CA 92108-4314 619-294-9400 Fax: 619-293-7920 m «f URS Greiner Woodward Clyde A Division of URS Corporation March 4, 1999 1615 Murray Canyon Road, Suite 1000 San Diego, CA 92108 Tel: 619.294.9400 Fax: 619.293.7920 Offices Worldwide Engineering Department City of Carlsbad 2075 Las Palmas Avenue Carlsbad, CA 92009-1576 Attention: Mr. Doug Helming Subject: Geotechnical Evaluation of the Slope Failure Along Railroad Right-of-Way Adjacent to Agua Hedionda Lagoon Carlsbad, California URSGWC Reference No. 589911017FOO-EC01 Dear Mr. Helming: URS Greiner Woodward Clyde (URSGWC) is pleased to provide the accompanying report, which presents the results of our geotechnical evaluation for the subject project. Our work was performed in general accordance with our proposal dated January 11, 1999 and with your verbal authorization to proceed of January 19, 1999. This report presents our conclusions and recommendations pertaining to the geotechnical aspects of the slope repair, as well as the results of our field investigation and laboratory testing. Further details are provided in the report. If you have any questions, please give us a call. Very truly yours, URS GREINER WOODWARD CLYDE eo D. Handfelt, R.G.E. Senior Associate SMF: Attachment teven M. Fitzwilham Project Manager W:\9911017REC01 -A-L. DOCV4-M AR-99VSDG TABLE OF CONTENTS Section 1 Introduction 1-1 1.1 Scope of Work 1-1 Section 2 Field Investigation and Laboratory Testing 2-1 Sections Site Conditions 3-1 3.1 Geologic and Subsurface Conditions 3-1 3.1.1 Seismicity 3-1 3.1.2 Fill Soils 3-1 3.2 Surface Conditions 3-1 3.2.1 Slope Slough 3-1 3.2.2 Adjacent Slopes 3-2 3.3 Groundwater and Surface Water 3-2 Section 4 Geotechnical Recommendations 4-1 4.1 Geologic and Seismic Hazard 4-1 4.2 Slope Repair 4-1 4.2.1 Site Preparation 4-1 4.2.2 Buttress Fill 4-2 4.3 Erosion Control 4-2 4.4 Surface Drainage 4-3 Section 5 Uncertainties and Limitations 5-1 Figures Figure 1 Figure 2 Figure 3 Figure 4 Vicinity Map Photographs of Slope Failure Schematic Cross Section Through Slope Failure Compaction and Index Property Data W:\9911017RECOA-A-R.DOC\4-Mar-99\SDG SECTIONONF Introduction This report presents the results of geotechnical services that URS Greiner Woodward Clyde (URSGWC) has provided with respect to the slope failure along the S.D.N.R. railroad alignment in Carlsbad, California. The site location is shown on the Vicinity Map (Figure 1). For our study, we have discussed the project with Mr. Doug Helming representing the City of Carlsbad. An approximately 60-foot long section of the east-facing slope of an access road along the east side of the railroad tracks has failed. Photographs of the failure are presented in Figure 2. A schematic cross-section through the failure is presented in Figure 3. An existing 72-inch wide trapezoidal storm drain empties into the Aqua Hedionda lagoon at the north edge of the slope failure. This report presents our conclusions and recommendations regarding the repair of this slope failure. 1.1 SCOPE OF WORK The purpose of our geotechnical study was to characterize the site conditions and provide recommendations for the repair of the slope. The scope of our services included a review of our files for other projects in the immediate vicinity, field explorations, laboratory testing, engineering evaluations and analyses, and preparation of this report. This study was designed to develop conclusions and recommendations regarding the following: • The geologic setting of the site • General surface and subsurface conditions • General extent of the slope failure • Repair recommendations including slope reconstruction and erosion protection. imSBrelnerWooOwartiCMe W:\9911017RECOA-A-R.DOC\4-Mar-99\SDG 1-1 SECTIONTWO Held Investigation and laboratory Testing Our field investigation consisted of a site reconnaissance and geologic mapping of the slope failure and sampling of near surface soils. The field investigation was performed by a geologist from our firm on January 21, 1999. Surface soil samples were collected and visually classified in accordance with the ASTM D2488 classification system. The samples were then returned to our laboratory for further examination and testing. The classifications were then substantiated by performing grain size analyses. Results of the grain size analyses are presented in Figure 4. The suitability of on-site soils for fill was evaluated by performing a laboratory compaction test (ASTM D1557). Results of the compaction test are also presented in Figure 4. The testing was performed in general accordance with ASTM standards. URSBrelnerWooawarti Clyde W:\9911017F\ECOA-A-R.DOC\4-Mar-99\SDG 2-1 SECTIOHTHREE Srte Conditions OUT knowledge of the site conditions has been developed from a review of area geology and field and laboratory programs undertaken for this project. 3.1 GEOLOGIC AND SUBSURFACE CONDITIONS The site is located along a man-made crossing of the Aqua Hedionda Lagoon. The site is approximately 1800 feet east of the Pacific Ocean shoreline. The site is underlain by artificial fill over Pleistocene-age terrace deposits over the Tertiary-age Santiago Formation. 3.1.1 Seismicity The Rose Canyon-Offshore Zone of Deformation-Newport Inglewood fault zone contains the nearest active faults to the site. This zone of faults is located offshore of the site at a distance of approximately 3 to 4 miles based on marine geophysical surveys. Other active faults in the vicinity include the Coronado Bank and San Clemente fault zones located further offshore at distances of approximately 20 miles and 30 miles, respectively, and the Elsinore fault zone located approximately 25 miles to the northeast. 3.1.2 Fill Soils The failed slope is within fill soils composed of silty fine sand. The near surface fill soils along the backscarp of the slide are loose. The fill soils at the toe of the slide were submerged by approximately 1 to 2 feet of water at the time of our site reconnaissance. These soils are very loose and could be easily penetrated with a footing probe. Buried rip rap was encountered at a depth of approximately 2 feet below the surface soils at the toe of the failed area. 3.2 SURFACE CONDITIONS 3.2.1 Slope Slough The slope failure is approximately 60 feet in length and 30 feet in height. Based on visual observations at the site, the toe of the slope has retreated by approximately 15 feet. The scarp of the slide is located approximately 3 to 5 feet east of the east edge of the dirt access road. No distress has been observed in the access road. Slope inclinations within the slope failure area vary from nearly vertical to approximately 5:1 (horizontal:vertical). A typical cross section of the slope failure is presented as Figure 3. A 12-inch diameter high pressure gas pipeline that traverses the failed area is currently unsupported in that area. This pipeline is located approximately 6 feet down (vertically) from the top of the slope. Gunite has been applied to two portions of the slope directly below the gas pipeline. Sand bags have been placed along the boundaries of the sloughing area. Concrete barriers have also been placed between the slough area and the access road. The outfall of a 72-inch wide trapezoidal storm drain is located just north of the slope failure. At present, there is no erosion control/slope protection existing below this outfall. It is our opinion that water from the storm drain had eroded away the toe of the slope, undermining the slope, and inducing the failure. Small trees, grassy vegetation and debris are located within the failure area. URS BttllKf H/OIHlWiinl Cl]fll8 W:\9911017RECOA-A-R.DOC\4-Mar-99\SDG 3-1 SECTIONTHREH Site Conditions 3.2.2 Adjacent Slopes The adjacent undisturbed fill slopes have inclination of approximately 1.5:1. An approximately three foot high nearly vertical slope is located at the toe of the nearby undisturbed slopes. Rip rap has been placed in front of the nearly vertical portions of the adjacent slopes. A 5 to 10 foot wide beach of sand is located between the toe of the rip rap at the toe of the slope and the lagoon water. These adjacent slopes are covered with grassy vegetation. Small to moderate sized erosional channels were observed on these surface slopes. 3.3 GROUNDWATER AND SURFACE WATER No groundwater or seeps out of slope were encountered during our site reconnaissance. Water was flowing from the storm drain into the lagoon at the time of our site visit. The water from Agua Hediondo Lagoon laps up against the toe of the slope failure. Groundwater at the site is tidally influenced. URSBrelnerH/MOwanl Clyde W:\9911017F\ECOA-A-R.DOCV»-Mar-99\SDG 3-2 SECTIONFQUR Geotechnlcal Becommendadons The discussions, conclusions, and recommendations presented herein are based on information provided to us, review of available information, results of field explorations, laboratory testing, empirical correlations, engineering analyses, and professions judgment. 4.1 GEOLOGIC AND SEISMIC HAZARD The primary geologic and seismic hazard potentially affecting the site is moderate to severe ground shaking in response to either a local moderate or more distance large magnitude earthquake. No known active faults cross the site and the area is not within an Alquist-Priolo special Studies Zone for fault rupture hazard. The Rose Canyon Fault Zone dominates the seismic exposure of coastal San Diego, including the site area. The maximum credible earthquake for the Rose Canyon fault zone consists of a three segment rupture and an estimated IV* magnitude event. In our opinion, the maximum credible earthquake for the project is a magnitude (Mw) 6.5 event, which corresponds to a single segment rupture along the nearest fault segment. Although not specifically studied for this project, soil liquefaction induced settlement may occur in the event of seismic shaking. It is our opinion that the slope failure was caused by erosional undermining of the slope by waters discharged from an adjacent storm drain. We do not believe that the failure was a deep seated slope instability. We understand that riprap and an energy dissipator is planned for the adjacent storm drain outfall. That, along with additional protection on the surface and toe of the repaired slope should mitigate the potential of a future failure. 4.2 SLOPE REPAIR We recommend that the failed area be repaired by rebuilding to match the 1.5:1 inclinations of the adjacent unfailed slopes. It is our opinion that the global stability of a 1.5:1 slope is adequate, however, measures will need to be undertaken to control erosion on the slope. The repair should be completed by removing the existing loose soils and constructing a soil buttress to rebuild the slope. The general extent of the slope repair is presented in Figure 3. We recommend that a pregrading conference be held at the site with the owner, contractor, civil engineer, and geotechnical engineer in attendance. 4.2.1 Site Preparation We recommend that existing stockpiles of soil, vegetation, and other debris and rubble be removed and disposed of off-site. We also recommend that soils containing organic matter be removed from the slope area. We recommend that material be removed from the backscarp of the failed area to create a %: 1 backslope for the soil buttress. Loose materials at the toe of the failed area should be overexcavated down to firm material, or to a maximum depth of 3 feet below the existing ground surface, to provide a foundation for the buttress. This excavation will need to be done below the lagoon water level. This overexcavation should extend from the toe of the backcut to the proposed new toe of slope; this horizontal distance is up to about 15 feet. The overexcavation W:\9911017F\ECOA-A-RDOC\4-Mar-99\SDG 4-1 SiCTIOHFOUR _ Geotechnlcal Recommendations and the backcut should extend laterally at least 5 feet into either side of the slope failure. We recommend that these excavations be observed by a qualified geologist or engineer to verify subsurface conditions. 4.2.2 Buttress Fill We recommend that backfills for the buttress placed below the lagoon level and for a vertical distance of 1 foot above the lagoon level (at the time of filling) be a 1 inch nominal size crushed rock. This 1-inch gravel should meet the specifications of Section 200-1.2 of the Standard Specifications for Public Works Construction (Green Book). The gravel can be placed in a single lift and should be compacted with a minimum of 4 passes with a heavy vibratory roller. A filter fabric should be placed on top of the gravel backfill prior to placement of the upper buttress fill soils. The filter fabric should have a minimum grab strength of 90 pounds and placed in accordance with Section 300-10. 1 . 1 of the Green Book. Select fill materials should be used for the upper buttress fills. Select fill is defined as nonexpansive (expansion index less than 50) granular (Unified Soil Classification of SM or coarser) materials. The select fills should contain no rocks or hard lumps greater than 6 inches in maximum dimension. Materials that contain perishable, spongy or otherwise compressible nature materials should not be used for the buttress fill. Materials that are removed from the face of the backscarp and the buttress foundation overexcavation should generally be suitable for use as select fill. Backfill materials should be placed in layers that, when compacted, should not exceed 8 inches. Each layer should be spread evenly and should be thoroughly mixed during the spreading to obtain uniformity of moisture and material in each layer. After each layer has been placed, mixed, and spread evenly, it should be uniformly compacted to relative compaction that is indicated by test to be not less than 90 percent. Relative compaction is defined as the ratio (expressed in percent) of the in-place dry density of the compacted fill divided by the maximum laboratory dry density evaluated in accordance with the ASTM Test Method D1557. A copy of results from an ASTM 1557 test on existing site soils is presented in Figure 4. The surface of the repaired slope should also be compacted to a minimum of 90 percent relative compaction. This could be accomplished by trackwalking of the slope, or overbuilding the slope and cutting back to the finished profile. Portions of the high pressure gas main will be unsupported during construction activities. The contractor should be responsible for providing adequate support of this pipeline during construction activities. Manually operated compaction equipment will be required in the vicinity of the gas main. 4.3 EROSION CONTROL The toe of the reconstructed slope should be protected with rip rap placed up to elevation of the existing slope rip rap and the rip rap proposed for the energy dissipator at the end of the new storm drain. The rip rap should consist of '/z ton rock and meet the requirements of Section 200-1.6 of the Green Book. The rip rap should be placed to interlock. A filter fabric should be URSGfSlllBf \HOOtlW8nlClyil6 W:\9911017F\ECOA.A-R.DOC\4-Mar-99\SDG 4-2 SEGTIONFOUR Beotechnlcal Recommendations m m placed below the rip rap to prevent migration of the fill soils through the rip rap. This filter fabric should have a minimum grab strength of 200 pounds and be placed in accordance with Section 300-9.1.1 of the Green Book. The newly graded slope surface should be protected from surface erosion with permanent revegetation. To provide temporary erosion control until the vegetation is established, a biodegradable erosion control blanket (rolled or hydraulically applied) should be installed with or over the selected seed mix. The rolled erosion control blanket should be comprised of a straw- coconut blend with netting; or the hydraulically applied blanket should be a blended fiber matrix with long fibers and a high strength adhesive that does not lose its strength upon rewetting. 4.4 SURFACE DRAINAGE We recommend that surface drainage at the top of slope be controlled to prevent ponding and infiltration of surface water into the slope. We recommend that a soil berm be constructed to direct water away from the slope face. URSBrelnermoOwartlCWe W:\9911017F\ECOA-A-R.DOC\4-Mar-99\SDG 4-3 SECTIOMFJVF DnceitaMlisiHUnludMS We have observed only a very small portion of the pertinent subsurface conditions. The recommendations made herein are based on the assumption that soil conditions do not deviate appreciably from those found during our field investigation. We recommend that URSGWC review the grading plans to verify that the intent of the recommendations presented herein has been properly interpreted and incorporated into the contract documents. We further recommend that the site earthwork be observed by a qualified engineer or geologist to verify that site conditions are as anticipated, or to provide revised recommendations, if necessary. This report is intended for design purposes only and may not be sufficient to prepare an accurate bid. Geotechnical engineering and the geologic sciences are characterized by uncertainty. Professional judgments presented herein are based partly on our understanding of the current conditions and partly on experience. Our engineering work and judgments rendered meet current professional standards; we do not guarantee the performance of the project in any respect. UHSBrelnermoOwaractyae W:\9911017RECOA-A-RDOC\4-Mar-99\SDG 5-1 CARLSBAD %\v<& ^ ¥>?)&? 3 ^^ & .c^V^V "Reproduced with permission granted by THOMAS BROS MAPS. This map is copyrighted by THOMAS BROS. MAPS. It is unlawful to copy to reproduce all or any part thereof, whether for personal use or resale, without permission." SITE VICINITY MAP CARLSBAD SLOPE FAILURE DRAWN BY: CM CHECKED BY:PROJECT NO: 589911017F.OO-OEC01 DATE: 2-3-99 FIGURE NO: 1 URS Greiner Woodward Clyde SLOPE FAILURE, LOOKING SOUTHWEST, 12-INCH GAS MAIN WITHIN FAILED AREA. SLOPE FAILURE, LOOKING NORTH. TRAPEZOIDAL OPEN CHANNEL STORM DRAIN AT TOP OF SLOPE. PHOTOS OF SLOPE FAILURE CARLSBAD SLOPE FAILURE FN: SECTION DRAWN BY: CM CHECKED BY:DATE: 2-10-99 PROJECT NO: 991107F-EC01 FIGURE NO: 2 I/as Greiner Woodward Clyde 1m If pi w Mm m m mm (N 00 CJ XOce D. Q- O UJ !<£ LU O- 3 </) LiJ 53 13 X Ul K- Q. O :fc o>o> o> toto o o !< oto o oLU Io o COMPACTION CURVE Test Method: •ASTMD1557 BASTMD698 +CA-DWR:S-10 O Other Effort Compaction Procedure: B Specimen Preparation Method: Moist 137 i M , 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 1 4. - , , , , - , , , , . , , , , - , . , . r 135 ::==:::_:_:_:::;.:=:: :_ 133 = = =:=::.=::=::::=:_:. I 131 F I I I I I I I I I I I I I I I I I I I I I I I I I I "5 129 =:..= : = -. = : = . = : = = = = ::.:-::a. :i_i: iiiin_:::ii::i::i-;;;a 01 125 *"Z 5 123 ::_=::==:::=:=::=::::=:::: Jc 119 -.-----------------^-------O :: 1 1 : 1 1 1 : : i ii : : 1 1 1 : : 1 1 :: 117 ::__:::._:::_.::::_::::=:: 113 : : ::__:: ::_:_:: ">i s_i_r::_ir:in_:i- z~ saturation = iuu* -I -.*Z--~- --------------- forGs= 2.70 s_ jj Assumed TMiTMTfii 111 m 1 1 If j^ __5_- ' ::: :r~i: :;i ::--=::-::::~: 3 3 4 5 6 7 8 9 10 11 12 13 14 Molding Water Content (%) _j ^ 15 PARTICLE-SIZE DISTRIBUTION CURVE GRAVEL SAND COBBLES COARSE | FINE COARSE) MEDIUM . FINE | SILT OR CLAY — _ s . 16 3- 2" r 3/4' 3/8" 4 10 20 40 60 100 200 U.S. Standard Sieve Size •I" on ' * * «. " O ^~ — iTi no, ^ ^ * 70 "' en .... ,.,Q DU - 50CO iS ^no_ iL_ on _ i IU *^rt •U "^ i HI -in i '•» : \ ^ 11 \ \ \ *\ \ •^• -i 100 10 1 0.1 0.01 0.001 GRAIN SIZE IN MILLIMETERS NOTATION: • Representative of entire sample • Representative of compacted specimen • Representative of compacted specimen and entire sample Exploration Sample Depth OPT.WC MAX. DUW LL P No. No. (ft) (%) (pel) B-1 1 9.0 128.5 NT N PROJECT NAME: Carlsbad Slope Failure PROJECT NUMBER: 589911 01 7F I Description and/or Classification Brown silty Sand (SIM) T COMPACTION AND INDEX FIGURE No 4 PROPERTY DATA SR-400 (11/98) (SNA)cpcl_b11 URS Greiner Woodward Clyde