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31C - CUP - 803 S SULLIVAN ST
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31C - CUP - 803 S SULLIVAN ST
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Last modified
9/16/2013 8:36:15 AM
Creation date
9/12/2013 4:38:02 PM
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City Clerk
Doc Type
Agenda Packet
Agency
Planning & Building
Item #
31C
Date
9/16/2013
Destruction Year
2018
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City of Santa Ana Environmental Checklist <br />• Establishing earthwork procedures to address soils and subsurface conditions, including <br />liquefaction. <br />• Recommending foundations, soils preparations, and slabs be designed to resist the effects of <br />lateral pressures. <br />a3. Seismic-related ground failure, including liquefaction? <br />Less-than-Significant Impact with Mitigation Incorporated. Soil liquefaction is a phenomenon in <br />which saturated, cohesionless soils layers, located within approximately 50 feet of the ground <br />surface, lose strength due to cyclic pore water pressure generation from seismic shaking or other <br />large cyclic loading. During the loss of stress, the soil acquires "mobility" sufficient to permit both <br />horizontal and vertical movements. Soils that are most susceptible to liquefaction are clean, loose, <br />saturated, and uniformly graded fine-grained sands that lie below the groundwater table within <br />approximately 50 feet below ground surface. <br />The Soil Report identified liquefaction as a potential geological condition of the project site <br />(Appendix B). Also, according to both Exhibit 5 of the Seismic Safety Element of the City's General <br />Plan and the California Department of Conservation Division of Mines and Geology (CDMG) Seismic <br />Hazards Zone Map for the Newport Beach Quadrangle (California Department of Conservation, <br />Division of Mines and Geology 1998), the project site is located within a liquefaction area where <br />historic occurrence of liquefaction or local geological, geotechnical, and groundwater conditions <br />indicate a potential for- permanent ground displacements. <br />Historical high groundwater elevations below the project site are as shallow as four feet bgs. For <br />preparation of the Soil Report, a 50-foot-deep boring was drilled at the project site to measure for <br />depths to groundwater. Groundwater was encountered at nine feet bgs. The geologic map of the site <br />shows that the project area is located within a broad flat alluvium/clluuvium area, and the Soil <br />Report identifies silty fine sand and silty clay underlying the project site. <br />The project site is mapped by the CDMG as an area of liquefaction hazard. The Soil Report includes a <br />liquefaction analysis that indicates the calculated total and differential settlements due to <br />liquefaction are about 1.55 and 1.0 inches, respectively. The Soil Report also states that to reduce <br />the potential adverse effects due to potential differential settlement due to potential liquefaction, the <br />project shall include a strengthened foundation system with grade beams, and states that a mat <br />foundation and/or caissons can be used for support of the purposed structure. <br />As described above, the proposed project would comply with all CBC requirements and standards <br />related to liquefaction. Additionally, as required in Mitigation Measure GEO.1, the proposed project <br />would comply with all geotechnical recommendations provided in the Soil Report (Appendix B) to <br />minimize potential impacts related to liquefaction. Therefore, potential impacts related to seismic- <br />related ground failure, including liquefaction, are less than significant with implementation of <br />Mitigation Measure GEO-1. <br />a4. Landslides? <br />Less-than-Significant Impact. Landslides and other slope failures are secondary seismic effects <br />that are common during or soon after earthquakes. Areas that are most susceptible to earthquake- <br />induced landslides are steep slopes underlain by loose, weak soils, and areas on or adjacent to <br />existing landslide deposits. As discussed in VLal, the proposed project site is located in a seismically <br />active region subject to strong ground shaking. However, according to the CDMG Seismic Hazards <br />The Bat Nha Buddhist Meditation Center 3-35 June 2013 <br />Initial Study/Mitigated Negative Declaration ICF W215.12 <br />31 C-88
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