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March 31, 2008 <br /> Mr. Paul Tessier <br /> L&A Job No. 8A027 <br /> Page 4 <br /> undisturbed state can provide good foundation support with little settlement expected for lighl to <br /> moderate residential structures. <br /> Soil Conditions <br /> We werc the gcotechnical engineer of rccord for a new duplex building project rccently <br /> constructed on the Refcrence Site, about a block south of the site of the to be renovated subject <br /> residence. We provided geotechnical enginecring and construction inspection services, and <br /> vcrified footing bearing soils and evaluate cut bank stability of footprint excavation for the <br /> Referencc Project. '1'he building footprint on the Refercnce Site was cut down to about 7 feet. <br /> The soil conditions exposed on the cut banks werc composed of 10 to 12 inches of dark-brown, <br /> loose, organic topsoil, underlain by 3 to 4 feet of light-brown, dense, fine to medium sand with a <br /> trace of gravcl. This sand laycr was underlain by a deposit of'gray, hard, fine sandy silt. A ste,�el <br /> 'I'-bar manually pushed into footing bearing soils at bottom of excavation could penetrate no <br /> more than an inch. 'Che cut banks of thc building footprint excavation had stooci very stable <br /> wilhout any signs of raveling or sloughing. We expect the soil conditions at the subject project <br /> site to be similar to those at the Rcference Site. <br /> Groundwater Conditiuns <br /> A very minor trickle of groundwater scepage (Icss than 0.25 gpm)out of the cut was observed on <br /> Scptcmber 5, 2007, at the southcast comer of the building footprint excavation on the Reference <br /> Site. This sceping groundwatcr was perching on top of the underlying fine sandy silt deposit <br /> which was of extremcly low pernicability. <br /> Wc cxpcct thc groundwatcr conditions at thc subjcct projcct sitc to be similar to thosc at the <br /> Refcrcnce Site. "I'he ncar-suri'ace perched groundwater would �uctuate seasonally, dcpending on <br /> LIU & ASSOCIATES, INC. <br /> ��i ; <br />