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April 17, 2019 <br /> BGG Job No. G001.05 <br /> _aQ'M'VIk <br /> Soil Borings and Test Pits <br /> On January 24,2019,we performed a percolation test in the area of the proposed guard station,as shown <br /> on Plate 2,Site Plan.The locations of our previous percolation tests at the site are also shown on the Site <br /> Plan. Percolation testing was performed in open test pits by manually digging or excavating with a <br /> backhoe to reach the desired,test depth. Materials encountered in the test pits were visually classified in <br /> —the field arid-togs were"recorded. The test pit logs are contained in Appendix B. <br /> \)-&V � , <br /> On September 25,2018, BGG conducted,a la exploration in the site vicinity,which consisted of <br /> drilling and logging two borings to depths of 20-feet and 29'/2-feet bgs,in the approximate locations <br /> shown on Plate 2—Site Plan. The borings were advanced using a truck-mounted drill rig equipped <br /> with solid flight augers and the soil was sampled with SPT (2-inch outer diameter [OD]) and <br /> Modified California(2.5-inch OD)split spoon samplers. Materials encountered in the borings were <br /> visually classified in the field and logs were recorded. The boring logs showing soil classification <br /> and blow counts are also contained in Appendix B. <br /> Based upon our previous field explorations,the general soil profile at the site can be characterized as <br /> a sequence of predominantly sandy and silty soils. The upper 3 to 4 feet of soil consists of light to <br /> medium brown, loose,dry,silty sand. This upper 3 to 4 feet is loose as a result of disturbance from <br /> vineyard removal. Below 3 to 4 feet is a weakly to moderately cemented hardpan layer consisting of <br /> brown and gray,dense,moist,silty sand and sandy silt. Below the hardpan,the silty sand is medium <br /> dense to a depth of 10 to 15 feet, whereupon the sandy soils become dense. More detailed <br /> information of materials encountered in the exploratory test pits and borings are included in the logs <br /> in Appendix B. <br /> Discussion of Soil Lithology <br /> Based on the soil observed in the test pits and borings and our previous percolation testing at the <br /> site,there appears to be potential for percolation. Sandy soils generally have a greater potential for <br /> percolation than fine-grained(silts and clays)or cemented soils. Percolation testing is discussed in <br /> the following section. <br /> Percolation Testing Procedure <br /> Field percolation testing has been performed at the site on several occasions.On January 24,2019,we <br /> performed a percolation test in the area of the proposed guard station septic system, as shown on <br /> Plate 2—Site Plan.The locations of our previous percolation tests at the site are also shown on the Site <br /> Plan. Percolation testing was performed in open test pits by manually digging or excavating with a C$ <br /> backhoe to reach the desired test depth. The soils encountered were classified and logged, and the L' <br /> bottom of the test its were then saturated b filling with water forapproximate l 2 hours. After <br /> P Y g --.Y- - <br /> saturating,double ring infiltrometers,having 6-inch diameter inner rings and 12-inch diameter outer <br /> rings,were utilized for percolation testing by setting the rings into the saturated soil surface at the <br /> bottom of the test pits, filling with water, and recording the rate of fall. <br /> Percolation Test Results <br /> The following are the results of the field percolation testing for the proposed guard station: <br /> BAEZ GEOTECHNICAL GROUP Soil Suitability Study and Nitrate Loading Study-DFV Guard Station Page 4 <br />