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2018.02.05 CC Packet
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2018.02.05 CC Packet
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2/20/2019 1:50:52 PM
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City Council
Document Type
Agenda/Packets
Meeting Date
2/5/2018
Meeting Type
Regular
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3. EXPLORATION RESULTS <br />3.1 Site and Geology <br />The borings were completed through the bituminous pavement section in the drive lanes of Oneka Lake <br />Boulevard and Harrow Avenue North. Boring elevations ranged from about 925.3 to 942.5 feet, and <br />indicate a moderately undulating terrain. <br />The Washington County Geologic Atlas indicates the surficial geology of the area is mostly lake deposited <br />sand and pockets of organic deposits. <br />3.2 Subsurface Soil and Groundwater Conditions <br />The boring profile generally consisted of the pavement section and fill materials overlying lake deposited <br />sandy soils. Boring PB -13 encountered organic deposits below the fills. <br />Pavement Section <br />The pavement section generally consisted of about 4 to 5 inches of bituminous asphalt, with an average <br />of 4 inches, and about 6 to 12 inches of aggregate base, with an average of 10 inches. <br />Fills <br />The fills encountered in the borings generally consisted of a mixture of sands with silt and sands with <br />gravel. These fills were commonly encountered to depths of about 2'/2 to 3 feet below grade, but at <br />Boring PB -5 was encountered to a depth of about 6 feet and at Boring PB -13 was encountered to a depth <br />of about 5 feet. <br />Organics <br />Boring PB -13 encountered peat and clays with organics below the fill materials. These organic soils were <br />encountered to a depth of about 20 feet below grade. The organic soils were black in color and generally <br />wet to saturated. <br />Lake deposits <br />The lake (lacustrine) deposits encountered in the borings ranged from sands with silt to silty sands to silty <br />sands with clay. These soils were brown in color where encountered in the upper 15 feet of the boring, <br />and at Boring PB -13 were gray to dark brown to brown in color. These soils were moist to wet to <br />waterbearing. <br />3.3 Strength Characteristics <br />The penetration resistance N -values of the materials encountered were recorded during drilling and are <br />indicated as blows per foot (BPF). Those values provide an indication of soil strength characteristics and <br />are located on the boring log sheets. Also, visual -manual classification techniques and apparent moisture <br />contents were also utilized to make an engineering judgment of the consistency of the materials. <br />Table 1 presents a summary of the penetration resistances in the soils for the borings completed and <br />remarks regarding the material strengths of the soils. <br />Table 1: Penetration Resistances <br />Soil Type <br />Classification <br />Penetration <br />Remarks <br />Resistances <br />Fill <br />Varies <br />5 to 8 BPF <br />Poorly compacted <br />Peat / Organics <br />PT, OL <br />2 to 3 BPF <br />Very soft <br />Lake Deposits <br />SP -SM, SM, SC <br />2 to 20 BPF <br />Very loose to medium dense <br />Average 8 /2 BPF <br />Generally loose <br />Geotechnical Report <br />Oneka Lake Boulevard and Harrow Avenue Improvements <br />Hugo, Minnesota <br />WSB Project No. 010893-000 <br />Page 3 <br />
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