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2017-00020 - new structure
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2800 Shadywood Road - 21-117-23-13-0023
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2017-00020 - new structure
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Last modified
8/22/2023 4:01:49 PM
Creation date
10/19/2018 3:01:21 PM
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x Address Old
House Number
2800
Street Name
Shadywood
Street Type
Road
Address
2800 Shadywood Road
Document Type
Permits/Inspections
PIN
2111723130023
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f <br /> Below the pavement or topsoil boring SB-lencountered about 6 feet of clayey sand and silty <br /> clay fill that extended to a depth of about 7 feet. Boring SB-2 encountered about 1 foot of <br /> sandy lean clay fill that extended to a depth of about 2 feet. <br /> Below the fill both borings encountered organic silt (swamp deposits) that extended to a <br /> depth of about 12 feet at boring SB-1 and 4 feet at boring SB-2. <br /> Underlying the pavement section,fill and/or organic silt the borings encountered sandy lean <br /> clay glacial till soils that extended to the boring termination depths at about 21 feet below the <br /> ground surface. <br /> The penetration resistance values (N-Values), shown as blows per foot (bp fl on the boring <br /> logs,within the clay glacial till soiLs ranged from 5 to 17 bpf. These values indicate the clays <br /> to have a medium to very stiff consistency with some upper soft zones. <br /> 3.2 Groundwater <br /> Groundwater was encountered in boring SB-1 at a depth of about 8 feet while drilling and at <br /> a depth of about 5 feet after drilling,which corresponds to elevations of about 9241/z and <br /> 9271/z feet,respectively. Groundwater was not encountered in boring SB-2 while drilling or <br /> after removing the augers from the borehole to a cave-in depth of 12 feet. The ordinary high <br /> water level of Lake Minnetonka is 929.4 feet. <br /> The soil borings were completed in clayey soils and given the cohesive nature of the site soils <br /> it is likely that insufficient time was available for groundwater to seep into the borings and <br /> rise to its hydrostatic level. Groundwater monitoring wells or piezometers in conjunction <br /> with deeper soil boring(s)would be required to more accurately determine water levels. <br /> Water levels were measured on the dates as noted on the boring logs and the period of water <br /> level observations was relatively short. Seasonal and annual fluctuations in the <br /> groundwater leveLs should be expected. <br /> 3.3 Laboratory Tests <br /> Laboratory moisture content tests were performed on selected samples recovered from the <br /> soil borings. Table 1 below summarizes the results of the laboratory tests. Results of the <br /> laboratory moisture content tests ranged from 16 1/z to 19 1/2 percent and are shown on the <br /> boring logs adjacent to the sample tested. <br /> Table 1. Summ of Laborato Tests <br /> Boring Moisture <br /> Number Sam le Number De th feet Content % '� <br /> SB-1 �2 21/z 161/� <br /> SB-2 S-11 5 19'/z <br /> *Values rounded to the nearest 1/z Percent <br /> 3 <br />
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