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7301 HARDESON RD 2019-01-11
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7301 HARDESON RD 2019-01-11
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1/11/2019 3:07:02 PM
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1/8/2019 10:42:26 AM
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Address Document
Street Name
HARDESON RD
Street Number
7301
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j . . <br /> Cadman,Inc. August 31,2018 Page 3 <br /> PILOT INFILTRATION TESTING <br /> One small-scale PIT was conducted in test pit PIT-1 in July 2017 and described in our previously issued <br /> geotechnical report dated August 10, 2017. The following is a summary of test methods, field measured <br /> infiltration rates, and design infiltration rates for the two additional small-scale PITs conducted as verification <br /> for the Hardeson Pond. <br /> Test Method <br /> Test pits PIT-2 and PIT-3 were initially excavated with a trackhoe to depths of approximately 21/2 and 41/2 feet, <br /> or Elevation 421.5 and 419.5, respectively, into the native advance outwash sand and gravel deposits. The <br /> bottom of each test pit was approximately 4 feet wide by 41/2 feet long. <br /> The soil in PIT-2 generally consisted of fine to coarse gravel with sand (advance outwash)at the depth tested. <br /> The soil in PIT-3 generally consisted of fine to medium sand with occasional gravel (advance outwash) at the <br /> depth tested. Groundwater seepage was not observed in the excavations during testing. Hydrograph showing <br /> the measured water levels in PIT-2 and PIT-3 throughout all stages of the small-scale PITs are shown on <br /> Figures 3 and 5,respectively. Plots of the measured infiltration rates calculated during each stage of the small- <br /> scale PITs are shown on Figures 4 and 6, respectively. Rapid infiltration was observed in PIT-2, whereas low <br /> infiltration was observed in PIT-3. <br /> During the PITs, a graduated yard stick was driven into the floor of the test pit as a visual reference for <br /> monitoring water levels during testing.A piezoelectric pressure transducer was secured to the bottom of the <br /> yard stick to provide accurate water level records in 10-second intervals throughout the duration of the tests. <br /> Water for infiltration was provided by Aero Construction using a 4,000-gallon water truck. <br /> Initial filling and maintaining of the water level in each test pit was done by monitoring the declining water level <br /> in a series of stages.The test pits were filled to a predetermined depth(approximately 14 inches)for the 6-hour <br /> pre-soaking period. During the pre-soaking,the water level was allowed to drain approximately 2 inches before <br /> the pit was refilled to the initial level again to maintain a constant minimum depth of 1 foot.This draining and <br /> refilling process was repeated a number of times(stages)in succession.At the end of the 6-hour pre-soaking <br /> period,the successive filling and draining was repeated at the same 12 and 14 inches of water depth for an <br /> additional hour, which is considered the testing period. Following this testing period,the water was turned off <br /> and the water level was recorded for an additional hour or until the test pit was drained. <br /> By periodically refilling the pit to the starting level, then allowing the water level drop between two <br /> pre-determined levels, the apparent infiltration rate for each cycle was determined accurately using <br /> measurements from the pressure transducer.The rate of decline in the falling water levels recorded after each <br /> filling cycle was used to calculate the apparent infiltration rate for each stage of the test. The overall testing <br /> process for each PIT took about 8 hours with water levels measured continuously(every 10 seconds). <br /> After each test pit was drained, it was excavated an additional 2 feet to observe and sample the soils below <br /> the level of the PITs. We did not observe hydraulically resistive layers, standing water, or seepage in the <br /> excavations below the elevation where the PITs were performed. <br /> Measured Infiltration Rate <br /> Plots of the apparent short-term infiltration rates calculated during each stage of the PITs are presented in <br /> Figures 4 and 6. Field measured infiltration rates were higher during the initial stages of the test as additional <br /> water was required to fill the pore space of the initially unsaturated soils until it approaches full saturation <br /> toward the end of the test. <br /> GEOENGINEERS� <br /> File No.7087-026-02 <br />
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