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2008-342C
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2008-342C
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Last modified
4/14/2016 10:05:41 AM
Creation date
10/1/2015 12:46:06 AM
Metadata
Fields
Template:
Official Documents
Official Document Type
Migration
Approved Date
10/21/2008
Control Number
2008-342C
Agenda Item Number
8.M.
Entity Name
J.W. Cheatham
Subject
Falcon Trace Subdivision
Area
17th Lane SW
Project Number
0803, 0837, 0838
Bid Number
2008073
Supplemental fields
SmeadsoftID
7658
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Indian River County <br /> File No . 06- 5699 -5- <br /> 4 . 2 Groundwater Control <br /> The groundwater level was measured in the boreholes on the date drilled after stabilization of the <br /> downhole water level . As shown on Figure 5 , the measured groundwater level in the auger borings <br /> was at approximate depths ranging from 2 . 5 to 5 . 2 feet . Fluctuations in groundwater levels should <br /> be anticipated throughout the year primarily due to seasonal variations in rainfall and other factors <br /> that may vary from the time the borings were conducted . <br /> Some form of groundwater control (dewatering ) will likely be required during construction , <br /> particularly for utility construction and roadway construction during the wet season . Means and <br /> methods of groundwater and surface water control should be the responsibility of the contractor. <br /> We suggest that the contractor be made aware of the presence of clayey and hardpan soils <br /> present through portions of the project corridor. Such material may influence the dewatering <br /> methods used during the project. <br /> 4 . 3 Typical Seasonal High Water Table <br /> The normal seasonal high groundwater level each year is the level in the August-September period <br /> at the end of the rainy season during a year of normal (average ) rainfall . The water table <br /> elevations associated with a flood level would be much higher than the normal seasonal high <br /> groundwater level . The normal high water levels would more approximate the normal seasonal <br /> high groundwater levels . <br /> The seasonal high groundwater level is affected by a number of factors . The drainage <br /> characteristics of the soils , the land surface elevation , relief points such as drainage ditches , lakes , <br /> rivers , swamp areas , etc . , and distance to relief points are some of the more important factors <br /> influencing the seasonal high groundwater level . <br /> Based on our interpretation of the site conditions using the boring logs and the soil survey , we <br /> preliminarily estimate the normal seasonal high groundwater level at the site to be approximately <br /> 1 foot above the groundwater levels measured in the boreholes at the time of our field exploration . <br /> The estimated normal seasonal high groundwater table levels are shown on the boring profiles on <br /> Figure 5 . We recommend additional explorations be conducted during design to further evaluate <br /> the normal seasonal high groundwater table estimate . If requested , Ardaman can verify the plotting <br /> of the estimated seasonal high groundwater levels on the cross sections . Also , we can verify that <br /> the bottom of the proposed base material elevation has proper separation from the seasonal high <br /> groundwater elevation , or make recommendations for special base treatment in deficient areas . <br /> We note that water will likely " perch " temporarily atop the shallow clayey and hardpan soils at the <br /> site , at depths shallower than the estimated normal seasonal high groundwater level , during <br /> periods of heavy or prolonged rainfall . <br />
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