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MEMNON <br /> A. M. ENGINEERING AND TESTING, INC. <br /> Geotechnical Exploration for Stormwater Management Planning <br /> Indian River County Parks Maintenance Complex , IRC Project No . 0710 <br /> A. M. Engineering Project No. PSL 1825 -2 <br /> inches of the ground surface for 1 up to 4 months per year. The Soil Survey describes Po <br /> sand, 0 to 5 percent slopes as a nearly level to gently sloping and moderately well drained smello generally at oil on <br /> low ridges and knolls on the flatwoods. The water table with unimproved drainage is <br /> a depth of 24 to 40 inches for about 1 to 4 months during the wet season. The three soil profiles <br /> generally consist of fine sand with little silt to depths of 6'/a feet. The soil profile for Myakka fine <br /> / to 43/4 feet, <br /> sand includes a layer of weakly cemented sand with trace to little silt at a depth of 4' <br /> and the soil profile for EauGallie fine sand includes a layer of sand with some silt and clay at a <br /> depth of 4 to 5 %4 feet. <br /> SFWMD WATER MANAGEMENT DISTRICT RAINFALL INFORMATION <br /> The rainfall has been considerably lower than normal during the three months prior to our <br /> explorations . According to the SFWMD the rainfall in Martin and St. Lucie Counties during the <br /> 30 days prior to April 10, 2007, was 41 percent of the normal; during the 30 days prior to March <br /> lM 2007, the rainfall was 15 percent of normal; and during the 30 days prior to February 10, <br /> 2007, it was 18 percent of normal. Furthermore, a news release from the SFWMD (January 4, <br /> 2007) indicated that despite above average December rains , 2006 ranked as the sixth driest on <br /> record. The Martin/St. Lucie Basin received only 61 percent of the expected historical average <br /> rainfall . <br /> „\ gg <br /> DISCUSSION AND CONCLUSIONS 1 <br /> The subsurface soils encountered in the auger borings corresponded well with the information <br /> presented in the Soil Survey. <br /> The recent rainfall history indicates that the observed water table levels are lower than normal. <br /> I <br /> Ground water and surface runoff will tend to flow towards the site and the canal since they are <br /> located in the low area paralleling the coastal ridge. The presence of the Lateral "G" Canal <br /> adjacent to the proposed pond and the pervious nature of the soils underlying the pond area <br /> indicate that the actual wet season water table levels will be strongly influenced by the water <br /> level of the canal . <br /> a <br /> Based on the above data and the results of our field exploration , we estimate that the average wet <br /> season high water table level is I foot or less above the level of the Lateral "G" Canal . However, <br /> should rainfall intensity and duration or total rainfall quantities exceed the normally anticipated <br /> rainfall quantities, the groundwater level may exceed our estimate of the average wet season <br /> high groundwater level . <br /> LIMITATIONS <br /> This report is for the exclusive use of the Indian River County Engineering Department in the <br /> design and construction of the previously described project. The right to rely on this report may <br /> _ not be assigned without written permission of A. M. Engineering and Testing, Inc. <br /> F <br /> 3 <br />