My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
2008-342C
CBCC
>
Official Documents
>
2000's
>
2008
>
2008-342C
Metadata
Thumbnails
Annotations
Entry Properties
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
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
30
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
Indian River County <br /> File No . 06- 5699 -3 - <br /> 2 . 2 Test Locations <br /> The approximate locations of the borings are schematically illustrated on an aerial photograph <br /> obtained on - line and presented as Figure 3 . These locations were determined in the field by <br /> estimating distances from existing site features and other points of reference , and should be <br /> considered accurate only to the degree implied by the method of measurement used . If you need <br /> to know the boring locations more accurately , we recommend that you retain the services of a <br /> licensed surveyor. <br /> 2 . 3 Groundwater Measurements <br /> The groundwater levels were measured in the boreholes after stabilization of the downhole water <br /> level . The measured groundwater levels are shown adjacent to the soil profiles on Figure 5 . As <br /> shown on Figure 5 , groundwater was encountered at approximate depths ranging from 2 . 5 to 5 . 2 <br /> feet below the ground surface on the dates indicated . 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 /> We note that water will likely " perch " temporarily atop the shallow clayey and hardpan soils at the <br /> site during periods of heavy or prolonged rainfall . <br /> 3 . 0 LABORATORY TESTING PROGRAM <br /> 3 . 1 Visual Examination and Classification Testing <br /> Representative soil samples obtained during our field sampling operation were packaged and <br /> transferred to our laboratory for further visual examination and classification to obtain more <br /> accurate descriptions of the existing soil strata . The soil samples were visually classified in general <br /> accordance with the American Association of State Highway and Transportation Officials <br /> (AASHTO ) Soil Classification System (ASTM D - 3282 ) . <br /> In addition , grain size analysis (ASTM Method D422 ) , Atterberg limits testing (ASTM Method D- <br /> 423/424) , moisture content (ASTM D-2216 ) and organic content tests (ASTM Method D -2974 ) were <br /> conducted on representative soil samples to aid in classification of the soils . The results of our <br /> tests are shown adjacent to the sample depth on the soil boring profiles presented on Figures 5 . <br /> The resulting soil descriptions and the results of our tests are also summarized shown on Table 3 . <br /> Particle size analysis results are included in Appendix II . <br />
The URL can be used to link to this page
Your browser does not support the video tag.