My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
SU0004714
EnvironmentalHealth
>
EHD Program Facility Records by Street Name
>
L
>
LOUISE
>
500
>
2600 - Land Use Program
>
UP-98-22
>
SU0004714
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/7/2020 1:05:24 PM
Creation date
9/6/2019 11:06:15 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0004714
PE
2627
FACILITY_NAME
UP-98-22
STREET_NUMBER
500
Direction
E
STREET_NAME
LOUISE
STREET_TYPE
AVE
City
LATHROP
APN
19119006
ENTERED_DATE
11/18/2004 12:00:00 AM
SITE_LOCATION
500 E LOUISE AVE
RECEIVED_DATE
1/3/1989 12:00:00 AM
P_LOCATION
99
P_DISTRICT
003
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\L\LOUISE\500\UP-98-22\SU0004714\APPL.PDF \MIGRATIONS\L\LOUISE\500\UP-98-22\SU0004714\CDD OK.PDF \MIGRATIONS\L\LOUISE\500\UP-98-22\SU0004714\EH COND.PDF \MIGRATIONS\L\LOUISE\500\UP-98-22\SU0004714\EH PERM.PDF
Tags
EHD - Public
Jump to thumbnail
< previous set
next set >
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
695
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
14 <br /> maximum dry density determined by ASTM D 1557. The internal friction angle for <br /> this sample exceeded 35 degrees. A design internal friction angle of 30 degrees <br /> is suggested for compacted structural fill composed of native silty sands or <br /> native silty sands blended with up to 20 percent glass particles. <br /> The strength of the lean clay stratigraphic sequence was determined by <br /> various laboratory tests. These tests suggest the clay to be stiff to very stiff <br /> in consistency. The clay is very stiff and has a slightly higher strength near <br /> the top of the sequence. In this crustal zone the undrained shear strength is <br /> interpreted to range from 1800 to over 2400 psf. Below the crustal zone, the <br /> strength decreases to 1500 to 2000 psf down to about 30-ft depth and then begins <br /> to increase slightly with additional depth. <br /> The silty sands and poorly graded sands present below about El -20 to -25 <br /> are judged based on blow counts and sample densities to be dense to very dense. <br /> A 35-degree angle of internal friction is recommended for design. <br /> Dynamic Soil Properties <br /> The dynamic properties of soils are typically estimated by observing shear <br /> wave and compression wave velocities through the soil. These velocities also can <br /> be approximated in the laboratory using a resonant column apparatus, or in situ <br /> measurements can be made using geophysical cross-hole techniques. Although <br /> actual dynamic testing was beyond the scope of this study, a discussion of <br /> typical dynamic properties is included. <br /> The surface materials encountered down to about 15-ft depth were primarily <br /> silty sand fill and glass. The relative density of the silty sand ranged from <br /> loose to dense. The materials were generally dry to slightly moist down to about <br /> 10 ft and wet below 10 ft. Below the surficial sand and glass fill, stiff to <br /> very stiff, lean clays and dense to very dense sands were encountered. <br /> The dynamic properties are influenced by the strain amplitude, overburden <br /> and confining pressures, void ratio, overconsolidation ratio, degree of satura- <br /> tion, and number of cycles of loading. Also, the variation of dynamic properties <br /> with depth may be important to the proper dynamic design of a mat or deep founda- <br /> tion. Suggested ranges of values for the shear wave velocity, Vs, shear modulus, <br /> Gmax, Poisson's ratio, u, elastic modulus, E, and modulus of subgrade reaction <br /> based upon the static test results and site conditions are tabulated below: <br /> 1144A/CC-14 LiMcClelland <br />
The URL can be used to link to this page
Your browser does not support the video tag.