My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
SU0000143 SSNL
EnvironmentalHealth
>
EHD Program Facility Records by Street Name
>
K
>
KOSTER
>
33510
>
2600 - Land Use Program
>
MS-98-07
>
SU0000143 SSNL
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
5/7/2020 11:27:38 AM
Creation date
9/6/2019 10:42:21 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0000143
PE
2622
FACILITY_NAME
MS-98-07
STREET_NUMBER
33510
Direction
S
STREET_NAME
KOSTER
STREET_TYPE
RD
City
TRACY
Zip
95376
APN
25516021
ENTERED_DATE
8/14/2001 12:00:00 AM
SITE_LOCATION
33510 S KOSTER RD
RECEIVED_DATE
3/11/1998 12:00:00 AM
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\K\KOSTER\33510\MS-98-07\SU0000143\SS STDY.PDF
Tags
EHD - Public
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
11
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
- [3] SOIL PROFILE AND PERCOLATION TESTING <br /> One shallow percolation test was conducted on Parcel 1 according to San Joaquin County <br /> Department of Environmental Health regulations. No perc test was performed on the Designated <br /> Remainder per Department regulations. The perc test location is illustrated on the attached <br /> Parcel Map. Percolation test results can be found on the Field Test Data Sheet in the Appendix. <br /> Perc test results indicate a comparatively fast percolation after the four hour test period. Soil <br /> structures consists of a tight sandy silt (SM) throughout the shallow soil profile. No hardpan <br /> layer was encountered. The borings were pre-saturated the total depth, 24 hrs prior to starting <br /> the perc tests to induce worst-case saturated soil conditions. <br /> Percolation test results indicate a perc rate of 5.5 min/in for Parcel 1. Considering the soil type, <br /> this rate can be considered very favorable. It is our opinion that the material at the test depth of <br /> 42 inches is of sufficient porosity to allow water infiltration and percolation. However, repeated <br /> saturations from septic effluent, in conjunction with the propensity of the soil to build up a <br /> biomat, leads to leachline failures as evidenced by the repairs. <br /> [4] LOCAL GROUNDWATER AND SURFACE WATER INFORMATION <br /> The static water table depth, or the zone of saturation is located at approximately 55 feet below grade <br /> from the sounding of a domestic well on Ohm Road. The 1996 "Lines of Equal Depth" published by <br /> the San Joaquin County Flood Control District does not reference the static water table depths in this <br /> area. It is possible there may be perched water table conditions under the subject property at a higher <br /> elevation than the static water level and this should be investigated if seepage pits are ever installed. <br /> There is no potential for septic impact to any surface waters, providing applicable distance <br /> requirements are followed. The property is not in the flood plain. <br /> Due to the fact that MS-98-6 and this Minor Subdivision, MS-98-7 are in close proximity to each <br /> other, permission was granted by the Environmental Health Department to use the waster analysis <br /> obtained from the domestic well at the farm labor residences near the intersection of Ohm Road and <br /> Koster Road. These two projects are less than an eighth of a mile apart. The nitrate concentration <br /> at this well was 22 ppm NO3. The Maximum Contaminant Level (MCL) for NO3 in drinking water <br /> is 45 ppm. The pesticides DBCP and EDB were not detected (ND). A nitrate concentration of 22 <br /> ppm indicates the underlying aquifers have been moderately impacted from nitrogen contributors, <br /> such as agricultural operations, septic systems or rainfall. No well logs were available in the area to <br /> verify if clay layers may have helped attenuate the downward migration of nitrate molecules. <br /> Groundwater directional flow is unknown, but appears to be to the southeast- <br /> 2 <br />
The URL can be used to link to this page
Your browser does not support the video tag.