My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
SU0006222_SSNL
Environmental Health - Public
>
EHD Program Facility Records by Street Name
>
N
>
99 (STATE ROUTE 99)
>
12401
>
2600 - Land Use Program
>
PA-0600465
>
SU0006222_SSNL
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
11/19/2024 1:52:17 PM
Creation date
9/8/2019 12:52:17 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0006222
PE
2627
FACILITY_NAME
PA-0600465
STREET_NUMBER
12401
Direction
N
STREET_NAME
STATE ROUTE 99
City
LODI
APN
05811048
ENTERED_DATE
8/28/2006 12:00:00 AM
SITE_LOCATION
12401 N HWY 99
RECEIVED_DATE
8/28/2006 12:00:00 AM
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\N\HWY 99\12401\PA-0600465\SU0006222\NL 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.
/
71
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
June 27,2005 <br /> NOA Project Number: E05087A <br /> 1 1 concentration level of the aquifer from which the well is drawing. It i <br /> -- q g s Neil O. Anderson and <br /> Associate's opinion that,in general,near surface aquifers are more likely to have elevated <br /> concentrations of Nitrate and DBCP than the deeper aquifers. However the contaminant <br /> concentration of one aquifer cannot give any indication as to the concentrations of any other aquifer <br /> regardless of proximity. <br /> The presence of nitrates is not uncommon in shallow ground water Joaquin County <br /> n i <br /> aquifers ifu <br /> a San J q <br /> and other parts of the Central Valley. Nitrate in ground water occurs as a result of die application of <br /> fertilizers, livestock waste, and untreated septic tank waste. Nitrate is mobile and often accumulates <br /> _4 in the shallow ground water zones. <br /> In the early 1900s, natural levels of nitrate in ground water were measured in forty-three (43) wells <br /> throughout the Sacramento Valley by Bryan (1923). It was thought that ground water at that time <br /> was close to "natural" conditions. Based on the work by Bryan,it is estimated that under"natural" <br /> conditions, ground water concentration containing nitrate is no more then about 13.5 mg/L-NO3 (3 <br /> mg/L-N). Areas having 24.75 mg/L-NO3 (5.5 mg/L-N) or more are those in which nitrate <br /> concentrations may be increasing (Hull, 1984). <br /> DBCP was not found in the water sample. DBCP is a nematocide and soil fumigant for vegetables <br /> and grapes. It is thought to cause health problems consisting of kidney damage,liver damage, and <br /> cancer. The use of DBCP was discontinued in 1979. The Environmental Protection Agency (EPA) <br /> set the maximum contaminant limit (MCL) at 0.2 parts per billion (ppb) because the EPA believes <br /> that given present technology and resources, this is the lowest level to which water systems can <br /> reasonably be required to remove this contaminant should it occur in drinking water. <br /> 4.5 Well Water Sample Collection, Handling, and Transportation <br /> The sample for nitrate was collected in a clean plastic container, the sample for DBCP was collected <br /> in two clean glass vials. The samples were then transported on ice and remanded under chain of <br /> custody to Precision Enviro-Tech, Stockton., <br /> 4.6 Chain of Custody <br /> The Chain of Custody document has been included in the appendix of this report. <br /> 5.0 SOIL PROFILE AND GEOLOGIC INFORMATION <br /> The Site is depicted on the Geologic Maps of the Sacramento-San Joaquin.Delta as within the <br /> Quaternary Modesto Formation and Quaternary Riverbank Formation (Plate 7). The Quaternary <br /> Modesto Formation (undifferentiated) is unit of undifferentiated alluvial deposits, mainly arkosic, <br /> forming toe of the Mokelumne alluvial fan,generally covered by 0.3 to 1.0 in of Holocene <br /> intertidal deposits. <br /> 6 <br />
The URL can be used to link to this page
Your browser does not support the video tag.