My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
SR0080810 SSNL
Environmental Health - Public
>
EHD Program Facility Records by Street Name
>
E
>
EDNA
>
1660
>
2600 - Land Use Program
>
SR0080810 SSNL
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
11/6/2019 4:52:28 PM
Creation date
11/6/2019 4:48:06 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0080810
PE
2602
STREET_NUMBER
1660
Direction
W
STREET_NAME
EDNA
STREET_TYPE
CT
City
TRACY
Zip
95304
APN
25530003
ENTERED_DATE
6/25/2019 12:00:00 AM
SITE_LOCATION
1660 W EDNA CT
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
Scanner
TSok
Tags
EHD - Public
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
72
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
Sources of Nitrate <br /> Dairies, orchards that require fertilization in sandy soils, and septic systems have been <br /> found to be the most significant sources of nitrate in ground water. <br /> Recharge Rate of Rainfall <br /> One of the most determinant factors in the Hantzsche and Finnemore equation is the <br /> rate of recharge from percolating waters, which mix with the downward-percolating <br /> effluent generated by on-site septic systems. In the original Hantzsche and Finnemore <br /> paper, only "average recharge rate of rainfall" was considered. <br /> Based on San Joaquin County Environmental Health Department policy (personal <br /> communication, March 18, 2019), the recharge input for the Hantzsche and Finnemore <br /> equation should be derived from average monthly precipitation of rainfall and <br /> evapotranspiration rates for the area; the data should be obtained from the California <br /> Irrigation Management Information System (CIMIS), preferably from stations located <br /> within San Joaquin County. Recharge is calculated by first determining whether the <br /> average monthly precipitation exceeds average monthly potential evapotranspiration. If <br /> so, then the difference is the percolating recharge water into the aquifer. Runoff and <br /> stream infiltration drainage are not factored into the calculation. This approach likely <br /> under-estimates recharge to the aquifer and, consequently, over-estimates nitrate <br /> loading. <br /> For the project Site, the local percolation and evapotranspiration rates are presented in <br /> Plate 12. The Site is located closest to the CIMIS Ripon station (249). Data for the <br /> Ripon station were available for 2017 and 2018; based on the calculation shown, the <br /> estimated rate of recharge from percolating waters for the Ripon station is determined to <br /> be 3.12 inches. A statistical error of 46 percent is associated with this value. <br /> Quality of Rainwater <br /> Hantzsche and Finnemore utilize 1 mg/L-N as the nitrate concentration of rainwater; in <br /> the past, Live Oak has utilized this value for the nitrate loading calculation. <br /> In May 2019, Live Oak collected rainwater during two storm events in Lodi; the samples <br /> were analyzed for nitrate by FGL Environmental of Stockton. Each sample was <br /> collected in a clean, dry, stainless steel bowl, then decanted into a plastic container and <br /> placed on ice for transport. <br /> Nitrate was detected in the May 17 sample at a concentration of 0.4 mg/L-N and in the <br /> May 19 sample at a concentration of 0.2 mg/L-N. The laboratory analytical results are <br /> attached as Appendix 6 of this report. Live Oak then averaged the concentrations of the <br /> two samples, for a value of 0.3 nig/L-N to represent the nitrate concentration of rain. <br /> LOGE 1925 Page 9 <br />
The URL can be used to link to this page
Your browser does not support the video tag.