My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
SR0080668 SSNL
Environmental Health - Public
>
EHD Program Facility Records by Street Name
>
E
>
EMERSON
>
3809
>
2600 - Land Use Program
>
SR0080668 SSNL
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
11/7/2019 10:19:37 AM
Creation date
11/7/2019 9:46:58 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0080668
PE
2602
STREET_NUMBER
3809
Direction
E
STREET_NAME
EMERSON
STREET_TYPE
RD
APN
00514511
ENTERED_DATE
5/28/2019 12:00:00 AM
SITE_LOCATION
3809 E EMERSON RD
P_LOCATION
99
P_DISTRICT
004
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.
/
66
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
• The Hantzsche and Finnemore equation is a conservative method for <br /> determining potential impacts, and actual nitrate loading experienced on the Site <br /> over time may be less than predicted. The requirement by San Joaquin County <br /> Environmental Health Department that the calculation use rainfall and <br /> evapotranspiration data to determine ground-water recharge is particularly <br /> conservative, as it does not include consideration of recharge from irrigation <br /> water or surface water sources. <br /> • Depth to ground water beneath the Site is estimated to be 83 to 93 feet. San <br /> Joaquin County experienced its highest recent ground-water levels in 1983 and <br /> 1999; according to the maps reviewed, depth to water would have been <br /> approximately 78 feet in 1983 and 72 feet in 1999. Even assuming a <br /> conservative depth to water of 72 feet, the vadose zone of the new septic system <br /> will be relatively deep, and significant nitrate attenuation would be anticipated <br /> over the course of this span. <br /> • Based on the clay soil type present on the Site, it is likely that adsorption of <br /> nitrate ions to clay will occur as percolating effluent travels downward through the / <br /> vadose zone. In their original paper, Hantzsche and Finnemore considered v <br /> developments with relatively shallow groundwater; as a result, the soil factors <br /> included in the equation may not reflect the true nitrate reduction experienced as <br /> the effluent travels down through a larger vadose zone. <br /> • The vicinity of the Site does not appear to be experiencing significant nitrate <br /> loading, despite considerable residential development. Nitrate was detected in <br /> the water sample collected from the on-site well at a concentration of 6.5 mg/L-N, <br /> well below the MCL. According to the San Joaquin County map reviewed, 11 <br /> wells within a half-mile radius of the subject Site have been tested for nitrate. <br /> Nitrate was detected in eight of these wells at concentrations between 0.1 and <br /> 5.0 mg/L-N, in two of the wells at a concentration between 5.1 and 10 mg/L-N, <br /> and in only one well at a concentration over 10 mg/L-N. <br /> It is the professional opinion of Live Oak that, based on the factors discussed above, <br /> effluent from a septic system on the subject Site is unlikely to contribute substantially to <br /> a build-up of nitrate in the ground water. <br /> LOGE 1920 Page 12 <br />
The URL can be used to link to this page
Your browser does not support the video tag.