My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
SR0056541 SSNL
Environmental Health - Public
>
EHD Program Facility Records by Street Name
>
B
>
BACON ISLAND
>
17247
>
2600 - Land Use Program
>
SR0056541 SSNL
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
1/7/2020 1:16:25 PM
Creation date
9/4/2019 10:11:36 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0056541
PE
2602
FACILITY_NAME
BULL FROG MARINA
STREET_NUMBER
17247
STREET_NAME
BACON ISLAND
STREET_TYPE
RD
City
STOCKTON
Zip
95219
APN
12917013
ENTERED_DATE
2/17/2009 12:00:00 AM
SITE_LOCATION
17247 BACON ISLAND RD
P_LOCATION
99
P_DISTRICT
003
QC Status
Approved
Scanner
SJGOV\sballwahn
Supplemental fields
FilePath
\MIGRATIONS\B\BACON ISLAND\17247\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.
/
58
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
E. SURFACE WATER INFORMATION Lr � <br /> Storm water management on the land-side of the levee is not too much of a concern since there is a <br /> ditch directly on the east side of the subject property that can manage runoff from the schoolhouse <br /> building and soil surface. <br /> Since the groundwater directional flow is predominately west-east based on water body orientation, <br /> Water in this ditch percolating into the top aquifer mixing layer may create a dilution effect on the <br /> crossgradient percolating septic system effluent. Groundwater dilution effects can only be truly <br /> r discerned with groundwater monitoring and modeling. According to a scientific paper authored by <br /> Shaw and Turyk (1994), reduction of nitrate concentrations in groundwater can occur primarily <br /> through dispersion, dilution, or by percolating rainwater recharge. <br /> Climatic Data: Rainfall versus Evapotranspiration <br /> NLS§3.2. 'It is generally and scientifically accepted that when precipitation exceeds evapotrans- <br /> piration (Eto); deep percolation of surface rainwater may occur. Evapotranspiration refers to water` <br /> evaporation that takes place both at the soil surface and transpiration by plants, and is defined as <br /> Water. loss from a large field of 4-to-7 inch tail, cool-season grass that is not water stressed. <br /> The following Table illustrates rainfall and evapotranspiration for the Stockton area, which was the <br /> closest data to the project site. Precipitation data was obtained from the Soil Survey of San <br /> Joaquin County. The conservative "2 years in 10" data was used and not the "average rainfall' <br /> data. Evapotranspiration data was obtained from the California Irrigation Management <br /> Information System (CIMIS): <br /> TABLE 5 <br /> FF <br /> PRECIPIT ' �4 ATION A1 �;Ety DATA,FOR STOCKTON CA,� .2 Years in 10 will have more Eto Average Potential Deep <br /> precipitation than: (in/mo) Percolation(in/mo) <br /> (in/mo) (in/day) <br /> January 4.42 1.24 0.04 3.18 <br /> February 3.20 1.96 0.07 1.24 <br /> March 3.43 3.41 0.11 -- <br /> April 1.92 5.10 0.17 <br /> May 0.50 6.82 0.22 -- <br /> June 0.25 7.80 0.26 -- <br /> July 0.23 8.06 0.26 -- <br /> August 0.40 7.13 0.23 -- <br /> September 0.76 5.40 0.18 -- <br /> 7 <br /> Chesney Consulting <br />
The URL can be used to link to this page
Your browser does not support the video tag.