My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
SU0006343 SSNL
EnvironmentalHealth
>
EHD Program Facility Records by Street Name
>
C
>
CLOVER
>
11770
>
2600 - Land Use Program
>
PA-0600630
>
SU0006343 SSNL
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
5/7/2020 11:32:20 AM
Creation date
9/4/2019 11:22:27 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0006343
PE
2632
FACILITY_NAME
PA-0600630
STREET_NUMBER
11770
Direction
W
STREET_NAME
CLOVER
STREET_TYPE
RD
City
TRACY
Zip
95376
APN
21226019
ENTERED_DATE
12/12/2006 12:00:00 AM
SITE_LOCATION
11770 W CLOVER RD
RECEIVED_DATE
12/12/2006 12:00:00 AM
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\C\CLOVER\11770\PA-0600630\SU0006343\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.
/
55
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
Groundwater dilution effects can only be truly discerned with groundwater monitoring and <br /> modeling. According to a scientific paper authored by Shaw and Turyk (1994), reduction of nitrate <br /> concentrations in groundwater can occur primarily through dispersion, or by percolating rainwater, <br /> or a water source including effluent water recharge. <br /> Climatic ta: 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 tall, cool-season grass that is not water stressed. <br /> The following Table illustrates rainfall and evapotranspiration for the Tracy area. Precipitation <br /> data was obtained from the Soil Survey of San Joaquin County. The conservative "2 years in 10" <br /> data was used and not the"average rainfall" data. Evapotranspiration data was obtained from the <br /> California Irrigation Management Information System (CIMIS): <br /> E <br /> TABLE 6 <br /> PRECIPITATION AND_Eto_DATA#0k1TRACY;,CA <br /> Month 2 Years in 10 will have more Eto Average Potential Deep <br /> precipitation than: (intmo) Percolation(in/;no) <br /> (in/mo) (in/day) <br /> January 2.93 1.55 0.05 1.35 <br /> February 2.21 2.24 0.08 -- <br /> March 2.38 3.72 0.12 -- <br /> April 1.51 5.10 0.17 <br /> May 0.71 6.82 0.22 -- <br /> June 2.09 7.80 0.26 -- <br /> July 0.28 8.68 0.28 -- <br /> August 1.05 7.75 0.25 -- <br /> September 0.84 5.70 0.19 -- <br /> October 1.06 4.03 0.13 -- <br /> November 2.10 2.10 0.07 -- <br /> December 2.38 1.55 0.05 4.83 <br /> r <br /> TOTALS(in.) 13.18 57.0 ------ 2.21 <br /> The Table illustrates that evapotranspiration far exceeds precipitation, even when using higher rainfall data <br /> that exceeds normal rainfall data by 28% (10.33 in. vs. 13.18 in.) Only in the months of December and <br /> January, and possibly November and February would deep percolation potentially occur. This data 11 <br /> illustrates a relatively high potential for there to be significant evapotranspiration(or bare soil surface <br /> evaporation) frorr a mound system disposal area,particularly around the edges of the mound. <br /> 10 <br /> �jj <br /> Chesney Consulting <br /> i. <br />
The URL can be used to link to this page
Your browser does not support the video tag.