My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
ARCHIVED REPORTS XR0000211
EnvironmentalHealth
>
EHD Program Facility Records by Street Name
>
B
>
B
>
1603
>
3500 - Local Oversight Program
>
PR0543430
>
ARCHIVED REPORTS XR0000211
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
2/5/2019 11:25:37 AM
Creation date
2/5/2019 10:40:04 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
3500 - Local Oversight Program
File Section
ARCHIVED REPORTS
FileName_PostFix
XR0000211
RECORD_ID
PR0543430
PE
3528
FACILITY_ID
FA0009377
FACILITY_NAME
CAL TRANS MAINT SHOP 10
STREET_NUMBER
1603
Direction
S
STREET_NAME
B
STREET_TYPE
ST
City
STOCKTON
Zip
95206
APN
16918002
CURRENT_STATUS
02
SITE_LOCATION
1603 S B ST
P_LOCATION
01
P_DISTRICT
001
QC Status
Approved
Scanner
WNg
Tags
EHD - Public
Jump to thumbnail
< previous set
next set >
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
272
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
SECTIONFOUR M(POSUrsASS®SSMOUR <br /> For low-volatility organics the model assumes there is an infinite source of organics in the surface <br />' soils and uses a volatilization rate based primarily on chemical properties The equation for low- <br /> volatility organics is described as <br /> VFss= (2wps 1 Uanrbair) Dse#H/nr(Bws+k"+HOhs)x103 <br /> where <br /> Dseff=Effective diffusivity in vadose zone soil (function of water content, porosity, and <br /> chemical Henry's constant) <br /> ms's= Volumetric water content in the vadose zone (cm3-H20/cm3-soil) <br />' ks = soil water sorption coefficient(g-H20/g-soil) <br /> H= Henry's law constant (cm3-H20)/(cm3air) <br />' Oas= Volumetric air content in vadose zone soil (cm3-atr/cm3-soul) <br /> The dilution of organics in ambient air above the source zone due to mixing with ambient air <br /> moving across the site is calculated using the box model The box model was used to estimate the <br /> steady-state average concentration of the chemicals at the site within a well-mixed cubic volume <br /> of air The model assumes that the volume of air is bound at the top of the mixing zone, and is <br /> ventilated by a steady flow of wind across the box Chemical mass enters the box through steady- <br /> state emissions from the soil, and leaves the box by advection Based on these assumptions, the <br /> steady-state average concentration in the box is computed as follows <br />' Cair = Q 103 /(mWH) <br />' where <br /> Carr = chemical concentration in air(mg/m) <br />' Q = average volatile chemical emission rate for the exposure period (g/s) <br /> in = mean annual wind speed (m/s) <br />' W = width of the box perpendicular to the predominant wind direction(m) <br /> H — height of the mixing zone (m) <br />' 103 — conversion factor(g to mg) <br /> The box model should only be used to estimate the average concentration within a volume of air <br /> and does not account for the decrease in concentration with distance or height from the source <br /> Box models have been found to be the most applicable for evaluating exposure to receptors <br /> working or living in the vicinity of the contaminated area, and typically result in very conservative <br /> Woodww1 <br /> a-M� T11 ae7w79008NA1s rocKmmr=PoRT%sF oREPlt+DocefaPwanoogNAw4A 4-10 <br />
The URL can be used to link to this page
Your browser does not support the video tag.