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SU0004094
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SU0004094
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Entry Properties
Last modified
10/27/2020 1:02:10 PM
Creation date
9/6/2019 10:43:21 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0004094
FACILITY_NAME
QX-01-0002
STREET_NUMBER
36736
Direction
S
STREET_NAME
KOSTER
STREET_TYPE
RD
City
TRACY
ENTERED_DATE
5/12/2004 12:00:00 AM
SITE_LOCATION
36736 S KOSTER RD
RECEIVED_DATE
1/8/2002 12:00:00 AM
QC Status
Approved
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SJGOV\wng
Supplemental fields
FilePath
\MIGRATIONS\K\KOSTER\36736\QX-01-02_PA-0200065\SU0004094\EIR 2004.PDF
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EHD - Public
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I <br /> 6. <br /> buoyancy in the unstable-to-neutrally stratified mixed layer. However,after the plume <br /> encounters the mixing lid and the stably stratified air above, its vertical motion is dampened. <br /> Dispersion modeling uses hourly averaged meteorological data, terrain elevation data, and <br /> �. emissions and source release data to compute downwind pollutant concentrations over averaging <br /> periods ranging from one hour to one year. This section presents the methodology used for the <br /> dispersion modeling analysis. The methodology is consistent with procedures documented in the <br /> EPA Guideline on Air Quality Models(Revised, 1993) and SJVUAPCD's Guide for Assessing <br /> Air Quality Impacts. <br /> Molecules of gas or small particles injected into the atmosphere will separate from each other as <br /> they are acted on by turbulent,eddies. The Gaussian mathematical model simulates the dispersion <br /> of the gas or particles within the atmosphere. The formulation of the Gaussian model is based on <br /> the following assumptions: <br /> • The predictions are not time dependent(all conditions remain unchanging with time); <br /> 'i • The wind speed and direction are uniform, both horizontally and vertically throughout the <br /> region of concern; <br /> • The rate of diffusion is not a fimction of position; and <br /> • Diffusion in the direction of the transporting wind is negligible when compared to the <br /> transport flow. <br /> The Gaussian dispersion model algorithm provides a simple analytical method of estimating <br /> v downwind concentrations,where concentration is a function of several basic elements: <br /> • Initial plume height(sum of the physical stack height and the plume rise); <br /> • The source emission rate; <br /> • The horizontal and vertical plume distribution(based on atmospheric stability); <br /> • The wind speed at source height; <br /> ` • The height of the receptor; <br /> • The off-centerline of the receptor; and <br /> • The downwind distance from the source to the receptor. <br /> 'r <br /> Screening Dispersion Modeling <br /> ` A screening dispersion modeling technique was used to initially estimate health risks due to <br /> increases in DPM impacts. The screening dispersion modeling analysis used a dispersion model <br /> to predict DPM impacts at sensitive receptors from haul trucks along roadways; the CALINE4 <br /> 6. model. The CALINE4 dispersion models are conservative (tend to overpredict). <br /> The CALINE4 model is the most recent in a series of line source air quality models developed by <br /> the California Department of Transportation(Caltrans). It is based on the Gaussian diffusion <br /> equation and employs a mixing zone concept to characterize pollutant dispersion over the <br /> roadway. The purpose of the model is to assess air quality impacts near transportation facilities. <br /> Given source strength,meteorology and site geometry, CALINE4 can predict pollutant <br /> concentrations for receptors located within 500 meters of the roadway. In addition to predicting <br /> �. concentrations of relatively inert pollutants such as CO and particle concentrations; it also has <br /> B <br /> v <br />
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