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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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TABLE AQ-7 <br /> EMISSION FACTORS (2021) FOR NONROAD EQUIPMENT AND MOTOR VEHICLES - <br /> Equipment <br /> Type Units ROG CO NOx SO2 PM10 <br /> Excavator g/hp-hr 0.07 0.44 0.93 0.38 0.10 <br /> Haul Trucks(onsite) g/hp-hr 0.10 0.82 1.55 0.64 0.16 <br /> Front End Loader g/bp-hr 0.14 1.39 0.91 0.29 0.19 <br /> Dozer g/hp-hr 0.10 0.82 1.58 0.64 0.16 <br /> Grader g/hp-hr 0.10 0.82 1.58 0.64 0.16 <br /> J <br /> Water Pull g/hp-hr 0.10 0.82 1.55 0.64 0.16 <br /> Bobcat Loader g/hp-hr 0.10 0.84 1.65 0.64 0.16 <br /> J <br /> Maintenance Trucks g/hp-hr 0.10 0.82 1.55 0.64 0..16 <br /> Lube&Fuel Truck g/hp-hr 0.10 0.82 1.55 0.64 0.16 <br /> Forklift g/bp-hr 0.12 2.30 1.90 0.71 0.32 <br /> Pickup Trucks(onsite) g/mile 0.051 1.658 0.211 0.004 0.040 <br /> Haul Trucks(offsite) g/mile 0.266 1.614 2.020 0.017 0.143 <br /> SOURCE: California Air Resource Board.2002.EMFAC2002 Version 2.2 and Environmental Protection Agency. <br /> 1991.Nonroad Engine and Vehicle Emission Study. <br /> Dispersion Modeling <br /> Dispersion is the process by which atmospheric pollutants disseminate due to wind and vertical <br /> stability. The results of a dispersion analysis are used to access pollutant concentrations at or <br /> near an emission source. The results of an analysis allow a direct comparison of predicted <br /> concentrations of pollutants to air quality or exposure standards. <br /> A rising pollutant plume reacts with the environment in several ways before it levels off. First, <br /> the plume's own turbulence interacts with atmospheric turbulence to entrain ambient air. This <br /> mixing process reduces and eventually eliminates the density and momentum differences that <br /> cause the plume to rise. Second,the wind transports the plume during its rise and entrainment <br /> process. Higher winds mix the plume more rapidly, resulting in a lower final rise. Third,the <br /> plume interacts with the vertical temperature stratification of the atmosphere, rising as a result of <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 />
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