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SU0014570
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Last modified
4/15/2022 4:02:57 PM
Creation date
12/27/2021 2:16:13 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0014570
PE
2600
FACILITY_NAME
SU-89-1
STREET_NUMBER
5653
Direction
E
STREET_NAME
QUASHNICK
STREET_TYPE
RD
City
STOCKTON
APN
08607014
ENTERED_DATE
12/8/2021 12:00:00 AM
SITE_LOCATION
5653 E QUASHNICK RD
QC Status
Approved
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SJGOV\jcastaneda
Tags
EHD - Public
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APPENDIX B <br /> 1., air Quality <br /> 'San Joaquin County has been designated as an Air Qui..lity Mainte- <br /> nance Area for photochemical oxidents and for particulates be- <br /> cause national ambient air quality standards (NAAQS) are not <br /> expected to be attained by 1980 and maintained through 1985. x _ <br /> either because of existing air quality or projected qr=�nvth and <br /> development in the area. " <br /> Air quality in San Joaquin County is affected by a combination of <br /> natural and man-made factors. Natural factors include thermal <br /> atmospheric inversions which prevent dispersion of pollutants and <br /> wind borne dust. Man-made factors include mobile and stationary <br /> sources of hydrocarbon and other pollutants, agricultural burning <br /> and generation of dust. <br /> San Joaquin Valley is an area of frequent thermal inversions which <br /> include radiation inversions and subsidence inversions. Radiation <br /> inversions occur most often in the fall and winter months, when the <br /> horizontal winds are lessened and when the nights are longer. The <br /> process for a radiation inversion is based on nightly loss of heat <br /> from the earth' s surface cooling the thin layer of air nearest the <br /> surface. As a result this layer of cool air is sandwiched between <br /> the earth and the warmer higher layers of air. Tule fogs are the <br /> result of radiation inversions combined with a high atmospheric <br /> humidity and a temperature below the dew point. These fogs and <br /> inversions remain until the sun warms the lower layer of air suffi- <br /> ciently to evaporate the moisture and produce the mixing of air. <br /> Subsidence inversions are the result of the compression and heating <br /> of a descending layer of upper air. This thermal inversion layer, <br /> which usually exists at an altitude of 7,000 or more feet, descends <br /> during the summer and fall, creating a canopy at 1,000 and 2,000 <br /> feet. Vertical and horizontal air movement is greatly constrained. <br /> The heating effect of the sun is much less effective in dispelling <br /> subsidence inversions than radiation inversions. The effect of <br /> these inversions is the restriction of dispersion of pollutants <br /> into the atmosphere causing ground levels of pollution to rise <br /> substantially. <br /> During early summer months westerly winds pass through the Carquinez <br /> Straits into the San Joaquin Valley. These winds carry peat dust <br /> and other soil particles throughout the Delta and into central <br /> portions of San Joaquin County. Wind borne particles are also <br /> attributed to agricultural planning, lack of adequate vegetative <br /> groundcover, and poor construction grading and excavation practice. <br /> Man-made sources of air pollution are the subject of air quality <br /> monitoring and standards administered by the Air Resources Board <br /> and the San Joaquin County Air Pollution Control District. <br /> E1 <br />
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