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ARCHIVED REPORTS_1981
EnvironmentalHealth
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4400 - Solid Waste Program
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PR0440058
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ARCHIVED REPORTS_1981
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Last modified
7/17/2020 2:16:11 PM
Creation date
7/3/2020 11:00:35 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
1981
RECORD_ID
PR0440058
PE
4433
FACILITY_ID
FA0004518
FACILITY_NAME
NORTH COUNTY LANDFILL
STREET_NUMBER
17720
Direction
E
STREET_NAME
HARNEY
STREET_TYPE
LN
City
LODI
Zip
95240
APN
06512004
CURRENT_STATUS
01
SITE_LOCATION
17720 E HARNEY LN
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
CField
Supplemental fields
FilePath
\MIGRATIONS\SW\SW_4433_PR0440058_17720 E HARNEY_1981.tif
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EHD - Public
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Under normal circumstances, it would not be possible for the ground- <br />water table to intercept waste directly since depth of waste placement would <br />only be between 30 to 40 feet below the present ground surface. The poten- <br />tial for groundwater degradation is further reduced since on-site borings <br />indicated no evidence of springs or perched waters.• The impact on the ground- <br />water is also related to the amount of "purification" the leachate attains <br />as it percolates through the subsoil beneath the waste. <br />Another possible source of groundwater quality degradation is carbon <br />dioxide (CO2) gas, generated during the waste decomposition process. Carbon <br />dioxide can be dissolved in water and can cause increased hardness or <br />corrosive conditions. Carbon dioxide could enter groundwater below the <br />study area through two mechanisms; (1) directly via movement of the gas <br />from the refuse through the soil to the groundwater; and/or (2) indirectly <br />via dissolution of CO2 in leachate, which in turn moves to mix with ground- <br />water. The extent to which CO2 gas moves through soil to groundwater is <br />related to travel distance, gas concentrations and soil type. Although these <br />mechanisms are theoretically possible, the overall impact of the groundwater <br />from CO2 gas would be negligible because of the travel distance to the water <br />table (around 100 feet) and proposed mitigation measures discussed in the <br />following section. <br />In general, the study area proposed for a sanitary landfill has attrac- <br />tive characteristics of adequate depth to the water table and the potential <br />for sufficient on-site impermeable material of at least 1 x 10-6 cm/sec or <br />slower which meets or exceeds State standards). With certain mitigation <br />measures discussed in the following section implemented, the direction of <br />groundwater movement affords the opportunity for monitoring and collection <br />of degraded groundwater and subsequent treatment, if necessary. <br />Air Quality <br />It is not anticipated that the proposed landfill operation will result <br />in significant degradation of air quality. Operation of the landfill would <br />simply be an extension of the existing landfill located one to two miles west <br />of the proposed site. The only change from the current situation would be <br />that most private and commercial vehicles hauling refuse to the new site would <br />have to travel an additional two to four miles, roundtrip. However, the State <br />EIR Guidelines require that individually minor actions which contribute to a <br />collectively significant impact must be discussed as a cumulatively signifi- <br />cant effect. <br />Estimates were made of the air quality impacts which could result from <br />the additional two to -four miles roundtrip. Assumptions made for these <br />estimates are as follows: <br />Refuse generation would be according to projections in the Solid Waste <br />Management Plan for San Joaquin County, June 1979. The "worst case", <br />or three percent annual increase, projections were used. <br />
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