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2200 - Hazardous Waste Program
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Last modified
6/9/2020 2:01:51 PM
Creation date
6/3/2020 9:20:42 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2200 - Hazardous Waste Program
File Section
COMPLIANCE INFO
RECORD_ID
PR0505948
PE
2227
FACILITY_ID
FA0007101
FACILITY_NAME
FORWARD INC LANDFILL
STREET_NUMBER
9999
Direction
S
STREET_NAME
AUSTIN
STREET_TYPE
RD
City
MANTECA
Zip
95336
APN
20106003
CURRENT_STATUS
01
SITE_LOCATION
9999 S AUSTIN RD
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\HW\HW_2227_PR0505948_9999 S AUSTIN_.tif
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EHD - Public
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0 0 <br /> TECHNICAL MEMORANDUM <br /> Evaluation of Bed Ash Disposal <br /> Forward Landfill <br /> San Joaquin, California <br /> November 1, 2016 <br /> Page 10 <br /> • Closest Monitoring Well and Thickness of Saturated Zone. The distance to the closest <br /> monitoring well to each of the disposal areas was measured from Figure 1. The thickness <br /> of the saturated zone was based on the Forward Landfill Revised Engineering Feasibility <br /> study and Annual Corrective Action Report (Andrew's Engineering). The well screen <br /> depth fraction for each well was based on ratio of screen length to the aquifer thickness. <br /> • Hydraulic Conductivity, Hydraulic Gradient, and Seepage Velocity. The hydraulic <br /> gradient and conductivity of the subsurface materials were based on site monitoring <br /> report data. The seepage velocity below the disposal site was calculated by the program <br /> using these values and the effective porosity of the materials. <br /> • Aquifer Temperature, pH, and Organic Content. The groundwater temperature and pH <br /> were estimated based on recent groundwater monitoring data. The organic content of <br /> the saturated zone was assumed to be zero. The retardation coefficient for the saturated <br /> zone was conservatively set at 1, which means the contaminant will move at the same <br /> rate at the groundwater and there is no retardation in the subsurface. <br /> The parameters that were used in the model are summarized in Table 5A and 5B for the <br /> alternative disposal area/source duration scenarios. The model was run in a transient mode to <br /> calculate the predicted maximum concentration in the closest downgradient monitoring well and <br /> the time required to reach this concentration. The results of these analyses are included in Tables <br /> 5A and 5B and are summarized below. As shown by these results, if copper were to leach from <br /> the bed ash, the worst-case condition indicates the maximum concentration in the closest <br /> downgradient monitoring well would be more than 1,900 times lower than the typical copper <br /> detection limit of 0.0011 mg/L and would require more than 10,000 years to migrate from the <br /> source to the monitoring wel1.6 These long transit times and low concentrations are primarily a <br /> 6 For comparative purposes,the most critical of the different disposal scenarios that were analyzed <br /> (Alternative 1,Area 2)was evaluated by running the MULTIMED model in steady-state mode. This is extremely <br /> conservative because under steady-state,the source never decays(i.e.,it leaches forever),leakage from the <br /> landfill continues forever,the thickness of the vadose zone is irrelevant,attenuation is not allowed,and partially- <br /> penetrating monitoring wells are not considered. The steady-state DAF under these conditions is calculated to be <br /> on the order of 1,932. This means that even if the source of copper never decayed and the landfill leaked forever, <br /> the maximum concentration in groundwater for the worst-case scenario would be about 0.017 mg/L. For <br /> comparison,this value is about 10 to 100 times lower than the copper Primary Maximum Contaminant Level(MCL) <br /> of 1.3 mg/L,Secondary MCL of 1.0 mg/L,California Public Health Goal(PHG)of 0.30 mg/L,and Agricultural Water <br /> Quality Goal of 0.20 mg/L. <br />
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