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2900 - Site Mitigation Program
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PR0009005
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Last modified
5/11/2020 11:50:28 AM
Creation date
5/11/2020 11:16:49 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
WORK PLANS
RECORD_ID
PR0009005
PE
2953
FACILITY_ID
FA0004053
FACILITY_NAME
LUSTRE-CAL NAME PLATE CO
STREET_NUMBER
110
Direction
E
STREET_NAME
TURNER
STREET_TYPE
RD
City
LODI
Zip
95240
APN
04124048
CURRENT_STATUS
01
SITE_LOCATION
110 E TURNER RD
P_LOCATION
02
P_DISTRICT
004
QC Status
Approved
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5.0 PRELIMINARY SITE CONCEPTUAL MODEL <br /> A Preliminary Site Conceptual Model (CSM) is a simplified representation of the vadose and <br /> groundwater flow system, frequently in the form of a block diagram or cross section (Anderson <br /> &Woessner, 1992). The purpose of the CSM is to establish an initial understanding of the <br /> vadose zone and groundwater systems and organize the associated field data so that the system <br /> can be analyzed more effectively. The CSM can be divided into three categories for the Site: (1) <br /> delineation of the hydrostratigraphic units; (2) evaluation of sources of chemicals in soil, soil gas, <br /> and groundwater; and; (3) evaluation of chemical migration. <br /> 5.1 Hydrostratigraphy <br /> The regional and local hydrogeology of the LNC area are presented in Section 3.2 of this <br /> workplan and are only briefly summarized here. Available data indicate that the sediments <br /> beneath the LNC site consist primarily of a heterogeneous, interbedded mixture of <br /> unconsolidated gravels, sand, silts, and clays to a depth of at least 120 feet bgs (Figure 6). Soil <br /> boring data indicate that the upper 15 feet of sediments consist of a heterogeneous mixture of <br /> interbedded sand, silty sand, clayey sand, and sandy silt. The shallow soils appear highly variable <br /> depending on location and historical land use. This variability may affect the distribution and <br /> detection of VOC vapors in shallow soil gas and on the parameters used to model potential VOC <br /> soil gas migration. <br /> Several intervals of sand have been identified that appear to be relatively continuous beneath the <br /> LNC site, although the thickness and permeability of the sand intervals vary(Figures 6 and 12). <br /> These sand intervals tend to coarsen and thicken towards the north (and the Mokelumne River), <br /> becoming thinner and finer-grained towards the south. Several fine-grained(predominantly silts <br /> and clay) intervals have been identified beneath the LNC site. These clay intervals appear to <br /> become more continuous and laterally extensive to the south of the LNC site. <br /> M ain\D:AEnvironmenta1\LN CV\10152007.wpd 30 <br />
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