My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
COMPLIANCE INFO_JTD 2/11/26
EnvironmentalHealth
>
EHD Program Facility Records by Street Name
>
H
>
HARNEY
>
17720
>
4400 - Solid Waste Program
>
PR0440058
>
COMPLIANCE INFO_JTD 2/11/26
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
3/25/2026 10:17:41 AM
Creation date
3/24/2026 4:20:07 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
COMPLIANCE INFO
FileName_PostFix
JTD 2/11/26
RECORD_ID
PR0440058
PE
4433 - LANDFILL DISPOSAL SITE
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
Active, billable
QC Status
Approved
Scanner
SJGOV\kblackwell
Supplemental fields
Site Address
17720 E HARNEY LN LODI 95240
Tags
EHD - Public
Jump to thumbnail
< previous set
next set >
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
1799
PDF
Print
Pages to print
Enter page numbers and/or page ranges separated by commas. For example, 1,3,5-12.
After downloading, print the document using a PDF reader (e.g. Adobe Reader).
View images
View plain text
Non-Water Release Corrective Action Plan <br />North County Recycling Center and Sanitary Landfill <br />AU24.1294.00 | Non-Water Release Corrective Action Plan Update 7 <br />October 2024 <br />associated dynamic settlement) at the site is low. Accordingly, based on site-specific seismic <br />design parameters and foundation materials strength characteristics, impacts resulting from <br />liquefaction and associated dynamic settlement are considered negligible, and outside of the <br />definition of a reasonably foreseeable impact. <br />4.1.5 Impacts from Potential Slope Failure <br />4.1.5.1 Slope Stability Analysis <br />To satisfy the requirements of CalRecycle’s BMPs, the final configuration of the landfill prism <br />and cover slopes were evaluated for dynamic stability by using a horizontal PGA of 0.15g (which <br />is greater than the predicted MCE). <br />The Excavation Plan from Shaw (2010), the liner/cover site descriptions from Shaw (2007), and <br />the groundwater contour map from CB&I (2013) were used as the basis to evaluate the <br />dynamic stability of the existing landfill slopes. An evaluation of the static stability of the site <br />slopes was not performed because it is not considered necessary for the dynamic analysis of <br />the site per the CalRecycle guidelines. <br />Groundwater levels are a minimum of 100 feet below the bottom of the waste and thus, <br />groundwater was not considered in the stability analysis. <br />Two cross sections were prepared to evaluate landfill refuse prism slope stability for the <br />ultimate build-out landfill configuration (see cross section locations on Figure 2). The two <br />chosen cross section locations were based on the cross section locations with the lowest factor <br />of safety of the six cross sections presented in Shaw (2009). The cross section locations follow: <br />• Cross section A-A’ was generated in the eastern portion of the landfill through the highest <br />proposed portion of the landfill slope in the area of the shallowest landfill base. <br />• Cross section B-B’ was prepared through the southern portion of the landfill in the area of <br />the highest landfill slope. <br />4.1.5.2 Geotechnical Parameters <br />The soil materials existing and proposed at the site include: native foundation materials, cover <br />soils, geosynthetic liner/slope materials, drainage materials, and municipal solid waste (MSW) <br />fill. All the landfill modules are lined with geomembrane (HDPE) liners. <br />Geotechnical parameters required for analysis include unit weight and shear strength <br />parameters (angle of friction and cohesion). Strength parameters for the MSW are based on <br />published information by Kavazanjian et. al., (1995). The shear strength of the slope and base <br />liners was obtained from Shaw (2009). The native alluvium/formational soils were set as <br />impenetrable bedrock to force the failure surface through the overlying weaker geosynthetic <br />interfaces. The strength of the proposed cover soils and geosynthetics was estimated from <br />review of the referenced boring logs from the site; references presented in Section 8.0, Koerner
The URL can be used to link to this page
Your browser does not support the video tag.