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ARCHIVED REPORTS PHASE II FIELD INVESTIGATION AND LNAPL MOBILITY EVALUATION REPORT
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ARCHIVED REPORTS PHASE II FIELD INVESTIGATION AND LNAPL MOBILITY EVALUATION REPORT
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Last modified
12/14/2018 4:37:48 PM
Creation date
11/6/2018 1:47:45 PM
Metadata
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Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
ARCHIVED REPORTS
FileName_PostFix
PHASE II FIELD INVESTIGATION AND LNAPL MOBILITY EVALUATION REPORT
RECORD_ID
PR0009049
PE
2960
FACILITY_ID
FA0004041
FACILITY_NAME
UP TRACY RAIL YARD
STREET_NUMBER
720
Direction
E
STREET_NAME
SIXTH
STREET_TYPE
ST
City
TRACY
Zip
95376
APN
25001014
CURRENT_STATUS
01
SITE_LOCATION
720 E SIXTH ST
P_LOCATION
03
P_DISTRICT
005
QC Status
Approved
Scanner
WNg
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\MIGRATIONS\S\SIXTH\720\PR0009049\PHASE II FIELD INVESTIGATION AND LNAPL MOBILITY EVALUATION REPORT.PDF
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tPhase II Field <br /> ARCADIS Investigation and LNAPL <br /> ' Mobility Evaluation Report <br /> Union Pacific Railroad Company <br /> Former Maintenance Facility <br /> ' Tracy, California <br /> displaces LNAPL with air via centrifugal force.The free-product mobility test <br /> ' provides a very conservative residual saturation, because the test is conducted at a <br /> centrifugal force of 1,000 times gravitational force. <br /> ' When field saturation equals residual saturation,the LNAPL is immobile. If field LNAPL <br /> saturation in a soil core is greater than the residual LNAPL saturation,then LNAPL is <br /> mobile at the pore-scale, but may not be migrating on a plume-scale. Hydraulic <br /> gradient, aquifer permeability, and LNAPL viscosity are a few factors that influence <br /> whether or not the LNAPL above residual saturation is capable of migrating. The <br /> LNAPL pore velocity calculations described below consider these additional factors. <br /> ' 5.1.3 LNAPL Pore Velocity Calculations <br /> ASTM International's E2531-06el Standard Guide for Development of Conceptual Site <br /> ' Models and Remediation Strategies for Light Non-Aqueous Phase Liquids (ASTM <br /> International 2006)suggests that a LNAPL mobility of less than 1 x 10-'centimeters <br /> per second (cm/s) is indicative that LNAPL in the formation is functionally immobile. <br /> When mobility exceeds this criterion, it is an indication that LNAPL is mobile at the <br /> pore-scale and capable of moving vertically or laterally within the formation.Additional <br /> ' analyses are needed to assess whether the LNAPL plume footprint is expanding due <br /> to LNAPL migration. <br /> Site-specific LNAPL mobility can be characterized through the use of site data and <br /> ' advanced LNAPL mobility calculations developed through the joint work of a number of <br /> research universities and private organizations. One of the more comprehensive <br /> bodies of work in this area has been completed by the API and published in numerous <br /> technical bulletins (e.g.,API Publications 4682,4711, 4729, and 4760). This science- <br /> based mobility assessment approach was formulated to support analysis of long-term <br /> movement of LNAPL plumes in the subsurface and is referenced as a component of <br /> t site management/characterization in a 2005 USEPA document titled A Decision- <br /> Making Framework for Cleanup of Sites Impacted with Light Non-Aqueous Phase <br /> Liquids(USEPA 2005). <br /> ' ARCADIS created a mobility calculation spreadsheet based on equations provided in <br /> API technical documents, predominantly API Bulletin 4760(API 2007).The <br /> ' spreadsheet model uses step integration functions to calculate the expected LNAPL <br /> saturation and corresponding LNAPL relative permeability based on input of the <br /> physical properties of the product and aquifer matrix and assumed water/LNAPL <br /> ' saturation conditions in the aquifer. LNAPL saturation and relative permeability are <br /> 19 <br /> ,plagrLacylnµl mo RY11-232010I.d. <br />
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