My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
ARCHIVED REPORTS_1992
Environmental Health - Public
>
EHD Program Facility Records by Street Name
>
H
>
HARNEY
>
14750
>
4400 - Solid Waste Program
>
PR0440007
>
ARCHIVED REPORTS
>
ARCHIVED REPORTS_1992
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
9/14/2020 2:06:18 AM
Creation date
7/3/2020 11:08:21 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
4400 - Solid Waste Program
File Section
ARCHIVED REPORTS
FileName_PostFix
1992
RECORD_ID
PR0440007
PE
4434
FACILITY_ID
FA0000595
FACILITY_NAME
HARNEY LANE LANDFILL
STREET_NUMBER
14750
Direction
E
STREET_NAME
HARNEY
STREET_TYPE
LN
City
LODI
Zip
95240
APN
06503006
CURRENT_STATUS
01
SITE_LOCATION
14750 E HARNEY LN
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\SW\SW_4434_PR0440007_14750 E HARNEY_1992.tif
Tags
EHD - Public
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
48
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
1 COMPUTATION SHEET <br /> 1 PROJECT TITLE: Harney Lane Sanitary Landfill PROJECT NO. 939-01.11 <br /> DESCRIPTION: Ground-water Flow Velocity SHEET 2 OF 2 <br /> PREP. BY: M Capps DATE: 8/31/92 CHKD BY: DATE: <br /> 1 <br /> Darcy's Law was used to calculate the ground water flow velocity <br /> 1 <br /> V = Ki / n <br /> 1 <br /> Where: V =Average linear velocity <br /> 1 K= Hydraulic conductivity <br /> i = Hydraulic gradient <br /> n = Porosity <br /> 1 The values used to solve the equation are as follows: <br /> 1 * K = 0.00900 <br /> i = difference in elevation between contours/horizontal distance between contours <br /> ** n = 0.3 <br /> * K value based on measurements taken at the site <br /> ** n value based on laboratory porosity measurements of samples collected from the water-bearing zone <br /> 1 The ground-water flow velocity was calculated between the -21 and-31 foot contour lines as follows: <br /> 1 Contour lines: -21 <br /> -31 <br /> Difference in elevation <br /> 1 between contours: 10 <br /> 1 Horizontal distance between lines: 2450 <br /> i= 0.0041 <br /> 1 V = 0.000122 centimeters per second <br /> 1 V = 126.78 feet per year <br /> 1 <br /> 1 <br /> me/h:HL3Qv <br /> 1 <br />
The URL can be used to link to this page
Your browser does not support the video tag.