My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
FIELD DOCUMENTS
Environmental Health - Public
>
EHD Program Facility Records by Street Name
>
S
>
SANTA FE
>
23665
>
2900 - Site Mitigation Program
>
PR0526080
>
FIELD DOCUMENTS
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
5/18/2020 8:53:58 AM
Creation date
5/18/2020 8:45:51 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2900 - Site Mitigation Program
File Section
FIELD DOCUMENTS
RECORD_ID
PR0526080
PE
2965
FACILITY_ID
FA0017647
FACILITY_NAME
RIVERBANK WASTEWATER TREATMENT PLNT
STREET_NUMBER
23865
Direction
S
STREET_NAME
SANTA FE
STREET_TYPE
RD
City
RIVERBANK
Zip
95367
CURRENT_STATUS
01
SITE_LOCATION
23865 S SANTA FE RD
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
Scanner
LSauers
Tags
EHD - Public
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
52
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
5 GROUND WATER INVESTIGATION RESULTS <br /> 5.1 GEOLOGIC FINDINGS <br /> As referenced in above and in previous reports, the geology beneath the site is <br /> dominated by Quaternary Age alluvial sediments of the ancestral Stanislaus River, <br /> derived from granitic parent material. Borings at the site indicate near surface is <br /> comprised of silty sand to sandy silt material with shallow lenses of clean sand and <br /> r sandy gravels at depth. Both borings encountered sand at depth (greater than 35 feet) <br /> and MW-10 encountered a laterally discontinuous sandy gravel/gravelly sand layer at 5 <br /> to 20 feet. Sand encountered was composed of poorly sorted fine to coarse grained sand <br /> f <br /> material. <br /> First encountered ground water while drilling at MW-10 was found in the shallow <br /> gravel layer at 15 feet below ground surface. This level was considered to be perched as <br /> the confining silt/clay layer below was dry and ground water receded to 23 ft after <br /> drilling. The first encountered ground water in MW-11 exhibited semi-confined aquifer <br /> behavior. First encountered ground water while drilling was 26 feet bgs which came up <br /> to 21.2 feet bgs after drilling. <br /> 5.2 GROUND WATER FINDINGS <br /> Ground water elevations at the site range from 79.35 to 84.31 ft. Ground water <br /> elevation is presented in Table 5. Ground water flow is influenced by mounding near <br /> MW-1, refer to Figure 2. Ground water mounding produces an increase in elevation <br /> near monitoring wells MW-1 and MW-3. Ground water flow is radial at a gradient <br /> between wells MW-11 and MW-6 calculated at 0.00187 ft/ft. <br /> Analytical parameters results are provided in Table 3. For the parameters Total <br /> Dissolved Solids, Bicarbonate as CaCo3, and Chloride results were elevated from MW- <br /> 10 relative to MW-11. TDS exceeds California and Federal Secondary Drinking Water <br /> Standard Maximum Contaminant Levels (MCL) in both wells and the duplicate. The <br /> MW-10 chloride result at 220 mg/L is elevated but still below the secondary MCL of 250 <br /> mg/L. <br /> City o RRiverbank Wastewater Treatment Plant Monitoring Well Installation <br /> DE Protect No 109 06 May 2006 <br /> 14 Rev.0 <br />
The URL can be used to link to this page
Your browser does not support the video tag.