My WebLink
|
Help
|
About
|
Sign Out
Home
Browse
Search
SR0033856_SSNL
Environmental Health - Public
>
EHD Program Facility Records by Street Name
>
E
>
ETCHEVERRY
>
8923
>
2600 - Land Use Program
>
SR0033856_SSNL
Metadata
Thumbnails
Annotations
Entry Properties
Last modified
11/16/2020 11:14:48 AM
Creation date
9/4/2019 6:10:10 PM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SR0033856
PE
2601
STREET_NUMBER
8923
Direction
W
STREET_NAME
ETCHEVERRY
STREET_TYPE
DR
City
TRACY
Zip
95304
APN
24812002
ENTERED_DATE
5/16/2003 12:00:00 AM
SITE_LOCATION
8923 W ETCHEVERRY DR
P_LOCATION
99
P_DISTRICT
005
QC Status
Approved
Scanner
SJGOV\wng
Supplemental fields
FilePath
\MIGRATIONS\E\ETCHEVERRY\8293\SS STDY\SR0033856.PDF
Tags
EHD - Public
There are no annotations on this page.
Document management portal powered by Laserfiche WebLink 9 © 1998-2015
Laserfiche.
All rights reserved.
/
36
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
r y <br /> r <br /> r <br /> sformations. The significance of cation exchange becomes important when the chemistry of <br /> tic effluent is analyzed. Nitrogen in septic tank effluent consists of approximately 75%N in the <br /> monium ion(NH4') form and 25%N in the organic form. If the ammonium ion is bound and <br /> eventually immobilized, nitrification cannot occur. <br /> The results of the soil nitrate-nitrogen concentrations were interesting. The soil sample from the <br /> future leachfield at the 42 inches in depth tested at 10 ppm NO3-N. Considering that this soil has <br /> been farmed in apricots for many years, a higher indigenous NO3-N content would have been <br />�. expected. <br /> 2.,, SUBSURFACEVSOILOIHYDRAULIC CONDUCTIVITY <br /> In addition to the conventional perc tests described below, hydraulic conductivity data of the <br /> 4 shallow soils from zero to 18 inches in depth was obtained with the test results illustrated on the <br /> PERCOLATION TEST DATA. After four hours of testing, it was determined that the shallow soils <br /> absorb 3,850 cc/hr (2,000 + 1,850 = 3,850 cc) of water. This is equivalent to 0.01695 gal/min or <br /> 24.4 gallons/day. Since the internal area of an 18-inch deep x 4.5 inch dia. boring is 270 in' or 1.9 <br /> ft', the application rate for the surface soils is theoretically 12.8 gallons/ft'/day. <br /> C. PERCOLATION TEST RESULTS <br /> The percolation test was conducted on May 13, 2003 under U.S.E.P.A. and San Joaquin County <br /> Environmental Health guidelines. Since the soil type at typical leachline depth of 42 inches is a <br /> loam soil, the test period was four hours in duration. As indicated on the attached PERCOLATION <br /> TEST DATA, the perc rate for the test boring reveals a comparatively rapid perc rate considering <br /> the loam soil. This phenomenon is regularly observed in Tracy area soils and may be attributed to <br /> the clay lattice structure in this area giving the clay soil a higher porosity. The test results are <br /> . summarized below: <br /> l <br /> aft?;eeaee.�ti-: �Vr ✓ , „� 'tdesets°rs-t! �ts . .aazae € @➢s[ �i �t�.rL; a i'�?&�=s z",� �� <br /> Pte, <br /> PERCOLATION AND �3"YDR 'ULICV0L. NDCJCTIVIT ;TESmT REEL LTS <br />� {tK...z re:4 :.'r:;e 0 �ni�$. •"l'w�t:31 da"n...,,.,3 �i'�rt=C F4d'€ -^ A✓s.cz£.?l�l <br /> SHALLOW PERC TEST PERC RATE IN HYD.GOND.TEST GALLONS/SO FTIDAY <br /> MIN/INCH <br /> Leachfield Area(42 in. Deep) 11.9 minlin Leachfield Area (18 in. Deep) 12.8 gals/ftZ/day <br /> Page -3- <br /> Chesney Consulting <br />
The URL can be used to link to this page
Your browser does not support the video tag.