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SU0001451
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SU0001451
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Entry Properties
Last modified
5/7/2020 11:28:45 AM
Creation date
9/9/2019 8:59:08 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
RECORD_ID
SU0001451
PE
2690
FACILITY_NAME
LA-97-40
STREET_NUMBER
2740
Direction
N
STREET_NAME
RAINIER
STREET_TYPE
AVE
City
STOCKTON
ENTERED_DATE
10/19/2001 12:00:00 AM
SITE_LOCATION
2740 N RAINIER AVE
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\R\RAINIER\2740\LA-97-40\SU0001451\APPL.PDF \MIGRATIONS\R\RAINIER\2740\LA-97-40\SU0001451\EH COND.PDF \MIGRATIONS\R\RAINIER\2740\LA-97-40\SU0001451\EH PERM.PDF \MIGRATIONS\R\RAINIER\2740\LA-97-40\SU0001451\CORRESPOND.PDF
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EHD - Public
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Evapotranspiration-Absorption (ETA) Septic System <br /> — General Design Approach & Construction Specifications — <br /> Design Approach: <br /> We propose utilizing an evapotranspiration absorption (ETA) septic system for septic <br /> effluent disposal. The ETA septic system can be used when the native soil absorption rate is not <br /> satisfactory for a conventional septic system, when shallow ground water is present, or where <br /> bedrock conditions are present. The ETA septic system design approach is described by Otis and <br /> Boyle(1980) for the U.S. Environmental Protection Agency. <br /> The ETA sewage loading rate for the subject project is the most important consideration <br /> for the design of the system. The ETA sewage loading rate was determined, in part, from <br /> information from a local agricultural weather station and from a percolation test performed at the <br /> site. The average daily pan evaporation and the average daily precipitation was gathered at Lodi <br /> weather station LODI.0 (NCDC #5032,Lodi) (http://www.ipm.ucdavis.edu/WEATHER/ <br /> AVERAGES/lodi.html). Daily pan evaporation was not available from the Stockton Station. The <br /> weather station data gathered for this design is from a period beginning in 1951 to several <br /> months ago. <br /> Reference Evapotranspiration(ETo) is a term used to estimate the evapotranspiration rate <br /> of a reference crop. The reference crop, in this case, is grass which is closely clipped, actively <br /> growing, completely shading the soil, and well watered. The ETo is expressed in inches/day <br /> (in/day) similar to pan evaporation however it is a slightly lesser value. The daily ETo has not <br /> been measured over the long term like pan evaporation; however, it can be extrapolated from pan <br /> evaporation by taking the pan evaporation value and multiplying it by a local conversion factor <br /> of 0.75 to obtain ETo(oral communication with CIMS help line, 2001). See Equation no. 1. <br /> Equation No. 1 <br /> Pan Evaporation (in/day) x 0.75 = ETo in/day <br /> A deficit curve was found by subtracting average daily precipitation from average daily <br /> ETo(see Equation No. 2 and Plate 1). The term "deficit"refers to a period occurring between <br /> November 15 to April 1 where average daily precipitation exceeds average daily ETo. The <br /> highest deficit rate was found to occur on January 22 when using a moving average filter with a <br /> two (2) day filter window. The highest deficit for the average year is 0.14 in/day. The deficit <br /> rate may be exceeded approximately five (5) isolated days per average year. <br /> Equation No. 2 <br /> (Also see Plate 2, December 24) <br /> Precipitation (in/day)- ETo (in/day) = Deficit Rate (in/day) <br /> The deficit rate i5 the condition where precipitation exceeds ET, <br /> —Calculations, Page I— <br />
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