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SU0002892 SSNL
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SU0002892 SSNL
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Entry Properties
Last modified
5/7/2020 11:29:31 AM
Creation date
9/9/2019 10:13:23 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0002892
PE
2633
FACILITY_NAME
SA-97-35
STREET_NUMBER
22713
Direction
S
STREET_NAME
SEVENTH
STREET_TYPE
ST
City
TRACY
Zip
95376
ENTERED_DATE
11/6/2001 12:00:00 AM
SITE_LOCATION
22713 S SEVENTH ST
QC Status
Approved
Scanner
SJGOV\rtan
Supplemental fields
FilePath
\MIGRATIONS\S\SEVENTH\22713\SA-97-35\SU0002892\NL STDY.PDF
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EHD - Public
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II. SOIL SUITABILITY STUDY FINDINGS <br /> The recent history (199 1) of the subject property reveals the site was an arena for horses, prior to <br /> its present use. The surrounding study area has a varied agricultural history of irrigated and non- <br /> irrigated cropland and dairies. Dairies have been recognized by the State of California as potential <br /> nitrate pollution sources. Certain crops grown on dairies such as alfalfa use, or "fix" atmospheric <br /> nitrogen for cellular synthesis which can lead to excess nitrate formation. Over application of <br /> manure or wastewater to cropland can leach nitrates into the groundwater. Nitrates can also form <br /> naturally, for example in geological formations or in atmospheric phenomena such as lightning. <br /> And of course, septic systems can contribute to nitrate contamination. <br /> There is medium density housing within the town of Banta, all with septic systems. When high <br /> nitrate levels are found in the groundwater, the sources may be diverse, as referenced above. This <br /> is probably the case with the Banta area. If conditions are favorable, a percentage of nitrogen <br /> introduced into the environment may undergo complex biological transformations with the product <br /> being nitrate molecules. When the various sources of nitrogen introduced exceed the assimilative <br /> capacity of the environment, nitrate contamination of the groundwater occurs. <br /> The static groundwater level has risen in comparison to the 1991 study when the water level was <br /> at 9.0 feet below grade. Currently, the groundwater level is approximately 7.5 feet under the <br /> proposed leachfield area. This rise in groundwater elevation can be attributed to the recent heavy <br /> rains. <br /> The on-site domestic well was analyzed for nitrate(See Appendix). The results indicate the subject <br /> well currently has a concentration of 70 mg/1 (70 ppm)of nitrate. As referenced above, the drinking <br /> water Maximum Contaminant Level (MCL) is 45 ppm. It is important that the Sant Nirankari <br /> Mission inform its Parishioners of this nitrate concentration and that pregnant women, nursing <br /> mothers, infants and young children should not drink the water from this well. The subject well <br /> should be tested for nitrate on a periodic basis,preferably every three months. <br /> The percolation rate determined by Mr. Tosch in September, 1991 was 53 minutes per inch (min/in). <br /> This test took place at the end of the summer when the soil profile was most likely dry. Our test <br /> results, performed after unprecedented rains during the month of February was 5.7 min/in. <br /> Although this appears to be a contradiction since a slower rate would be expected after heavy rains, <br /> this phenomenon has been documented before. The native clay soils under the site are considered <br /> unciform, which refers to abundant earthworm activity throughout the soil profile. <br /> 2 <br /> 'Dalley Ag P pearch <br />
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