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SU0000030 SSNL
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MS-01-04
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SU0000030 SSNL
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Entry Properties
Last modified
5/7/2020 11:27:34 AM
Creation date
9/4/2019 10:18:18 AM
Metadata
Fields
Template:
EHD - Public
ProgramCode
2600 - Land Use Program
FileName_PostFix
SSNL
RECORD_ID
SU0000030
PE
2622
FACILITY_NAME
MS-01-04
STREET_NUMBER
7855
Direction
W
STREET_NAME
BATES
STREET_TYPE
RD
ENTERED_DATE
8/8/2001 12:00:00 AM
SITE_LOCATION
7855 W BATES RD
RECEIVED_DATE
2/1/2001 12:00:00 AM
P_LOCATION
99
P_DISTRICT
004
QC Status
Approved
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SJGOV\rtan
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FilePath
\MIGRATIONS\B\BATES\7855\MS-01-04\SU0000030\NL STDY.PDF
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EHD - Public
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x 4p -+-eople per.household x 2 houses 1 person/2.08 Ac x 365 d/vr=4.0 in/yr <br /> rr7_&ajs/verson/dav <br /> 43,560 cu ft/Ac ft x 7.48 gal/cu ft x (I ft/12 in) <br /> Nw= 66 mg/L - 20% reduction in each of 2 septic tanks =40%reduction total = 40 mg/L N <br /> d = 10% from biomat and 25% from clay soil under leachlines. <br /> Nb = Assumed to be 0.1 ppm NO3-N <br /> 4.0 in/yr 40 mg N/L I - 0.35 + 13 in/yr x 0.1 m /L <br /> Nr = (4.0 in/yr+ 13 in/yr) <br /> Nr = 6.2 ppm as NO3-N or 27.6 ppm as NO3 <br /> IV. CONCLUSIONS AND RECOMMENDATIONS FOR IMPACT MITIGATION <br /> Analyses of soil under the Cole's leachfield reveals apparent denitrification occurring within the <br /> soil environment in a relatively short distance: 20%denitrification in 7 ft. It can be assumed that <br /> since there was virtually no ammonia-nitrogen(NH4), which is the precursor to nitrate formation, <br /> that only the organic fraction of the total nitrogen assessed can contribute to further nitrate <br /> formation. This is going to occur only under aerobic, ideal conditions, which are normally not <br /> found within the microscopic pore spaces of clay soil. <br /> With regard to the nitrate-nitrogen loading to the underlying groundwater, it is important to <br /> recognize that when adding one concentration of a solute (e.g.,NO3-1v in recharge water) to <br /> another concentration of a solute (e.g.,NO3-N in groundwater), where both solutes are in ppm,the <br /> result is not cumulative or the sum of the two solutes. Parts per million is a mass-to-mass ratio. <br /> For example, the Nr(the resultant average concentration of nitrate-nitrogen in recharge water in <br /> PPM of NO3-N) above, was determined to be 6.2 ppm. This equals 6.2 milligrams of nitrate in 106 <br /> milligrams of water(one liter). If this 6.2 ppm concentration is added to the same volume of water <br /> (I x 10'milligrams) with the concentration determined in the underlying groundwater from the <br /> Cole domestic well, which was 8.5 ppm NO3-N (38 ppm NO3), then the resultant concentration is <br /> now 6.2 milligrams+ 8.5 milligrams= 14.7 milligrams in 2 x 106 milligrams (2 liters, or parts per <br /> 2 million) of water. Therefore, to convert back to ppm, the numerator and denominator must be <br /> divided by 2 with the result of 7.4 milligrams per 1 x 106 milligrams, or 7.4 ppm. On a mass-to- <br /> mass ratio basis,there can be a dilution effect of nitrate concentration;from the resultant recharge <br /> water(Nr) as long as the underlying aquifer(s) have a higher nitrate concentration than the recharge <br /> water. And further degradation to waters of the State do not theoretically occur. <br /> To assess nitrate impact to the top aquifer(the water table) using the premise above,the nitrate <br /> concentration in the top aquifer under the Cole's residence must be lolown, which it is.not. <br /> Pinpoint sampling within the top mixing layer would be difficult to accomplish. The mixing layer <br /> is where the resultant recharge mixes with the groundwater. On a mass-to-mass ratio basis, the <br /> water table cannot exceed a nitrate concentration of: x+27.6 (Nr)-2 =45 ppm; x= 62 ppm NO3. <br /> Therefore,the top aquifer(water table) cannot exceed 62 ppm NO3 in order to stay below the <br /> drinking water MCL of 45 ppm NO3. <br /> Page -7- <br /> Na.Cfey Ag Research <br />
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