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IC Additives <br /> During the use of the water for waste disposal, nutrients are dissolved and <br /> rmicroorganisms are introduced on the way to the treatment system. Once the liquid <br /> reaches the recirculating filter, over 99% of the BOD & SS are removed. The soil will <br /> remove the microorganisms and most of the nutrients. All the nutrients are removed or <br /> utilized by plants with the exception of nitrates. During the summer, they will be used <br /> by the trees and shrubs. However, during the winter months, they will travel vertically <br /> in the soil, r <br /> The recirculating filter will remove half of the nitrates leaving a concentration of 30 1 <br /> mg/I in the effluent. As the liquid travels downward, three reactions can occur - 1) <br /> Plants and microorganisms can consume it; 2) Denitrification can occur turning it into <br /> nitrogen gas; and/or 3) Leaching can carry it to the water table. Recent studies on <br /> nitrate movement show that denitrification occurs in the portion of the soil that is dry in <br /> the summer, but is saturated in the winter. N0 <br /> The exact amount of nitrate getting to the water table is impossible to predict. We know Dey��ss <br /> that no more than 30 mgll of nitrogen (N-NO3) will enter the soil. (see Table 1) AGGa&JS <br /> When this 30mg/I of N-NO3 enters the soil it can be lost through denitrification. As the <br /> NO3 enters zones where there is little or no oxygen, the oxygen attached to the N is used !. <br /> by organisms. The N is released as a gas. The amount of denitrification is site specific. <br /> The well log for B-6 shows there is a grey clayey silt at 21 to 27 feet. (see attached ' <br /> log) The groundwater probably fluctuates in this layer. If this is true, a great deal of <br /> the nitrate could be lost due to denitrification. A conservative estimate of NO3 reaching <br /> the groundwater would be 20 mg/I. (This could be 0 if the correct soil conditions are 4 <br /> encountered.) <br /> 9 <br /> F <br /> r <br />