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The approximation of m??ate concentrations obtained Typical Sfttions \ <br /> from equation(1)also ignores dispersion,lateral flow,and <br /> Solution of the foregoing equations requires input d <br /> mixing with ground-water flow from upgradient areas. for several disposal system and site variables, all of wl; <br /> These processes would generally contribute to additional can have a significant effect on the predicted nits <br /> reduction of nitrate-nitrogen concentrations in ground nitrogen concentration. Graphical solutions are presen <br /> water to the extent that the nitrate-nitrogen concentration here for typical ranges of these variables,as an aid in self. <br /> of ground-water flow from upgradient areas is lower. ing appropriate values, and in identifying situations <br /> Equation (1) thus provides a conservative(worst case)first potential concern. <br /> approximation of ground-water nitrate-nitrogen concentra- The predicted resultant average ground-water nitre <br /> tion resulting from the combined effect of on-site sewage nitrogen concentration, nr, computed from equation (1 <br /> disposal systems and precipitation.This is for estimation of plotted for convenience in Figure 1 against the fraction <br /> long-term effects(i.e.,over years)on ground-water quality, waste-water recharge,I,relative to rainfall recharge,R,fc <br /> and is not intended for prediction of seasonal changes. selected range of values for soil denitrification,d,and wa-, <br /> A common land use planning dilemma is that of water nitrogen loading, n,r. Background nitrate-nitro] <br /> determining acceptable development densities, sometimes loading,n b,typically falls in the range of 0.5 to 1.0 mg/1,a <br /> referred to as the carrying capacity of the land. From the is assumed here to be 1.0 mg/I. Exceptions to this would <br /> standpoint of ground-water nitrate-nitrogen impacts, the if the area has large numbers of confined livestock or sign <br /> critical minimum gross acreage per developed lot,A,may be cant expanses of fertilized crops or turf areas (e.g., park <br /> defined as that which would result in a value of nr equal to 10 which would tend to increase background nitrate-nitrog <br /> mg/l,the commonly accepted drinking-water limit. By set- loadings above the typical values suggested here.The resu <br /> ting I=0.01344 W/A and nr= 10 mg/I,and then rearrang- plotted in Figure 1 show a wide range of potential effec <br /> ing equation (1), A is then given by highly sensitive to the initial selection of values for nw and <br /> Two curves are plotted for the average value of nw = <br /> A ( <br /> 0.01344W[nw — dnw— 10] 2) mg/1, with denitrification rates of 0 and 0.25, respective <br /> = <br /> R(10 — n b) The typical range is represented on the high and low sides <br /> the curves for(a)nw=50 mg/1,d=0 and(b)nw=30 mg <br /> in which A is expressed in terms of gross acres/dwelling unit d=0.25.The curve for nw=40 mg/1 and d=0.25 would . <br /> (DU); W is the average daily waste-water flow,per dwelling considered the most representative of typical on-site sewa <br /> unit, in gailons; and 0.01344 is a conversion factor having disposal situations (U.S. EPA, 1980; 1981). In addition <br /> units acre inch day DU yr I gal-I. proper selection of values of nw and d, the importance <br /> 40 <br /> a 36 <br /> E nb= 1.0 mg/L <br /> = 30 <br /> O <br /> it d y 0 <br /> w 25 OIL' ; <br /> v � 60m <br /> O <br /> O ow m0 <br /> 201L. d <br /> 40 ti a'Iff"G.2b <br /> ;hw__AO ntgf�. <br /> O <br /> Z Drinking v I <br /> Z 16 Water x nw= 30 mg/L. d= 0.26 <br /> y<t Standard i,�< v <br /> f- <br /> 7 <br /> uj <br /> TiY uj 5 <br /> 0L LL <br /> 0 0.20 0.40 0.60 0.80 1.00 1.20 1.40 1.60 1.60 2.0 <br /> .` WASTEWATER RECHARGE RELATIVE TO RAINFALL RECHARGE. I/R <br /> Predicted Zone for most Common Values <br /> Fig. 1. Resultant ground-water nitrate-nitrogen concentration as a function of effluent quality,denitrification,and 1/R. <br /> 492 <br />