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3 3 Auparl 1979 I Table 2. Parameters measured and <br /> Application Rate•0.55 m3/hr frequency of analysis. <br /> I <br /> I <br /> e I Vorameter Analyses/wk' <br /> I BOD 3 <br /> E z I TSS 5 <br /> -- I TKN 1 <br /> E I <br /> NH,-N 5 <br /> I <br /> NO,-N 5 <br /> Ranoti Rale•0.45-3/hr TotalP 1 <br /> _ PO„ 1 <br /> E I I Turbidity 5 <br /> u 4 pH 5 <br /> Specific conductivity 1 <br /> 1 I Chloride 1 <br /> I— —Steady Stole Period—� Fecal coliforms 1 <br /> I I Fecal streptococci 1 <br /> 1 I <br /> I <br /> *Based on five application periods <br /> 0 2 4 6 B per week. <br /> ON Time(Ilya) OFF <br /> Figure 3. Typlcolrunoffhydrograph. m' hr t. Altogether,50 detention times were <br /> measured at the CRREL site during this study (see <br /> 160 APP•A)• <br /> Flow-proportioned composite samples were taken <br /> Section B 3 of the applied primary effluent and runoff during <br /> Application Rote=0.6 m/hr. <br /> each application period. Primary effluent samples <br /> were taken at fixed time intervals with an automatic <br /> 120 composite sampler. Runoff samples were taken by <br /> small peristaltic pumps which were activated by relay <br /> switches during each operating cycle of the catch <br /> Ei basin's sump pump. The water quality parameters <br /> measured and the frequency of analysis are shown <br /> 80 i in Table 2. Analtyical techniques are discussed in <br /> a ' <br /> Appendix B. <br /> I <br /> I <br /> o I <br /> U <br /> I <br /> V 1 <br /> ao , <br /> HYDRAULIC DETENTION TIME <br /> The hydraulic detention time on an overland flow <br /> terrace is dependent on many factors including appli- <br /> cation rate,slope, length of terrace, surface micro- <br /> 01 1 topography,soil infiltration rate,evapotranspiration <br /> 0 loo zoo 300 <br /> Time (min.) and vegetation density. Of all these factors, only <br /> application rate is controllable by the operator. <br /> Figure 4. Typical chloride response curve for meas- Slope and length of terrace are largely dependent on <br /> uring detention time. site characteristics. Surface microtopography is con- <br /> trollable to some extent by careful site preparation, <br /> but each terrace will develop different hydraulic path- <br /> in the constant head weirbox. Composite samples ways. Infiltration rate and evapotranspiration will <br /> were taken of the runoff at various intervals and vary from site to site depending on soil characteristics <br /> analyzed for chloride. Chloride concentrations were and climate conditions. Vegetation density, or surface <br /> then plotted vs time, and the peak of the response roughness,varies with the type of vegetation and the <br /> curve was chosen to represent detention time. The maturity of the terrace. A mature terrace usually has <br /> center of mass was not chosen to represent detention a higher vegetation density and will normally have an <br /> time because 36%of the tracer was lost in the perco- organic mat near the soil surface caused by a buildup <br /> late and plants. An example of a typical chloride re- of grass clippings from previous harvests. This <br /> sponse curve is shown in Figure 4. The detention time organic mat increases the resistance to flow which, <br /> in this case was 40 min for an application rate of 0.6 in turn, increases detention time. <br /> 4 <br />