Mapping the Hudson Estuary's submerged lands, JW Ladd et al. PCBs in the Hudson River: Role of sediments, EA Garvey et al. Hudson River restoration: Role of natural resources trustees, TM Brosnan et al. Ecosystem indicators for Lake Ontario, F Luckey et al. Effect of lower chlorine dosage at Buffalo WWTP, KN Irvine et al. Livestock waste management and lake rehabilitation, CB Lind
Plant profiles
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by Kim N. Irvine, Gary W. Pettibone, Salmatou Bako, Jim Caruso, Roseanne Frandina, Gary Aures, Jane Ork, and Dan Bentivogli
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Web extra: Background on chlorination Web extra: Bird Island Treatment Plant Sampling and analysis Results Discussion Lesson for treatment plant operation
The Buffalo Sewer Authority (BSA) investigated the consequences of reduced chlorine dosage and chlorine residual on its final effluent without increasing the risk of potential pathogenic contamination in the receiving water body. The study was conducted at the Bird Island Wastewater Treatment Plant (WWTP).
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Background on chlorination
(opens new browser window). Chlorine dosage rates were sequentially reduced in one of four chlorine contact chambers to determine the minimum practicable chlorine residual that still provided adequate disinfection. Factors that influenced disinfection also were examined in making recommendations regarding optimum chlorine residual levels. At the time of study, the minimum permitted chlorine residual was 0.5 mg/L, although historical practice at the WWTP maintained a chlorine residual in the range of 1.0-1.5 mg/L. The Bird Island Treatment Plant is the second largest WWTP in New York State and one of the twelve largest in the nation. Between July 1991 and June 1996, the mean secondary sewage flow from the plant was 154 MGD. A catchment area with 675,000 people contributes sanitary and storm flows. During storm events, flows may exceed 500 MGD. Clarified wastewater has a residence time in the chlorine contact chamber of 15 min at design flow of 360 MGD.
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Bird Island Treatment Plant
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Sampling and analysis
Samples were collected in chlorine contact chamber
number 1. This chamber was chosen for study because it
had the easiest access for sample collection. Manual
grab samples for chlorine residual levels and fecal
coliform levels were collected at the upper and
downstream ends of the chamber, at a depth of 3 ft
(Figure 1). The sample locations and depths were
determined based on results of chlorine residual
profiling done on May 29, 1996, before the start of
the full sampling program.
Summer sampling began on June 3, 1996 and was completed on August 20 of that year. The sampling normally was done on Mondays and Tuesdays so that all bacterial analyses could be completed without requiring personnel to work weekends. Samples were collected four times each day: 8:45, 10:30, 12:30, and 14:30. Winter sampling began on February 10, 1997 and was completed on March 25 of that same yearagain, normally on Mondays and Tuesdaysbut samples were collected only twice each day, 9:00 and 12:30. Analysis for the chlorine residual was done in the field immediately upon sample collection using a Hach colorimeter and following Standard Methods. Fecal coliform analysis was done using a 5-tube MPN approach following Standard Methods.
Treatment plant operators routinely measure various
wastewater quality parameters and flow rates as part
of SPDES permit requirements. Analysis of these data
enabled us to place our sequential dosage reduction
tests in the context of general plant operation. Data
obtained from the BSA included monthly mean levels of
chlorine residual and fecal coliforms, as well as
secondary sewage flows for July 1991 through June
1996. Daily mean data from January 1, 1996 through
March 31, 1997 also were obtained for the following:
Results
Effects of chlorine reduction
BSA personnel noted, during the design of the chlorine
dosage reduction experiment, that some seasonality in
WWTP plant performance could be expected. Their
observation was confirmed by examining the geometric
monthly mean fecal coliform values for the final
effluent (1991-1996). Because the fecal coliform
levels tended to be lower in the winter, it was
decided to present the results of our summer (1996)
and winter (1997) sampling separately. Table 1
presents the results of our sampling.
Table 1b. Daily mean results, winter 1997
Notes to Tables 1a and 1b: -Mean value for fecal coliforms is geometric mean; all others are arithmetic mean. The high fecal coliform level observed on 7/15/96 was related to a temporary plant upset (a solids washout). Results of all samples can be obtained from the authors. For brevity, we show only the results for the downstream end of the chlorine contact chamber. A correlation analysis was done to investigate possible relationships between the sampled chlorine residual, the logarithm of fecal coliform levels, and secondary sewage flow (as a surrogate for flow rate through the individual contact chamber). We found a significant correlation (alpha=0.05) between fecal coliform levels in the summer and flow (0.26) and between fecal coliform levels and chlorine residual (-0.69). In the winter, we found a significant correlation (alpha=0.05) between fecal coliform levels and flow (0.54) and fecal coliforms and chlorine residual (-0.75).
Given the significant relationship between fecal
coliform levels and chlorine residual for both
seasons, a simple linear regression analysis was done.
Table 2 and Figures 2 and 3 summarize the results. The
Student's
t
values indicated that the slope of the regression line
(b1) was significant (alpha=0.05) for each equation in
Table 2.
Regression results between fecal coliforms and chlorine residual at the downstream sample site. See Table 2 for regression equation.
Regression results, although significant, exhibited considerable scatter or unexplained variation. It appears that while chlorine residual was an important determinant, other factors also affected the level of fecal coliforms. The only other data that were available for our sample times were plant flows; the plant operator recorded this value about hourly. Qualitative inspection of the data indicated that during storm events, when suspended solids levels and flow increased due to runoff, the fecal coliform levels also increased. It appears that storm water runoff in some way influences the effectiveness of chlorination. Plant flow, therefore, was used as a second predictor variable in a multiple regression analysis for the summer sampling. A multiple regression with flow was not done for the winter sampling because chlorine residual and flow were significantly correlated. The multiple regression equation for the summer data was calculated as: log F.C./100 ml = 2.64 + 0.00521(flow, MGD) - 1.87(chlorine residual, mg/L) Both of the predictor coefficients were significantly different from 0 (p <= 0.001) and the r² value increased from 48% to 55% (0.55). Data from plant and contact chamber number 1Samples for discussion purposes in this paper were collected at the downstream end of chlorine contact chamber number 1. However, samples routinely collected by WWTP operators for permit purposes represent the final effluent, and they comprise a mix of flow from all operating contact chambers. To investigate how representative data from contact chamber number 1 was of the general plant discharge, we examined mean chlorine residual and fecal coliform levels for common sample days:
The lower correlation between fecal coliform levels in the winter may be related to the general limited variability in the data and the higher fecal coliform values reported for our samples collected on 2/11/97 and 3/10/97. Discussion
Variability of fecal coliform levelsThe WWTP is a complex engineered system, and several factors appear to have a significant influence on fecal coliform levels. Our data for the downstream sample site indicated that there was a significant inverse relationship between chlorine residual and fecal coliform levels. It is not unexpected that as chlorine residual levels rise (to some limit), the levels of fecal coliforms will fall. A significant positive relationship also was observed between peak flow rate and fecal coliform levels. The higher peak flow rates generally were associated with storm-generated runoff discharging to the combined sewer system in Buffalo. Fecal coliform levels may be higher with the greater flow rates because of a shorter and less efficient contact time. The contact efficiency may itself be influenced by the levels and quality of total suspended solids as well as mixing efficiency in the contact chambers. A more detailed study of chlorine contact chamber hydraulics and the three-dimensional distribution of bacteria in the chamber would have to be done to determine whether the contact time or mixing efficiency were more important in optimal disinfection. Together, chlorine residual and peak flow rate accounted for over half of the variability observed in the summer fecal coliform levels. However, other factors clearly need to be considered in explaining some of the remaining variability. For example, total suspended solids concentration, size distribution, and organic carbon content influence bacteria dynamics in natural systems, and these relationships may extend to engineered systems. Certainly, the physical and chemical characteristics of the flocculated suspended sediment in the combined sewage varies both through and between storms and may vary seasonally. Suspended solids concentrations in combined sewage also typically are greater than in sanitary flow. Others have noted that variable influent conditions (including industrial spills) can be an important cause of plant upsets. The variable influent conditions of suspended sediment flocs and attached bacteria, therefore, may influence the relationships observed for plant effluent. It is generally acknowledged that there is a complex relationship between sludge floc characteristics (including the capacity to settle and the presence of filamentous organisms) and dissolved oxygen levels, nutrient levels, nature of organic substrate, sludge age, and reactor configuration. These complex and dynamic interactions may confound a fully satisfactory explanation of the variability in fecal coliform levels. Fecal coliform levels were less variable during the winter sample period than during the summer sample period, with the coefficient of variation in the winter being 0.204 compared to the summer value of 0.267. The higher variability in the summer may be related to a greater number of storm events, general plant upsets, and periodically incomplete nitrification (resulting in some chlorine reacting with the nitrites rather than being involved with disinfection). Furthermore, the greater solubility of chlorine in colder water and lower temperatures may produce a greater control on bacterial levels in the winter. Fecal coliform and chlorine residual levelsThe SPDES permit limit for fecal coliforms in the final effluent is a 30-day geometric mean of 200 MPN/100 ml or a 7-day geometric mean of 400 MPN/100 ml. These limits are based on a minimum of 1 sample/day (although the BSA routinely takes 3 samples/day). Because we sampled only on 2 consecutive days each 7-day period, direct comparisons of our results cannot be made with the permit levels. Still, we chose to use the 400 MPN/100 ml level as a guideline in the discussion of our results for the bacteria and chlorine residual levels. A qualitative inspection of our data for the summer (Table 1a) suggests that a chlorine residual level of at least 0.6-0.7 mg/L is required to maintain fecal coliform levels within the regulatory limit. See, in particular, sample dates 7/2, 7/8, 7/22, 8/19, 8/20. These five sample dates appear unaffected by storm events and exhibit fecal coliform levels < 400 MPN/100 ml. Chlorine residual values < 0.6 mg/L may be associated with acceptable fecal coliform levels. See, for example, sample dates 7/23 and 8/6 with residuals of 0.35 and 0.42 mg/L. Nevertheless, higher fecal coliform levels were observed with greater frequency at these lower chlorine residual values. For example, see data for 8/5, 8/12, 8/13.
The daily fecal coliform (geometric mean) and chlorine
residual (mean) values for the final effluent, as
reported by the BSA for 6/2/968/20/96, support the
results of our sampling.
The BSA sample results indicated that it may be possible to reduce the chlorine residual level to the 0.4-0.49 mg/L range, but to minimize the problems of non-compliance with fecal coliform levels, the chlorine residual should be maintained in the 0.5-0.7 mg/L range in the summer.
During the winter sampling, the lowest chlorine residual levels were in the 0.65-0.75 mg/L range. Table 1b indicates that there were no problems with high fecal coliform levels (>400 MPN/100 ml) at any time during the winter sampling period. Similarly, the BSA data for our sample period 2/10/973/25/97 (data available from authors, but not reproduced here) show that the lowest chlorine residual values were in the 0.6-0.65 mg/L range. Chlorine residual values in this range were observed on 21 days during the sample period, and no days exhibited fecal coliform levels greater than 400 MPN/100 ml. Our data and the data from the routine BSA sampling suggest that it may be possible to maintain a chlorine residual level even lower than 0.6 mg/L during the winter. Lesson for treatment plant operationOur study indicated that it was possible to operate at lower chlorine residuals without violating permit limits. As a result, the BSA target chlorine residual range was set at 0.5-0.7 mg/L during the summer and 0.3-0.5 mg/L during the winter. Our study has benefited both the BSA and the environment. The reduction in chlorine dosage reduces the potentially undesirable environmental effects of chlorine by-products while maintaining acceptable disinfection. The BSA was able to reduce the sodium hypochlorite dosage by over 180,000 gal/yr. This action also saved over $65,000/yr.
Acknowledgements
Funding for this study was provided by a grant from
the New York State Great Lakes Protection Fund
administered through the NYSDEC.
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