,, j i. Redacted for privacy Donald C. Phillips. treatment processes employed in this study included coagulation, Treated Effluent Abstract approved:

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AN ABSTRACT OF THE THESIS OF Ching -lin Chang for the / M. S. (Name of student) (Degree) in Civil Engineering presented on (Major),, j i v i r 7 (Dáte) Title: Effect of Carbon Adsorption on Chlorine Requirement of Treated Effluent Abstract approved: Redacted for privacy Donald C. Phillips 1 The chlorination curves of treated domestic wastewater were investigated both before and after carbon adsorption. The tertiary treatment processes employed in this study included coagulation, sedimentation, sand filtration and carbon adsorption. Ammonia nitrogen and total organic carbon were determined for the samples studied to evaluate their effect on the breakpoint chlorination. Based on this study, the following conclusions were made: 1. The chlorination curve of the carbon column effluent which is the final effluent of the tertiary waste treatment is of similar shape to those reported for potable water supplies. The Cl:NH3 -N ratio for the carbon column effluent obtained in this study was about 5. 0-6..0:1 at the humps and 7.4-8.8:1' at breakpoint. These values are also close to the values reported for the chlorination of potable waters. 2. The carbon adsorption significantly reduces the chlorine

requirement of the treated wastewater. However, the reduction of chlorine requirement has little correlation with the reduction of total organic carbon content in the carbon adsorption process. 3. The chlorination curve of the treated domestic wastewater without carbon adsorption appears in somewhat irregular shapes. In some cases, two humps and two breakpoints were obtained. Possibly this phenomenon is due to the effect of organic chloramines. 4. When the ammonia content in the treated wastewater is low, it is economically feasible to chlorinate the effluent beyond the breakpoint to achieve the dual objects -- satisfactory disinfection and ammonia removal.

Effect of Carbon Adsorption on Chlorine Requirement of Treated Effluent by Ching -lin Chang A THESIS submitted to Oregon State University in partial fulfillment of the requirements for the degree of Master of Science June 1968

APPROVED: Redacted for privacy Professor of Civil Engineering in charge of major Redacted for privacy ead of Depart/1i/ Dean of Graduate School t of Civil Engineering Redacted for privacy Date thesis is presented Alc-J v IC; % Y 7 Typed by Opal Grossnicklaus for Ching -lin Chang

ACKNOWLEDGMENTS The author wishes to express his appreciation to Dr. Donald C. Phillips for his advice and direction in all phases of this work. The author is also indebted to the faculty and staff of the Department of Civil Engineering for the preparation and use of the experimental facilities.

TABLE OF CONTENTS INTRODUCTION 1 MECHANISM OF CHLORINE IN WATER 4 REACTION OF CHLORINE WITH AMMONIA 5 REACTION OF CHLORINE AND ORGANIC NITROGEN 6 BREAKPOINT CHLORINATION 8 GENERAL PROCEDURE OF THE EXPERIMENTS 11 RESULTS Experimental Apparatus Experimental Procedure Analytical Methods 11 11 12 14 The Shape of Chlorination Curve 14 The Cl:NH3 -N Ratio 26 The Change of Water Quality after Carbon Adsorption 26 The Effect of Total Organic Carbon Content on the Chlorine Requirement 27 Breakpoint Chlorination and Ammonia Removal 28 DISCUSSION 30 CONCLUSION 33 BIBLIOGRAPHY 34

LIST OF TABLE Table Page 1. Analytical data for samples 17 LIST OF FIGURES Figure Page 1. Chlorination curves of organic chloramines 10 2. Flow diagram of the pilot plant. 15 3. Chlorination curve for distilled water plus ammonia 15 4. Chlorination curves, Test 1 and 2. 19 5. Chlorination curves, Test 3 and 4. 20 6. Chlorination curves, Test 5 and 6. 21 7. Chlorination curves, Test 7 and 8. 22 8. Chlorination curves, Test 9 and 10. 23 9. Chlorination curves, Test 11. 24 10. Comparison of chlorination curves before humps 25 at various ammonia contents. 11. Schematic diagram showing oxidation of ammonia by 29 chlorine.

EFFECT OF CARBON ADSORPTION ON CHLORINE REQUIREMENT OF TREATED EFFLUENT INTRODUCTION It has been 60 years since the first plant scale application of sewage chlorination at Red Bank, N. J. Due to economical consid- erations, the general practice in sewage chlorination has been to maintain less than 2 ppm of residual chlorine after 15 or 30 minutes of contact time (8), in spite of the fact that there is no real assur- ance that the maintenance of this level of residual chlorine will cor- respond to the required colicidal effect (7). The high organic con- tent in the effluent of secondary waste treatment makes it prohibitive to chlorinate the effluent to reach the breakpoint. The conditions, however, may be different for the chlorination of the effluent of the tertiary treatment because the organic content will be greatly reduced. Activated carbon adsorption is one of the most effective processes in tertiary waste treatment as demonstrated at Lake Tahoe (2). Considerable research has been done on breakpoint chlorination of natural water and water supply but little has been reported on the breakpoint chlorination of treated sewage. The purpose of this study is to evaluate the effect of carbon adsorption on breakpoint chlorination.

2 MECHANISM OF CHLORINE IN WATER When chlorine gas is added to water, the following equilibrium is established: C12 + H20 HOC1 + Cl + H+ (1) [ HOCl] [ Cl ] [ H+] -h [ C12] (2) The hydrolysis of chlorine gas is almost instantaneous and the Kh value is reported as 4.5 X 10-4 at 25 C(3, p. 803). Based on this Kh value, ph from 5 to 9, and chlorine dosage of 100 mg /1, the [ HOC1] /[ C12] ratio will range from 1.6 X 10 4 to 1.6 X 108. Therefore, it can be said that, in the ordinary practice, the chlorine gas added to water is completely hydrolized. The hypochlorous acid, HOC1, ionized partially as follows: HOC1 = H+ + OC1 (3) K. i [ H +] [ 0C1 ]_ [ HOC1] 2. 7 X 10 8 at 25 C (4) The distribution of HOC1 and 0C1 depends on ph and temperature. The ratio of HOC1 to OC1 can be calculated from the relationship: [ HOC1] 1 1 [ HOC1] + [ OC1 ] 1 + [ OC1 ] /[ HOC1] 1 + Ki/[ H+] (5)

3 The reaction of sodium or calcium hypochlorite in water is similar to that of chlorine gas: NaOC1 -,- Na + + OC1 (6) Ca(OC1)2 > Ca++ + 2 0C1 (7) The hypochlorite ions combine with H+ to establish the equilibrium as shown in Equation (3).

4 REACTION OF CHLORINE WITH AMMONIA Ammonia is normally present in sewage in a significant amount. Ammonia hydrolyzes in water as follows: NH3 + H2O.--- NH4+ + OH (8) [ NH4+ ] [ 011-] -5-1. 8 X 1 0 at 25 C (9) [ NH3] The ratio of NH4+ to NH3 also depends on ph and may be calculated by the following equation: [NH4 +] [ NH4+] + [ NH3 ] 1 + [ NH3 ] /[ NH4+] l+[ OH ] /1.8 X 10 5 At ph 6. 0, 99. 95% of ammonia is in the form of NH4 +, 99.45% at ph 7. 0 and 94. 77% at ph 8.0. process: Hypochlorous acid reacts with ammonium ion in a stepwise (10) NH4+ + HO C1 - H20 + H+ + NH2C1 (11) NH2C1 + HOC1 H20 + NHC1 ---> (12) 2 NHC12 + HOC1 - H2O + NC13 (13)

The ratio of monachloramine to dichloramine is dependent on dosage, and the resulting ph of the solution. The equilibrium of the ammonium ion with mono- and dichloramine is shown as: 5 2 NH2C1 + H+ NH4+ + NHC12 (14) [ NH4+] 4 [ NHC1 2] 5 =K=6.7x10 at25 C [ H+] [ NH2C1] 2 (15) Nitrogen trichloride does not exist in a significant amount above ph 4 unless an excess HOC1 is present. Its mechanism and rate of formation are still not clear (10).

6 REACTION OF CHLORINE AND ORGANIC NITROGEN According to Morris (10), the reaction of unipositive chlorine with organic nitrogen may be generalized as: X-Cl + R2NH --. C1NR2 + H+ + X- (16) In which X may represent either HO, NH2 or NHC1 and defines the reaction when either hypochlorous acid, monochloramine or dichloramine are involved. The reaction rates of several simple nitrogenous compounds have been determined by Morris. However, at present, there is no way to predict the mechanism of organic chloramines in sewage. Hypochlorous acid and monochloramine react with organic nitrogenous compounds to form various forms of chloramines. Nusbaum (11) stated that when ammonia nitrogen is low compared with albuminoid nitrogen, protein chloramine formation is accelerated. The organic chloramines have a much lower bactericidal effect than monochloramine. Rhines' experiment (12)showed a marked reduction in colicidal effect upon the addition of L- serine. According to Feng (4), many organic chloramines are titrated as available residual chlorine by the starch - iodide method but show little lethal activity, and many organic chloramines which do not react with orthotolidine have some lethal activities at certain ph levels.

7 This may be the reason of Heukelekian and Faust's finding that little correlation is found between the reduction of coliform bac- teria and residual chlorine (7).

8 BREAKPOINT CHLORINATION Nitrogen that exists in the form of NH3 or NH4+ is considered as ammonia nitrogen (NH3 -N). As shown in Equation (1 1) and (12), hypochlorous acid reacts with the ammonium ion to form mono- and dichloramine at neutral ph levels. When the molar ratio of Cl:NH3 -N is less than 1:1, or the weight ratio of 5.07 :1 (ammonia is expressed as nitrogen), the monochloramine predominates and there is no sig- nificant change in ammonia concentration if dechlorinated before ammonia determination. When the molar ratio of Cl:NH3 3-N exceeds 1:1, oxidation of ammonia and reduction of chlorine is noted and both the concentration of available chlorine and ammonia begin to decrease until the breakpoint, or zero point, is reached. At this point, neither residual chlorine nor ammonia is present. After the breakpoint, addition of chlorine produces hypochlorous acid. The mechanism and endproduct of the breakpoint reaction are not fully understood. Formerly it was considered that dichloramine was oxidized to form nitrogen gas (6), (9): NH2C1 + NHC12 -> N2 + 3H+ + 3 Cl (16) or 2 NH2C1 + HOC1 > N2 + H2O + 3 H+ + 3 Cl (1 7)

9 Morris et al (9) suggested that the breakpoint reaction starts with the decomposition of dichloramine as: NHC12 + H2O NOH + 2 H + + 2 Cl (18) 2 NOH + HOC1-2 NO + H20 + H+ + Cl (19) And the NO formed would combine with dissolved oxygen to give NO2 and finally be oxidized to nitrate. Sawyer (13, p. 252) stated that nitrous oxide, nitrogen, and nitrogen trichloride had been identified among the gaseous products of the breakpoint reaction. Sawyer also suggested that the formation of nitrous oxide could be represented by: NH2C1 + NHC12 + HOC1 -> N2O + 4 HC1 (20) Equation (16 and 17) indicate that the weight ratio of Cl:NH3 -N at the breakpoint is about 7. 6:1. Equation (18-19) show a ratio of 12. 7:1, and Equation (20) shows a ratio of about 10:1. A survey of the literature shows that the ratio ranges mostly from 7. 6-10:1, although some reported the ratio as high as 15-20:1 for natural waters. It seems that there might be two or more endproducts, or the endproduct depends on the concentrations of reactants involved in the breakpoint reaction, thus making the Cl:NH3-N ratio quite variable with the experimental conditions.

lo The shapes of chlorination curve of organic chloramines depend on the nature of the organic substances (1 ), (5 ). They are shown schematically in Figure 1. 1, egg albumen / 2, tryptose Residual chlorine /A 3, high albumoid -N 4, amino acetic acid Chlorine dosage Figure 1. Chlorination curves of organic chloramines.(curves 1, 2, and 4 after Calvert; curve 3, after Griffin and Chamberlin.)

11 GENERAL PROCEDURE OF THE EXPERIMENTS Experimental Apparatus The experiments were conducted at the Water Research Demonstration Laboratory at the Corvallis Sewage Treatment Plant. The plant treats about 5 MGD of domestic sewage utilizing the processes of primary sedimentation, high -rate trickling filtration, final sedimentation and chlorination. The effluent of the high -rate trickling filter was pumped to the pilot plant in the laboratory. The processes in the pilot plant consisted of alum coagulation and sedimentation, followed by sand fil- tration and carbon adsorption. The sand filter was 51 inches in diameter and 36 inches deep. The effective size of the sand was 0. 50 mm with a uniform coefficient of 1.55. The carbon column was 5 i inches in diameter and 48 inches deep. The activated car- bon used was Calgon Filtrasorb Type 300, 8 X 30 mesh. The flow diagram of the pilot plant is shown in Figure 2. Experimental Procedure The effluents of the sand filter and the carbon column were collected after more than one hour of continuous flow for each test series. The filtration rate was kept at 2. 5 gpm per square foot.

12 After the samples were collected, the filters were shut down and backwashed with tap water. The coagulation and sedimentation units were in continuous operation most of the time. A sodium hypochlorite solution with a concentration of about 3.0 to 3.5 mg /ml was used for the chlorination. The exact concentration of the hypochlorite solution was determined before the chlorination. The volume of each batch of samples was 900 ml. Increasing dosages of the hypochlorite solution were added to two series of samples. The dosage increments were varied from 0. 5 to 2 ml so as to adequately define the chlorination curves. After 60 minutes of contact time, the residual chlorine was titrated using 250 ml to 400 ml of samples. Since the turbidity of the samples was low, the direct starch -iodide method as described in the Standard Methods (Water) was used for the determination of residual chlorine. During the titration, the ph of samples was buffered to ph 4. 0 to minimize the interference by nitrite. Analytical Methods The following analyses were made for each test series: ph, alkalinity, turbidity, temperature, ammonia nitrogen, and total carbon. The alkalinity was titrated potentiometrically with 0.02 N sulfuric acid solution to ph 4. 5 or 4. 0.

13 The turbidity was determined with Hach turbidimeter model 1860. The direct nesslerization method was used for the determina- tion of ammonia nitrogen with a Spectronic 20 at the wavelength 460 mµ and light path 10 mm. The total carbon was determined by a Beckman infrared carbon analyzer. First the samples were injected to determine both inorganic and organic carbon. Then the samples were acidified with HC1 to ph of about 2 and aerated with CO2 -free air for about five minutes. This process removed the inorganic carbon. The acidified and aerated samples were injected to the carbon analyzer again to determine the organic carbon.

14 RESULTS The Shape of Chlorination Curve When chlorine is applied to water containing ammonia, the ammonia will react with chlorine to form monochloramine. The concentration of monochloramine increases as the dosage of chlorine increases up to the point where all the ammonia is converted to monochloramine. This point is referred to as the "hump ". After the hump, the oxidation of ammonia begins and the residual chlorine decreases. Theoretically, the breakpoint should be at the point where all the ammonia is oxidized and no residual chlorine exists. However, this exact point is difficult to attain. Furthermore, if nitrogen trichloride and organic chloramines are formed, they are titrated as residual chlorine by the starch -iodide method. The humps and breakpoints in the following discussion are determined from the intersections of two slopes on the chlorination curves. This method is subject to some error, but it is not the purpose of this study to determine the exact locations of the humps and breakpoints. As discussed previously, the C1:NH3 -N ratio at the breakpoint varies with the nature of the water. The approximate location of the breakpoint is sufficient for the determination of the range of Cl:NH 3-N ratio.

15 Figure 3 shows the chlorination curve of distilled water containing 3.47 mg /1 of ammonia nitrogen. The water was not buffered. The hypochlorite ions combine with hydrogen ions to form hypochlorous acid and cause the ph of water to rise according to Equations (6) and (3). Oxidation of ammonia releases hydrogen ions and lowers the ph value. After the breakpoint, the residual chlorine exists as HOC1 thus the ph value rises again. The variation in ph values can be used as a check for the location of the hump at the breakpoint (Figure 3). In natural waters or sewage, the variation of ph value is slight due to the buffering action of bicarbonates. The chlorination curve near the breakpoint, or usually called the "valley ", in Figure 3 is flatter than for those reported in the literature in which the ammoniated distilled water is buffered. Organic substances, especially nitrogenous compounds, complicated the shape of chlorination curves. Figures 4, 5, 6, 7, 8 and 9 show the chlorination curves of sand and carbon filter effluents at various ammonia nitrogen levels. The letters C and S of the samples refer to the effluent of carbon column and sand filter respectively. The numbers following the letters C and S identify the number of the test. No coagulant was added before filtration for samples C -1 to C -3 and S -1 to S -3. Other samples were coagulated before filtration. The analytical data of the samples are shown in Table 1.

Trickling Filter Effluent Flash Mixing -0 Alum Solution Coagulation Tank Settling Tank > Q Feed pump Tank Sand Carbon Filter Column /1 mg chlorine, Residual K 20 10 /. i / x XI /,,, 1 Figure 2. / X, `x % % % \ Flow diagram of the pilot plant. \.x 7--- \ / \ \ / / `x \ \\x / / \ x-//...-- ph residual chlorine NH3-N 3. 47 mg/1 9 8 7 6 5 i. 0 0 10 1 I 1 I I 20 30 40 50 Figure 3. NaOC1 Dosage mg /1 as Cl Chlorination curve for distilled water plus ammonia. os

Table 1. Analytical data for samples Sample C-1 S-i C-2 S-2 C-3 S-3 C-4 S-4 C-5 S-S C-6 S-6 Water temperature C 22-22- 22.5-22- 22-22- 22-22- 21-21- 22-22- Turbidity, units 23 23 24 23, 23.5 23.5 23. 23. 22 22 23.5 23. 3.9 4.5 3.7 4.4 3.8 4.6 5.2 6.2 7.5 8.8 1.4 3.3 Alkalinity, mg /1 83. 7a 74. 7a 72. Oa 64. Oa 63.5 58.0 63.3 45.0 54.7 51.3 40.6 21.6 ph 7.68 7.28 Total Carbon, mg /1 7.50 7.23 7.28 7.20 7.31 6.70 7.16 6.90 7.10 6.31 inorganic + organic 23 28. 5 22 26 19. 0 24. 5 17. 5 22. 5 organic 4 11 3.0 7.0 5.0 19.5 2.5 9.5 NH3 -N, mg /L 5. 70 5. 70 3. SO 4.04 4. 50 4.70 4. 50 5.00 Cl:NH3 -N ratio 5.00 5. 30 1. 93 2. 50 hump 5. 9 6.11 6. 8 7.7 5. 8 6.6 5. 1 6. 2 5.0 5. 9 5. 6 8. 3 breakpoint 8.7 9.5 11.7 11.7 8.8 9.9 8.2 8.9 8.2 9.4 7.4 10.4 Sample C-7 S-7 C-8 S-8 C-9 S-9 C-10 S-10 C-11 S-11 Water temperature C 22-22- 21-21- 21-21 - 21.5-21.5-21- 21-23 23 22.5 22.5 22 22 23 23 22.5 22.5 Turbidity, units 3.1 4.3 12 13 4.6 6.4 6.2 8.5 9.8 13 Alkalinity, mg /1 98.2 36.4 52.7 48.3 69.2 49.1 53.6 53.3 57.0 56.0 ph Total Carbon 7.10 6.70 6.80 6.68 7.18 6.60 7.10 6.90 7.01 6.81 inorganic + organic 27 17 17. 5 21. 5 organic 1 6 2 6.5 NH3 -N, mg /1 4.10 4.80 6.24 6.60 6.42 6.58 5.40 6.00 6.00 6.30 Cl:NH3 -N ratio hump 5. 5 6. 8 5. 9 5. 9 5. 1 * 5. 5 5. 9 6. 0 * breakpoint 7.6 9.4 7.9 8.8 7.6 7.8 7.7 8.5 8.3 9.2 a Endpoint at ph 4. 0. All other samples are at ph 4. 5. * Two humps, ratio not calculated. v

The chlorination curves for the effluent of the carbon column are all of similar shape. This indicates that the chlorination curve of the carbon column effluent is controlled predominantly by the concentration of ammonia nitrogen in water. The humps and valleys are steeper in the carbon column effluent than in the sand filter effluent. Before the humps, the chlorination curves are relatively close regardless of the ammonia concentration (Figure 10). The chlorination curves of the sand filter effluent are consistently lower than those of carbon column. This is conceivable because the organic content of the sand filter effluent is higher than that of the carbon column effluent. The shapes of the curves for the sand filter effluent are somewhat irregular. In some cases two humps and two valleys are observed as shown in Figures 7, 8 and 9. Originally, it was suspected that there might be some experimental errors involved. After repeated experiments, however, it was found that the cause of irregular shapes might be due to some unknown organic substances or some reducing substances in water, which would be oxidized at the chlorine dosage of about 40 mg /l. The cas- es of double humps were observed in the sand filter effluent only, and were not experiencedin the carbon column effluent. In those samples which showed two humps, a faint septic odor (but not of H2S) was noticed. The sand filter effluent was slightly yellowish, and color decreased with the increasing chlorine dosage. The 18

/1 mg chlorine, Residual 20 C-2 Z NH3 3. 50 mg/1, '\ / \ " \ \\ /\ \ \ \ i x\r2---- S-2 q \. NH3 4.04 mg/1 10 0 0 L 1 10 20 30 40 Chlorine dosage, mg /1 I `x \ \ \ \ \\ 1\ / \i 1 50 60 Figure 4. Chlorination curves, Test 1 and 2..p

20 \+-2- S-3, NH 4. 70 mg/1 \x 10 mg chlorine, /1 Residual 0 20 C-4 NH3 4. 50 mg/1 \r S-4, NH3 5.00 mg/1 10 0 0 i I I I 1 10 20 30 Chlorine dosage, mg /1 40 50 60 Figure 5. Chlorination Curves, Test 3 and 4. N O

20 x...x 10 NI-I3 5.00 mg/1 C-5-----e_t N S-5, NH3 vc 5, 30 mg/1 /1 mg chlorine, Residual 0 20 NH3 C-6 Z i 1(/ i 1.93 mg/1 "4-2-- 5-6, NH3 2. 50 mg/1 10 0 I I I 0 10 20 30 40 50 60 Chlorine dosage, mg /1 Figure 6. Chlorination curves, Test 5 and 6. N

20 10 S_7, NH3 4, 70 mg/1 /1 mg chlorine, Residual 0 20 10 I NH3 6. 24 mg/1 C-8Z} \ x '42.- S_8 x l \ o NH3 6. 60 mg/1 I 0 l 0 10 20 30 40 ii X / // i 50 60 l Chlorine dosage, mg /1 Figure 7. Chlorination curves, Test 7 and 8.

\ \ 20 C- NH3 6. 42 mg/1 /'N x S-9, NH3 6. 58 mg/1 10 g/1 m chlorine, Residual ri 20 C-1 NH3 5. 40 mg/1 S-10, NH3 6. 00 mg/1 10.x x-""-- 0 0 I I I 10 20 30 Chlorine dosage, mg /1 40 \ ' x 50 60 Figure 8. Chlorination curves, Test 9 and 10.

\ `x `x \ C-11 NH3 6.00 ----2._ mg/1 \`-P S 11, NH3 6.30 mg/1 0 10 20 30 40 50 60 Chlorine dosage, mg /1 Figure 9. Chlorination curves, test 11.

20 NH3 Conc. Ammoniated Dist. Water 3. 47 mg /1 C-1 5.70 C-5 -- _ C-1 C-2 3.50 C-3 C-3 4.50 C-2 C-4 4. 50 C-5 5.00 C-4 C-11 6. 00 chlorine Residual 10 C 11 -Ammoniated Distilled Water 00 0 I t 10 20 Chlorine dosage, mg /1 I I 30 Figure 10. Comparison of chlorination curves before humps at various ammonia contents.

locations of breakpoints in these cases were judged from the chlorina- tion curves and the complete decoloration of the samples. 26 The Cl:NH3 -N Ratio The Cl:NH3 -N ratio for carbon column effluent ranges from 5. 0-6. 0 :1 at the humps and 7.4-8.8:1 at the breakpoint (C-2 has higher values) as listed in Table 1. For the sand filter effluent, most of the ratios fall in the range from 5.9-6. 8:1 at humps and 8-10:1 at breakpoints. From the results of the experiments, it appears that, at the same NH3 -N concentration, the chlorine dosage required to reach the hump for the carbon column effluent is about 15-20% less than for the sand filter effluent. To reach the breakpoint, the chlorine dosage required is about 10-15% less for the carbon column effluent than for the sand filter effluent. All the Cl:NH3 -N ratios fall in the range of 7. 6-10:1 as reported in the literature for the natural waters. This indicates that other forms of nitrogenous compounds play only a minor role in the chlorination. The Change of Water Quality After Carbon Adsorption The effluent of the sand filter was slightly yellowish in color and, occasionally, had a faint septic sewage odor. The color and

27 odor were completely removed after carbon adsorption. No ph adjustment was made in the coagulation process. Accordingly, the turbidity removal in the process was not very efficient. Addition of alum in the coagulation process depressed the ph of the influent from about 7. 5 to less than 7. 0. The ph and alkalinity increased after carbon adsorption. Probably, this was due to adsorption of organic acids by the activated carbon. The amount of total organic carbon in the sand filter effluent was 6-11 mg /1, and 1-5 mg /1 in the carbon column. It is difficult to evaluate the efficiency in terms of percent removal since the precision of the total carbon determination at 1 to 2 mg /1 level was estimated to be approximately ± 0. 5 mg /1. The Effect of Total Organic Carbon Content on the Chlorine Requirement Since the organic chloramines affect the chlorination curve to a greater extent than the carbonaceous compounds, it would be more logical to use the organic nitrogen as a parameter for chlorine consumption instead of total organic carbon. Unfortunately, the kjeldahl method is very time consuming and requires a large amount of samples. The carbon analyzer takes only about two minutes to obtain a result with a fairly good precision. Since the chlorine requirement increases with the increase of COD and BOD, an attempt was made

28 to find what correlation could be obtained from the total organic carbon in the sample. The results are shown in Table 1. Various approaches were used in attempting to correlate the amount of total organic carbon to the differences in the chlorine requirements, locations of humps and breakpoints, and the shape of the chlorination curves. No correlation was established. This is possibly due to: (a) The carbon content of organic nitrogeneous compounds is quite varied. (b) Some organic carbonaceous compounds do not consume chlorine. Breakpoint Chlorination and Ammonia Removal When the chlorine dosage is less than the amount required to reach the hump, there is little change in ammonia nitrogen. After the hump, the ammonia nitrogen is oxidized to some unknown end - product. After the breakpoint, there is definitely no ammonia nitrogen remaining. The amount of ammonia nitrogen remaining after chlorination varies with the contact time. Due to the technical difficulties and time involved, the data obtained were only semiquantitative. The relation of ammonia nitrogen and chlorine dosage is shown schematically in Figure 11.

29 Residual chlorine -3- _ 1 \ NH -N \ z \ Chlorination curve \ \ \ t um m z Chlorine dosage Figure 11. Schematic diagram showing oxidation of ammonia by chlorine.

30 DISCUSSION It is generally recognized that the free residual chlorine has a much greater bactericidal activity than chloramines. The present practices of sewage chlorination are not sufficient to eliminate the water -borne pathogenes (8),(7) Since the primary objective of the tertiary treatment of sewage is the reuse of wastewater, it seems that chlorination beyond breakpoint is a proper solution for the safeguard to public health. In addition, if there is a trace amount of phenol remaining in the effluent, the odor resulting from chlorophenol is unacceptable for the use of water supply. Again, breakpoint chlor- ination will solve this problem. Ammonia nitrogen cannot be removed by the coagulation and filtration processes. Breakpoint chlorination not only eliminates ammonia but also reduces total nitrogen in the treated effluent. Based on the data obtained from this study, the following calculations show the amount and cost of chlorine required to obtain breakpoint chlorination: When there is 7 mg /1 of NH3 -N in the carbon column effluent, and Cl:NH3 -N ratio taken at 8. 5, the chlorine dosage of (7X8.5) + 2= 61.5 mg/1 of chlorine is required to remove all the ammonia nitrogen

31 and to maintain 2 mg /1 of free residual chlorine. At $125 /ton of liquid chlorine, or 6.25ç/lb, the cost of chlorine will be 6. 25 X 61.5 X 10-6 X 1000 X 8.34 = 3. 2M000 gal. This cost is reasonable considering satisfactory disinfection and ammonia removal are obtained. The cost of chlorine will be reduced to about 1. 9W000 1000 gal when NH3 -N is at 4 mg /1. The prerequisite for using breakpoint chlorination for ammonia removal is that the ammonia content in the treated wastewater must be low, or less than 10 mg /1, otherwise the cost will be prohibitively high. From the data obtained, it shows that, at low organic content (less than 10 mg /1 as carbon), the total organic carbon is not suit- able as a parameter for the chlorine requirement. Two humps and two valleys in the chlorination curves of sand filter effluent indicate that some organic chloramines can be oxidized by the chlorine. These organic chloramines may affect the oxidation of the mono - chloramine. Unfortunately, the methods available at the present time cannot differentiate the mono- and dichloramine from the vari- ous forms of organic chloramines. If the chlorine requirement is defined as that amount of chlor- ine which must be added to produce a specified amount of free resi- dual chlorine beyond the breakpoint, the effect of carbon adsorption is obvious. To what extent the chlorine requirement will be reduced

is not predictable from the amount of total organic carbon present. It seems that ammonia and total organic nitrogen are better parameters for the determination of the chlorine requirement. Until the mechanism of organic chioramines is understood, the chlorine requirement of the treated wastewater still must be determined for each individual wastewater. 32

33 CONCLUSION 1. The chlorination curve of the carbon column effluent,which is the final effluent of the tertiary waste treatment, is of similar shape to those reported for potable water supplies. The C1:NH3 -N ratio for the carbon column effluent obtained in this study was about 5. O-6. 0:1 at the humps and 7.4-8.8:1 at breakpoint. These values are also close to the values reported for the chlorination of potable waters. 2. The carbon adsorption significantly reduces the chlorine requirement of the treated wastewater. However, the reduction of chlorine requirement has little correlation with the reduction of total organic carbon content in the carbon adsorption process. 3. The chlorination curve of the treated domestic wastewater without carbon adsorption appears in somewhat irregular shapes. In some cases, two humps and two breakpoints were obtained. Possibly this phenomenon is due to the effect of organic chloramines. 4. When the ammonia content in the treated wastewater is low, it is economically feasible to chlorinate the effluent beyond the breakpoint to achieve the dual objects -- satisfactory disinfection and ammonia removal.

34 BIBLIOGRAPHY 1. Calvert, C. K. Treatment with copper sulfate, chlorine, and ammonia. Journal of the American Water Works Association 32:1155-1164, 1940. 2. Culp, G. and R. Culp. Reclamation of waste water at Lake Tahoe. Public Works 97(2):86-90. 1966. 3. Fair, G. M. and J. C. Geyer. Water supply and waste -water disposal. New York, Wiley, 1954. 973 p. 4. Feng, T. H. Behavior of organic chloramines in disinfection. Journal of the Water Pollution Control Federation 38:613-628. 1966. 5. Griffin, A. E. and N. S. Chamberlin. Some chemical aspects of breakpoint chlorination. Journal of the New England Water Works Association 55:371-383. 1941. 6. Harvill, C. R. et al. Practical application of ammonia -induced break -point chlorination. Journal of the American Water Works Association 34 :275-287. 1942. 7. Heukelekian, H. and S. D. Faust. Compatibility of wastewater disinfection by chlorination. Journal of the Water Pollution Control Federation 33:932-942. 1961. 8. Laubusch, E. J. State practices in sewage disinfection. Journal of the Water Pollution Control Federation 30:1233-1240. 1958. 9. McKee, J. E. et al. Chemical and colicidal effects of halogens in sewage. Journal of the Water Pollution Control Federation 32:795-819. 1960. 10. Morris, J. C. Kinetics of reactions between aqueous chlorine and nitrogen compounds. In: Principles and applications of water chemistry, ed. by S. D. Faust and J. V. Hunter. New York, Wiley, 1967. p. 23-53. 11. Nusbaum, I. Sewage chlorination mechanism. Water and Sewage Works 99:295-297. 1952.

35 12. Rhines, C. E. The fundamental principles of sewage chlorination. Water and Sewage Works 113:97-101. 1966. 13. Sawyer, C. N. Chemistry for sanitary engineers. New York, McGraw-Hill. 1960. 367 p.