2. Mechanisms and Kinetics
The mechanism of the formation of bromate under chlorination is well understood, with the first step being the formation of hypochlorite.
At the temperatures of interest in the storage and transmission of product water in the Kingdom of Saudi Arabia (15–45 °C), reaction (2) is dominant, and most of the dissolved oxidant is hypochlorite, rather than hypochlorous acid [
18,
19].
The second step is the oxidation of bromide to hypobromite under basic (reaction (3)) or acidic (reaction (4)) conditions.
Both reactions are thermodynamically favourable over the temperature range of interest. However, the reaction rate for the reaction under acidic conditions is about 10
6 times higher, and the reaction is acid-catalyzed [
20]. It is intuitive that this should be the more favourable reaction because it does not involve bringing two anions together. Thus, the reaction will be dominated by reaction (4) even at relatively high pH and the reaction under basic conditions can be ignored over the pH range of interest.
The third step is the oxidation of hypobromite to bromate. There is a significant body of literature on mechanisms for this reaction under ozonation conditions, but relatively little work has been conducted on the mechanism in the presence of an oxidant. Stoichiometrically, this is reported to occur by the disproportionation of hypobromous acid to give bromate and bromide [
21,
22]:
Trimolecular reactions are statistically implausible, so this process is likely to proceed in two steps, for example, as proposed by Margerum and Huff Hartz [
23]:
A similar second step for the formation of bromate from hypobromite has been previously reported with ozone as an oxidant [
24]. Margerum and Huff Hartz found that reaction (5) was second order in HOBr in the presence of HOCl, and thus proposed [
23]:
with the first step clearly being rate limiting. The apparent rate coefficient
k increased with total chlorine, but this only became evident above 5 mM (>175 ppm) Cl; Margerum and Huff Hartz reported that the rate constant for the second-order decomposition of HOBr has a maximum at pH ~7.2 and fit this with a complex mechanistic model, but this maximum is dependent on only one data point at pH 7.6 [
23]. In contrast to this, we have consistently observed more bromate formation at higher pH over the range of pH values seen in product water (7.5–9.0) in routine assessments of water quality in the SWCC production and transmission systems. Therefore, we postulate a significant contribution of the cross-reaction between hypobromite and hypobromous acid:
This reaction should be favourable since it requires less charge separation overall, and if it goes at a slower rate than the 2HOBr reaction, it could contribute negligibly at pH ~7 but give elevated rates any higher pHs, as observed in the SWCC transmission system, for example, if the HOBr + BrO
− reaction proceeds at one-third the rate of the 2HOBr reaction (
Figure 1).
The overall scheme of bromate formation with estimated kinetic and thermodynamic parameters of importance is summarized below (
Scheme 1).
Ammonia can initially impact the system as outlined above (
Scheme 1) in two primary ways [
24]:
- (i)
Reducing the amount of HOCl available for the oxidation of bromide [
26]:
- (ii)
Reacting with HOBr so it is unavailable for oxidation to bromate [
27]:
Given the relative concentrations expected of HOCl and HOBr, reaction (11) is likely to be more important than reaction (12) despite the order of magnitude difference in rates. Because of the impact of ammonia on reducing the amount of HOCl (while not losing disinfectant capacity, as monochloroamine is also a disinfectant), Ling et al. recommended the addition of ammonia before chlorination in ozonation reactions [
24].
These main reactions removing HOBr and hence reducing bromate formation are shown below (
Scheme 2).
The monochloramine and monobromamine can react further [
30]:
Meanwhile, NH
2Br may disproportionate reversibly in a base-catalyzed reaction [
31]:
Following that, it will then react with NH
2Cl [
32]:
These haloamines may also react with any remaining bromide present in the system, giving bromamine [
33],
bromochloramine [
33,
34],
or dibromamine [
24,
35]:
The net result of these reactions should be the sequestration of the initially present bromide as haloamines, predominantly as NHBrCl [
33,
36]. The net of reactions of the haloamines is summarized below (
Scheme 3).
NHBrCl has been reported to be less reactive than the mono- and dibromamines [
37], giving an expected impact on the yield of halogenated organic contaminants, as well as bromate (pace Valentine [
38]). It is not wise to trust an experimental result until it has been validated by theory [
39], and the experimental observation is supported by the free energies calculated for bromamines and chloramines in aqueous solution by Trogolo and Aret [
40]. These free energy values suggest that for a generic bromination reaction,
the free energy of the reaction will be higher for NHBrCl than for NH
2Br (2.5 kJ/mol less) and NHBr
2 (5.5 kJ/mol less). Thus, the ammoniation before chlorination process can be expected to strongly reduce the incidence of other brominated disinfection products. The addition of ammonia before chlorination will cause the formation of increased levels of chloramine. Ammoniation after chlorination is more problematic, because if the rate coefficients quoted above are correct, this will lead to a significant population of NH
2Br and NHBr
2, which are good brominating agents [
41,
42]. However, minimizing the time between chlorination and ammoniation to approximately 30 s has also been shown to give primarily NHBrCl [
43]. Sun et al. reported in a similar system to desalination (secondary effluent chlorination) that trihalomethane (THM) production was reduced but haloacetic acid concentrations were increased at a bromide concentration of 140 ppb and not reduced at 50 ppb; it is unclear from the description of this study whether ammonia was added before or after chlorination [
44]. This is consistent with other reports of reduced THM yields under conditions where bromamines replace hypobromous acid [
29] and that bromamines are more reactive in forming haloacetic acids [
41].
As long as there is residual chlorine in the system, it is expected that this chlorine will continue to generate dibromochloramine. Only when there is no remaining oxidant is NBr
2Cl expected to decompose in aqueous solution to H
+, N
2, Cl
−, Br
−, and BrO
− [
35]. Luh and Mariñas (2014) studied the decomposition of NH
2Cl with a large excess (by 5 to 50 times) of Br
− over NH
2Cl and clearly observed the replacement of NH
2Cl by NHBrCl, which decomposed at a slower rate [
35]. At the lower relative concentrations of bromide in desalination product water (~100 ppb), this suggests that the bromide-consuming reactions discussed here will not deplete the NH
2Cl available. Hu et al. calculated for a system also containing relatively high concentrations of bromide, but with an excess of chloramine over bromide (0.05 mM NH2Cl, 1.6–3.2 ppm 0.02/0.04 mM Br
−), that almost all bromine would be present as NHBrCl, and found it to be rapidly degraded by CuO [
45].
The body of data obtained up until now and outlined here on the mechanism and kinetics of the interactions between ammonia, chlorine, and bromide therefore suggests that chlorination followed by ammoniation of the water produced by seawater desalination is a potential strategy for controlling the formation of bromate and other disinfection by-products of concern.
3. Materials and Methods
Water samples were collected from the Shoaibah Phase 2 desalination plant of the SWCC and from a number of storage tanks adjacent to the plant, pumping stations on transmission lines originating at the Shoaibah desalination complex, and storage tanks in communities near the termini of these transmission lines (Arafa and Taif), in 2022 and 2023. The production and transmission system is complex, and a simplified diagram showing the relationship between the different sampling points is given below (
Figure 2).
Analysis of the parameters of interest was carried out within three weeks of collection in the laboratories of the Desalination Technologies Research Institute of the SWCC in Al Jubail, Kingdom of Saudi Arabia, using standard methods as follows:
pH: Potentiometry using a standard hydrogen electrode [
46];
Ammonium, bromide, bromate, chloride, and nitrate: Ion chromatography with chemical suppression of eluent conductivity [
47].
Trihalomethanes and other organic contaminants: EPA 524 (Gas chromatography-Mass spectrometry, GC-MS). One sample (5 May 2022) was analyzed in the WTIIRA laboratories; one sample (25 May 2023) by ALS Arabia, Dammam, Saudi Arabia; and one sample (6 June 2023) by SGS Inspection Services, Jubail, Saudi Arabia.
Ammonia was added to an existing post-treatment system utilising chlorination via sodium hypochlorite. The ammonia addition point was located about 50 m downstream of the chlorination point.
Two rounds of trials were made, in 2022 and 2023.
The 2022 trials were carried out in several stages:
- (0)
Addition of sufficient seawater to bring the TDS up to 82–94 ppm, which should have given bromide concentrations in the range 49–72 ppb if there was no selective rejection or permeation of bromide (14–16 April 2022);
- (1)
Addition of 120 ppb NH3 along with sufficient seawater to bring the TDS up to 81–89 ppm, which should have given bromide concentrations in the range 47–64 ppb (17–19 April 2022);
- (2)
Addition of 120 ppb NH3 along with sufficient seawater to bring the TDS up to 106–115 ppm, (96–113 ppb Br−) (20–25 April 2022);
- (3)
Addition of 200 ppb NH3, along with sufficient seawater to bring the TDS up to 110–132 ppm (104–132 ppb Br−) (26 April–3 May 2022);
- (4)
Addition of 200 ppb NH3 and sufficient sodium hydroxide to adjust the pH to 8.7, along with sufficient seawater to give a TDS of 114 ppm (112 ppb bromide) (4–5 May 2022).
For a number of locations, control data were also collected on 12–13 April 2022.
A second series of tests was carried out in 2023, with the application of chlorination/ammoniation in both Phase 1 and Phase 2 of the Shoaibah Desalination plant:
- (1)
Addition of 100 ppb NH3 only (23 April–5 May 2023);
- (2)
Addition of 100 ppb NH3 along with sufficient seawater to bring the TDS up to 119–242 ppm, which should have given bromide concentrations in the range 116–325 ppb. (4–14 May 2023);
- (3)
Addition of 100 ppb NH3, along with sufficient seawater to bring the TDS up to 130–230 ppm, (134–305 ppb Br−) (15 May–17 June 2023);
- (4)
Addition of 100 ppb NH3 along with sufficient seawater to bring the TDS up to 82–125 ppm (52–126 ppb Br−) (19 June–12 July 2023);
- (5)
Addition of 90 ppb NH3 along with sufficient seawater to bring the TDS up to 82–129 ppm (52–133 ppb Br−) (13 July–7 Aug 2023).
As each phase in the 2022 and 2023 test series corresponds to multiple measurements of a number of days, the average value and an error value calculated from the standard deviation in the measured values are reported for each measured parameter for each phase.
4. Results and Discussion
The key parameters of interest in both the 2022 and 2023 trials were the concentrations of bromide, bromate, ammonium, and nitrate in the product waters. Bromide and bromate were taken as the critical input and output of the complex system outlined in the introduction, and ammonium and nitrate were taken as potentially problematic by-products of the ammonia added to the system.
4.1. 2022 Trials
The measured bromide concentrations before chlorination and ammoniation were significantly below the predicted values, with 87 ± 4 ppb measured during stages 3 and 4. These were also below the value that could be predicted from measurements of the chloride concentration in the water (99 ± 3 ppb) using the expected ratio of Cl:Br in seawater. As the absolute number of bromine-containing species is less important than their relative proportions, the correlation between chloride and bromide concentration was used to estimate the total bromine concentration in product water samples after chlorination and compared to the amount of bromide.
After chlorination and ammoniation, the treated water was passed on to tanks within the Shoaibah desalination plant complex, which also receive water from other sources, some of which produce low-TDS water with no significant bromate problems, while others are more problematic; these in turn proceed to pumping stations which draw upon multiple tanks.
While the net of reactions described in
Scheme 3 suggests that very little free bromide will be observed, being sequestered as bromamines if it is not present as hypobromite ion/hypobromous acid, ion chromatography found significant amounts of bromide ions in all waters investigated. In waters treated with ammonia, concentrations of bromide were consistently higher. Unless there are serious issues with the mechanisms postulated in the literature, this suggests that the bromamines are not stable under the conditions of ion chromatography. High levels of bromide in IC have also been observed by Pearce et al. in studies where high concentrations of chloramine were added to product water [
48].
From
Table 1, it can be seen that the apparent ratio of non-bromide bromine-containing species (presumably primarily BrO
−) as a fraction of the total bromine in the stream decreases on addition of 120 ppm ammonia (cf. the values obtained in Tank 5 with Tanks 4, 13, and 14), decreasing further as ammonia concentrations are increased to 200 ppm, and decreasing further again when pH is increased.
From other indicators (F, SO
4, Ca) the water sampled in PS-1A was not derived from the water treated by chlorination–ammoniation during this time, but from the Phase 1 MSF plant (
Figure 2). No residual NH
4 was measured in this water at any time during the study.
Note the clear fall in non-bromide bromine in Tanks 4, 13, and 14 and pumping station 1B over the time of the test: a small reduction at 100 ppb NH3 treatment, followed by a larger fall at 200 ppb NH3 and a larger fall again when pH was adjusted upwards.
Bromate reduction is not clearly significant with 120 ppb NH
3 addition (stages 1 and 2) but is marked at 200 ppb bromate addition (stages 3 and 4) (
Table 2).
The day-by-day bromate data for the tanks containing untreated water (Tank 5) and primarily treated water (Tanks 4, 13, and 14) are displayed in
Figure 3.
Ammonium concentration should be a good indicator for the presence of treated water. It can be seen that there is essentially no ammonium at any of the pumping stations and disproportionately greater quantities of residual ammonium with 200 ppb treatment (
Table 3). See, for example, Tank 4 at stage 2, where the effect of the treatment appears to be significant in terms of the bromide/hypobromite ratio and the amount of bromate observed. It is also clear that the analysis is not quantitative, as concentrations of ammonium up to twice the predicted concentration of the ammonia added are observed in some instances. There are also occasional outliers with no clear explanation at locations where ammonium should not be present, and an absence of ammonium under conditions (Tank 4, stages 1–2) where it would be expected; there are thus concerns about the methodology of ammonium determination.
One concern about addition of ammonia is its potential oxidation to nitrate, with implications for the quality of water delivered to the consumer. The ppb of nitrate present in the system was also assessed (
Table 4). There is no clear relationship between the amount of nitrate observed and the amount of ammonia added to the system. Although nitrate levels in Tank 5, not receiving the treated water, were assessed as lower than Tanks 4, 13, and 14 in phases 2 and 3, comparable values were obtained for all four tanks in phase 4.
The data on sites taking water not treated by this protocol illustrate the range in values found within the systems due to variations in the quality of the water produced, the mixing of these waters in different proportions, and the different environmental factors affecting these waters as they move through the transmission system.
Under the phase 4 trial conditions, samples of water from different parts of the Shoiabah plant were analyzed for trihalomethanes (
Table 5). Trihalomethanes were only detected in the waters that were chlorinated and not ammoniated. Note that these species were most likely generated during the time when the samples were transported to the laboratory for analysis.
4.2. 2023 Trials
As in 2022, a significant reduction in non-bromide bromine was seen in 2023 in the tanks being fed by the Phase 2 Shoiabah desalination plant where the combined chlorination/ammoniation post-treatment was employed, as well as at in pumping station 1 (
Table 6) Reductions in bromate at these tanks were also observed (
Table 7). Data are given to compare water further down the transmission line not deriving from the treated water (at the PS Jeddah, Quiza, Mina A and Mina B) and also for water deriving from the treated water. The impact of the treatment on the proportion of non-bromide bromine appears to be clear at tanks (Arafa and Taif) located hundreds of kilometres from the water production site. While there is also a dramatic reduction in non-bromide bromine at Mina B pumping station between the control period, which did not receive the ammoniated water, taking the values in aggregate it is clear that this arises from an outlier in the upwards direction during the control period.
Note that in stages 4 and 5 of the trial, a different set of parameters was measured, and this fact was not realized until the data sets were analyzed later.
The bromate results clearly show minimization of bromate in Tanks 3, 13, and 14, Pumping Station 1, and the Arafa and Taif tanks under all treatment conditions (
Figure 4. The bromate values seen under condition 1 at the Arafa and Taif tanks reflect the time delay in transmitting water through the network; if one additional day is included in the control period, the Taif Tank values become 8 ± 2 for the control period and 0 for condition 1. This is the most significant result of this study: the demonstration that the procedure of sequential chlorination and ammoniation can effectively control bromate formation in transmitted water containing up to 300 ppb bromide which has been transported hundreds of kilometres at significant temperatures (average daytime maxima in Jeddah 34/37 °C April/May, in Taif 29/33 °C April/May). A bromate concentration below the target of 10 ppb was observed at Taif under the conditions prevailing in June/July (average daytime maxima Jeddah 38/39 °C, Taif 35/35 °C).
The ammonium results obtained imply that significant amounts of ammonia are present in parts of the system that should not be affected by the trial, while at the same time low values are obtained at the Arafa and Taif tanks where excellent control of bromate was demonstrated (
Table 8). Unfortunately, these results thus convey primarily concern about the methodology used to analyze for ammonium.
Increases in nitrate are seen across the system in the trial period compared to the control period, whether or not waters were subjected to chlorination/ammoniation treatment (
Table 9). There is no consistent trend of a higher nitrate concentration with the addition of ammonia, but there is some evidence that ammonia addition may be leading to an increase in nitrate in that all tanks have a higher concentration of nitrate on first addition of ammonia in both studies—moving from the control case to condition 1 in this study, just as they did on moving from condition 0 to condition 1 in the 2022 study.
It should also be noted that as part of the 2023 study, the waters at the Arafa and Taif tank outlets were tested for the presence of organic disinfection products on two dates: on May 25th, when ammoniation was carried out together with the addition of seawater to increase the bromide concentration to approximately 130 ppb, and on June 6th, when enough seawater to increase the bromide concentration to approximately 115 ppb was added. For the ammoniated sample, analysis was conducted for bromodichloromethane, bromoform, and dibromochloromethane, and in all cases concentrations were found to be below the detection threshold of 2 ppb. For the control sample, bromodichloromethane and dibromoacetonitrile were found to be below the detection threshold of 0.10 ppb, while bromoform was identified in the Arafa tank at a concentration of 1.92 ppb and the Taif tank at a concentration of 3.77 ppb, and dibromochloromethane was detected at a concentration of 0.27 ppb in the Arafa tank and 0.33 ppb in the Taif tank. While not as definitive as would be ideal, this indicates that disinfection of water containing 130 ppb bromide did not lead to detectable brominated organic by-product when combined with ammoniation. On June 6th, analysis was also done for monochloracetic acid (detection limit 1.0 ppb), dichloroacetic acid (detection limit 0.5 ppb) and trichloroacetic acid (detection limit 0.5 ppb), with none of these substances detected at either Arafa or Taif tanks, suggesting the treatment did not lead to an increase in haloacetic acids. Comprehensive tests were carried out by a third party for samples collected in August, when temperatures in Makkah province are at a maximum so the rate of generation of bromate and other disinfection by-products should be highest, and water at the Arafa and Taif tanks was found to meet regulatory limits for all disinfection by-products controlled by the Saudi Arabian authorities.