Accepted Manuscript Advanced oxidation of iodinated X-ray contrast media in reverse osmosis brines: The influence of quenching Sara P. Azerrad , Shirra Gur-Reznik , Lilly Heller-Grossman , Carlos G. Dosoretz PII:

S0043-1354(14)00413-8

DOI:

10.1016/j.watres.2014.05.041

Reference:

WR 10695

To appear in:

Water Research

Received Date: 24 March 2014 Revised Date:

22 May 2014

Accepted Date: 25 May 2014

Please cite this article as: Azerrad, S.P., Gur-Reznik, S., Heller-Grossman, L., Dosoretz, C.G., Advanced oxidation of iodinated X-ray contrast media in reverse osmosis brines: The influence of quenching, Water Research (2014), doi: 10.1016/j.watres.2014.05.041. This is a PDF file of an unedited manuscript that has been accepted for publication. As a service to our customers we are providing this early version of the manuscript. The manuscript will undergo copyediting, typesetting, and review of the resulting proof before it is published in its final form. Please note that during the production process errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain.

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Advanced oxidation of iodinated X-ray contrast media in reverse osmosis brines: The ACCEPTED MANUSCRIPT influence of quenching

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Sara P. Azerrad, Shirra Gur-Reznik, Lilly Heller-Grossman and Carlos G. Dosoretz*

Faculty of Civil & Environmental Engineering and Grand Water Research Institute, Technion-

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Israel Institute of Technology, Haifa, Israel.

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*Corresponding author: Faculty of Civil and Environmental Engineering, Technion-Israel Institute of Technology, Haifa 32000, Israel. Tel.: +972 4 8294962; fax: +972 4 8228898.

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E-mail address: [email protected] (C.G. Dosoretz).

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Abstract

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Among the main restrictions for the implementation of advanced oxidation processes (AOPs) for

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removal of micropollutants present in reverse osmosis (RO) brines of secondary effluents account

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the quenching performed by background organic and inorganic constituents. Natural organic matter

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(NOM) and soluble microbial products (SMP) are the main effluent organic matter constituents.

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The inorganic fraction is largely constituted by chlorides and bicarbonate alkalinity with sodium

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and calcium as main counterions. The quenching influence of these components, separately and

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their mixture, in the transformation of model compounds by UVA/ TiO2 was studied applying

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synthetic brines solutions mimicking 2-fold concentrated RO secondary effluents brines. The

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results were validated using fresh RO brines. Diatrizoate (DTZ) and iopromide (IOPr) were used as

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model compound. They have been found to exhibit relative high resistance to oxidation process and

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therefore represent good markers for AOPs techniques.

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Under the conditions applied, oxidization of DTZ in the background of RO brines was strongly

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affected by quenching effects. The major contribution to quenching resulted from organic matter (≈

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70%) followed by bicarbonate alkalinity (≈30%). NOM displayed higher quenching than SMP in

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spite of its relative lower concentration. Multivalent cations, i.e., Ca+2, were found to decrease

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effectiveness of the technique due to agglomeration of the catalyst. However this influence was

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lowered in presence of NOM.

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Different patterns of transformation were found for each model compound in which a delayed

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deiodination was observed for iopromide whereas diatrizoate oxidation paralleled deiodination.

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Keywords: Advanced oxidation processes, radicals quenching, brines desalination, synthetic brines,

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secondary effluents, titanium dioxide oxidation, iodinated X-ray contrast media.

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1. Introduction

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Safe reuse of treated wastewater in agriculture is of vital importance especially in countries with

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scarcity of natural water resources. Reuse and discharge of conventionally treated wastewater

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results in release of micropollutants into the environment that can contaminate ground/surface

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water, accumulate in soils and perhaps adsorb into crops (Ternes and Hirsch, 2000; Kormos et al.,

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2011; Shenker et al., 2011). High pressure-driven membranes such reverse osmosis (RO) applied to

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treat wastewater effluents represent an useful technology that confines micropollutants into brines

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(Kimura et al., 2004; Košutić et al., 2007; Oulton et al., 2010; Gur-Reznik et al., 2011a) while

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releasing high quality water for unrestricted irrigation. However, a proper treatment of brines is

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necessary before releasing them into de environment (Westerhoff et al., 2009; Gur-Reznik et al.,

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2011b; Zhou et al., 2011).

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Iodinated X-ray contrast media (ICM) used in medicine for imaging of organs or blood vessels are

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metabolically stable in the body and are eliminated via urine or feces (Pérez and Barceló, 2007).

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Conventional wastewater treatment plants (WWTPs) are not able to remove them effectively from

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wastewater, and therefore they are expected contaminants in treated effluents (Ternes and Hirsch.,

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2000; Carballa et al., 2004; Oulton et al., 2010; Kormos et al., 2011). Because of their chemical

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stability and high solubility, ICM have been found at µg/L level in municipal effluents and at ng/L

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level in surface water (Pérez and Barceló, 2007). ICM were found at almost undetectable levels in

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groundwater. Reported concentrations of diatrizoate and iopromide (in µg/L) in surface water

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ranged between 0.05 to 0.23, in municipal effluents from 0.25 to 9, and in groundwater from

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undetectable levels to 0.05 (Putschew et al., 2000; Ternes and Hirsch, 2000; Ternes and Joss, 2006;

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Pérez and Barceló, 2007). In RO brines results are expected to increase according to the recovery

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ratio, up to 10-fold for the case of 90% recovery higher than those obtained in effluents. ICM were

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chosen as model compounds in this work due to their multiple halogenation and aromatic structure,

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which confers them relatively high resistance to oxidation, with the additional advantage of iodine

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as an intrinsic labeling for tracking purposes (Gur Reznik et al., 2011b; Sugihara et al., 2013).

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Several oxidation techniques have been studied in order to remove ICM from water and wastewater

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effluents such as non-thermal plasma (NTP) (Gur-Reznik et al., 2011b), ozonation (Ternes et al.,

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2003; Seitz et al., 2008), electrochemical oxidation (Zwiener et al., 2009; Lütke el al., 2014) as well

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as advanced oxidation processes (AOPs) (Doll and Frimmel, 2004; Pereira et al., 2007a; Pérez et

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al., 2009; Malato et al., 2009; Sugihara et al., 2013). These techniques exhibited only partial

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transformation. Although removal efficiency is strongly dependent on the conditions applied,

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reported transformations applying UV-TiO2 oxidation in UPW were ~65% for diatrizote after 1

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hour (k1st≈0.02 min-1) and ~70% for iopromide after 5 minutes (k1st≈0.18-0.22 min-1) (Doll and

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Frimmel, 2004; Sugihara et al., 2013). Scavenging capacity of the water matrix is a constraint for

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significant removal of ICM by AOPs.

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Secondary effluent is a complex water matrix composed by a variety of organic and inorganic

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components. The effluent organic matter (EfOM) is constituted mainly by humic-like compounds

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originated from natural water, better known as natural organic matter (NOM) and soluble microbial

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products (SMP) resulting from biomass activity and decay during biological treatment and to a

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minor extent by micropollutants (Shon et al., 2006; Jarusutthirak and Amy, 2007). It has been

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reported that SMP represent most of the chemical oxygen demand in effluents (Aquino et al., 2003)

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and contain polysaccharides, proteins, and organic colloids as the main chemical constituents

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(Rosenberger et al., 2006). There were a few attempts to characterize influence of EfOM as OH·

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radical scavenger. Dong et al. (2010) reported an inverse relationship between molecular weight

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and OH· radical scavenging, i.e., the lower the molecular weight the higher is the reactivity with

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hydroxyl radicals. Reactivity toward OH· radicals was measured in different water sources based on

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different water matrix characteristics such as molecular weight, polarity, SUVA, hydrophobicity

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and fluorescence (Rosario-Ortiz et al., 2010). Lin and Lin (2007) reported a decrease in

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photodecomposition of model compounds due to presence of humic acids in TiO2/UV system. Gur-

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Reznik et al. (2011b) using NTP system showed decrease in first order reaction rates of two ICM,

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iopromide (IOPr) and diatrizoate (DTZ), as the organic matter and electrical conductivity in the

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water matrix increased. The inorganic fraction of wastewater effluent is largely formed by

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chlorides, alkalinity (constituted mainly by bicarbonate) and sulphate with sodium and calcium as

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main counterions, whereas phosphate, nitrate, magnesium and potassium are to a lesser extent.

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Influence of individual inorganic ions in water matrix, especially bicarbonate, was reported to

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decrease the oxidation of target compounds by hydroxyl radicals. Degradation and reaction rate

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constants for chloride, carbonate, bicarbonate and phosphate with hydroxyl radicals have been

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studied (Jayson et al., 1973; Buxton and Elliott, 1986; Abdullah et al., 1990; Liao et al., 2001;

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Piscopo et al., 2001; Neppolian et al., 2002; Wu and Linden, 2010).

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However, the radical scavenging capacity of individual or combined main constituents of RO

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brines is still not well defined. The aim of the present research was to evaluate the patterns and

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factors governing the oxidation of micropollutants present in reverse osmosis brines by UVA/ TiO2.

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Synthetic brines comprising the main RO brines components were designed and applied to

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understand the quenching contribution of individual and groups of constituents on the extent and

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kinetics of oxidation of the ionic ICM diatrizoate, used as model compound. In experiments aimed

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to determine oxidation patterns, the non-ionic ICM iopromide was also used. Results were

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validated using fresh RO brines (2-fold concentrated secondary effluents) and ultrapure water

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(UPW) as reference.

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2. Material and methods

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2.1 Materials

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TiO2 used in the experiments was Degussa P-25. Sodium diatrizoate dihydrate and iopromide were

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purchase from Sigma-Aldrich and U.S. Pharmacopeia, respectively with purity ≥ 99%. Fulvic acid

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sodium salts (technical grade) and soluble potato starch (reagent grade) were purchased from

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Sigma-Aldrich. Yeast extract was of microbiological quality (Bacto BD). Other chemicals used for

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the experiments (buffer, eluents, standards) were at least of analytical grade.

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2.2 Water matrixes

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Experiments were performed in ultrapure water, fresh RO brines and synthetic brines. Water

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matrixes were spiked with DTZ (~700±70 µg/L) as model compound. In experiments addressed to

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determine patterns of oxidation also IOPr (~700±70 µg/L) was spiked. The chemical structure of

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model compounds is presented in Fig. 1.

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Reverse osmosis brines: Brines were obtained from the Technion secondary effluent desalination-

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pilot plant with a nominal capacity of 10 m3/h, located at a commercial activated sludge-WWTP

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(Nir Etzyon, Israel). The pilot comprises an ultrafiltration stage (~40 nm molecular weight cut off –

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MWCO, Dow) followed by a two stages-reverse osmosis system (8” and 4” BW Toray membranes,

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respectively) as detailed elsewhere (Gur-Reznik et al., 2011b). A schematic diagram of the

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desalination process is presented in Fig. 2. Fresh RO brines (2-fold concentrated with respect to the

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feed) for this study were obtained from the first stage.

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Synthetic brines: Synthetic brines were prepared mimicking composition of stage one-RO brines.

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Dissolved organic matter (DOM) was set to ~20±1 mg/L of which approximately 80% was

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attributed to SMP and 20% to NOM. SMP was reconstituted adding 10.4±0.5 mg/L (as C) soluble

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potato starch (polysaccharide) plus 5.6±0.3 mg/L (as C) yeast extract (protein) whereas NOM were

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reconstituted as 4±0.2 mg/L (as C) humic acid-sodium salts (HA). Inorganic components were

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added as follows: 25±3 mg/L phosphate (as KH2PO4), 31±1 mg/L nitrate (as NaNO3), 373±31

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mg/L carbonate alkalinity (as NaHCO3) and 240±7 mg/L sulfate (as Na2SO4). To reach the desired

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concentration of chloride as well as calcium and potassium NaCl, CaCl2 and KCl were added to

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obtain a final solution containing 613±25 mg/L chloride, 112±15 mg/L calcium, 63±0.14 mg/L

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potassium. In experiments focused on study the influence of anions, either combined or

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individually, UPW was supplemented with sodium as the main counterion.

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Ultrapure water (0.055 µS/cm electrical conductivity) was generated from double distilled water

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through purification in a Purelab system (Elga).

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2.3 Photocatalysis experiments

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Experiments were carried out at room temperature in 500 ml glass reactors containing 180 ml of

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either water matrix spiked with the model compounds, as indicated. TiO2 at 1 g/L was added and

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stirred prior to irradiation to achieve thermodynamic adsorption equilibrium. The reactors were

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placed in a dark chamber on a magnetic stirrer to facilitate mixing and illuminated from the top

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with a UVA lamp (Eversun, 40W) emitting radiation between 300 and 420 nm with a maximum at

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350 nm. UVA lamps were preheated for 20 min prior to runs. At different times, aliquots of the

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solution were collected for analysis and immediately supplemented with excess NaHCO3 to

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facilitate TiO2 removal, and kept in ice in the dark. Then samples were centrifuged during 20 min at

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4000 rpm (Heraeus, Megafuge 1.0R centrifuge) and filtered with 0.45 µm syringe filter units

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(Millipore) prior to analysis. Light intensity was measured by ferrioxalate actinometry (Hatchard

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and Parker, 1956) and was found to be 990 µW/cm2. The UV fluence was calculated multiplying

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the light intensity by the exposure time and it was found to be 3564 mJ/cm2 per hour of experiment.

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2.4 Analytic techniques

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Determination of diatrizoate, iopromide, p-chlorobenzoic acid (pCBA) and organic bound iodine

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were performed using liquid chromatography with electrospray tandem mass spectrometry LC-MS3

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in an Agilent 1200 HPLC system (Hewellet Packard) coupled through a ion spray interface to an

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API 3200 triple quadrupole mass spectrometer (Applied Biosystems). Chromatography was

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performed on a reverse-phase column LiChroCART® Purospher STAR RP-18 (Merck) endcapped

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column (4.6 mm×15 cm) with 5 µm pore size. The compounds were detected in multiple-reaction

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monitoring (MRM) mode. Methods for determination of diatrizoate and iopromide were similar to

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those described by Gur-Reznik et al. (2011a). pCBA determination was performed according to

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Vanderford et al. (2007) with some modifications, using 0.1% formic acid (v/v) in water (A) and

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100% methanol (B) as eluents. The gradient was as follows: 5% B was held for 2 min, than

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increased linearly to 100% during another 8 min and held for 4 min, afterwards the gradient

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decreased linearly again to 5% and finally held for 3 min. The total run time was 19 min, the flow

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rate was 350 µL/min with injection volume of 15 µL and the column temperature was set at 30°C.

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The quantification limit under these conditions was 5 µg/L.

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Organic bound iodine was determined using ion negative electrospray ionization according to

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Putschew and Jekel (2003) with some modifications. The first quadrupole was used in single ion

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monitoring mode and was set to m/z 126.8. The source parameters were set as follow: curtain gas

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25 psi, temperature 600°C, spray gas (GS1) 35 psi, dry gas (GS2) 40 psi, ion spray voltage -4500,

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declustering potential -120 V, entrance potential -10 V. The same eluents as detailed before were

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applied in a linear gradient as follows: from 5% B to 100 % B in 7 min, held for 3 min, then back to

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5% B in 3 min and held for 3 min. The column temperature was set at 30°C.

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Total adsorbable iodine was measured following the procedure described by Oleksy-Frenzel et al.

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(2000) modified as reported by Gur-Reznik et al. (2011b). Dissolved organic carbon (DOC) was

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analyzed on a total organic carbon (TOC) analyzer (multi N/C 2000, Analytic Jena) and ultraviolet

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absorbance (UV) at a wavelength of 254 nm (A254) was measured in a UV-visible

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spectrophotometer (Agilent 8453 series) with a 1 cm quartz cell. Fourier transform infrared (FTIR)

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spectra of freeze-dried samples were recorded on an FTIR (iS10 Nicolet) using Smart iTR single

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bounce attenuated total reflectance (ATR) Diamond/ZnSe crystal.

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Total concentration of elements (Na, Ca, P, S, K) was measured by ICP-AES (iCAP-6300, Thermo

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Sci). Anions concentration (nitrate, sulphate, phosphate, chloride, iodide) were measured in a 881

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compact IC Pro ion chromatograph (Metrohm), equipped with Metrohm A supp 5-150 (with 4 µm

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pore size) column. A solution of 3.2 mM sodium carbonate and 1.0 mM sodium bicarbonate in 5%

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acetonitrile was used as eluent. Alkalinity was measured according to standard methods 2320

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(APHA 2005).

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3. Results and discussion

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3.1 Effect of operating conditions on UVA/TiO2 oxidation in UPW

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The effect of the operating conditions on the performance UVA/TiO2 on diatrizoate transformation

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at trace concentrations was first characterized in UPW as water matrix. The results are presented in

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Table 1. The effect of pH and TiO2 concentration were first studied. The highest pseudo-first order

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rate constant for diatrizoate was detected at pH 3.5 (2-folds higher than at pH 7 and 3-folds higher

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than at pH 10). These results denote that TiO2 is more effective under acidic conditions in line with

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previous reports (Westerhoff et al., 2009). Furthermore, under acidic conditions (pH 3.5) approx.

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50% DTZ is present in the anion form (pKa=3.4) and TiO2, which is positively charged under

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isoelectric point (pH 6.3), may adsorb it promoting its direct oxidation. pH values in RO brines are in

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the range of 7.5±0.5 and for this reason the experiments were performed at pH 7. The effect of TiO2

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concentration on the rate of DTZ oxidation was carried out in the concentration range of 0.25-2 g/L

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(see Table 1). Increasing TiO2 concentration over 1 g/L did not show significant improvement of

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the pseudo-first order rate constant. Therefore 1 g/L TiO2 concentration was chosen as optimal dose

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for this work.

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In order to evaluate the extent of quenching due to alkalinity, transformation of DTZ in UPW

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supplied with bicarbonate alkalinity was further studied. Total alkalinity in brines can be expressed

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as in equation (1):

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Alktotal = [HCO3− ] + 2[CO3−2 ] + [NH3 ] +[H2 PO4− ] + 2[HPO4−2 ] + 3[PO4−3 ] + [OH − ] −[H + ]

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Since ammonia concentration was very low in the brines used in this study whereas phosphate was

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negligible in comparison to the carbonate system and pH of brines was 7.4 ±0.5, bicarbonate

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alkalinity was considered the dominant specie. Bicarbonate alkalinity at four different

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concentrations 18, 54, 159 and 413 mg/L (as CaCO3) was therefore tested. The results are presented

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in Table 1, showing a decrease in the pseudo-first order rate constant for DTZ as alkalinity

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increases. At concentrations above 159 mg/L changes in DTZ rate constant were very small. At

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alkalinity of 413 mg/L approx. 80% DTZ transformation could be achieved after 3 hours run,

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indicating that quenching due to alkalinity in UPW is approx. 20%.

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The influence of carbonate quenching was taken into account in models in where scavenging

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capacity of the water matrix was studied (Pereira et al., 2007a; Pereira et al., 2007b; Rosario-Ortiz

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et al., 2010; Wu and Linden, 2010).

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Chloride is a major ionic component in brines. In order to test the direct effect of Cl- on DTZ

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oxidation, typical concentrations ranging from tap water to reverse osmosis brines (200-800 mg/L

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as Cl-) were spiked into UPW at neutral pH. Pseudo-first order rate constants values slightly

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changed among the different concentrations tested (see Table 1). The extent quenching performed

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by chloride was approximately 2% after 3 hours experiment. Other authors also reported the slight

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influence of chlorides in degradation of model compounds (Neppolian et al., 2002; Wang et al.,

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2000). The influence of chloride on DTZ transformation can be explained by : (1) Chloride

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recombines with free radicals, decreasing the amount of free radicals available to react with model

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compounds; (2) At pH lower than TiO2 isoelectric point (~6.3), chloride compete with organic

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compounds for active sites on the TiO2 (Piscopo et al., 2001) whereas at pH higher than isoelectric

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point the TiO2 surface is weakly negatively charged and adsorption of chloride may be hindered

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(Wang et al., 2000), as in our experiments (pH of RO brines was 7.4±0.5). Competence for OH·

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radicals appears to be the main quenching mechanism performed by chloride in brines. Jayson and

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Parsons (1973) proposed the following reactions between chloride and hydroxyl radicals:

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OH • + Cl − ↔ HOCl •−

k eq = 0.70 ± 0.13 M −1

(2)

HOCl •− + H + ↔ Cl • + H 2O

k eq = 1.6x107 M −1

(3)

Cl − + Cl • ↔ Cl2•

k eq = 1.9x105 M −1

(4)

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3.2 DTZ oxidation in reverse osmosis-brines

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Experiments with 2 fold-concentrated RO brines were carried out in order to determine the overall

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scavenging capacity of the water matrix, to quantify the quenching performed by alkalinity and to

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estimate the influence of dilution. Characteristic composition of the RO brines applied in this study

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is presented in Table 2.

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3.2.1 Effect of alkalinity

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Influence of alkalinity in brines on DTZ transformation was studied removing it from the water

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matrix by acidification (Fig. 3). Alkalinity concentrations in the raw brines applied in the different

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experiments ranged from 290-655 mg/L (as CaCO3) corresponding to a TOC value of 20.9±3.5

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mg/L (see Table 2). Three sets of experiments were performed: raw brines (control), brines

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acidified to pH 3.5 in a current of N2 to strip out CO2, and brines without CO2 at neutral pH

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(performed by pH correction of acidified brines under N2). The last two sets represent the influence

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of pH without influence of alkalinity. The extent of DTZ transformation achieved after 3 hour

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experiments in raw brines, pH 3.5 and pH 7 where 2%, 49% and 33%, respectively. From these

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results can be concluded that extent of quenching due to alkalinity is roughly 30%.

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Taken together the results from RO brines and UPW suggest that natural alkalinity is responsible

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for about 20-30% quenching of micropollutants oxidation in brines. Our results are in line with data

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reported in other water matrixes for other target pollutants. Neppolian et al. (2002) found a decrease

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in degradation of Reactive Blue 4 as the concentration of carbonate ions increased. Wu and Linden

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(2010) obtained 10-15% and 50% reduction in reaction rates of two pesticides with an addition of

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0.5 and 10 mM of bicarbonates, respectively.

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3.2.2 Brines dilution

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The effect of brines dilutions was tested at two ratios, 1:2 and 1:4 in which 18% and 61% DTZ

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transformation were achieved respectively after three hours experiment compared to only 2%

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transformation in undiluted fresh brines (inset in Fig. 3). The 1:2 dilution which corresponds to

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secondary effluent concentration, still displayed a high radical scavenging capacity. However, high

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diatrizoate transformation was observed at dilution ratio 1:4, most probably due to the dilution of

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the radical scavenger components and divalent cations present in the water matrix that are known to

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cause agglomeration of the photocatalyst (see section 3.3.2 below). Gur-Reznik et al. (2011b) using

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NTP system obtained approximately 42% DTZ transformation in a background of RO brines, and

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64 and 100 % transformation at dilution ratio of 1:2 and 1:5 respectively. These results clearly

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depict a higher influence of dilution in UVA-TiO2 than in NTP.

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3.3 Synthetic brines experiments

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3.3.1 Characterization of synthetic brines

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Synthetic brines made possible the evaluation of the individual and combined scavenging capacity

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of the main organic and inorganic components in brines. In order to evaluate its similarities to fresh

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RO brines, synthetic brines were first optimized for their composition and characterized for their

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ability to oxidize pCBA.

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Functional groups similarities of organic and inorganic constituents was performed by FTIR

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spectroscopy (Fig. 4). Fresh and synthetic brines displayed very similar spectral pattern. Peaks at

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wavenumbers between 960-1170 cm-1 represent polysaccharides or polysaccharides-like

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substances. A peak around 1660 cm-1 (amine I, N-C=O stretch) indicates presence of N-acetyl

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amino sugars. Peaks between 665-910 cm-1 (amine I, amine II, N-H wag) and a peak around 1416

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cm-1 (amide I, stretch of aromatic bonds) suggest the presence of proteins. Peaks around 1410 cm-1

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(COH bend) and 1495 cm-1 (COO- stretching) suggest the presence of humic matter (Cho et al.,

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1998; Jarusutthirak and Amy, 2001; Drewes and Croue, 2002; Leenheer and Rostad, 2004; Ivnitsky

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et al., 2005; Gur-Reznik et al., 2008). Peaks around 1090 cm-1 represent sulphate and peaks around

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1420 cm-1 and 850 cm-1 represent bicarbonates (online NIST library). These results show a good

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correspondence between synthetic and fresh brines in terms of functional groups structure.

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The scavenging capacity of pCBA was then determined (Fig. 5). pCBA is a compound widely used

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to test the quenching of OH· radicals in different water matrixes. It reacts with OH· with a rate

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constant of 5.109 M-1s-1 (Rosenfeldt et al., 2006). Steady state OH· concentration were calculated

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from the pseudo-first order rate constant (obtained from the slope in the graph ln(pCBA)/(pCBA)0

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vs. time) (Westerhoff et al., 2009). Experiments were performed in comparison to UPW as a blank,

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in fresh and synthetic RO brines. pCBA was spiked at concentration of 5 µM. Both brines,

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synthetic and fresh, displayed a relatively similar strong quenching effect on pCBA oxidation

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compared to UPW. Indeed, while complete pCBA disappearance of UPW was attained during the

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first 30 min, only 20 and 30% transformation was achieved after 3 h run in fresh and synthetic

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brines, respectively. Steady state OH· concentration resulted slightly higher in synthetic brines

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7.32x10-15 M in comparison to 4x10-15 M in fresh brines. Similarly, an inverse relationship between

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the scavenging capacity of the water matrix and the fraction of OH· radicals available to react with

280

pCBA was reported (Rosenfeldt et al., 2006; Rosario-Ortiz et al., 2010).

281

All in all, these results show a good correspondence between synthetic and fresh brines both in

282

terms of group’s functionality and scavenging capacity.

283

3.3.2 Contribution to quenching of individual and combined brines components on DTZ

284

transformation

285

In order to evaluate the contribution of each individual component and the overall mixture on DTZ

286

oxidation, a gradual reconstitution of the synthetic brines solution was performed and compared to

287

UPW as control. The results are summarized in Fig. 6, displaying a plot of the relative DTZ

288

concentration (Ce/Co) vs. time for each case.

289

In the presence of the complete mixture of synthetic brines approx. 8% DTZ degradation was

290

achieved after 3 h of oxidation (Fig.6- left). These results are fairly well correlated to those

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obtained with fresh RO brines, which displayed around 2% DTZ transformation. Addition of SMP

292

(16±0.8 mg/L as C) and NOM (4 ±0.2 mg/L as C)-like materials representing the main components

293

of the organic matter fraction present in treated effluent-organic matter depicted a quenching effect

294

on DTZ transformation in the order of ~70±3%. These results are well correlated with those

295

obtained using fresh brines upon alkalinity removal where quenching was found to be ~70%. These

296

results confirm that organic matter present in brines performs the strongest quenching. Humic acid

297

sodium salts representing NOM was the individual largest contributor to quenching during DTZ

298

oxidation in synthetic brines, followed by alkalinity and SMP. Although OH· radicals are

299

unselective, they display affinity for carbon double and triple bonds (Haang and Yao, 1992;

300

Westernhoff 1999). Due to their high level of aromaticity, humic acids react faster with OH·

301

radicals than proteins and polysaccharides (typical SMP-like materials constituents). Moreover, HA

302

absorbs light in the wavelength range of 200-500 nm, leading to the formation of electronically

303

excited states and photochemically induced reactions (Frimmel, 1994). In consequence, hydroxyl

304

radicals and photons preferably react with HA over SMP-like compounds. This behavior along with

305

the adsorption of HA onto the TiO2 surface explain the higher quenching capacity of NOM

306

compared to SMP-like materials, in spite of a 4–fold higher TOC concentration of the latter.

307

Though HA follow anionic-type adsorption on TiO2, non-negligible amounts of HA can adsorb

308

onto the TiO2 surface, even at pH 7, due to the complex HA structure containing several functional

309

groups, such as carboxyl and phenol, having different acid dissociation constants (Yang et al.,

310

2006). Our results showed in presence of HA a lag phase of DTZ degradation during the first 60

311

min of reaction, followed by a decrease in DTZ concentration. It was reported that initial decrease

312

in TOC followed by an increase was attributed to TOC adsorption and the formation of

313

intermediate products as result of NOM oxidation (Huang et al., 2008). In consequence, NOM

314

might compete with model compounds for active sites in TiO2 surface, reducing their reaction rates

315

(Epling and Lin, 2002). Previous studies showed that NOM from lakes decreased model

316

compounds transformation to a higher extent than commercial humic acids (Lin and Lin, 2007),

317

representing a possible increase of scavenging capacity in fresh brines in comparison to synthetic

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brines. In summary, the main effects of NOM in the photocatalyst system include

319

deactivation/competition for active sites in the surface of the semiconductor, scavenging effects,

320

light absorption and reduction in light transmittal (Frimmel, 1994; Epling and Lin, 2002; Lin and

321

Lin, 2007).

322

Interestingly, the quenching performed individually by NOM and SMP-like materials after 3 h of

323

experiment were 25±4 and 15±6%, respectively (see Fig.6- left), suggesting a synergistic effect

324

when combined together (~70%). The synergistic effect in presence of SMP-like materials and

325

NOM together might be explained by the abovementioned interactions between HA and TiO2

326

leaving less OH· radicals available to react with the model compounds. Indeed, as can be seen from

327

Fig. 6-left, an almost identical lag phase during the first hours of experiment was observed in

328

presence of HA alone and HA together with SMP, suggesting initial adsorption of HA on TiO2

329

surface.

330

A mixture of phosphate, sulphate and nitrate (Fig. 6-right) displayed negligible quenching effect

331

and after 3 h of experiment more than 99% DTZ transformation was achieved, most probably due

332

to their relative low concentration and the fact that at pH> isoelectrical point adsorption of anions

333

onto the TiO2 surface is hindered. It has been reported that H2PO4-/HPO4 and sulphate react with

334

OH· to form HPO 4 -• and a SO4-· respectively, which are less reactive than OH· radicals

335

(Maruthamuthu and Neta, 1978; Wang et al., 2000). Influence of nitrate in model compounds

336

mineralization was reported almost insignificant even at acidic pH (Abdullah and Matthews, 1990).

337

Bicarbonate displayed the main quenching effect among all anions tested, around 80% DTZ

338

transformation was found. These results indicated that bicarbonate alkalinity is the main

339

responsible for radical scavenging among the inorganic components. When calcium was present

340

along with sodium and potassium in the anions mixture, only 21% DTZ transformation was

341

achieved (see Fig. 6-right). It has been reported that at the same ionic strength, Ca+2 exhibited a

342

stronger influence on TiO2 particles than Na+. Addition of CaCl2 leaded to a faster aggregation than

343

NaCl due to reduction of surface charges in TiO2 at pH 8. As the Ca+2 concentration increases,

344

absolute value of zeta potential decreases and hydrodynamic diameter of TiO2 increases and above

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1 mM CaCl2 no further change in TiO2 aggregation takes place (French et al., 2009; Thio et al.,

346

2011). However, when humic acid was supplemented to a solution of 130 mg/L Ca+2 as CaCl2

347

(≈3.25 mM Ca), corresponding to RO brines concentration, the effect of Ca+2 was almost

348

completely suppressed, achieving at the end of the experiment 65% DTZ transformation (compare

349

both panels in Fig. 6). This hindering of Ca+2 effect in water containing NOM can be attributed to:

350

(a) calcium promotes high adsorption of HA onto the catalyst surface by bridging, electric double

351

layer compression or charge neutralization, (b) possible formation of chelates in solution (Fang et

352

al., 1999; Zhang et al., 2009; Thio et al., 2011). Based on these interactions and our results, it is

353

clear that the effect of Ca+2 in the presence of NOM is weaker in either fresh RO or synthetic brines

354

as compared to ultrapure water.

355

To conclude this section, our findings clearly indicate that the whole synthetic brine solution and its

356

individual components as well as quenching factors considered, cover and explain the most relevant

357

issues involved in AOP of trace chemicals in brines and related water matrixes.

358

3.4 Transformation and deiodination of diatrizoate and iopromide in UPW

359

To take advantage of intrinsic iodine label in the model compounds, transformation and

360

deiodination were tracked by different procedures. Organic bound iodine technique has been used

361

successfully to test electrochemical reduction as a selective technique to remove organic iodine

362

from X-ray contrast media (Zwiener et al., 2009). In order to gain insights regarding the

363

deiodination mechanism, DTZ oxidation was compared with IOPr (Fig. 7). The transformation

364

mechanism for diatrizoate shows predominantly decrease in DTZ with scarce presence of

365

intermediates containing organic iodine (Fig. 7-bottom). During iopromide transformation,

366

decrease in its concentration and formation of a series of intermediates containing organic iodine

367

were observed (Fig. 7-top). Peak at 7.7 min represents organic bound iodine in IOPr, whereas peaks

368

at 7, 8.2 and 8.5 min represent other organic iodine containing compounds, i.e., oxidation products.

369

Inset graphs in Fig. 7 show percentage of transformation and deiodination of IOPr and DTZ vs.

370

time (deiodination was tested using adsorbable organic iodine). DTZ displayed higher resistance to

371

oxidation. The rate of IOPr transformation resulted higher than DTZ, and after 5 min oxidation

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IOPr reached 95% transformation whereas DTZ only 55%. Furthermore, deiodination of IOPr

373

reached 45% in 5 min and 84% in 25 min whereas DTZ showed 34 and 77% deiodination in 5 and

374

45 min, respectively. During the five first minutes in the experiment ratio

375

deiodination/transformation was higher in DTZ than in IOPr with values of 0.72 and 0.44,

376

respectively. These results suggest that in IOPr, transformation starts at side chains, whereas in

377

DTZ seems to be deiodination the predominant transformation in the initial steps.

378

Previous studies reported transformation of IOPr and DTZ in non-thermal plasma, it was found that

379

DTZ oxidation mechanism involves direct deiodination of the aromatic ring, whereas in IOPr

380

oxidation of side chains preceded ring deiodination (Gur-Reznik et al., 2011b). Lütke et al. (2014)

381

identified IOPr transformation products (TPs) in electrochemical treatment. Three different starting

382

reactions were found in the anodic compartment where oxidation took place, and only TP-681 was

383

partial deiodinated. Four DTZ transformation products were identified by Sugihara et al. (2013) at

384

oxic conditions in UVA-TiO2, two of them exhibited partial deiodination. However iodide

385

measurements showed almost a complete dehalogenation of the DTZ at each time point. These

386

results support our findings that side chain transformation in IOPr is the main initial mechanism.

387

Our results differ from those reported by Jeong et al. (2010) for treatment of DTZ and IOPr with γ

388

radiation. They identified for DTZ TP-586, in which the triiodobenzene structure remained

389

unaltered, at high relative concentration. For IOPr they found TP-789, TP-665 and TP-681 as initial

390

starting reactions, in which only TP-789 maintained the triiodinated structure unaltered. A possible

391

explanation to these differences may be other mechanism acting in γ radiation out of hydroxyl

392

attack.

393

4. Conclusions

394

This study presented a systematic characterization of the pattern and extent of quenching of the

395

major individual constituents of RO brines during TiO2 oxidation of iodinated contrast media

396

through application of a specially designed synthetic brines solution. The major contribution to

397

quenching resulted from the organic matter followed by alkalinity. Among the organic matter

398

components, NOM-like materials present in wastewater effluent displayed a higher quenching

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399

compared to soluble microbial products, in spite of their 4-times lower TOC concentration. This

400

behavior can be attributed both, to the interaction, i.e., adsorption, between humic acid and TiO2

401

and the significantly higher reactivity of hydroxyl radicals with the highly aromatic HA compared

402

to proteins and polysaccharides in SMP. A synergistic effect was observed when NOM and SMP

403

were present together resulting in a net higher decrease of available OH· radicals. Ca+2 reduced

404

TiO2 effectiveness due to agglomeration of the photocatalyst; however, this influence was reduced

405

in the presence of NOM. These interactions possess high importance in effluents and brines, and

406

have to be taken into account especially in oxidation processes catalyzed by particles. The

407

quenching performed by the main brines constituents individually can be categorized in the

408

following order: NOM>alkalinity≅ SMP >Cl->(NO3+PO4-3+SO4-2). Concluding, synthetic brines

409

are a useful tool for rational characterization of quenching made by the individual background

410

components present in effluents and brines whereas iodinated contrast media are good markers for

411

evaluation of AOP oxidation potential.

412

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Acknowledgments

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This work was funded by the Joint German-Israeli Research Program BMBF-MOST (Contract No.

415

WT 0903/2194). The financial support of Sanofi by a research grant through the Peres Center for

416

Peace and the generous support of the Rieger Foundation are gratefully acknowledged.

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products. Analytical and Bioanalytical Chemistry 395(6), 1885–1892.

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National Institute of Standards and Technology (NIST):

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http://webbook.nist.gov/cgi/cbook.cgi?ID=B6000512&Mask=80

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http://webbook.nist.gov/cgi/cbook.cgi?ID=B6004671&Mask=80

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Figure legends

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Figure 1. Chemical structures of diatrizoate and iopromide.

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Figure 2. Schematic process diagram of the secondary effluents-desalination process applied in this

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study.

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Figure 3. Influence of alkalinity and pH of RO brines on DTZ transformation. Inset shows influece

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of brines dilution on transformation. The undiluted brines (control) corresponds to the fresh brines

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in the main graph.

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Figure 4. FTIR spectra of fresh (left panel) and synthetic RO brines (right panel).

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Figure 5. Effect of the water matrix in p-chlorobenzoic acid degradation. [pCBA]o ≈ 5 µM.

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Figure 6. Influence of the water matrix components on DTZ transformation. Left: Solutions

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containing organic matter, alkalinity and composite synthetic brines. Na+ was the main counterion.

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In synthetic brines 112±15 mg/L Ca+2 were also added. Right: Solutions containing mono and

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multivalent anions or their mixture (NO3-, SO4-2, PO4-3, Cl- and HCO3-) or humic acid. Na+ was the

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main counterion. Where specified Ca+2 at 112±15 mg/L was added.

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Figure 7. LC-MS chromatograms denoting the evolution of organic iodine during UVA-TiO2 in

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UPW. Top: IOPr, Bottom: DTZ. Insets show transformation and deiodination time profiles.

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Table 1. Pseudo-first order reaction rate constants (k’, in min-1) for diatrizoate oxidation in UPW. TiO2

Alkalinity

k'×10-2

R2

mg/L TiO2

k'×10-2

R2

mg/L as CaCO3

3.5

11.50±0.40

0.98

0.25

4.77±0.52

0.86

control UPW

7

5.70±0.11

0.99

0.5

6.35±0.10

0.99

18

10

2.36±0.04

0.99

1

9.37±0.30

0.99

84

2

11.70±0.60

0.96

Chloride

k'×10-2

R2

mg/L Cl-

k'×10-2

R2

5.70±0.11

0.99

control UPW

5.69±0.11

0.99

2.20±0.09

0.98

185

1.98±0.01

0.99

1.33±0.03

0.99

390

1.85±0.01

0.99

159

1.10±0.03

0.99

800

1.87±0.02

0.99

413

0.94±0.01

0.99

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units

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pH

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Values represent average±standard deviation (R2 coefficient of determination). In most cases at least 3 replicates were performed.

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Conditions: [TiO2] = 1g/L; pH= 7 for chloride and alkalinity, 5.5 in TiO2 dose; UV fluence = 3564 mJ/cm2; irradiation time = 3 hours.

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Units

Value

pH

-

7.4±0.5

UV-254

-

0.6±0.03 20.9±3.5

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TOC Alkalinity as

448.1±157.9 CaCO3

132.1±8.3

K

P S Cl-

mg/L

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NO3-

63.7±6.1

NH4+ -N

353.4±9.9

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Na

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Ca

7.9±3.1

85.0±41.1

513.2±26.1 32.9±1.1 2.8±0.1

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Values represent average±standard deviation of at least 3 replicate samples.

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Contribution of main OH radical scavengers in RO brines were studied in UVA-TiO2



Quantitative quenching of individual components was studied with synthetic



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brines

Dissolved organic matter performs the higher quenching (≈ 70%) followed by alkalinity (≈30%)

NOM-like materials displayed higher quenching than SMP in spite of its lower

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concentration.

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Reduction of UVA-TiO2 effectiveness by Ca+2 is lowered in presence of NOM

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Advanced oxidation of iodinated X-ray contrast media in reverse osmosis brines: the influence of quenching.

Among the main restrictions for the implementation of advanced oxidation processes (AOPs) for removal of micropollutants present in reverse osmosis (R...
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