rational design of advanced oxidation processes using...
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Daisuke Minakata1, Ke Li2,
John C. Crittenden1, David Hand3
1 School of Civil and Environmental EngineeringGeorgia Institute of Technology2 Faculty of Engineering, University of Georgia3 Civil and Environmental EngineeringMichigan Technological University
AOT 16, November 15-18, 2010 San Diego, CA.
Rational Design of Advanced Oxidation Processes using Computational Chemistry
1
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Modeling AOPs
1. Simplified Pseudo-Steady-State Model
2. AdoxTM – AOP simulation software
3. Conventional Approach for Kinetic Model
4. Computer-based Kinetic Model
2
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3. H2O2 is added to a water containing O3, i.e. [O3]0 is known.
3
2. H2O2 and O3 are added simultaneously
3 3O O
ss, 09 2 10 2 2 11 3 12 130 0 00 0
HOHO H O HCO R NOM
LK a P H
k k k k k
UV/H2O2 H2O2/O3 Simplified pseudo-steady-state model
R 12 ss, 0HOk k
H O2 2pH p
1 2 2 30 resss, 0
11 3 12 130 00
2 H O 10 OHO
HCO R NOM
Kk
k k k
2 2 2 2
-A
H O 0 H O
ss,0
10 2 2 0 11 3 0 12 0 13 0
2 I f (1- e )[HO ]
k [H O ] k [HCO ] k [R] k [NOM]
g
1. UV/H2O2
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4
Flow Models: Ideal flow at steady state (1st order reaction)
1. Plug Flow Reactor (PFR)
k
0C C e
2. Completely Mixed Flow Reactor (CMFR)
0CC
(1 k)
3. Tank-in-series (TIS)
0
n
CC
1 kn
1/ n
0C nQV 1
C k
0Q C CV
r
0CQV ln
k C
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5
Flow Models: Non-ideal flow
4. Dispersed flow model closed system
A
2 2Ao
1 vL4a exp
2 EC
a vL a vLC (1 a exp (1 a exp) )2 E 2 E
a 1 4k (E / vL)
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7
Known reaction rate constants
Compoundk HO•
M-1
s-1 [HO•]=10
-9 M [HO•]=10
-10 M [HO•]=10
-11 M
MtBE 1.6×109 0.01 0.1 1
Oxalic acid 1.4×106 8 83 825
Acetate ion 7×107 0.2 2 17
Trichloromethane 5.0×106 2 23 231
1,1,2-Trichloroethane 1.1×108 0.11 1 11
Chloroform 5×106 2 23 231
Chloroacetic cid 4.3×107 0.3 2.7 27
Glycolic acid 6×108 0.02 0.2 2
1,1,1-Trichloroethane 4×107 0.3 3 29
Benzene 7.8×109 0.001 0.01 0.1
Phenol 6.6×109 0.002 0.02 0.2
Halflife, min
kHCO3- = 8.5×106 M-1s-1
kCO3-- = 3.9×108 M-1s-1
H2CO3* ↔ H+ + HCO3-
(pKa=6.3)HCO3- ↔ H+ + CO3
2-
(pKa=10.3)
kNOM =(3.0 ~ 4.5)×108 M-1s-1
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Hypothesis -GCM-
Essence is same as the GCM for the gaseous phase Observed experimental reaction rate constant for a
given organic compound is the combined rate of all elementary reactions involving HO•, which can be estimated using Arrhenius kinetic expression.
The Ea consists of two parts: (1) Base part from main reaction mechanisms (i.e.,
H-atom abstraction, HO• addition to alkenes and aromatic compounds and HO• interaction with S, N, or P-atom-containing compounds).
(2) Functional group contribution partially from neighboring and/or next nearest neighboring functional group.
= aE
RTk Ae
Minakata, Li, Westerhoff, Crittenden, 2009 ES&T 43, 6220-6227
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• Over or under prediction for the oxygenated multifunctional group compounds due to solvation effects, and for the halogenated and carboxylic compounds due to larger steric hindrance
GCM Results -overall 2/2-
1.0E+05
1.0E+06
1.0E+07
1.0E+08
1.0E+09
1.0E+10
1.0E+11
1.0E+05 1.0E+06 1.0E+07 1.0E+08 1.0E+09 1.0E+10 1.0E+11
kca
l (M
-1s-1
)
k exp (M-1s-1)
Ideal fit
kexp/kcal = 0.5 and 2.0
H-atom abstraction (Calibrated)
HO addition to alkene (Calibrated)
HO interaction with N,S,P-atom-
containing compounds (Calibrated)
HO addition to aromatic compounds
(Calibrated)
H-atom abstraction (Prediction)
HO interaction with N, S, P-atom-
containing compounds (Prediction)
HO addition to aromatic compounds
(Prediction)
Minakata, Li, Westerhoff, Crittenden, 2009 ES&T 43, 6220-6227
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GCM is limited because:1. Many datasets are required to calibrate parameters2. Only deal with molecules for which all required group rate constants
and group contribution factors have been calibrated before.3. Limited number of literature-reported experimental rate constants
for other reaction mechanisms than HO•4. Assumed that a functional group has approximately the same
interaction properties under a given molecule, so that the GCM disregards the changes of the functional properties that can arise from the intramolecular environment by electronic push-pull effects, hydrogen bond formation, or by steric effects.
Application of computational chemistry (quantum mechanical calculations) for predicting reaction rate constants in aqueous phase
Looking at reaction energies (transition states)
10
Challenges still remains
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Modeling AOPs
1. Simplified Pseudo-Steady-State Model
2. AdoxTM – AOP simulation software
3. Conventional Approach for Kinetic Model
4. Computer-based Kinetic Model
11
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AdOxTM, AOPs Simulation Software• AdOxTM is a part of the Environmental Technologies Design
Option Tools (ETDOTTM). It contains mechanism-based models
that can be used to evaluate and design advanced oxidation
processes.
• The final version of AdOx will include the following models:
– H2O2/UV model (available in version 1.0)
– H2O2/O3 model
– UV/O3 model
• A comprehensive database is also included in AdOxTM to provide
powerful support to the above models as well as ease-of-use
features for the user. 12
Crittenden et al., 1999. Wat. Res. 33, 2315-2328
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Features of Current Version AdOxTM 1.0 for UV/H2O2
H2O2 + hν → 2HO•
H2O2 = quantum yield of H2O2 (=0.5) I0 = incident light intensity, einstein cm-2 sec-1 A=2.303b(εH2O2CH2O2+εRCR + εSCS + εHO2-CHO2-) b=pathlength, cm fH2O2= 2.303 b (εH2O2CH2O2 + εHO2-CHO2-)/A
H2O2/HO2- + HO H2O/OH- + HO2 2.7×107, 7.5×109
H2O2 + HO2/O2- HO + H2O/OH- + O2 3.0, 0.13
HO + HO H2O2 5.5×109
HO + HO2/O2- H2O/OH- + O2 6.6×109, 7.0×109
HO2 + HO2/O2- H2O2/HO2
- + O2 8.3×105, 9.7×107
R + hv Products
R + HO Products kMtBE=1.6×109, ktBA=6.0×108
HO + CO32-/HCO3
- CO3- + OH-/H2O 3.9×108, 8.5×106
HO + NOM Products 2.4×104 (mgC/L)-1s-1
NOM + hv Products 14
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• Reactor Options
– Completely mixed reactor (CMBR)
– Completely flow type reactor (CMFR) w/o TIS
– Plug flow reactor
– Non-ideal Mixing
• Main Process Operational Variables :
– Initial hydrogen peroxide concentration
– Incident UV-light intensity
• Water quality parameters:
– TOC concentration
– pH
– Concentrations of target compounds
– Byproducts can be included if they are known
Features of Current Version AdOxTM 1.0
15
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Concern about residual H2O2
• H2O2 has low UV light absorption
• Need to increase H2O2 concentration to lower EE/O
• High residual H2O2 will require treatment to reduce H2O2 such as chlorine
16
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Simulation Results (LPUV/H2O2) – NAIX + Dealkalization -
0.00
0.50
1.00
1.50
2.00
2.50
3.00
3.50
4.00
0.0
2.0
4.0
6.0
8.0
10.0
12.0
14.0
16.0
5 10 15 20
EE
O (k
Wh
/kg
al-
ord
er)
H2O
2re
sid
ua
l co
nc.
(m
g/L
)
H2O2 Dosage (mg/L)
Residual of H2O2 MtBE tBA
• 10 mg/L of H2O2 dosage would be the better choice although the optimum dosage of H2O2 is over 20 mg/L. This is because the cost required for over 20 mg/L of H2O2 dose overweigh the energy cost. • At 10 mg/H2O2 dosage, UV dose was calculated as 2,100 mJ/cm2.
17Li; Hokanson; Crittenden; Trussell; Minakata. Wat. Res. 2008, 43, 5045-5053
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References that were used for model validation
Glaze, W. H.; Lay, Y.; Kang J. W. Advanced oxidation processes. A kinetic model for the oxidation of 1,2-dibromo-3 chloropropane in water by the combination of hydrogen peroxide and UV radiation. Ind. Eng. Chem. Res. 1995, 34, 2314-2323.
Li, Ke.; Stefan, M.I.; Crittenden, J.C. UV photolysis of trichloroethylene: Product study and kinetic modeling. Environ. Sci. & Technol. 2004, 38, 6685-6693.
Li, Ke.; Stefan, M.I.; Crittenden, J.C. Trichloroethylene degradation by UV/H2O2 advanced oxidation process: Product study and kinetic modeling. Environ. Sci. & Technol. 2007, 41(5), 1696-1703.
Li, Ke.; Hokanson, D.R.; Crittenden, J.C.; Trussell, R.R.; Minakata, D. Evaluating UV/H2O2 processes for methyl tert-butyl ether and tertiary butyl alcohol removal: Effect of pretreatment options and light sources
18
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AdOxTM 2 Simulation Software for O3, O3/H2O2, and mitigation of bromate
and THM formation
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Concern about bromate
• Formation of bromate (BrO3-) during ozonation
in the presence of bromide ion (Br-)
• A nationwide survey of Br- in drinking water sources: approximately 80 μg/L (Amy et al., 1994)
• Br- in costal area is expected higher
• 10 μg/L of BrO3- standard of MCL associated with
cancer risk, Stage 1 of the Disinfectant/Disinfection
By-Product (D/DBP) Rule (EPA, 1998)
• When ozone is applied to disinfection, tradeoffs
between inactivation of cryptosporidium and
bromate formation should be evaluated. 20
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Mechanisms of bromate formation
Simplified reaction scheme for bromate formation during ozonation
Ozone involving pathway HO• involving pathway
O3 + Br - → OBr
- + O2 160
OBr- + O3 → 2O2 + Br - 330
OBr- + O3 → O2 + BrO2 - 100
HOBr + O3 → O2 + BrO2 - + H+ <0.013
BrO2 - + O3 → BrO3 - + O2 5.7×10
4
O3 + Br• → BrO• + O2 1.5×108
HO• + HOBr → BrO• + H2O 2.0×109
HO• + OBr- → BrO• + OH- 4.2×10
9
HO• + Br- → Br• + OH- 1.1×109
BrO• + BrO• + H2O → BrO2- + OBr- +2H+
5.0×109
BrO• + BrO2- → OBr- + BrO2• 4.0×108
At lower pH (pH<pKa=8.8), less BrO3- is produced via ozone
pathway since HOBr is dominant. As a result, O3 decay is slower.
pKa = 8.8
Disproportionation
k (M-1 s-1)
21
Haag and Hoigné, 1983von Gunten and Hoigné, 1994
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Control of bromate formation 1 – pH depression-
• pH depression resulting in more HOBr due to pKa=8.8 of
HOBr reduces BrO3- formation. However, in drinking water
treatment at around neutral pH, HOBr is mainly oxidized by
HO•. Therefore, pH depression does not reduce BrO3-
formation drastically.
• At reduced pH, O3 decay is slower and the *HO•+/*O3] is
decreased during ozonation. As a result, reduction of BrO3-
at the steady state is distinctive. It is noted that it cannot
be expected the proportional relationship between
*HO•+/*O3] and BrO3- formation.
22
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Model simulation - pH effect (O3 with NOM)-HO• + NOM → products k = 19000 (mgC/L)-1s-1 Westerhoff et al 2007
Br• + NOM → Br- + products k = 83000 (mgC/L)-1s-1 Pinkernell and von Gunten 2001
0.0
0.2
0.4
0.6
0.8
1.0
0 10 20 30 40 50 60
O3
(mg
/L)
Time (min)
pH=6.0
pH=6.5
pH=7.0
pH=7.5
pH=8.0
pH=8.5
0
20
40
60
80
100
120
140
160
0 10 20 30 40 50 60
BrO
3-
(ug/
L)
Time (min)
pH=6.0
pH=6.5
pH=7.0
pH=7.5
pH=8.0
pH=8.5
Reactor type CMBR
Init O3 (mg/L) 1.0
pH 6, 6.5, 7, 7.5, 8, 8.5
Br- (µg/L) 300
NOM (mgC/L) 1.0
* CMBR: completely mixed batch reactor 23
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Control of bromate formation 2 - NH3 addition -
Simplified reaction scheme for controlling bromate formation
• The maximum effect is at high NH3 as HOBr becomes very small. However, it is observed that excess NH3 decreases the efficiency of bromate control. • Not efficient in water containing medium to high NH3
k (M-1
s-1
)
HOBr + NH3 → NH2Br + H2O 7.5×107
OBr- + NH3 → NH2Br + OH- 7.6×104
NH2Br + OH- → OBr- + NH3 7.5×106
25
Pinkernell and von Gunten, 2001
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Model simulation - NH4+ addition (O3 with NOM)-
0.0
0.2
0.4
0.6
0.8
1.0
0 10 20 30 40 50 60
O3
(mg/
L)
Time (min)
NH4+ = 0 ug/L
NH4+ = 50 ug/L
NH4+ = 100 ug/L
NH4+ = 200 ug/L
0
20
40
60
80
100
120
140
0 10 20 30 40 50 60
BrO
3-
(ug/
L)
Time (min)
NH4+ = 0 ug/L
NH4+ = 50 ug/L
NH4+ = 100 ug/L
NH4+ = 200 ug/L
NH4+ = 400 ug/L
NH4+ = 800 ug/L
Reactor type CMBR
Init O3 (mg/L) 1.0 (= 21 µM)
pH 8.0
Br- (µg/L) 300 (= 3.8 µM)NOM (mgC/L) 1.0
NH4+ (µg/L)0, 50, 100, 200, 400, 800
(0, 2.9, 5.8, 11, 23, 47 µM of NH3 tot)
26
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Control of bromate formation 3 – Cl2-NH3 process -
• HOCl hinders Br- oxidation to Br• by HO•
NH3 additionCl2 addition OzonationSource water
HOCl + Br- → HOBr + Cl- 1550
OCl- + Br- → OBr- + Cl- 0.001
HOCl ↔ OCl- + H+ pKa = 7.5
• NH3 reacts with both HOBr and HOCl
• Effective to hinder HO• during ozonation to reduce BrO3-• HOCl and NH2Cl oxidize specific moieties of NOM and reduces their reactivities toward O3, and also scavenge HO•.
* HOCl, NH2Br, and HOBr react with NOM to produce THMs and TOX
HOBr + NH3 → NH2Br + H2O 7.5×107
OBr- + NH3 → NH2Br + OH- 7.6×104
HOCl + NH3 → NH2Cl + H2O 4.2×106
27
Buffle et al., 2004
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Model simulation – Cl2-NH3 process 2 -
0.0E+00
2.5E-07
5.0E-07
7.5E-07
0 0.5 1
HO
Br
(M)
Time (min.)
HOCl = 5 uM
HOCl = 10 uM
HOCl = 15 uM
• NH3 addition (1 min.):HOBr is significantly masked by NH3.
• O3 (60 min.): Pre-addition of HOCl followed by NH3 decreased BrO3- by factor of 2~7 as compared with the case of only NH3
addition.
0.0
0.2
0.4
0.6
0.8
1.0
0 20 40 60
O3
(mg
/L)
Time (min.)
HOCl = 0 uMHOCl = 5 uMHOCl = 10 uMHOCl = 15 uM
0.0
1.0
2.0
3.0
4.0
5.0
6.0
0 20 40 60
BrO
3-(
ug/
L)
Time (min.)
HOCl = 0 uM
HOCl = 5 uM
HOCl = 10 uM
HOCl = 15 uM
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[TTHM] = [Cl2]{ATTHM(1-exp(-kt)}
ln(k) = 5.41 – 0.38 ln + 0.27 ln([NH3-N]) – 1.12 ln(Temp) + 0.05 ln([Br-]) – 0.854 ln(pH)
ln(ATTHM)=-2.11-0.87 ln -0.41 ln([NH3-N]) + 0.21 ln([Cl2]) + 1.98 ln(pH)
[TTHM]=predicted trihalomethane conc. in initial phase (~5h), µg/L
[Cl2]=applied chlorine dose, mg/L
[DOC] = dissolved organic carbon, mgC/L
[NH3-N] = ammonia-nitrogen conc., mg/L as N
[Br-]= bromide concentration, µg/L
Temp = temperature, °C
t = reaction time, h
Model simulation – Cl2-NH3 process 4 –
TTHM formation
Improved EPA 1998 empirical model (Sohn et al., 2004)
0
2
4
6
8
10
12
14
16
0 10 20 30 40 50 60
TTH
M (
ug/
L)
Time (min)
HOCl = 5 uM
HOCl = 10 uM
HOCl = 15 uM
HOCl (uM) 0, 5, 10, 15
Br- (ug/L) 300
TOC (mgC/L) 1.0
pH 8.0
phosphate (M) 0.001
NH4+ (ug/L) 400
Chlorination 5 min.
Ammonia addition 1 min.
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O3/H2O2 processfor MtBE removal and bromate mitigation
• Advanced oxidation process: O3/H2O2 process:
– HO2- + O3 → HO• + O2•- + O2 k = 2.2×106 M-1s-1
– H2O2 + O3 → O2 + H2O k = 0.0065 M-1s-1
– produce more HO• at higher pH due to pKa = 11.6 of H2O2
– H2O2 also scavenges HO•
• H2O2 + HO• → HO2• + H2O k = 2.7×107 M-1s
• optimum ratio: [H2O2]/[O3] = 0.5 mole/mole
• H2O2 addition keeps the O3 concentration low.
• In the presence of Br-, H2O2/HO2- reacts with HOBr/OBr- to produce Br- resulting in BrO3- formation. In addition, there is significant contribution of the reaction of O3 with Br• in regard with BrO3- formation (von Gunten and Oliveras, 1998).
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Simulation – O3 with H2O2 process–
Simulation parameters
• MtBE = 300 ug/L
• pH = 7.6
• NOM = 1.4 mg/L
• Alkalinity = 318 mg/L as CaCO3
• initial O3 = 3 mg/L
• molar ratio: [H2O2]/[O3] = 0.5 (optimum), 0.75, 1.0
• H2O2 = 1.06, 1.59, 2.12 mg/L
• Br- = 300 ug/L
• Completely Mixed Batch Reactor (CMBR)
33
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Simulation results – O3 with H2O2 process–
0.0
0.5
1.0
1.5
2.0
2.5
3.0
[O3]
(mg
/L)
[H2O2]/[O3]=0.5
[H2O2]/[O3]=0.75
[H2O2]/[O3]=1.0
0.0
0.5
1.0
1.5
2.0
0 20 40 60 80 100 120
[H2O
2]
(mg
/L)
Time (sec)
0
5
10
15
20
25
30
0
50
100
150
200
250
300
[tB
A]
(ug/
L)
[MtB
E]
(ug
/L)
MtBE tBA
0
1
2
3
4
5
6
7
0 20 40 60 80 100 120
[BrO
3-]
(u
g/L
)
Time (sec)34
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Summary • A kinetic model for bromate formation during
ozonation was formulated at non-steady state and non-constant pH with various parameters (pH, alkalinity, NOM, Br-).
• 3 main bromate mitigation techniques (pH depression, NH3 addition, Cl2-NH3 process) give quantitative insight of bromate formation control.
• A kinetic model for O3 with H2O2 was simulated for MtBE and tBA along with bromate formation
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Modeling AOPs
1. Simplified Pseudo-Steady-State Model
2. AdoxTM – AOP simulation software
3. Conventional Approach for Kinetic Model
4. Computer-based Kinetic Model
36
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Conventional Approach for Kinetic Model in AOP 1. One “hot” parent organic chemical contaminant2. Conduct batch experiments to measure byproducts using GC/MS etc. 3. Obtain rate constant/Measure rate constant (e.g., pulse radiolysis)4. Build kinetic model based on both experimental findings and
literature-reported rate constants. Unknown rate constants are usually obtained by fitting with experimental data.
Parent compoundMajor byproducts
(yield 10-30 mole%)
Minor byproducts
(yield 2-5 mole%)
Acetone
*Stefan and Bolton, 1999
acetic, pyruvic, and oxalic acids
pyruvaldehyde
formic and glyoxylic acids
hydroxyacetone, formaldehyde
MtBE
* Stefan et al., 2000
acetone, acetic acid, formaldehyde,
tert-butyl formate (TBF), pyruvic acid,
tert-butyl alcohol (TBA), 2-methoxy-2-
methyl propionaldehyde (MMP), formic,
methyl acetate
hydroxy-iso-butylaldehyde,
hydroxyacetone,
pyruvaldehyde and hydroxy-
iso-butyric, oxalic acid
Dioxane
*Stefan and Bolton, 1998
1,2-ethanediol diformate, formic acid,
oxalic acid, glycolic acid, formaldehyde,
1,2-ethanediol monoformate
methoxyacetic acid glyoxal
TCE
* Stefan and Bolton, 2002formic acid, oxalic acid
dichloroacetic acid,
mono-chloroacetic acid 37
A few studies examined entire reaction mechanisms
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39
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
0 5 10 15 20 25 30 35
Time / min
[Ch
lori
de
Io
n]
/ m
M
0.00
0.05
0.10
0.15
0.20
0.25
0.30
0.35
0.40
0.45
[In
term
ed
iate
s]
/ m
M
Chloride
Oxalic Acid
DCA
Formic Acid
MCA
Conventional Approach for Kinetic Model in AOP
Byproducts in TCE Destruction based on experimental studies
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• UV irradiation ranging from 200 nm to 300 nm inan interval of 1 nm
• Molar extinction coefficients of TCE, H2O2 and 4types of main byproducts are measured andsimulated in an interval of 1 nm from 200 to 300nm
• pH change of the system
• Dissociation of 8 organic/inorganic acids
• 22 literature reported rate constants are used in the model
The model is a kinetic model and considers:
TCE UV/H2O2 Modeling
40
Li, Stefan and Crittenden, 2004, ES&T 38, 6685-6693Li, Stefan and Crittenden, 2007, ES&T 41, 1696-1703
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• Complex radical reactions between hydrogen peroxide, hydroxyl radical, superoxide radical and formyl radical
• TCE direct photolysis and reactions with OH • and Cl•
• Formation and destruction of main byproducts and intermediates, such as di-chloroacetic acid (DCA), mono-chloroacetic acid (MCA), oxalic acid and formic acid
• Intermediate byproducts those are not detected: glyoxylic acid and phosgene
• Scavenging of hydroxyl radical by bicarbonate species
The model contains 34 differential equations for 8 molecules and 6 radicals, including:
TCE UV/H2O2 Modeling
41
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0.E+00
2.E-03
4.E-03
6.E-03
8.E-03
1.E-02
1.E-02
0 5 10 15 20 25 30 35
Time (min)
Co
nc
en
tra
tio
n (
mo
l/L
)
exp
mod
0.E+00
2.E-04
4.E-04
6.E-04
8.E-04
1.E-03
1.E-03
0 10 20 30 40
Time (min)
Co
nc
en
tra
tio
n (
mo
l/L
)
mod
exp
0.E+00
1.E-06
2.E-06
3.E-06
4.E-06
5.E-06
6.E-06
7.E-06
8.E-06
9.E-06
0 10 20 30 40
Time (min)
Co
nc
en
tra
tio
n (
mo
l/L
)
exp
mod
0.E+00
2.E-06
4.E-06
6.E-06
8.E-06
1.E-05
1.E-05
0 10 20 30 40
Time (min)
Co
nc
en
tra
tio
n (
mo
l/L
)
mod
exp
Comparison of Modeled and Experimental Concentration Profiles 1/2
TCE
MCADCA
H2O2
TCE UV/H2O2 Modeling
42
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Comparison of Modeled and Experimental Concentration Profiles 2/2
0.E+00
1.E-05
2.E-05
3.E-05
4.E-05
5.E-05
6.E-05
7.E-05
8.E-05
9.E-05
1.E-04
0 5 10 15 20 25 30 35
Time (min)
Co
nc
en
tra
tio
n (
mo
l/L
)
exp
mod
Oxalic acid
0.E+00
5.E-05
1.E-04
2.E-04
2.E-04
3.E-04
3.E-04
4.E-04
4.E-04
5.E-04
0 10 20 30
Time (min)
Co
nc
en
tra
tio
n (
mo
l/L
)
exp
mod
Formic acid
0
1
2
3
4
5
6
7
0 10 20 30 40
Time (min)
pH
exp
mod
pH
TCE UV/H2O2 Modeling
43
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Modeling AOPs
1. Simplified Pseudo-Steady-State Model
2. AdoxTM – AOP simulation software
3. Conventional Approach for Kinetic Model
4. Computer-based Kinetic Model
44
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A Computer-Based Kinetic Model in AOPs
Why so important?
We now know the general reaction mechanisms that HO• initiates in the aqueous phase AOPs based on a number of experimental studies.
We have a large number of datasets for reaction rate constants in the aqueous phase AOPs.
Concern about emerging contaminants
Greater than 50 million chemical compounds registered in CAS and more than 40 million chemicals are available
Is it feasible?
We now have robust tool (e.g., computational chemistry) and computational resources
We can make it feasible
45
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“All models are wrong but some are useful.”
-- George E.P. Box
“Let’s develop some useful ones and make good use of them.”
-- an optimistic modeler
46
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Reaction Pathway Generator (Graph theory)
Reaction Rate Constant Predictor (Quantum mechanical calculations)
Ordinary Differential Equations (ODEs) Solver
47
Reaction Pathway Generator
Reaction Rate Constant Predictor
ODE Generator and Solver
ToxicityProfiles
Toxicity Estimator
ConcentrationProfiles
A Computer-Based Kinetic Model in AOPs
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Reaction Pathway Generator
48
H-atom abstraction by HO•or HO• addition
O2 addition
Uni/Bi molecular decay
HydrolysisHO• reactions
Β-scission, 1,2-H shift
Peroxyl radical mechanisms
Parent compound
Carbon centered radical
Peroxyl Radical
Oxy radical
Intermediates (aldehydes, alcohols etc.)
Carbon centered radical
Carboxyl acid
CO2/Minerals
Li and Crittenden, 2009 ES&T 43, 2931-2837
General reaction mechanisms that HO• initiates based on past experimental studies
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ClHC=CCl2
ClCH(OH)-CCl2
HO
hv *Cl
Cl2HC-CCl2
ClH2CCOOH
ClHC-COOH
HO
O2
HC(O)ClCO2
-
OHC-COOH
HCl +CO
O2
OHC-CCl2+HCl
O2
OHC-CCl2+HCl
OHC-CCl2+HCl C(O)Cl2
CHO HCOOH
CO2+HCl
HCOOHOHC-CClO+Cl
OHC-COOH
H2O
HO
CO2-+H++H2O
H2O2
HCOOHCO2
H2O
HO
HOOC-COOH
HO
CO2-+CO2+H+
Cl2HCCOOH
Cl2C-COOH
HO
O2
C(O)Cl2
CO2
HOOC-C(O)Cl
HOOC-COOHHOOC-COOH
Cl2CHCHO
HCCCl
ClCCCl
H2O
HO
HO
Cl2CHCOOH
CO2 + Cl-
CO2 + Cl-
Proposed Mechanism4949
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Details of TCE pathway accounts for the formation and decay of formic, glyoxylic, oxalic acids and phosgene.
Cl2C=CHCl
Cl2CCH(OH)Cl Cl2C
CHCl2
Cl2C-CHO
-HCl
HO
Cl
OO-Cl2C-CHO
OCl2C-CHO
O2
Cl(O)C-CHO
+ Cl
HOOCCHOCO2 + HCl
H2OH2O
CHO +C(O)Cl2
H2O
HC(OH)2
O2
OOCH(OH)2
HCOOH + HO2
HCOOH
H2O2
O2
OOCCl2CHCl2
OCCl2CHCl2
O2
+OCHCl2
Cl2CHC(O)Cl C(O)Cl2 + CHCl2
- Cl
Cl2CHCOOH
O2
OOCHCl2
C(O)Cl2
+(OH)CHCl2
C(O)Cl2
+H2O2
C(OH)Cl2HC(O)Cl
CO + HCl OOC(OH)Cl2
CCl2COOH
OOCCl2COOH
C(O)Cl2 +HO2
OCCl2COOH
C(O)Cl2+ COOH ClC(O)COOH
HOOCCOOHO2
OOCOOH
CO2 + HO2
H2O
HOOCCOOH
HO
CO2 + CO2
HO
CO2 H2O2O2
CO2 + O2
CO2 + HO 50
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Another Challenge:
To predict reaction rate constants
in aqueous phase
51
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GCM is limited because:1. Many datasets are required to calibrate parameters2. Only deal with molecules for which all required group rate constants
and group contribution factors have been calibrated before.3. Limited number of literature-reported experimental rate constants
for other reaction mechanisms than HO•4. Assumed that a functional group has approximately the same
interaction properties under a given molecule, so that the GCM disregards the changes of the functional properties that can arise from the intramolecular environment by electronic push-pull effects, hydrogen bond formation, or by steric effects.
Application of computational chemistry (quantum mechanical calculations) for predicting reaction rate constants in aqueous phase
Looking at reaction energies (transition states)
54
Challenges still remains
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Linear Free Energy Relationships (lnk =-a∆G≠+b)
1
2
3
45
6
7
9
10
11
12 12
141516
17
1922
23
2425
26
13
21
8
y = -0.222x + 9.356R² = 0.746
0
2
4
6
8
10
12
-4 -2 0 2 4 6 8 10 12
log
kH
∆ G≠rxn,aq, kcal/mol
Neutral (G3 + COSMO-RS)
Ioznized (G4 + SMD)
y = -0.542x + 11.768R² = 0.817
0
2
4
6
8
10
12
0.0 2.0 4.0 6.0 8.0 10.0
log
kE
XP
∆GactI , kcal/mol
Neutral
Ionized
55
LFER based on calculated ∆G≠LFER based on experimental ∆G≠
• LFER is established for H-atom abstraction from a C-H bond of saturated aliphatic compounds. • kexp and ∆Gact
I represents experimentally obtained overall rate constant and activation energy, while kH is equal to kexp/(# of C-H bond) and ∆G≠
rxn,aq represents the lowest free energy of activation.
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Free energy profiles for HO• with CH4
56
*CH3 + H2O, -23.27 *OOCH3, -30.01
CH4 + HO*, 0
CP,
-0.69
TS, 5.89
CP, -20.69
*OCH3 + O, 23.67
CH3OOOOCH3, -58.40
H3COOCH3 + O2 , -80.66
2*OCH3+O2, -33.66
2HCHO + H2O2, -95.75
HCHO+CH3OH+O2, -122.22
TS, 21.96
TS, -21.44
*CH3 + O2, 0
-150
-100
-50
0
50
0 1 2 3 4 5 6
Delt
a G
aq
, k
ca
l/m
ol
Reaction cordinate
H-atom abstraction
O2 addition
Tetroxide uni-molecular decay
Formation of tetroxide
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57
Free energy profile for HO• with CH4 (continued)
*OCH3, 0.00
TS, 21.97
*C(OH)H2, -13.43
-20
-15
-10
-5
0
5
10
15
20
25
0 0 .5 1 1 .5 2 2 .5 3 3 .5
Delt
a G
aq
, k
ca
l/m
ol
Reaction cordinate
H-shift (Rearrangement of alkoxyl radical)
*OCH3 + H2O, 0.00
*C(OH)H2, -13.43
TS *OCH3-H2O,
18.56
CP OCH3+H2O,
5.23
CP *C(OH)H2 + H2O,
-9.73
*OCH3, 0
TS , 21.97
-20
-15
-10
-5
0
5
10
15
20
25
0 0 .5 1 1 .5 2 2 .5 3 3 .5
Delt
a G
aq
, k
ca
l/m
ol
Reaction cordinate
HCHO + 2H2O, 0.00
TS, 36.63
HOCH2OH + H2O, -1.65
CP HCHO+2H2O, 12.45
CP, 10.06
HCHO + H2O, 0 complex, 5.34
TS, 40.17
-10
0
10
20
30
40
50
0 0 .5 1 1 .5 2 2 .5 3
Delt
a G
aq
, k
ca
l/m
ol
Reaction cordinate
H2O-assisted hydrolysis
Oxygen-transfer
We should be able to establish a library of reaction rate constant predictors once the LFER for each elementary reaction is established.
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Summary • Four different approaches have been shown to model aqueous phase advanced oxidation processes.
• A simplified pseudo-steady-state model is precise enough to examine the feasibility of the process.
• AdoxTM (UV/H2O2) simulation software can be used to design AOPs not assuming constant pH, steady-state.
• Conventional approach to establish kinetic model in AOP is time consuming and does not consider all possible by-products.
• Our under-developing computer-based kinetic model is robust for rational design of AOPs but there are still some challenges remains.
58
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Aquatic toxicity assessment of AOPs byproducts- Relative toxicity of TCE degradation byproducts -
59
• 96-hr Green Algae ChV: most sensitive indicator among the acute and chronic endpoints for fish, daphnia, and green algae (EPA 2005)• TQ(Toxicity Quotient): {Concentration ÷ 96-hr Green Algae ChV} ∑TQ = Relative toxicity of a mixtureTQ or ∑TQ ≥ 1 : Toxic and unacceptable (Belden et al. 2007)
Green Algae
96-hr ChV (mg/L)
TCE 2.9
Formic acid 83.0
Oxalic acid 1050.0
MCA 529.0
DCA 556.00
5
10
15
20
0 5 10 15 20 25 30
Rela
tive T
oxic
ity
(Co
ncen
trati
on
/Ch
V)
Time (min)
Composite of TCE, formic acid, oxalic acid, MCA, and DCA
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0
100
200
300
400
500
600
700
0 5 10 15 20 25 30
Re
lati
ve t
oxi
city
(C
on
cen
trat
ion
/ D
WEL
)
Time (min)60
Non-carcinogenic effect assessment - TCE degradation byproducts -
• DWEL (Drinking Water Equivalent Level): A lifetime exposure concentration protective of adverse non-cancer health effects from drinking water
• Relative toxicity = ∑[concentration / DWEL]
*Oxalic acid and Formic acid are not included in the drinking water criteria.
Composite of TCE, MCA, and DCADWEL
(mg/L)
TCE 0.25
MCA 0.35
DCA 0.14
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Carcinogenic effect assessment - TCE degradation byproducts -
• Cancer Classification
TCE : sufficient evidence in animals and inadequate or no evidence in human (B2)
MCA : inadequate information to assess carcinogenic potential (I)
DCA : likely to be carcinogenic to humans (L)
• 10-4 Cancer risk concentration:
The concentration of a chemical
in drinking water corresponding
to an excess estimated lifetime
cancer risk of 1 in 10,000. (EPA 2006)
Chemical10-4 Cancer Risk
(mg/L)
TCE 0.003
MCA
DCA 0.007
0
1
2
3
4
5
6
0 5 10 15 20 25 30
Rela
tiv
e t
oxic
ity
(Co
ncen
trati
on
/ c
an
cer
risk
)x
10
00
0
Time (min)
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Acknowledgement
• National Science Foundation (NSF): 0607332 and 0854416
• Water Reuse Foundation: WRF-05-010• Georgia Tech College of Computing, Office of
Information Technology and CEE IT Services for high computational resources.
• High Tower Chair and Georgia Research Alliance at Georgia Tech
• Brook Byers Institute for Sustainable Systems• University of Notre Dame Radiation Center and
Department of Energy
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