Presented by Tanzina Rahman July 25, 2013 SiViRT Student Meeting Department of Civil and Environmental Engineering University of Texas at San Antonio Modeling.

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Presented by Tanzina Rahman July 25, 2013 SiViRT Student Meeting Department of Civil and Environmental Engineering University of Texas at San Antonio Modeling and Sensitivity Analysis on the Mobility of Aluminum Oxide Nanoparticles in Saturated Sand

Outline Background Materials and Methods Results and Discussion Conclusions

Nanoparticles Are….. Nanometers_________________________________ Enhanced chemical and physical properties  Small size  Increased specific surface area Focus on understanding and creating systems, devices, and materials for real-world applications Membranes E.g. water treatment Adsorbents E.g contaminant removal Oxidants E.g Disinfection Catalysts E.g. Industrial Application Sensing E.g. Water Quality Analytical E.g. Increasing Detection Limits

Why is it Important to Understand Nanoparticle Behavior in Environment? Image credit: University of California at Santa Barbara

 Characterization of Al 2 O 3 nanoparticles and sand  Experimental setup  Bromide tracer test  Measurement instruments Materials and Methods for Experiments

Characterization of Al 2 O 3 Nanoparticle Primary Particle Size (nm) DLS Size (nm) Surface Area (m 2 /g) PZC at pH 18.4 ± ±

Characterization of Quartz Sand Mesh SizeParticle Size (μm) Surface Area (m 2 /g) PZC at pH ±

Experimental Setup ParameterValue NanoparticleAl 2 O 3 Initial Concentration50,150,400 mg/L Column inner diameter 15 mm Porous mediumWhite quartz Sand Length of porous medium 70 mm Flow rates (µl/min)212.17, , 1273 and 2546 Darcy Velocity (m/d)4.2 m/d, 16.9 m/d, 25.4 m/d, and 50.8 m/d Temperature22-23 o C pH (S_82nm)4.8 ± mV pH (P_244nm)7.0 ± mV 1 Pore Volume (PV)~ 4.5 mins

Bromide Tracer Test To determine the hydrodynamic diffusion coefficient and porosity of the sand column Potassium bromide (KBr) was used as tracer chemical (1 mg/L of KBr in 1 mM NaCl/0.065 mM NaHCO3 solution) The porosity of the sand was obtained by minimizing the sum of the squares between the (C/Co ) experimental data and solution of advection-dispersion equation (ADE) for each effluent sample applying the least square method Average Porosity was calculated to be ± 0.015

Measurement Instruments ICP-OESICP-MS SonicatorDigester Delsa-Nano

Modeling the transport behavior of Al 2 O 3 nanoparticles in sand Modeling Experimental Results

Two Site Transport Model C= concentration of NP Al suspended in aqueous phase ρ b = bulk density of soild phase λ= dispersivity f = porosity ψ = site blocking term S = amount of NP Al attached to solid phase S max = maximum solid phase concentration k 1, k 2 = removal rate constants for fast and slow attachment, respectively 0

How Was the Model Used?  The breakthrough curves for aluminum oxide nanoparticles for various conditions were fitted using Hydrus 1D software.  Two kinetic site model was used for the purpose. The model was used in the following ways:  Model M1: Only k 1 was fitted  Model M2: k 1 and S max were fitted  Model M3: k 1, k 2 and S max were fitted  The dispersivity was fitted from tracer data for each flow velocity using ADE (advective-dispersion equation) by minimizing the square of the difference between experimental data and calculated values.

Fitting Experimental Data with M1, M2 and M3 Models ModelR 2 of fit M M M ModelR 2 of fit M M M30.995

Modeling for Varying Ionic Strength ISk 1 (min -1 )k 2 (min -1 )S max (mg/g)R 2 of fit DI water mM NaCl mM NaCl mM NaCl

Modeling for Varying Flow Rate and Nanoparticle Concentration Flow Rate (µl/min) k 1 (min -1 ) k 2 (min -1 ) S max (mg/g) R 2 of fit Conc. (mg/L) k 1 (min -1 ) k 2 (min -1 ) S max (mg/g) R 2 of fit

Simulating transport behavior of Al 2 O 3 nanoparticles in sand using two kinetic sites model and calculating the confidence interval of the breakthrough curves. Performing probabilistic sensitivity analysis to determine the effects of parameter variability on the breakthrough. Simulation and Probabilistic Sensitivity Analysis for Modeling

Methodology Latin Hypercube Sampling (LHS) for normal distribution was used to generate 100 samples for a set of parameters using mean and standard deviation The response from the model was generated using the direct solution of Hydrus 1D code for all the samples generated using two kinetic sites model The model generates time dependent nanoparticle effluent concentrations The variance of the effluent concentrations at each time (or pore volume) point was calculated. Thus, 95% confidence interval was calculated from the mean and standard deviation of effluent concentration for each point of time Probabilistic sensitivity analysis was performed to determine the effects of the parameters ((k 1, k 2 ), dispersivity (λ), porosity (f), and maximum solid phase concentration (S max )) on the model response

Input Parameters ParametersDescription Experimental Conditions Mean Standard deviation CoV (%) How mean and standard deviation are found? dcdc Sand particle diameter all237 μm21.5 μm9.07 Screening of sand particles or sieve analysis dpdp Particle (diameter) size DI water81.7 nm2.5 nm3.06 Measured particle size by DLS 1mM NaCl81.8 nm12.9 nm mM NaCl83.7 nm9.8 nm mM NaCl324.5 nm34.6 nm10.66 vPore-water velocity µl/min 0.29 cm/min ± 3 (standard normal variate) 1 Accuracy of measurement according to manufacturer µl/min 1.18 cm/min 1273 µl/min 1.77 cm/min 2546 µl/min3.53 cm/min f Porosity of sand column all Experiments λDispersivity µl/min0.575 cm cm1.04 From experiments µl/min0.144 cm cm µl/min0.097 cm cm µl/min0.048 cm cm1.04 k1k1 Fast Attachment Coefficient all- -- k2k2 Slow Attachment Coefficient all- - - S max Maximum nanoparticle concentration on solid phase Next table- - - Calculated from the two replicated experiments

Input Parameter S max IS (mM) Flow Rate (μL/min) Nanoparticle Concentration (mg/L) Mean S max (M t /M i )/g sand Standard Deviation CoV(%)

UQ of DI water Background

UQ of 1mM NaCl Background

UQ of 10mM and 100mM NaCl Background

UQ for Flow Rates of µl/min and µl/min

UQ for Flow Rates of 1273 µl/min and 2546 µl/min

UQ for 50 mg/L, 150 mg/L, and 400 mg/L Nanoparticle Concentrations

Global sensitivity analysis  is a variance based method that is used to determine how to apportion the variance of the output among the input random variables.  Each sensitivity is normalized by the variance of the output.  1 st order sensitivity Conditional variance as X i is being fixed Having frozen one potential source of variation, the resulting variance is less than the total of unconditional variance

Sensitivity Analysis Results First order sensitivity for parameters in two kinetic sites model for effluent concentration at 30 mins or 6.5 PV in the breakthrough curve of 150 mg/L Al 2 O 3 in 1 mM NaCl background and at 43 mins or 8.6 PV in the breakthrough curve of 150 mg/L Al 2 O 3 in 100 mM NaCl background at 1273 µL/min Parameters First Order Sensitivity for 1mM NaCl background (S i ) First Order Sensitivity for 100 mM NaCl background (S i ) f λ k1k k2k S max ∑S i

Sensitivity Analysis Results First order sensitivity for parameters in two kinetic sites model for effluent concentration at 30 mins or 6.5 PV in the breakthrough curve of 50 mg/L Al 2 O 3 in 1 mM NaCl background at 1273 µL/min ParametersFirst Order Sensitivity (S i ) f λ k1k k2k S max ∑S i

Conclusions NPs and nano-aggregates less than 100nm show high mobility even at ionic strength as high as 10 mM NaCl  Increased NP concentration increased mobility  Increasing flowrate had an insignificant effect on mobility Blocking was the most likely mechanism for transport of S_82nm nanoparticles suggested by experimentation and modeling results Sensitivity analysis showed that k 2 (slow attachment) and S max (max. solid retention capacity) are the most sensitive parameters to cause variability in the mobility for high and low nanoparticle concentrations, respectively This work indicates important implications regarding aluminum oxide and metal oxide nanoparticle mobility in sand filtration systems, groundwater remediation sites or natural subsurface porous media

Questions ? Thank You !

Filtration Equations Ref: Tufenkji, N. and Elimelech, M. (2004). Correlation equation for predicting single-collector efficiency in physicochemical filtration in saturated porous media. Environmental science & technology 38(2): η 0 = single collector contact efficiency D= diffusion I= interception G=gravitation

η o : Theoretical single collector contact efficiency; η D : Transport by diffusion; η I : Transport by interception; η G : Transport by gravitation; η : Single collector removal efficiency; α: attachment efficiency; f=Porosity; d c : porous media diameter N R = Aspect ratio = dp/dc Peclet No. Attraction No. N vdW = Van der Waals no. = A/kT A= Hamaker constant k = Boltzmann constant Ref: Tufenkji, N. and Elimelech, M. (2004). Correlation equation for predicting single-collector efficiency in physicochemical filtration in saturated porous media. Environmental science & technology 38(2): Gravity No. As= porosity dependent parameter = f = porosity of the transport medium U= Approach velocity dc = collector diameter µ= fluid viscosity ap = particle radius Attachment Efficiency Single Collector Removal Efficiency Equations

Monte Carlo

LHS