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Engineered Slippery Surface to Mitigate Gypsum Scaling in Membrane Distillation for Treatment of Hypersaline Industrial Wastewaters vasiliki Karanikola, Chanhee Boo, Julianne Rolf, and Menachem Elimelech Environ. Sci. Technol., Just Accepted Manuscript • DOI: 10.1021/acs.est.8b04836 • Publication Date (Web): 14 Nov 2018 Downloaded from http://pubs.acs.org on November 15, 2018

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Engineered Slippery Surface to Mitigate Gypsum Scaling in Membrane Distillation for Treatment of Hypersaline Industrial Wastewaters

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Submitted to 8

Environmental Science & Technology

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Revised: November 6, 2018 11 12

Vasiliki Karanikola,† Chanhee Boo,† Julianne Rolf,

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and Menachem Elimelech*

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Department of Chemical and Environmental Engineering, Yale University, New Haven, Connecticut 06520-8286, United States

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V.K. and C.B. contributed equally to this work. *Corresponding author: e-mail: [email protected]; Tel: +1 (203) 432-2789

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ABSTRACT

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Membrane distillation (MD) is an emerging thermal desalination process, which can potentially

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treat high salinity industrial wastewaters, such as shale gas produced water and power plant

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blowdown. The performance of MD systems is hampered by inorganic scaling, particularly when

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treating hypersaline industrial wastewaters with high-scaling potential. In this study, we

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developed a scaling-resistant MD membrane with an engineered “slippery” surface for

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desalination of high-salinity industrial wastewaters at high water recovery. A polyvinylidene

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fluoride (PVDF) membrane was grafted with silica nanoparticles, followed by coating with

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fluoroalkylsilane to lower the membrane surface energy. Contact angle measurements revealed

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the “slippery” nature of the modified PVDF membrane. We evaluated the desalination

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performance of the surface-engineered PVDF membrane in direct contact membrane distillation

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using a synthetic wastewater with high gypsum scaling potential as well as a brine from a power

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plant blowdown. Results show that gypsum scaling is substantially delayed on the developed

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slippery surface. Compared to the pristine PVDF membrane, the modified PVDF membranes

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exhibited a stable MD performance with reduced scaling potential, demonstrating its potential to

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achieve high water recovery in treatment of high-salinity industrial wastewaters. We conclude

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with a discussion of the mechanism for gypsum scaling inhibition by the engineered slippery

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surface.

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TOC Art

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INTRODUCTION

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Thermoelectric power plants use a substantial amount of water, which accounts for

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approximately 40% of freshwater withdrawals in the United States. 1-3 There is a critical need to

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impose stringent discharge regulations on power plants to reduce their freshwater consumption,

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wastewater discharge, and environmental impact. The U.S. Environmental Protection Agency

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(EPA) established a regulatory limit of wastewater discharge from power plants to the

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environment to be reduced by ~57 billion gallons per year. 4 Brine discharge from thermoelectric

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power plants are strictly prohibited in regions with limited freshwater supplies. In such

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conditions, the facilities need to achieve zero liquid discharge (ZLD) for waste (brine) streams.

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Sustainable management of wastewaters from steam electric power generation is of critical

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importance at the water-energy nexus.

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Steam-driven electric power plants require water in two processes: one as the means to

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generate steam to drive a turbine and one as the cooling water to remove heat from the

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condensed steam and the system components; 5 the latter accounts for the majority of the water

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consumption. During cooling tower operation, the process water is continuously concentrated up

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to eight times due to evaporation, environmental losses, and infrastructure leakage, 6 which

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causes scaling and corrosion of the system. To prevent scaling and corrosion, many chemicals,

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including biocides, biodispersants, corrosion inhibitors, pH adjusters, and anti-scalants are added

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to the cooling water.5 In addition, many power plants are designed to use reclaimed municipal

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wastewater effluent or surface water as cooling process water, which contain diverse inorganic

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and organic matter as well as microorganisms.6 The concentrated cooling water contains high

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concentrations of total dissolved solids (TDS) and chemical additives. Hence, wastewater from a

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power plant is challenging to treat by conventional water treatment practices.

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Membrane distillation (MD) is a thermal separation process driven by a vapor gradient

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resulting from a temperature gradient created across a hydrophobic microporous membrane. 7

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Theoretically, MD can achieve complete salt rejection, owing to its phase-change based

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desalination mechanism. Furthermore, performance of MD is only slightly sensitive to the feed

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salinity, because the vapor pressure of feed solution does not change much with salt

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concentration.8 Nonetheless, MD is energetically intensive as any thermal separation process. 9 3

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Energy-efficient MD operation is possible if abundant waste or low-grade heat is readily

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available10. The waste heat produced from a power plant cooling tower can be exploited to drive

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the MD process. With its effective incorporation into the thermoelectric power plant scheme,

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MD can provide sustainable process water management by achieving ZLD for waste streams. 11

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Membrane scaling is of critical concern when treatment of high-salinity industrial wastewater

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at high water recovery is desired, such as desalination of power plant blowdown. 12, 13 At higher

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MD system recovery, TDS concentrations in the feed increases to supersaturated conditions. 14

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Nucleation of the crystals in the bulk solution and subsequent crystal deposition on the

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membrane surface, as well as heterogeneous nucleation of the crystals on the membrane surface,

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take place under such supersaturated conditions.15, 16 The scaling mechanisms in MD are closely

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related to the membrane surface properties, feed solution chemistry, and the system

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hydrodynamic conditions.15,

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desalination performance of MD membranes.18 In addition, the scaling layer aggravates

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temperature and concentration polarization by reducing the effectiveness of heat and mass

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transfer near the membrane surface.19

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Scaling leads to pore wetting and subsequent decrease in the

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Recent studies have shown that engineering the surface with special wettability can enhance

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MD membrane performance.20-22 Polyvinylidene fluoride (PVDF) is one of the commercially

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available hydrophobic membranes widely used for MD applications. 23-26 However, in many

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cases, conventional PVDF membranes are susceptible to scaling. 27-29 The non-adhesive surface

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nature adapted from a lotus leaf can potentially be leveraged to fabricate anti-scaling MD

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membranes.28,30-32 Coating a hydrophobic substrate with ultralow interfacial energy material can

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create a surface with unique properties, including a significantly high water contact angle, low

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contact angle hysteresis, and non-adhesive slipperiness. Such unique surface properties are

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expected to reduce scaling potential of MD membranes by limiting energetically favorable

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regions for crystal growth.33-36

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In this study, we demonstrate the potential application of MD membranes with

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superhydrophobic, slippery surface properties in treatment of high-salinity industrial wastewaters

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at high water recovery. MD membranes with a slippery surface were prepared via facile and

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scalable surface engineering of hydrophobic PVDF membranes. Water flux and salt rejection 4

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performance of the slippery membrane were evaluated and compared to membranes with

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hydrophobic and hydrophilic surfaces in direct contact membrane distillation, using

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supersaturated gypsum feed water. We further evaluated MD performance of the slippery-surface

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membrane in the desalination of power plant blowdown wastewater. Based on the observed

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results, we discuss possible mechanisms for reduced scaling potential of the engineered slippery

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surface.

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MATERIALS AND METHODS

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Materials and Chemicals. ACS grade sodium hydroxide (NaOH, J.T. Baker), (3-

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Aminopropyl)triethoxysilane (99%, APTES) (Sigma-Aldrich), anhydrous ethanol (100%, Decon

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Laboratories, Inc., PA), silica nanoparticles (SiNPs, Ludox SM, avg. diameter 8 nm, 30%,

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Sigma−Aldrich), and (heptadecafluoro-1,1, 2 ,2- tetrahydrodecyl)trichlorosilane (FDTS, Gelest

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Inc., PA) were used for the surface modification of the polyvinylidene fluoride substrate.

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Supersaturated gypsum (CaSO4·2H2O) solution was prepared by mixing calcium chloride

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dihydrate (CaCl2·2H2O, Sigma-Aldrich) and sodium sulfate (Na2SO4, Sigma-Aldrich) in

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deionized (DI) water.

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Surface Modification of PVDF Membrane. A four-step protocol was used to modify a

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flat sheet polyvinylidene fluoride (PVDF) hydrophobic membrane with a nominal pore size of

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0.45 μm and an average thickness of 125 μm (HVHP, Millipore). 20 The first step was to immerse

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the PVDF substrate into a 7.5 M NaOH solution at ∼70 °C for 3 h to functionalize the surface

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with hydroxyl groups. The alkaline-treated PVDF membrane was then rinsed with DI water and

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oven-dried at 80 ºC for 1 h. The dried membranes were subsequently placed in 1% v/v APTES in

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ethanol under continuous stirring for 1 h. APTES covalently binds with the hydroxyl groups to

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produce amine terminal groups, rendering the membrane surface positively charged. Then, the

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amine-functionalized PVDF substrate was immersed in an aqueous SiNP suspension for 1 h

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under gentle mixing. SiNPs are negatively charged and bound electrostatically to the positively

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charged PVDF membrane surface. The aqueous SiNP suspension was prepared by adding 1

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wt % SiNPs in acetate buffer with an ionic strength of ~1 mM. The pH of the SiNP suspension

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was adjusted to 4 to promote effective electrostatic attraction between the negatively charged 5

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SiNPs and the positively charged amine terminal groups on the PVDF substrate. Before use, the

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SiNP suspension was bath sonicated for 30 minutes to minimize particle aggregation. Finally, the

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SiNP-coated PVDF substrate was functionalized with fluoroalkylsilane via covalent bonding (i.e.,

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(heptadecafluorotetrahydrodecyl)trichlorosilane, hereafter denoted as 17–FAS) to lower the

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membrane surface energy via vapor phase silanization for 12 h under vacuum and heating at 70

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ºC.

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Membrane Characterization. Surface morphology of the pristine and modified PVDF

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membranes was examined by scanning electron microscopy (SEM, Hitachi SU-70). Before

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imaging, membrane samples were sputter-coated with a 4-nm iridium layer (BTT-IV, Denton

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Vacuum, LLC, Moorestown, NJ). The SEM images were obtained to confirm SiNP coating after

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surface modification and to observe scalants formed on the membrane surface after MD scaling

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experiments. Scaling of MD membranes on the surface and inside the pores was further analyzed

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by elemental mapping using SEM equipped with an energy dispersive X-ray spectroscopy (EDS,

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Bruker XFlash 5060FQ Annular detector). The scaled membrane samples were sputter-coated

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with a 4-nm iridium layer (BTT-IV, Denton Vacuum, LLC, Moorestown, NJ) to eliminate

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charging during EDX analysis. We note that EDX elemental analysis is not affected by the

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iridium coating as it has binding energy far from the elements expected on our samples.

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The elemental composition of the pristine and surface modified PVDF membranes was

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analyzed by X-ray photoelectron spectroscopy (XPS, PHI VersaProbe II, Physical Electronics

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Inc., MN). Membrane samples were oven dried at 70 ºC overnight prior to performing XPS. The

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XPS spectra were collected using monochromatic 1486.7 eV Al Kα X-ray source with a 0.47 eV

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system resolution. The energy scale was calibrated using Cu 2p3/2 (932.67 eV) and Au 4f7/2

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(84.00 eV) peaks on a clean copper plate and a clean gold foil.

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Static contact angle and dynamic surface wettability of the PVDF membranes with

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hydrophobic, hydrophilic, and slippery surface were measured by a contact angle goniometer

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(OneAttension, Biolin scientific instrument) using the sessile drop method. Static water contact

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angles were measured by placing a 5-μL droplet on the membrane surface. The shape of water

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droplet was photographed for 30 s using a digital camera. The digital images obtained were

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analyzed by a postprocessing software (OneAttension software), and the data were averaged. 6

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Dynamic surface wettability was tested by dropping a 10-μL water droplet from a 4-cm height

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and monitoring the movement of the droplet on the surface over time.

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Synthetic and Blowdown Feed Waters. DI water (1 L) at 60 and 20 °C was used as

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feed and permeate streams, respectively, for initial one hour direct contact membrane distillation

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(DCMD) runs. Calcium chloride (1 M) and sodium sulfate (1 M) stock solutions were prepared

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in advance and filtered with a 0.45 m cellulose acetate membrane filter (Corning, Tewksbury,

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MA). After 1 h stabilization, stock solutions were added to the feed reservoir to obtain a scaling

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solution comprising 20 mM CaCl2 and 20 mM Na2SO4 without pH adjustment. The gypsum

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(CaSO4·2H2O) saturation index (SI) of this solution at 60 °C was calculated using OLI Stream

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Analyzer (OLI Systems, Inc., Morris Plans, NJ) at 1.1. The gypsum scaling experiments were

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conducted until the permeate flux nearly reached to zero and the conductivity of the permeate

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begun to increase.

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Blowdown water from the cooling towers at Redhawk Power Station in Arlington, Arizona,

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was prefiltered through 11-μm filter (Ashless grade 44, GE Whatman, PA) to remove particulate

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and suspended organic matter prior to DCMD experiments. The major composition and key

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properties of the prefiltered blowdown water were analyzed by a third-party environmental

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laboratory (Environmental Service Laboratories, Inc., PA) (Table S1). The blowdown water was

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treated with chlorine and stored at 4 °C to prevent biological growth. The DCMD experiments

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with blowdown water were conducted until the maximum amount of feed solution (initial

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volume of 1 L) was recovered before the conductivity of the permeate started to increase  an

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indication of pore wetting.

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Membrane Distillation Scaling Experiments. We evaluated the scaling behavior of the

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pristine and surface-modified PVDF membranes using a laboratory-scale direct contact

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membrane distillation (DCMD) unit. A custom-made acrylic cell with channel dimensions of 77

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mm in length, 26 mm in width, and 3 mm in depth, translating to an effective membrane area of

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20.0 cm2, was used for testing. The temperatures of feed and permeate solutions were maintained

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at 60 and 20 °C, respectively. A low (8.5 cm/s) and high (17 cm/s) feed cross-flow velocities

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were employed to investigate the effect of hydrodynamics on the membrane scaling behavior.

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The water vapor flux, Jw, across the membrane was determined by measuring the increase in 7

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permeate weight over time. Concentration of salt in the permeate was measured using a

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calibrated conductivity meter (Oakton Instruments, Vernon Hills, IL). The electrical conductivity

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of the permeate solution was monitored to calculate the salt rejection.

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RESULTS AND DISCUSSION

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Properties of Slippery Surface Membrane. Figure 1a schematically illustrates the steps to

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synthesize a slippery surface on a hydrophobic PVDF substrate. The PVDF substrate is first

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treated with an NaOH (7.5 M) solution at 70 ºC to functionalize the surface with hydroxyl groups.

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During this process, simultaneous defluorination and oxygenation take place on PVDF polymer

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chains by substitution of fluorine into hydroxyl moieties.37 The NaOH-treated PVDF membrane

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remained mechanically robust and flexible as shown in Figure S1-A, and no morphological

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differences were observed in SEM images of the PVDF membranes before and after alkaline

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treatment (Figures S1-B and S1-C). The alkaline treated PVDF substrate is then aminosilanized

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(APTES 1% v/v in ethanol) to render the surface positively charged. APTES binds covalently

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with the hydroxyl groups on the membrane and serves as a substrate for SiNP deposition onto the

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membrane surface. The negatively charged SiNPs are electrostatically bound with the amine-

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functionalized substrate surface. Finally, the PVDF membrane with attached SiNPs is vapor

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silanized with 17–FAS through a hydrolysis-condensation reaction to produce a surface with

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ultralow interfacial energy.33

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FIGURE 1

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Scanning electron microscopy (SEM) and energy dispersive X-ray spectroscopy (EDS) were

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used to confirm SiNP coating on the PVDF substrate. The top-down view of the SiNP-coated

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membrane clearly shows a dense layer of the spherical nanoparticles on the PVDF substrate

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(Figure 1b). The cross-section image of SEM-EDS elemental mapping for the SiNP-coated

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membrane indicates that SiNP modification creates a several micrometer thick coating layer on

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the porous substrate (Figure 1c). We also observed SiNP coating inside the substrate pores,

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consistent with our previous studies.33 The internal pore functionalization is expected to increase 8

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the resistance to pore wetting and potentially reduce scaling potential, as we discuss later in this

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paper.

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XPS spectra for the pristine PVDF membrane (denoted as hydrophobic), SiNP-coated PVDF

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membrane (denoted as hydrophilic), and SiNP and 17–FAS functionalized PVDF membrane

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(denoted as slippery) verify the substrate coating with SiNPs and surface fluorination with 17–

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FAS (Figure 1d). The pristine hydrophobic PVDF membrane exhibits two major peaks at 289

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and 285 eV, which are assigned to the binding energies of carbon to fluorine (CF 2) and carbon to

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hydrogen (CH2), respectively.38 The peak intensities for CH2 and CF2 are nearly equal, consistent

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with the chemistry of PVDF. The hydrophilic surface membrane exhibits binding energy peaks

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identical to those of the pristine hydrophobic membrane; however, their intensities are lower

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because the SiNP coating covers the surface elemental composition of the native PVDF. Instead,

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we observed strong XPS spectra relevant to oxygen (O) and silicon (Si) for the SiNP-coated

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PVDF membrane (Figure S2). After functionalization with 17–FAS, the slippery membrane

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exhibits a slightly different spectrum, which displays an energy peak at 293 eV ascribed to the

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terminal CF3 group of 17–FAS chain. We also observed a shift of the CF2 peak to 291 eV due to

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the formation of CF2-CF2 after surface 17–FAS functionalization. The obtained XPS spectrum

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corroborates successful surface modification of the pristine hydrophobic substrate to produce

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membranes with an engineered slippery surface that provides a high water repellency (Figure 1e).

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Surface wettability and the non-stick slippery nature of the pristine and surface-modified

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PVDF membranes were evaluated using a contact angle goniometer with DI water as the testing

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liquid (Figure 2). The pristine hydrophobic surface membrane showed a relatively high static

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contact angle of ~120º. As expected, the hydrophilic surface membrane exhibited the lowest

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static water contact angle of ~70º, while the slippery surface membrane showed the highest

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hydrophobicity with a water contact angle of > 150º (Figure 2a). When the pristine hydrophobic

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membrane was subjected to dynamic surface wettability testing, the water droplet remained in

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place with no bouncing (Figure 2b-1). This observation indicates that water and the surface do

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not strongly repel each other despite the inherent surface hydrophobicity. The hydrophilic

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surface membrane exhibited the lowest tendency to repel water as demonstrated by stable droplet

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settling on the surface during the dynamic surface wettability test (Figure 2b-2). This observation

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indicates that the attraction between the hydrophilic surface and water is higher than the kinetic 9

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energy exerted by the bouncing droplet. In contrast, the slippery surface membrane illustrates

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immediate bouncing of water droplet upon contact with the engineered slippery surface (Figure

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2b-3). This observation suggests that the modification produced a low energy surface where the

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kinetic energy of the bouncing droplet can overcome the attractive forces between the droplet

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and membrane surface. FIGURE 2

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Gypsum Scaling Behavior. The gypsum scaling behavior of the hydrophobic,

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hydrophilic, and slippery surface membranes was studied through DCMD experiments. Permeate

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flux was measured over time as the membranes were exposed to a supersaturated gypsum feed

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solution (SI = 1.1) prepared by mixing 20 mM of CaCl2 and Na2SO4. We assessed the gypsum

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scaling potential of these membranes by monitoring the flux and electric conductivity of the

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permeate simultaneously in a batch DCMD mode (i.e., feed solution was concentrated over time).

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The effect of cross-flow rate was examined by applying two cross-flow velocities (i.e., 8.5 and

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17 cm/s), both in the laminar flow regime.

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Figure 3a illustrates the water flux decline (expressed as normalized permeate flux) and

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permeate conductivity of the hydrophobic, hydrophilic, and slippery surface membranes obtained

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during MD scaling experiments at a low feed cross-flow velocity (8.5 cm/s). The hydrophobic

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and hydrophilic surface membranes exhibited similar flux decline behavior, with the hydrophilic

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membrane allowing for a slightly higher water recovery (~12.5%) before a rapid flux decline.

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With the sudden drop of permeate flux, we observed a sharp increase of permeate conductivity,

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which is attributable to the onset of scaling-induced pore wetting. 39 The slippery surface

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membrane outperformed both the hydrophobic and hydrophilic surface membranes by delaying

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both the decline in permeate water flux and increase of permeate conductivity. This observation

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clearly indicates that the MD membrane with an engineered slippery surface resists gypsum

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scaling better than those with hydrophobic and hydrophilic surfaces.

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FIGURE 3

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We further performed the gypsum scaling experiments at a higher feed cross-flow velocity

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(17 cm/s) to evaluate the effect of hydrodynamics on the scaling behavior of membranes with

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different degrees of surface wettability (Figure 3b). The high cross-flow velocity reduced the 10

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gypsum scaling potential of the hydrophobic and slippery surface membranes but not the

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hydrophilic surface membrane. The reduced gypsum scaling potential at a higher feed cross-flow

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velocity is attributed to better mixing, which in turn reduces the buildup of scale near the

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membrane surface.40 Interestingly, the gypsum scaling potential of the hydrophilic surface

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membrane is likely independent of the flow hydrodynamics as this membrane exhibits similar

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flux decline rate at the two different feed cross-flow velocities. The hydrophilic surface is

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expected to strongly attract the hydrated gypsum scalants to form a strong hydration layer by

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increasing hydrogen bonding interactions with water molecules.41 Once the gypsum scalants are

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deposited on the hydrophilic surface they are harder to remove by shear force (i.e., higher cross-

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flow) compared with the hydrophobic and slippery surfaces that provide lower interaction with

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the scalants.42 Thus, cross-flow velocity has less influence on sweeping away the deposited

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gypsum scalants from the hydrophilic surface membrane.

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To better understand the effect of surface wettability on gypsum scaling behaviors of MD

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membranes, we investigated the gypsum scalants formed on the membrane surface at two stages

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of scaling. The first is identified as the early stage of scaling, which occurs just before the flux

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started to decline (points b-1 and b-3 in Figure 4a), at approximately 150 mL cumulative

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permeate volume. The second is identified as the long-term stage which occurs when the

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permeate flux reached nearly zero and simultaneously the conductivity of the permeate began to

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rapidly increase (points b-2 and b-4 in Figure 4a). The membranes were taken out of the cell as is

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and examined under SEM. Figure 4b shows the SEM images of the membrane surface after each

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scaling experiment. The slippery surface membrane taken at the earlier scaling stage exhibited a

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clean surface without discernible nucleation of gypsum crystals (Figure 4b-3), while rosette-like

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embryo gypsum crystals were found on the hydrophobic surface membrane (Figure 4b-1), a

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manifestation of heterogeneous surface nucleation. 43, 44 SEM images of both the hydrophobic and

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slippery surface membranes obtained after long-term scaling experiments showed that the

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surfaces were substantially covered with needle-like crystals resulting from bulk deposition of

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gypsum scalants (Figures 4b-2 and 4b-4).45 The slippery surface membrane, however, achieved a

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higher water recovery compared to the hydrophobic surface membrane before a significant water

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flux decline appeared, suggesting a retardation of bulk crystal deposition on this membrane.

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Such an enhanced resistance to deposition of gypsum crystals further reduced the potential of 11

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pore wetting of the slippery surface membrane as demonstrated by the delay of conductivity

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increase in the permeate (Figure 4a). FIGURE 4

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Desalination Performance with a Blowdown Wastewater. We conducted DCMD

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experiments with a brine collected from the cooling tower at the Redhawk Power Station

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(Phoenix, AZ) to evaluate the desalination performance of the pristine hydrophobic and modified

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slippery surface membranes. Major composition and key properties of the prefiltered blowdown

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water are given in the Supporting Information (Table S1). Redhawk’s blowdown has a neutral

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pH (~7.1) and a high conductivity (23.9 mS/cm) attributed to the high concentrations of various

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inorganic salts. In particular, relatively high levels of calcium (620 mg/L) and sulfate (6390

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mg/L) were measured, implying that the blowdown water has a significant gypsum scaling

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potential.

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Flux decline curves expressed as normalized water flux and permeate conductivity as a

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function of water recovery were obtained from DCMD experiments with the Redhawk’s

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blowdown as the feed solution (Figure 5a). A rapid increase in permeate conductivity, which

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indicates a failure of MD desalination capacity by pore wetting, was observed at ~ 40% of water

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recovery for the hydrophobic surface membrane. At this point, the hydrophobic surface

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membrane experienced ~ 85% reduction in water flux compared to the initial performance

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(Figure 5a). In contrast, no substantial increase of permeate conductivity was observed for the

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slippery surface membrane until water recovery reached ~ 60%. Note that we were not able to

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continue DCMD experiments beyond this water recovery due to limitations of the experimental

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DCMC bench-scale setup. Nonetheless, the results demonstrate that membranes with an

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engineered slippery surface increase water recovery significantly compared to the conventional

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hydrophobic surface membrane in treatment of saline power plant blowdown with high-scaling

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potential.

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FIGURE 5

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To explain why the slippery surface membrane outperformed the hydrophobic surface

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membrane, SEM imaging (Figure S3) and SEM-EDS elemental mapping (Figure 5b) were

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conducted for the cross-section and top surface of the membranes after long-term scaling 12

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experiments with the blowdown wastewater. Only representative crystal elements expected to

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form on the membrane were examined. We also note that the green signal represents fluorine (F),

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which is the main elemental composition of the PVDF substrate. The SEM-EDS analysis showed

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high intensity of Na and Ca on the surface of the hydrophobic membrane (Figure 5b-2) possibly

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due to accumulation of Na2SO4 and CaSO4 crystals. We also detected a wide distribution of Na

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inside the pores of the hydrophobic surface membrane, which suggests membrane pore wetting.

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In contrast, the slippery surface membrane showed less crystal accumulation on the surface

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(Figure 5b-4) and very little presence of Na and Ca inside the pores (Figure 5b-3) compared to

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the hydrophobic surface membrane. This observation clearly demonstrates that the slippery

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surface membrane provides a higher resistance to scaling than the hydrophobic surface

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membrane, thereby allowing less crystal deposition on the surface as well as inside the pores

350

and, consequently, a lower potential for pore wetting.

351

Mechanism for Reduced Scaling with Slippery Surface. Classical nucleation theory

352

(CNT) explains the influence of surface properties on heterogeneous surface nucleation of

353

gypsum crystal based on the thermodynamic expression that describes the Gibbs free energy

354

required for the formation of spherical particles. 46 The Gibbs free energy, ∆G, of the forming

355

phase, assuming spherical nuclei of radius r and molecular volume υ, was calculated by an

356

energy balance between the sum of surface excess Gibbs free energy (positive) and volume

357

* excess Gibbs free energy (negative).47 The maximum Gibbs free energy, Ghomogeneous ,

358

corresponding to the energy barrier that must be overcome by the nuclei to form a crystal in the

359

bulk solution (also referred to as homogeneous nucleation) can be calculated using 48  G h*o m o geneo us 

  3 2 ( kT )

2

1 ln 2 S

(1)

360

where β is the surface geometrical factor (16π/3 for spheres), γ is the precipitate surface energy

361

(here CaSO4), υ is the molecular volume of the CaSO4 crystallizing phase, k is the Boltzmann

362

constant, T is the temperature, and S is the supersaturation index.49 The potential of

363

* by incorporating membrane heterogeneous surface nucleation can be deduced from Ghomogeneous

364

properties, including surface hydrophobicity and porosity, using the following equation: 50

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G

* heterogeneous

 G

* homogeneous

2  1  cos θ    2 1  2  4  2  cos θ 1  cos θ   1      1  cos θ  

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3

(2)

365

where θ is the apparent contact angle between the solution and membrane and ε is the membrane

366

surface porosity.

367

Figure 6a presents the calculated maximum Gibbs free energy of heterogeneous nucleation,

368

* Gheterogeneous , indicating that a membrane with higher hydrophobicity and lower surface porosity

369

provides a higher energetic barrier, which translates to lower scaling potential. We previously

370

observed a relatively clean surface with no discernible gypsum crystals on the slippery surface

371

membrane while the hydrophobic surface membrane showed sparse growth of rosette-like

372

embryo crystals at the earlier stage of scaling experiments (Figures 4b-1 and 4b-3). Provided that

373

reduction of the membrane surface porosity after a thin layer coating with relatively small SiNPs

374

(~ 8 nm) is insignificant, the obtained lower heterogeneous scaling potential of the slippery

375

surface membrane compared to the hydrophobic surface membrane is attributed to its higher

376

surface hydrophobicity (or lower surface energy shown in Figure 2a), which develops a larger

377

energetic barrier for surface gypsum crystallization.

378

FIGURE 6

379

Given the use of supersaturated gypsum feed solution (SI = 1.1) during DCMD experiments,

380

deposition of scalant crystals on the membrane surface (bulk deposition) is expected to be an

381

important mechanism governing MD membrane scaling behavior.51 Previous studies claim that a

382

rapid flux decline with concomitant increase in permeate conductivity during MD scaling

383

experiments are mainly attributed to bulk crystal deposition on the membrane surface followed

384

by pore wetting.52 Figure 6b illustrates the impact of surface wettability on the contact between

385

the gypsum crystals and the membrane surface. MD membranes with an engineered slippery

386

surface make minimal contact with the scaling solution due to their high surface hydrophobicity,

387

and thus allowing limited gypsum crystal deposition on the surface. The non-stick, slippery

388

surface nature (Figure 2b-3) further reduces the chance of crystal accumulation on these

389

membranes. In contrast, a moderately hydrophilic surface (i.e., water contact angle, θ, ~ 70º) and

390

a conventional hydrophobic surface (i.e., θ ~ 120º) form much more intimate contact with the

391

scaling solution compared to the slippery surface (i.e., water contact angle, θ is ~ 150º) (Figure 14

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392

6b), resulting in an increased probability of gypsum crystals deposition or heterogeneous

393

nucleation on the membrane surface.

394

In summary, we demonstrated the fabrication of MD membranes with an engineered slippery

395

surface that provides improved resistance to scaling. The modified slippery surface membrane

396

exhibited a stable MD performance with high water recovery of a supersaturated gypsum scaling

397

solution as well as brine from a power plant blowdown. Based on the results obtained, we

398

discussed the mechanisms responsible for the reduced scaling potential of the slippery surface

399

for further improvement of anti-scaling properties. MD membranes that are highly resistant to

400

scaling will be a critical component of a high recovery MD system for sustainable treatment of

401

hypersaline industrial wastewaters with minimal production of waste (brine) streams.

402

ASSOCIATED CONTENT

403

The Supporting Information is available free of charge on the ACS Publication website at DOI:

404

Composition and properties of power plant blowdown wastewater after pretreatment through an

405

11-μm filter (Table S1); Mechanical stability and SEM imaging of the PVDF and NaOH-treated

406

PVDF membrane (Figure S1); XPS survey spectra of the hydrophilic, hydrophobic, and slippery

407

surface membranes (Figure S2); Cross-section and top view SEM images of scaled membranes

408

taken after an experiment with an industrial blowdown wastewater (Figure S3);

409

ACKNOWLEGMENTS

410

This research was made possible by the postdoctoral fellowship (to Vasiliki Karanikola)

411

provided from the Agnese Nelms Haury Program in Environment and Social Justice and the

412

University of Arizona. We acknowledge the National Science Foundation (NSF) Graduate

413

Research Fellowship Program (GRFP) for the support to Julianne Rolf (Fellowship 2016227750).

414

Facilities used were supported by the Yale Institute of Nanoscale and Quantum Engineering

415

(YINQE). The author also thanks the assistance of Dr. Min Li (Yale West Campus Materials

416

Characterization Core) with the XPS measurements and SEM imaging. The characterization

417

facilities were supported by the Yale Institute for Yale West Campus Materials Characterization

418

Core (MCC).

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REFERENCES

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41. Tiraferri, A.; Kang, Y.; Giannelis, E. P.; Elimelech, M., Highly Hydrophilic Thin-Film Composite Forward Osmosis Membranes Functionalized with Surface-Tailored Nanoparticles. ACS Applied Materials & Interfaces 2012, 4, (9), 5044-5053. 42. Chen, L.; Thérien-Aubin, H.; Wong, M. C. Y.; Hoek, E. M. V.; Ober, C. K., Improved antifouling properties of polymer membranes using a ‘layer-by-layer’ mediated method. Journal of Materials Chemistry B 2013, 1, (41), 5651-5658. 43. Lee, S.; Lee, C.-H., Effect of operating conditions on CaSO4 scale formation mechanism in nanofiltration for water softening. Water Research 2000, 34, (15), 3854-3866. 44. Jawor, A.; Hoek, E. M. V., Effects of feed water temperature on inorganic fouling of brackish water RO membranes. Desalination 2009, 235, (1), 44-57. 45. Benecke, J.; Haas, M.; Baur, F.; Ernst, M., Investigating the development and reproducibility of heterogeneous gypsum scaling on reverse osmosis membranes using real-time membrane surface imaging. Desalination 2018, 428, 161-171. 46. Volmer, M.; Weber, Α., Keimbildung in übersättigten Gebilden. Zeitschrift für physikalische Chemie 1926, 119, (1), 277-301. 47. Clouet, E., Modeling of nucleation processes. arXiv preprint arXiv:1001.4131 2010. 48. Becker, R.; Döring, W., Kinetische behandlung der keimbildung in übersättigten dämpfen. Annalen der Physik 1935, 416, (8), 719-752. 49. Tröger, J.; Lunkwitz, K.; Bürger, W., Determination of the surface tension of microporous membranes using contact angle measurements. Journal of colloid and interface science 1997, 194, (2), 281-286. 50. Curcio, E.; Fontananova, E.; Di Profio, G.; Drioli, E., Influence of the structural properties of poly (vinylidene fluoride) membranes on the heterogeneous nucleation rate of protein crystals. The Journal of Physical Chemistry B 2006, 110, (25), 12438-12445. 51. Di Profio, G.; Curcio, E.; Drioli, E., Supersaturation Control and Heterogeneous Nucleation in Membrane Crystallizers: Facts and Perspectives. Industrial & Engineering Chemistry Research 2010, 49, (23), 11878-11889. 52. Gryta, M., Calcium sulphate scaling in membrane distillation process. Chemical Papers 2009, 63, (2), 146-151.

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(b)

(c)

(a) F

F

NH3+ NH3+ NH3+ NH3+

OH OH OH OH OH

OH OH OH OH OH

PVDF

PVDF

(i) Alkaline Treatment

(ii) APTES Grafting

Si O

Si O O Si O O

Si O

PVDF

(iii) SiNP Coating

PVDF

(vi) Slippery, NonAdhesive Surface

546 547 548 549 550 551 552 553 554 555 556 557 558

F FF FF FF FF F FF FF FF

F F F F F F F F Si

O

O

F

Si

F F F F FF F F F F F F F F

F F

O

F F

Membrane Cross-Section

F F F F

O

(d)

O

Tape

30 m

(e)

Hydrophobic Hydrophilic Slippery CF2CH2 CH2 CF2CF2

PVDF

(iv) 17 - FAS Coating

Si F

0.5 m

Si

CPS (a.u.)

SiNP

F F

CF3

(v) 17 – FAS Coating 295

290

285

280

Binding Energy (ev)

Figure 1. (a) Schematic illustrating the protocol of engineering a slippery surface of PVDF membrane. (i) The surface of a hydrophobic PVDF membrane is hydrolyzed by alkaline treatment with a 7.5 M NaOH solution. (ii) (3-Aminopropyl)triethoxysilane (APTES) is grafted on the hydrolyzed PVDF membrane surface. (iii) Negatively charged silica nanoparticles (SiNPs) bind electrostatically on the APTES functionalized PVDF membrane. (iv-v) SiNPs are covalently bound with (heptadecafluorotetrahydrodecyl)trichlorosilane (17–FAS) via vapor-phase silanization, creating (vi) a non-adhesive, slippery surface. (b) SEM top-down image of the SiNP-coated PVDF membrane. (c) SEM-EDS cross-section image of the SiNP-coated PVDF membrane, revealing a thin-layer SiNP surface coating. (d) XPS analysis of the hydrophobic PVDF membrane, SiNP-coated PVDF membrane (denoted as hydrophilic membrane), and modified slippery PVDF membrane. (e) Photograph of water droplet on the modified slippery PVDF membrane.

559 560

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0.05 s

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0.15 s

0.25 s

Water Contact Angle ()

(b-1) Hydrophobic

200

(a)

150

(b-2) Hydrophilic

100 50 0

(b-3) Slippery Hydrophobic Hydrophilic

Slippery

561 562 563 564 565

Figure 2. (a) Static contact angle of hydrophobic, hydrophilic, and slippery surface PVDF membranes measured with a 5-μL DI water droplet placed on the sample surface. (b) Dynamic surface wettability of the membranes evaluated by dispensing a 10-L DI water droplet from a syringe at a 4-cm height and recording the motion of the water droplet with time.

566

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Permeate Normalized Conductivity (S) Water Flux (J /J0)

(a) Low Cross-Flow Velocity 1.0 0.8 0.6

Hydrophobic Hydrophilic Slippery

0.4 0.2 0.0 100 80 60 40 20 0 0

567

50

100

150

200

250

300

350

Cumulative Permeate Volume (mL)

Normalized Permeate Conductivity (S) Water Flux (J /J0)

(b) High Cross-Flow Velocity 1.0 0.8 0.6

Hydrophobic Hydrophilic Slippery

0.4 0.2 0.0 100 80 60 40 20 0 0

568 569 570 571 572 573 574 575 576 577

50

100

150

200

250

300

350

Cumulative Permeate Volume (mL)

Figure 3. Normalized water flux and permeate conductivity of the hydrophobic, hydrophilic, and slippery surface PVDF membranes obtained during MD scaling experiments at (a) low feed cross-flow velocity (8.5 cm/s) and (b) high feed cross-flow velocity (17 cm/s). The feed solution contained 20 mM CaCl2 and 20 mM Na2SO4, with a gypsum (CaSO4·2H2O) saturation index (SI) of 1.1, pH 7.08, and temperature of 60 °C. An initial volume of 1 L was employed for both feed and permeate solutions. Temperature of permeate solution was maintained at 20 °C. The average initial water flux was 18.0, 18.5, and 14.0 L m−2 h−1 at a low feed cross-flow velocity and 21.0, 22.6, and 15.5 L m−2 h−1 at a high feed cross-flow velocity for the hydrophobic, hydrophilic, and the slippery surface membranes, respectively.

578

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(b-1) Hydrophobic at 150 mL (b-2) Hydrophobic ‒ Long-term

Permeate Normalized Conductivity (S) Water Flux (J /J0)

(a) Low Cross-Flow Velocity

50 m

0.8

(b-3)

0.6 0.4 0.2 0.0

580 581 582 583 584 585 586 587 588 589

500 m

(b-4)

(b-2)

(b-3) Slippery at 150 mL

Hydrophobic - Long-term Hydrophobic - Early Terminated Slippery - Long-term Slippery - Early Terminated

100 80 60

500 m

(b-4) Slippery ‒ Long-term High 50 m

40 20 0 0

579

High

(b-1)

1.0

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50

100

150

200

250

300

350

500 m

500 m

Cumulative Permeate Volume (mL)

Figure 4. (a) Normalized water flux and permeate conductivity of hydrophobic and slippery surface PVDF membranes obtained during scaling experiments at low feed cross-flow velocity (8.5 cm/s). The feed solution contained 20 mM CaCl2 and 20 mM Na2SO4, with a gypsum (CaSO4·2H2O) saturation index (SI) of 1.1, pH 7.08, and temperature of 60 °C. The average initial water flux under these conditions was 18.0 and 14.0 L m −2 h−1 for the hydrophobic and the slippery surface membranes, respectively. Long-term scaling experiments were conducted until a significant decline in permeate flux was observed. Independent scaling experiments were conducted until the cumulative permeate volume reached 150 mL (indicated as ‘Early Terminated’). (b) SEM images of the membrane surface after long-term and early terminated gypsum scaling experiments.

590

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(b-1) Hydrophobic – Cross-Section (b-2) Hydrophobic – Top View

Permeate Normalized Conductivity (S) Water Flux (J / J0)

(a) Blowdown Wastewater 1.0 0.8 0.6 0.4

PVDF Membrane

0.2

Na

0.0 80

592 593 594 595 596 597 598 599

F

40 m

Na

Ca

F

100 m

(b-4) Slippery – Top View

60 40 20 0 0

591

Si

(b-3) Slippery – Cross-Section

Hydrophobic Slippery

100

Ca

10

20

30

40

50

Water Recovery (%)

60

PVDF Membrane Na

Ca

Si

F

40 m

Na

Ca

F

100 m

Figure 5. (a) Normalized water flux and permeate conductivity of the hydrophobic and slippery surface PVDF membranes as a function of water recovery obtained during DCMD experiments with an industrial blowdown wastewater. Feed cross-flow velocity of 8.5 cm/s and temperature of 60 °C were employed. The average initial water flux under these conditions was 18.0 and 10.7 L m−2 h−1 for the hydrophobic and the slippery surface membranes, respectively. (b) Images of SEM-EDS elemental mapping for cross-section and top surface of the scaled membranes after DCMD experiments with the blowdown wastewater. Chemical composition of the blowdown wastewater is presented in Table S1.

600 601 602 603 604 605 606 607 608 609 610 611 23

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(a) Heterogeneous Nucleation

Contact Angle ()

160

Gibbs Free Energy (G, mJ mol-1)

150 140 130 120 110 100

0.2

0.4

0.6

0.8

1.0

35 31 28 25 21 18 14 11 7 4 0

Porosity 612 613 614 615 616 617

Figure 6. (a) Gibbs free energy of gypsum crystals (CaSO 4·2H2O) as a function of surface porosity and contact angle which corresponds to the energy that the gypsum crystal must overcome to start forming heterogeneous crystallization on a surface (calculated based on classical nucleation theory). (b) A diagram illustrating the effect of surface wettability on gypsum crystal deposition on the MD membrane. θ1, θ2, and θ3 indicate the static water contact angles of the hydrophilic, hydrophobic, and slippery surface membranes measured in Figure 2a.

618 619 620 621 622 623 624 625 626 627 628 629

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