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Impaired Performance of Pressure-Retarded Osmosis due to Irreversible Biofouling Edo Bar-Zeev, François Perreault, Anthony P. Straub, and Menachem Elimelech Environ. Sci. Technol., Just Accepted Manuscript • DOI: 10.1021/acs.est.5b03523 • Publication Date (Web): 01 Oct 2015 Downloaded from http://pubs.acs.org on October 9, 2015
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Environmental Science & Technology
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Impaired Performance of Pressure-Retarded
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Osmosis due to Irreversible Biofouling
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Environmental Science & Technology
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Revised: September 26, 2015
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Edo Bar-Zeev1*, François Perreault2, Anthony P. Straub3, and Menachem
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Elimelech3
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Department of Environmental Hydrology & Microbiology, Zuckerberg Institute for Water Research (ZIWR), Ben-Gurion University of the Negev, Israel.
School of Sustainable Engineering and the Built Environment, Arizona State University, Tempe, AZ, 85287. 3
Department of Chemical and Environmental Engineering, Yale University, New Haven, Connecticut 06520-8286.
*Corresponding author; Address: Ben-Gurion University, Sade Boker, 8499000, Israel email:
[email protected] 1 ACS Paragon Plus Environment
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ABSTRACT
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Next-generation pressure-retarded osmosis (PRO) approaches aim to harness the energy potential 32
of streams with high salinity differences, such as wastewater effluent and seawater desalination 33
plant brine. In this study, we evaluated biofouling propensity in PRO. Bench-scale experiments 34
were carried out for 24 hours using a model wastewater effluent feed solution and simulated 35
seawater desalination brine pressurized to 24 bar. For biofouling tests, wastewater effluent was 36
inoculated with Pseudomonas aeruginosa and artificial seawater desalination plant brine was 37
seeded with Pseudoalteromonas atlantica. Our results indicate that biological growth in the feed 38
wastewater stream channel severely fouled both the membrane support layer and feed spacer, 39
resulting in ~50% water flux decline. We also observed an increase in the pumping pressure 40
required to force water through the spacer-filled feed channel, with pressure drop increasing 41
from 5 to 17 bar m-1 due to spacer blockage from the developing biofilm. Neither the water flux
42
decline nor the increased pressure drop in the feed channel could be reversed using a pressure43
aided osmotic backwash. In contrast, biofouling in the seawater brine draw channel was 44
negligible. Overall, the reduced performance due to water flux decline and increased pumping 45
energy requirements from spacer blockage highlight the serious challenges of using high fouling 46
potential feed sources in PRO, such as secondary wastewater effluent. We conclude that PRO 47
power generation using wastewater effluent and seawater desalination plant brine may become 48
possible only with rigorous pretreatment or new spacer and membrane designs. 49
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INTRODUCTION
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Global climate change due to increasing carbon dioxide emissions has led scientists to seek
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new, sustainable energy sources with a low carbon footprint. Capitalizing on the chemical
59
potential released when mixing two streams of different salt concentrations, researchers have
60
recognized salinity gradient energy as a promising renewable energy source
61
potential to provide up to 13% of global electricity requirements 3.
62
1,2
with the
Salinity gradient energy can be extracted by several different processes, such as pressure4–6
, and capacitive mixing
9,10
retarded osmosis (PRO)
64
PRO is well studied
65
PRO technology generates power by using an osmotic pressure difference across a
66
semipermeable membrane to produce a flux of water from a low concentration feed solution to
67
a high concentration draw solution. The expanding volume of the draw solution can be
68
restricted to create hydraulic pressure and drive a hydro-turbine.
5,11–13
, reverse electrodialysis
7,8
63
. Of these,
and considered promising in terms of both efficiency and cost
14,15
.
69
Studies of PRO technology focused primarily on harnessing the energy released from
70
mixing fresh river water and saline seawater. However, it was recently shown that
71
river/seawater pairing might not be feasible due to the relatively low theoretical extractable
72
energy and other challenges such as pumping costs, non-ideal membranes, and pretreatment
73
requirements 16–18. Instead, alternative salinity combinations, such as seawater reverse osmosis
74
(SWRO) brine mixing with wastewater effluent or hypersaline Great Salt Lake water mixing
75
with river water, were suggested to yield greater specific energies of up to 2.26 kWh per cubic
76
meter of total source water used 19.
77
Mixing SWRO brine with wastewater effluent in PRO appears especially promising due to
78
several factors. First, the osmotic pressure difference (∆π) is twice that of the river water and
79
seawater solution pairing, hence doubling the maximum obtainable specific energy to a value
80
of 0.551 kWh m-3
81
reducing adverse impacts once the brine is discharged into the aquatic environment. Third,
82
various trace contaminates that pass the secondary wastewater treatment stage will be retained
83
by the PRO membrane and thus will avoid discharge to the environment.
19
. Second, the SWRO brine is diluted during the PRO process, thus
84
One possible hurdle associated with the use of wastewater effluent as a feed source is
85
membrane fouling, which is known to be detrimental to system performance and shortens the 4 ACS Paragon Plus Environment
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membrane life. It was recently demonstrated that fouling with inorganic matter
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organic matter
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water flux in bench-scale PRO setups. However, these studies have suggested that inorganic
89
and organic fouling were reversibly attached and could be partially cleaned by osmotic
90
backwashing, resulting in permeate water flux recovery of 50% to 63% 18,23.
18,22,23
24,25
, and other organic foulants
, natural
resulted in severe decline in permeate
91
In fully operational PRO systems, feed water will always comprise a combination of
92
microbial, organic, and inorganic foulants that will cause biofouling, a phenomenon that can
93
cripple membrane performance and lifetime
94
clusters of live and dead bacterial cells encased in self-produced extracellular polymeric
95
substances (EPS), primarily composed of polysaccharides and proteins
96
biofilms are notoriously resistant to removal by chemical and physical treatments due to the
97
protection provided by the EPS matrix 32. Despite the ubiquitous nature of biofouling and the
98
detrimental effect of biological fouling on membrane performance, no study has yet explored
99
the effects of microbial fouling on PRO feasibility.
26–28
. Biofilm is typically found as multilayered 29–31
. Once established,
100
In the present study, we explore the efficiency and practicability of PRO under biofouling
101
conditions using synthetic wastewater effluent and SWRO-brine pairing. Our results indicate
102
that biofouling was irreversibly attached to the feed channel spacers and throughout the
103
membrane support structure, severely impairing membrane performance. We further provide
104
new insights on the implications of pairing wastewater effluent with SWRO-brine for PRO
105
system operation and viability.
106 107
MATERIALS AND METHODS
108
Lab-Scale PRO Setup, Membranes, and Spacers. Experiments were conducted in a
109
bench-scale PRO setup (Figure S1), with commercial flat-sheet TFC forward osmosis
110
membranes, obtained from Hydration Technology Innovations (Albany, OR). The permeate
111
flow rate, temperature, and conductivity were automatically recorded in real time. Both the
112
feed and draw channels were 10.7 cm long and 3.6 cm wide, with a smaller 9.9 cm by 3.4 cm
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section of the membrane exposed. The feed and draw channel heights were 0.5 and 1 mm,
114
respectively, to mimic a membrane module design. Figure 1 presents the spacers and
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membrane orientation in the cell: the feed channel was filled with two fabric spacers (Sp1 and
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Sp2), each 0.225 mm thick (Hornwood, Gloversville, NY), while the draw channel was filled
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with a ~1 mm thick plastic spacer (Sp3). The draw solution flow rate was maintained at 0.4 L
118
min-1 and the feed solution flow rate was initially set to 0.04 L min-1. Both initial flow rates
119
were set to allow for suitable hydrodynamic mixing without incurring excessive frictional
120
pressure losses along the membrane channel 33.
121
Figure 1.
122
Media and Bacterial Strains. Ten liters of artificial sterile wastewater secondary effluent
123
(hereafter WW) was used as feed solution (recipe modified from Glueckstern et al.
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supplemented with 0.01 % D-glucose as additional carbon source. Pseudomonas aeruginosa
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(ATCC® 27853TM) monoculture was used as a model biofilm strain in all WW biofouling
126
experiments.
127
34
)
Assuming a 50% recovery 35, SWRO brine solution (10 L) was made by doubling artificial 36
128
seawater (F2) concentration
. SWRO-brine was supplemented with 0.005 % D-glucose as
129
additional carbon source. Pseudoalteromonas atlantica (ATCC® BAA-1087) monoculture was
130
used as a model biofilm strain in the SWRO-brine (draw) biofouling runs. A detailed
131
description of the WW and SWRO-brine recipes as well as growing conditions of both model
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bacteria strains is available in the Supporting Information.
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Biofouling Experiments. The membrane and spacers were fitted into the PRO unit after
134
an extensive cleaning procedure that included circulating 10% bleach and 95% ethanol through
135
the system for one hour. The system was then stabilized at a zero permeate water flux with DI
136
water in both the feed and draw reservoirs (2 L and 10 L volumes, respectively). After
137
increasing the hydraulic pressure to 26.2 bar, the draw reservoir was supplemented with 5 M
138
NaCl to reach a final concentration of 50 mM, and salt rejection (> 96%) was evaluated to
139
verify membrane integrity. The draw solution was then replaced with 10 L of synthetic SWRO-
140
brine (excluding D-glucose) and the feed solution was replaced with 10 L of artificial WW
141
(excluding sodium citrate and D-glucose). The osmotic pressure difference (∆π) between the
142
solutions was 59.9 bar, calculated using OLI software. Once initial permeate water flux was
143
stabilized at 12 ± 2 L m-2 h-1, a baseline was collected for 24 hours to determine the decrease in
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water flux due solely to dilution of the draw solution and concentration of the feed reservoir as
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water and salt diffuse across the membrane.
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At the conclusion of the baseline run, both the feed and draw were replaced with 10 L of
147
fresh WW or SWRO brine solutions, while maintaining the hydraulic pressure (26.2 bar). Prior
148
to addition, late exponential stage P. aeruginosa and P. atlantica (OD600 of 0.6-0.8) were
149
centrifuged for 20 minutes at 4,000 rpm and 4 °C to remove the Lysogeny broth (LB) or
150
marine broth (MB). Cells were re-suspended in 10 mL of sterile WW (for P. aeruginosa) or
151
seawater (for P. atlantica) by vortexing for 30 seconds.
152
Two feed biofouling experiments were carried for ~24 hours by inoculating the feed WW
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reservoir with P. aeruginosa to achieve an initial bacterial concentration of ~2.4 × 106 cells
154
mL-1. WW was then supplemented with 0.01% D-glucose. Two draw solution biofouling runs
155
were carried for ~24 hours by inoculating the reservoir with P. atlantica to achieve an initial
156
bacterial concentration of ~3.7 × 106 cells mL-1. D-glucose (0.005%) was then added to the
157
SWRO brine draw solution.
158
Pressure drop across the feed channel, permeate water flux, temperature, and conductivity
159
were measured continuously throughout the experiments. Feed and draw water sub-samples
160
(50 mL) were routinely collected (every 6 to 8 hours) to monitor pH, conductivity, and
161
bacterial concentration (via plate counts and OD600 measurements). The pH and the
162
temperature of the feed (7.3 ± 0.3, 25 ± 0.5 °C) and draw (8.13 ± 0.02, 25 ± 0.5 °C) reservoirs
163
were kept constant. Bacteria and nutrient concentrations used in this study were in the range
164
reported for secondary wastewater effluents from wastewater treatment facilities 34,37
165
PA-OBW Procedure. Two pressure-aided osmotic backwash (PA-OBW) experiments
166
were performed to test biofouling reversibility and cleaning efficiency (Figure S2). PA-OBW
167
experiments were initiated after the feed channel was inoculated and fouled with P. aeruginosa
168
for ~20 hours as described earlier. After fouling, PA-OBW was carried out by switching the
169
WW feed reservoir with SWRO brine (1.2 M NaCl) and the draw reservoir to DI water while
170
maintaining the hydraulic pressure, ∆P, of 26.2 bar (Figure S2).
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hydraulic pressure differences both driving flow from the draw to the feed reservoir, the PA-
172
OBW produced a reverse water flux of 32 ± 4 L m-2 h-1 for 60 min. PA-OBW was terminated
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by replacing both the feed and draw reservoirs with the initial configuration (WW and SWRO
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brine, respectively) for 1 hour.
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Biofilm Characterization with CLSM. Biofilm biovolume and morphology were
176
determined using confocal laser scanning electron microscopy (CLSM). At the end of the
177
experimental run, a central section (1 cm × 1 cm) was cut from the membrane coupon as well
178
as the draw or feed spacers (Sp1 and Sp3, respectively). Sub-samples were then imaged and
179
analyzed in a custom made biofilm in vivo characterization chamber according to Bar-Zeev et
180
al., 2014 38. Further details of the CLSM sample preparation, staining, and image analysis are
181
available in the Supporting Information.
182
SEM and TEM Analysis. Scanning electron microscopy (SEM) and transmission
183
electron microscopy (TEM) were used to further understand the extent of biofilm formation.
184
Membrane and spacer samples were cut and fixed in a 1.5 mL eppendorf with a Karnovsky
185
fixative solution (2% paraformaldehyde, 2.5% glutaraldehyde in 0.2 M Sorenson’s buffer, pH
186
7.2) overnight at 4 °C. After fixation, samples were stained with osmium tetroxide and
187
sequentially dehydrated. Samples were then freeze fractured in liquid nitrogen, and imaged
188
with an Hitachi SU-70 SEM (Hitachi High Technologies America, Inc. Clarksburg, MD).
189
For TEM imaging, dried samples were infiltrated with epoxy resin (Embed 812, Electron
190
Microscopy Sciences, Hatfield, PA) at room temperature. Embedded samples were cut into
191
0.07 µm thick slices and imaged with an FEI Tecnai Osiris microscope, operating at an
192
acceleration voltage of 200 kV. Energy dispersive X-ray spectroscopy elemental mapping was
193
performed in scanning TEM mode (STEM-EDX) with 10 cycles compiled per image.
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Bacterial Cell Counts. Membrane or spacers (Sp1, Sp2, and Sp3) sub-sections were re-
195
suspended in 1.5 mL eppendorf tubes with 1 mL sterile WW for the feed and F2 for the draw
196
samples
197
(AQUASONIC, PA, USA) for 5 minutes to remove cells from the surface, plated on LB or MB
198
agar plates, and incubated for 24 hours at 37 °C (feed samples) and 26 °C (draw samples).
199
Bacteria abundance was determined by counting colony forming units (CFU) and normalized
200
by the sample area.
to
maintain
experimental
conditions.
Samples
were
then
bath-sonicated
201
Protein Assay. Membrane or spacer sub-sections were re-suspended in 1.5 mL
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sucrose, 0.1% 3-[(3-cholamidopropyl)-dimethylammonio]-1 propanesulfonate, and 10 mM
204
dithiothreitol). Samples were then probe sonicated on ice (two 30-second cycles) using an
205
ultra-cell disruptor (MISONIX Inc. NY, USA). Cell extracts were centrifuged at 12,000 rpm
206
for 10 minutes, and supernatant was collected for protein quantification (BCA Protein Assay
207
Kit, Thermo Scientific, Rockford, IL, USA). Protein concentrations were normalized according
208
to the sample area.
209
TOC Analysis. For total organic carbon (TOC) analysis, membrane or spacer sub-
210
sections were placed in acid-cleaned glass vials and resuspended in 20 mL DI water with 40
211
µL of 1 M HCl. Samples were probe-sonicated (two 30 second cycles) using an ultra-cell
212
disruptor (MISONIX Inc. NY, USA) to remove all the cells from the surface. Total organic
213
carbon was then analyzed using a TOC analyzer (TOC-V, Shimadzu Corp., Japan) and
214
normalized according to the sample area.
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RESULTS AND DISCUSSION
217
Effect of Biofouling on PRO Performance. In our bench-scale PRO system, an initial
218
permeate water flux of 13.1 ± 1.8 L m-2 h-1 was achieved by the osmotic pressure difference
219
(∆π = 59.9 bar), which was opposed by the applied hydraulic pressure (∆P = 26.2 bar) in the
220
draw channel (Figure 1). Prior to each biofouling run, the membrane active layer properties,
221
structural parameter, and draw channel mass transfer coefficient were determined. All our
222
experiments showed consistent values for these parameters, with an average water permeability
223
coefficient, A, of 3.71 ± 0.14 L m-2 h-1 bar-1; salt permeability coefficient, B, of 1.20 ± 0.12 L
224
m-2 h-1; structural parameter, S, of 627 ± 124 µm; and draw mass transfer coefficient, k, of 11.3
225
± 1.2 µm s-1. A detailed description of the methodology used to determine these values is
226
available in the Supporting Information. Using these initial operating parameters, the
227
performance of PRO under biofouling conditions was evaluated over 24 hours by
228
independently inoculating the feed or draw streams with either P. aeruginosa (WW feed) or P.
229
atlantica (SWRO-brine draw), respectively.
230
Inoculating the WW feed solution with P. aeruginosa (1.6 to 3.4 ×106 cells mL-1) induced a
231
permeate water flux decline 3 hours after the addition of bacteria, which corresponded to a 9 ACS Paragon Plus Environment
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normalized cumulative permeate volume of ~36 L m-2 (Figure 2A). A sharp decrease in
233
permeate water flux (~50%) occurred for 8 hours after the initial fouling event. In the final 11
234
hours of the experiment, permeate water flux remained relatively constant, and was 6 ± 0.9 L
235
m-2 h-1 at the end of the ~24 hour run (Figure 2A). Throughout the experiment, bacterial
236
concentration in the WW reservoir increased, reaching a final value of ~1.9 × 107 cells mL-1 Figure 2.
237 238
We attribute the permeate water flux decline during the biofouling experiments on the feed
239
side of the membrane to three factors: (i) biofilm development within the feed channel, across
240
the spacers (Sp1 and Sp2), and on the membrane support surface, resulting in cake-enhanced
241
concentration polarization; (ii) internal biofilm formation within the membrane support layer,
242
leading to increased internal concentration polarization, and (iii) biofilm growth at the active
243
layer−support interface, which increases the hydraulic resistance of the membrane 23.
244
In addition to the reduction in permeate water flux, biofouling in the feed spacers resulted
245
in decreased cross flow rate and increased pressure loss along the feed channel (Table S1). In
246
all experiments, the cross flow rate through the feed channel spacers (Sp1 and Sp2) was
247
initially set at 0.038 ± 0.005 L min-1 and decreased to 0.013 ± 0.004 L min-1 at the end of the
248
biofouling experiment. Normalized pressure drop along the feed channel amounted to 6.4 ± 0.8
249
bar m-1 at the start of the biofouling experiment and increasing by 84% over the course of the
250
run, resulting in a normalized feed channel pressure loss of 11.7 ± 0.2 bar m-1. This dramatic
251
increase in the feed channel pressure loss is due to the accumulation of a dense biofilm within
252
the fabric feed spacer.
253
Unlike results in the feed channel, inoculating the SWRO brine draw solution with P.
254
atlantica (1.4 to 6.0 ×106 cells mL-1) did not lead to any change of permeate water flux (Figure
255
2B). Moreover, no pressure drop was measured along the draw channel and the flow rate
256
through the draw channel spacer (Sp3) remained constant at 0.4 L min-1. We suggest that the
257
convective permeate water flux (from the support surface to the active layer side) transports
258
foulants and bacteria away from the membrane surface, thereby limiting deposition and
259
hindering the development of biofouling. Additionally, we surmise that the hypersaline (1.2 M
260
NaCl) environment restricted both bacterial growth in the SWRO-brine stream, which was
261
reduced to 3.4 ± 1.4 × 104 cells mL-1at the end of the run, and biofilm development on the 10 ACS Paragon Plus Environment
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active layer surface. However, it is possible that longer exposure of the membrane surface to
263
natural SWRO-brine will result in biofilm development by various halophilic microorganisms,
264
such as protobacteria and archaea 39,40.
265
Biofilm Development and Characteristics in PRO. Overall, PRO experimental
266
measurements indicated extensive biofouling of the fabric spacers and the TFC membrane
267
structure on the WW feed side. However, minimal changes were observed after fouling along
268
the spacer (Sp3) or membrane active layer on the SWRO brine draw side. We further probed
269
biofilm formation in the system using microscopic imaging and biofilm characterization
270
techniques.
271
In the fabric spacers that filled the feed channel, biofilm was found, by SEM imaging, to be
272
clogging openings between the spacer fibers (Figures 3A, B). CLSM imaging confirmed that
273
these large clusters—hundreds of micrometers in length—were composed of both live cells
274
and EPS-polysaccharides (Figure 4A).
275
Biofilm was also observed on the membrane support surface, which faces the wastewater
276
feed stream. SEM (Figures 3C, 3D) and CLSM (Figure 4B) images showed biofilm on the
277
surface of the membrane support, primarily around the openings of the exposed polyester
278
mesh. CLSM image analysis indicated that the average biofilm thickness was 60 ± 7.1 µm,
279
while biovolume was 35.7 ± 6.8 µm3 µm-2 (biovolume was calculated as the sum of live/dead
280
cells and EPS-polysaccharides). However, large biofilm structures (a few hundreds of
281
micrometers thick) were often captured above the membrane support surface (Figure 4B),
282
indicating that biofilm was interlocked with the overlying spacer (Sp1).
283
The permeating flow of water into the support layer led to biofilm formation inside open
284
voids on the surface of the membrane. Polysaccharides were found along the membrane
285
support layer surface as well as in funnel-shaped structures within openings in the support
286
layer that formed around the polyester mesh during fabrication (Figure S3). In addition, dense
287
biofilm was observed attached in voids beneath the support surface (Figure 3E).
288
Figure 3
289
Figure 4
290
Growth of cells was also observed far within the fingerlike polysulfone support layer
291
(Figure 3F). TEM images of the support layer cross-section, complemented with EDX 11 ACS Paragon Plus Environment
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elemental mapping, confirmed the presence of bacteria in voids throughout the support
293
structure (Figure 5). Cells were typically found as small clusters within the fingerlike
294
polysulfone matrix, as close as ~200 nm from the active layer (Figure 5). We conclude that the
295
development of biofilm within the membrane structure resulted from continuous flow of WW
296
feed through breaches in the support surface facilitating nutrient (e.g. polysaccharides)
297
transport as well as bacterial deposition and growth.
298
Figure 5
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Biofilm biomass developed on the membrane and spacers was also analyzed by
300
determining cell, TOC, and protein coverage as well as biofilm biovolume (Figure 6).
301
Throughout feed spacers Sp1 and Sp2, cell coverages were respectively four- and two-fold
302
higher than on the TFC membrane (Figure 6A). The extensive cell proliferation in the spacers
303
may have resulted from favorable growth conditions, such as high nutrient levels and a well-
304
oxygenated environment
305
biomass, measured as TOC and proteins, between the feed spacers and membrane structure
306
(Figures 6B and 6C). We surmise that the discrepancy between the spacers and membrane with
307
respect to cell coverage (higher coverage on the spacers) and biofilm biomass (proteins and
308
TOC similar in both spacers and membrane) is attributable to the yield in extracting the
309
biomass for analysis. Specifically, cells remained attached within the membrane support
310
structure, while TOC and proteins, for which a stronger cell-disrupting sonication treatment
311
was used, were completely removed from the membrane.
312
29,41,42
. However, no significant difference was detected in biofilm
Figure 6
313
In contrast to the feed channel, no viable cells were found attached to the draw spacer (Sp3)
314
or the surface of the membrane active layer (Figures 6A, 6D, and S4). The absence of cells on
315
the draw spacer and active layer is attributed to the outward convective permeate water flux
316
and to induced osmotic stress by the hypersaline SWRO-brine solution, hindering P. atlantica
317
growth. In addition, the adsorbed biomass (TOC and proteins) extracted from the draw spacer
318
and membrane active layer was ~80% lower than the amount found in the feed channel
319
(Figures 6B and 6C). The lower fouling propensity in the draw channel is in agreement with
320
previous studies of organic fouling propensity in PRO18.
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Membrane Orientation is the Culprit for Severe Biofouling in PRO. The
322
substantially greater biofilm accumulation on the feed side, as evidenced by the marked water
323
flux decline and biofilm accumulation, is a direct consequence of the membrane orientation in
324
PRO. Since the porous support layer faces the WW feed stream with high organic and bacteria
325
concentrations (Figure 1), the flow of WW in the feed channel continuously carries dissolved
326
nutrients and bacterial cells to the spacers, membrane surface, and membrane support layer.
327
We suggest that proliferation of cell clusters and EPS secretions within the membrane support
328
structure may lead to irreversible biofilm attachment. Moreover, it is highly likely that
329
continuous production of EPS will gradually accumulate at the membrane support−active layer
330
interface and further hinder permeate flux, as previously suggested for organic fouling
331
Therefore, we estimate that, in PRO systems using treated WW effluent as feed, biofouling
332
proliferation inside the support structure will cause detrimental effects to membrane
333
performance over short (days to weeks) time scales.
22
.
334
Minimizing cell attachment on the TFC membrane support surface and preventing bacteria
335
from colonizing the polysulfone structure was attempted by reversing the membrane
336
orientation, with the active layer facing the WW feed solution rather than the SWRO brine.
337
However, membrane failure was recorded at 6.9 bar, indicated by a rapid increase in reverse
338
salt flux and water flux, most probably due to the delamination of the active layer.
339
Is Biofouling Reversible? Pressure-aided osmotic backwashing (PA-OBW) was carried
340
out to physically disperse biofouling from the membrane and spacer by reversing the permeate
341
water flow direction
342
and permeate water flux was reduced by 50% (Figure 7A). PA-OBW was initiated through a
343
reversal of the osmotic driving force by exchanging the draw solution with deionized water and
344
the feed solution with model SWRO brine, while maintaining a constant ∆P of 26.2 bar (Figure
345
S2). Reverse water flux during PA-OBW (from the active layer side to the porous support side)
346
was 32 ± 4 L m-2 h-1 and remained constant for 60 min (Figure 7B).
347
18,23,43,44
. We applied PA-OBW after the PRO membrane was biofouled
Figure 7
348
The intensive PA-OBW resulted in low (12%) permeate water flux recovery (Figure 7A)
349
and no significant change in the feed channel pressure drop (Table S1). Overall, the surface of
350
the spacers (Figure S5) and membrane support were cleaner following the PA-OBW as 13 ACS Paragon Plus Environment
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351
indicated by a reduction in cell, TOC, protein coverage, and total biovolume (Table 1). In
352
addition to a reduction in cell biovolume after PA-OBW, there were 36% more dead cells than
353
live cells on the membrane surface and the feed (Sp1) spacer (Table 1, Figure S6). We attribute
354
the high dead to live cell ratio to an osmotic shock to bacteria induced by the highly saline
355
solution 45. Table 1
356 357
However, PA-OBW was only effective for the outermost layers of the biofilm, and no
358
change was found in the distribution of biofilm within the support layer after the 60-minute
359
PA-OBW (Figure S7). Biofilm was irreversibly attached within the polysulfone support matrix,
360
and sporadic bacterial cells remained in the finger-like structure (Figures S7 E and F). In
361
addition to bacterial cells, organic fouling, such as EPS, also remained trapped within the
362
support layer, even after rigorous backwash (Table 1).
363
It has been recently reported that organic fouling in PRO resulted in 30% to 46% permeate
364
flux decline, while various backwashing procedures recovered significant percentage (50-63%)
365
of the water flux, suggesting that organic fouling was in part reversible
366
biofouling can be partially removed from the feed spacer and the membrane support surface by
367
PA-OBW. However, biofilm and EPS as well as bacterial cells remain irreversibly confined
368
within the polysulfone support layer. We attribute the limited recovery of permeate water flux
369
(12%) following PA-OBW to the detrimental effects of biofilm that remained irreversibly
370
attached to the membrane support structure.
18,23
. We show that
371
Surprisingly, although feed spacers appeared cleaner following PA-OBW (Figure S5),
372
pressure drop along the feed channel was not significantly different (Table S1). We suggest
373
that the recorded pressure drop along the feed channel may be the result of biofilm residues
374
blocking micro-channels within the spacers, thus retaining the overall hydraulic resistance.
375
Feasibility of PRO using Wastewater and SWRO-Brine. Compared to river and
376
seawater pairing in PRO, harnessing the energy of mixing WW and SWRO-brine for power
377
production has been conceived as more viable due to the increased extractable energy 46–48. The
378
promise of this system configuration was further emphasized by the high reversibility of
379
organic and inorganic fouling observed in PRO, with 50% to 63% permeate flux recovery
380
following OBW 18,23.
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381
Our present work conducted with model WW, simulated SWRO-brine, and live bacteria
382
indicates that significant irreversible biofouling along the feed channel and within the TFC
383
membrane support layer causes (i) 50% permeate water flux decline and (ii) severe pressure
384
drop along the feed channel (up to 17 bar m-1). A rigorous PA-OBW cleaning procedure was
385
only able to recover 12% of the permeate water flux and could not lessen the feed channel
386
pressure drop.
387
The amount of energy extractable from a PRO module is proportional to the applied
388
hydraulic pressure, ∆P, multiplied by the water flow rate across the membrane 19. Hence, the
389
50% reduction in water flux of the fouled membrane will cause a correspondingly reduced
390
power output and require a PRO system with significantly larger membrane area 49. Both these
391
effects would significantly reduce the feasibility of the process.
392
The effect of biofouling will extend beyond reducing the water flux across the membrane
393
module; it will also necessitate a higher energy input into the system. At the end of the feed
394
fouling tests, we observed a dramatic increase in pressure loss across the feed channel,
395
reaching values up to 17 bar m-1 as compared to 6.4 bar m-1 at the beginning of the
396
run. Pressurizing the feed solution before it enters the membrane module represents a
397
substantial energy cost
398
pumped in at 17 bar, while the energy extractable from the system would come from the flow
399
rate permeating across the membrane entering at turbine at 26.2 bar. Since the flow rate
400
entering the feed side of the module must always exceed the flow rate across the membrane.
401
into the turbine, we can estimate that a fouled meter-long module would consume at least 65%
402
of the energy that is extractable from the system pumping the feed solution.
24
. For a meter-long module, the feed flow rate would need to be
403
Our results stress that using a high fouling potential solution, such as secondary WW
404
effluent, as a feed solution for PRO will cripple the performance of the process in short time
405
periods, due to irreversible biofilm formation. These results also extend to other natural waters,
406
such as river water, since dissolved organic matter and bacteria are ubiquitous in natural
407
waters. However, for other feedwaters, the time scale for biofilm development hindering PRO
408
performance will depend on the source of the water and the level of pretreatment.
409
To minimize biofouling development in the feed channel, rigorous feedwater pretreatment
410
will be necessary, requiring both more energy input into the system and enhanced chemical
411
use. This energy input for pretreatment will be significant, and a more extensive analysis is 15 ACS Paragon Plus Environment
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412
necessary to determine the net energy output of a system accounting for the cost of
413
pretreatment. Alternatively, it may also be possible to reduce biofouling using new and
414
innovative membrane and spacer designs that reduce bacteria adhesion with the membrane
415
support or allow for improved cleaning efficacy.
416 417
SUPPORTING INFORMATION AVAILABLE
418
Detailed descriptions of the membrane characterization method; media and bacteria that were
419
used; cleaning procedures of the PRO setup; detailed description of CLSM, SEM and TEM
420
preparation; PRO experimental setup (Figure S1); pressure aided-osmotic backwash procedure
421
(Figure S2); pressure drop and WW flow rate through the feed channel (Table S1); CLSM
422
orthogonal views of biofouling on the membrane support (Figure S3); CLSM 3D images of
423
biofilm on the active layer and draw spacer (Figure S4); feed channel spacers before and after
424
OBW (Figure S5); CLSM 3D images (Figure S6) and SEM micrographs (Figure S7) of biofilm
425
that remained attached following OBW. This material is available free of charge via the
426
Internet at http://pubs.acs.org.
427 428
Notes
429
The authors declare no competing financial interest.
430 431
ACKNOWLEDGMENTS
432
We acknowledge support received from the National Science Foundation under Award Number 433
CBET 1232619. We would also like to thank Dr. Ming Xie and Evyatar Shaulsky for special 434
technical assistance. A.P.S. acknowledges support from the National Science Foundation 435
Graduate Research Fellowship (DGE-1122492). F.P. acknowledges financial support from the 436
Natural Sciences and Engineering Research Council of Canada postdoctoral fellowship. E.B-Z 437
acknowledges financial support of the postdoctoral fellowship provided by the United States438
Israel Binational Agricultural Research and Development (FI-474-12) Fund. Facilities used were 439
supported by the Yale Institute of Nanoscale and Quantum Engineering (YINQE) and NSF 440
MRSEC DMR 1119826. 16 ACS Paragon Plus Environment
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REFERENCES
442 443
(1)
Logan, B. E.; Elimelech, M. Membrane-based processes for sustainable power generation using water. Nature 2012, 488, 313–319.
444 445
(2)
Pattle, R. E. Production of electric power by mixing fresh and salt water in the hydroelectric pile. Nature, 1954, 174, 660–660.
446 447
(3)
La Mantia, F.; Pasta, M.; Deshazer, H. D.; Logan, B. E.; Cui, Y. Water salinity difference. Nano 2011, 11, 1810–1813.
448 449
(4)
Loeb, S.; Van Hessen, F.; Shahaf, D. Production of energy from concentrated brines by pressure-retarded osmosis. J. Memb. Sci. 1976, 1, 249–269.
450 451
(5)
Helfer, F.; Lemckert, C.; Anissimov, Y. G. Osmotic power with pressure retarded osmosis: theory, performance and trends - A review. J. Memb. Sci. 2014, 453, 337–358.
452 453
(6)
Achilli, A.; Childress, A. E. Pressure retarded osmosis: From the vision of Sidney Loeb to the first prototype installation - Review. Desalination 2010, 261, 205–211.
454 455 456
(7)
Post, J. W.; Hamelers, H. V. M.; Buisman, C. J. N. Energy recovery from controlled mixing salt and fresh water with a reverse electrodialysis system. Environ. Sci. Technol. 2008, 42, 5785–5790.
457 458 459
(8)
Daniilidis, A.; Vermaas, D. a.; Herber, R.; Nijmeijer, K. Experimentally obtainable energy from mixing river water, seawater or brines with reverse electrodialysis. Renew. Energy 2014, 64, 123–131.
460 461 462
(9)
Rica, R.; Ziano, R.; Salerno, D.; Mantegazza, F.; van Roij, R.; Brogioli, D. Capacitive mixing for harvesting the free energy of solutions at different concentrations. Entropy 2013, 15, 1388–1407.
463 464 465
(10)
Hatzell, K. B.; Beidaghi, M.; Campos, J. W.; Dennison, C. R.; Kumbur, E. C.; Gogotsi, Y. A high performance pseudocapacitive suspension electrode for the electrochemical flow capacitor. Electrochim. Acta 2013, 111, 888–897.
466 467 468
(11)
Yip, N. Y.; Elimelech, M. Performance limiting effects in power generation from salinity gradients by pressure retarded osmosis. Environ. Sci. Technol. 2011, 45, 10273– 10282.
469 470
(12)
Thorsen, T.; Holt, T. The potential for power production from salinity gradients by pressure retarded osmosis. J. Memb. Sci. 2009, 335, 103–110.
471 472 473
(13)
Chou, S.; Wang, R.; Fane, A. G. Robust and High performance hollow fiber membranes for energy harvesting from salinity gradients by pressure retarded osmosis. J. Memb. Sci. 2013, 448, 44–54. 17 ACS Paragon Plus Environment
Environmental Science & Technology
Page 18 of 28
474 475 476
(14)
Yip, N. Y.; Elimelech, M. Comparison of energy efficiency and power density in pressure retarded osmosis and reverse electrodialysis. Environ. Sci. Technol. 2014, 48, 11002–11012.
477 478
(15)
Ramon, G. Z.; Feinberg, B. J.; Hoek, E. M. V. Membrane-based production of salinitygradient power. Energy Environ. Sci. 2011, 4, 4423.
479 480 481
(16)
Straub, A. P.; Lin, S.; Elimelech, M. Module-scale analysis of pressure retarded osmosis: performance limitations and implications for full-scale operation. Environ. Sci. Technol. 2014, 48, 12435–12444.
482 483
(17)
http://www.statkraft.com/media/news/News-archive/2013/Statkraft-halts-osmoticpower-investments.
484 485 486
(18)
Kim, D. I.; Kim, J.; Shon, H. K.; Hong, S. Pressure retarded osmosis (PRO) for integrating seawater desalination and wastewater reclamation: Energy consumption and fouling. J. Memb. Sci. 2015, 483, 34–41.
487 488
(19)
Lin, S.; Straub, A.; Elimelech, M. Thermodynamic limits of extractable energy by pressure retarded osmosis. Energy Environ. Sci. 2014, 7, 2706–2714.
489 490
(20)
Zhang, M.; Hou, D.; She, Q.; Tang, C. Y. Gypsum scaling in pressure retarded osmosis: Experiments, mechanisms and implications. Water Res. 2014, 48, 387–395.
491 492 493
(21)
Chen, S. C.; Wan, C. F.; Chung, T.-S. Enhanced fouling by inorganic and organic foulants on pressure retarded osmosis (PRO) hollow fiber membranes under high pressures. J. Memb. Sci. 2015, 479, 190–203.
494 495
(22)
Thelin, W. R.; Sivertsen, E.; Holt, T.; Brekke, G. Natural organic matter fouling in pressure retarded osmosis. J. Memb. Sci. 2013, 438, 46–56.
496 497 498
(23)
Yip, N. Y.; Elimelech, M. Influence of natural organic matter fouling and osmotic backwash on pressure retarded osmosis energy production from natural salinity gradients. Environ. Sci. Technol. 2013, 47, 12607–12616.
499 500 501
(24)
She, Q.; Hou, D.; Liu, J.; Tan, K. H.; Tang, C. Y. Effect of feed spacer induced membrane deformation on the performance of pressure retarded osmosis (PRO): Implications for PRO process operation. J. Memb. Sci. 2013, 445, 170–182.
502 503 504
(25)
Li, X.; Cai, T.; Chung, T.-S. Anti-fouling behavior of hyperbranched polyglycerolgrafted poly(ether sulfone) hollow fiber membranes for osmotic power generation. Environ. Sci. Technol. 2014, 48, 9898–9907.
505 506 507
(26)
Matin, A.; Khan, Z.; Zaidi, S. M. J.; Boyce, M. C. Biofouling in reverse osmosis membranes for seawater desalination: Phenomena and prevention. Desalination 2011, 281, 1–16. 18 ACS Paragon Plus Environment
Page 19 of 28
Environmental Science & Technology
508 509
(27)
Mansouri, J.; Harrisson, S.; Chen, V. Strategies for controlling biofouling in membrane filtration systems: challenges and opportunities. J. Mater. Chem. 2010, 20, 4567.
510 511 512
(28)
Bar-Zeev, E.; Passow, U.; Romero-Vargas Castrillón, S.; Elimelech, M. Transparent exopolymer particles: from aquatic environments and engineered systems to membrane biofouling. Environ. Sci. Technol. 2015, 49, 691–707.
513 514 515
(29)
De Beer, D.; Stoodley, P. The Prokaryotes. In The Prokaryotes; Rosenberg, E.; DeLong, E. F.; Lory, S.; Stackebrandt, E.; Thompson, F., Eds.; Springer Berlin Heidelberg: Berlin, Heidelberg, 2013; pp. 343–373.
516 517 518
(30)
Herzberg, M.; Kang, S.; Elimelech, M. Role of extracellular polymeric substances (EPS) in biofouling of reverse osmosis membranes. Environ. Sci. Technol. 2009, 43, 4393– 4398.
519 520
(31)
Herzberg, M.; Elimelech, M. Biofouling of reverse osmosis membranes: Role of biofilm-enhanced osmotic pressure. J. Memb. Sci. 2007, 295, 11–20.
521 522
(32)
Flemming, H.-C.; Wingender, J. The biofilm matrix. Nat. Rev. Microbiol. 2010, 8, 623– 633.
523 524 525
(33)
Straub, A. P.; Osuji, C. O.; Cath, T. Y.; Elimelech, M. Selectivity and mass transfer limitations in pressure-retarded osmosis at high concentrations and increased operating pressures. Environ. Sci. Technol. 2015, In Press. DOI: 10.1021/acs.est.5b01317
526 527
(34)
Glueckstern, P.; Priel, M.; Gelman, E.; Perlov, N. Wastewater desalination in Israel. Desalination 2008, 222, 151–164.
528 529
(35)
Elimelech, M.; Phillip, W. A. The future of seawater and the environment. Science. 2011, 333, 712–717.
530 531
(36)
Guillard, R. R.; Ryther, J. H. Studies of marine planktonic diatoms: Cyclotella nana hustedt, and Detonula confervacea (cleve) gran. Can. J. Microbiol. 1962, 8, 229–239.
532 533 534
(37)
Gombos, E.; Felföldi, T.; Barkács, K.; Vértes, C.; Vajna, B.; Záray, G. Ferrate treatment for inactivation of bacterial community in municipal secondary effluent. Bioresour. Technol. 2012, 107, 116–121.
535 536 537
(38)
Bar-zeev, E.; Zodrow, K. R.; Kwan, S. E.; Elimelech, M. The importance of microscopic characterization of membrane biofilms in an unconfined environment. Desalination 2014, 348, 8–15.
538 539 540
(39)
Khan, M. T.; Manes, C. D. O.; Aubry, C.; Gutierrez, L.; Croue, J. P. Kinetic study of seawater reverse osmosis membrane fouling. Environ. Sci. Technol. 2013, 47, 10884– 10894.
19 ACS Paragon Plus Environment
Environmental Science & Technology
Page 20 of 28
541 542 543
(40)
Zodrow, K. R.; Bar-Zeev, E.; Giannetto, M. J.; Elimelech, M. Biofouling and microbial communities in membrane distillation and reverse osmosis. Environ. Sci. Technol. 2014, 48, 13155–13164.
544 545
(41)
Donlan, R. M. Biofilms: Microbial life on surfaces. Emerg. Infect. Dis. 2002, 8, 881– 890.
546 547
(42)
Stoodley, P.; Sauer, K.; Davies, D. G.; Costerton, J. W. Biofilms as complex differentiated communities. Annu. Rev. Microbiol. 2002, 56, 187–209.
548 549
(43)
Qin, J.; Liberman, B.; Kekre, K. A. Direct osmosis for reverse osmosis fouling control: principles, applications and recent developments. Open Chem. Eng. J. 2009, 3, 8–16.
550 551 552
(44)
Bar-Zeev, E.; Elimelech, M. Reverse osmosis biofilm dispersal by osmotic backflushing: cleaning via substratum perforation. Environ. Sci. Technol. Lett 2014, 2, 162–166.
553 554 555
(45)
Katebian, L.; Jiang, S. C. Marine bacterial biofilm formation and its responses to periodic hyperosmotic stress on a flat sheet membrane for seawater desalination pretreatment. J. Memb. Sci. 2013, 425-426, 182–189.
556 557 558
(46)
Achilli, A.; Prante, J. L.; Hancock, N. T.; Maxwell, E. B.; Childress, A. E. Experimental results from RO-PRO: A next generation system for low-energy desalination. Environ. Sci. Technol. 2014, 48, 6437–6443.
559 560 561
(47)
Song, X.; Liu, Z.; Sun, D. D. Energy recovery from concentrated seawater brine by thinfilm nanofiber composite pressure retarded osmosis membranes with high power density. Energy Environ. Sci. 2013, 6, 1199.
562 563 564
(48)
Prante, J. L.; Ruskowitz, J. a.; Childress, A. E.; Achilli, A. RO-PRO desalination: An integrated low-energy approach to seawater desalination. Appl. Energy 2014, 120, 104– 114.
565 566
(49)
Banchik, L. D.; Sharqawy, M. H.; Lienhard, J. H. Limits of power production due to finite membrane area in pressure retarded osmosis. J. Memb. Sci. 2014, 468, 81–89.
567 568
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TABLE 1. Biofilm characteristics and percent cleaning efficiency for each biofilm component following 60 min of pressure aided osmotic backwash.
571 Units Cell coverage
TOC
Protein
Membrane 2
“Dead cells”
EPS Polysaccharides Total biovolume
Spacer
(Sp1)
(Sp2)
Cell / µm
0.7 ±