Water Transport in Gas Diffusion Layers of PEMFCs Shawn Litster, Aimy Bazylak, David Sinton and Ned Djilali ECS Trans. 2006, Volume 3, Issue 1, Pages 409-414. doi: 10.1149/1.2356161 Email alerting service Receive free email alerts when new articles cite this article - sign up in the box at the top right corner of the article or click here To subscribe to ECS Transactions go to: http://ecst.ecsdl.org/subscriptions © 2006 ECS - The Electrochemical Society Downloaded on 2012-09-19 to IP 128.100.48.214 address. Redistribution subject to ECS license or copyright; see www.esltbd.org ECS Transactions, 3 (1) 409-414 (2006) 10.1149/1.2356161, copyright The Electrochemical Society Water Transport in Gas Diffusion Layers of PEMFCs Shawn Litster, Aimy Bazylak, David Sinton, Ned Djilali IESVic, University of Victoria, Victoria, BC V8W 3P6, Canada We present an ex-situ analysis of water transport in the carbon paper gas diffusion layers for PEM fuel cells. We employ florescent imaging that allows us to distinguish liquid water from air through an optical microscope by seeding the water with fluorescent molecules. We were able to infer the vertical location of water and create three-dimensional reconstructions of the water surface by correlating surface height with image intensity. Our study investigated water phase movement in an uncompressed GDL as well as the additional effect of the localized compression that a fuel cell’s bipolar plate introduces. The visualizations indicate that localized compression promotes regions of increased wettability. We put forth that the increased wettability results from fractured carbon fibers and the degradation of the PTFE coating. Introduction Proper water management in polymer electrolyte membrane fuel cells (PEMFC) is required to maintain an adequate level of hydration in the PEM while avoiding performance decline due to liquid water flooding. Flooding occurs in both the gas delivery channels and within the pores of the gas diffusion layers (GDLs). There are numerous strategies for removing water from the gas channels (1, 2), which can be as simple as running high gas flow rates. However, flooding in gas diffusion layers can be more difficult to address since the surface tension in the porous media can entrap the water. The common remedy is to treat the porous carbon material with a hydrophobic agent to ensure that liquid water exists in only a small fraction of pore network and place a micro-porous layer between the catalyst layer and macro-porous GDL (3). However, the concepts of the transport mechanisms in GDL materials have largely been speculative. In our initial work (4) we performed ex-situ visualizations of liquid flow in a carbon paper GDL to elucidate the liquid water transport mechanism. Our visualization method utilized fluorescence microscopy techniques that distinguish the gas and liquid phases by an optical means. The spatial resolution of images was 5.35 µm pixel-1 and the vertical resolution was 0.11 µm. Sinha et al. (5) explored the use of microtomography to determine the saturation of gas diffusion layer materials. An advantage of their method is that it enables vertical scanning of the GDL layer to generate three-dimensional reconstructions. However, the vertical resolution of their method was 13.4 µm (5), which was too large to visualize water interactions with individual fibers in the GDL that are roughly 8 µm in diameter. Zhang et al. (6) used neutron radiography to measure water saturation in the gas diffusion layers during fuel cell operation. Their method proved capable of detecting the variation in saturation at the scale of the fuel cell channel, but not at the pore scale. In this paper, we present our method for visualizing capillary transport Downloaded on 2012-09-19 to IP 128.100.48.214 address. Redistribution subject to ECS license or copyright; see www.esltbd.org 409 ECS Transactions, 3 (1) 409-414 (2006) of water in GDLs at the pore-level and report on the extension of this method for studying flow in GDLs under the localized compression caused by a fuel cell’s flow fields. Experimental We optically distinguish water from air in the GDL by seeding the water with fluorescent molecules. The fluorescent molecules absorb photons at the excitation beam wavelength (blue light, λ = 513 nm); the molecules then dissipate a portion of the photon energy and emit photons at a longer wavelength (green light, λ = 490 nm). In our experiments, we visualized the capillary transport of water in Toray TGP-H-60 gas diffusion media (10% wt. PTFE treatment). We seeded the water with a 0.5mM concentration of fluorescein dye (332 MW, Molecular Probes) and pumped that solution at a constant flow rate through a GDL, which was compressed above a large fluid reservoir (4). A mask featuring a 2 × 2 mm opening was placed on the reservoir side of the GDL to control the location of water flux. A Leica Microsystems DM LM optical microscope with an 8-bit cooled CCD camera captures the transient images. To quantify the liquid height in each pore, we exploit the depth of field property of the microscope objective (5X, NA = 0.15), which provides a vertical range of 30µm when inferring fluorescein solution height from image intensity (4). This vertical range allows us to resolve water transport within four fiber cross-sections of the GDL. Figure 1. Schematic of the fluorescence microscopy apparatus for visualizing liquid transport in GDLs. Results Uncompressed GDL The left hand image in Figure 2 presents the water rise in the GDL where the fluorescein/water solution produces the dark areas. The right hand image is the threedimensional rendering of the liquid height that we inferred from the image intensity data. Figure 3 presents a plot of surface height versus time for five specific pores in the images Downloaded on 2012-09-19 to IP 128.100.48.214 address. Redistribution subject to ECS license or copyright; see www.esltbd.org 410 ECS Transactions, 3 (1) 409-414 (2006) of Figure 2. Path 1 rose quickly, but abruptly stopped when it intersected a small fiber cross-section, and at that time paths 2 and 3 began to rise more rapidly to maintain the flow rate. At approximately 200 s, the coupling between flow in adjacent pores is evident when the flow in path 2 rapidly rose due to a local pore expansion, and the height in path 3 dropped due to the local pressure drop induced by the lowered capillary pressure in path 2. Figure 2. Image of dye transport in a TGP-H-060 GDL with 10% wt. PTFE treatment with the contrast inverted (left) and 3D rendering of the liquid height (right) at 145 sec. Figure 3. Identification of individual water pathways in the GDL (left). Water height in the pathways of the GDL (right). Key characteristics include the rapid rise of path 2 that correlates the drop in water height in Path 3 at 200 sec., which indicates pore breakthrough phenomena. From our experimental observations, we propose a revised hypothesis for the water transport mechanism in GDLs. Prior works (7, 8) depict capillary transport in GDLs as a network of pore flows that converge at the GDL surface, which resemble an “upsidedown tree.” However, our analysis indicates that a fingering and channeling hypothesis is more correct. These results show that the water will travel from the catalyst layer to the gas channel via a path constructed from the series of interconnected pores with the greatest pore radii. When the liquid path intersects a small fiber cross-section, the flow stops at that location and redirects itself through the largest available empty pore. Our Downloaded on 2012-09-19 to IP 128.100.48.214 address. Redistribution subject to ECS license or copyright; see www.esltbd.org 411 ECS Transactions, 3 (1) 409-414 (2006) hypothesis has implications for the modeling of two-phase flow in PEMFCs as it implies that the liquid saturation in GDLs is highly dependent on the heterogeneity and anisotropy of the porous structure. Effect of Channel Structure and Compression PEMFCs are typically compressed to ensure proper sealing and minimize contact resistance. Various studies have examined the effect of compression: Lee et al. (9) presented polarization curves as a function of the compression pressure; Escribano et al. (10) showed that higher compression induced lower performance due to increased mass transfer losses; Ge et al. (11) found that generally performance decreases with increasing assembly pressure. In a working fuel cell, a bipolar plate imposes the entire compression force onto the GDL over the land area. The reduced area amplifies the mechanical stresses on the GDL and may cause the GDL to fracture. It is previously unknown to what degree this fracturing affects capillary flow in GDLs. We have modified the previous set-up to investigate the effect of land area interfaces and compression on liquid water transport in GDLs. Figure 5 provides a schematic of the new apparatus for holding the GDL. The channel land area is composed of borosilicate glass with a uniform thickness of 150µm. Figure 4. Schematic of Plexiglas GDL holding apparatus. Figure 5 shows the fluorescein distribution in a GDL, placed beneath a horizontal gas flow channel located midway through the image. The second image capture is 300 ms after the first. The gas flow channel floods immediately following the liquid breakthrough under the land area. In our observations, it was evident that the water flooding the channel was emerging from under the land area. Unfortunately, the frame rate of the image capturing system was not fast enough to capture this phenomenon. The results indicate that preferential pathways for liquid transport exist under the land area due to the relative hydrophilic surface of the land area combined with locations of relatively hydrophilic pathways created by the local compression. Downloaded on 2012-09-19 to IP 128.100.48.214 address. Redistribution subject to ECS license or copyright; see www.esltbd.org 412 ECS Transactions, 3 (1) 409-414 (2006) Figure 5. Image of dye transport in a TGP-H-060 GDL with 10% wt. PTFE treatment below a gas flow channel (left) and a 3D rendering of the liquid height (right). The compression of gas diffusion layers under the land area introduces morphological changes in the material that can affect the capillary transport of water. SEM images made before and after compression, shown in Figure 6, illustrate these changes. The images show that compression fractured a large portion of the fibers and degraded the hydrophobic PTFE coating. The degraded PTFE coating exposed areas of bare carbon surface, which are significantly more hydrophilic. The wettability of the locally compressed GDL visibly increased due to larger mean pore diameters and lower contact angles generated by fiber breakage and PTFE degradation. Our observations of a preferential water pathway under the land area support the suggestion that increased wettability exists under the land area. The consequence of the increased wettability is problematic for PEM fuel cell operation since the advective action of the gas flow for removing water is limited under the land area. Figure 6. SEM image of an uncompressed Toray TGP-H-060 GDL (left), and a SEM image of the same material after being compressed for five minutes at 0.68 kPa (right). Downloaded on 2012-09-19 to IP 128.100.48.214 address. Redistribution subject to ECS license or copyright; see www.esltbd.org 413 ECS Transactions, 3 (1) 409-414 (2006) Conclusion We visualized water transport through the gas diffusion layer of a PEM fuel cell in two scenarios. The first scenario is a uniform GDL that is not under compression but has a mask with a small opening to control the location of the water flux. In a second scenario, we imposed a clamping pressure on a GDL using the geometry of a fuel cell channel. The analysis of water transport in individual pores in the first scenario supports a “channeling and fingering” model of water transport. In this model, the pore size distribution dictates the direction of the water transport. 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