The overall predictions of water profile evolution within the GDL agree with the data visualized from the X-ray CT experiment for all cases studied. They also reveal that the water saturation profiles inside the GDL samples and breakthrough pressure are different when the location of water injection point is changed. In addition, the non-compressed GDL provides significantly different mechanism of water transport compared to compressed GDL. Figure 2 shows example of the predictions and experimental data of water evolution inside the SGL10BA GDL with and without compression. The results clearly show that without compression, water spreads to the side of the GDL before it moves up to the top of the GDL. For the compressed GDL, the water transports directly to the top of GDL, where breakthrough pressure is reached. This work will also be extended to include the effect of non-uniform wettability of GDL on water transport and saturation.
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