A pore-level direct numerical investigation of water evaporation characteristics under air and hydrogen in the gas diffusion layers of polymer electrolyte fuel cells

被引:21
作者
Safi, Mohammad Amin [1 ,4 ]
Mantzaras, John [1 ]
Prasianakis, Nikolaos I. [2 ]
Lamibrac, Adrien [3 ]
Buchi, Felix N. [3 ]
机构
[1] Paul Scherrer Inst, Lab Sci Comp & Modeling, CH-5232 Villigen, Switzerland
[2] Paul Scherrer Inst, Lab Waste Management, CH-5232 Villigen, Switzerland
[3] Paul Scherrer Inst, Lab Elechtrochem, CH-5232 Villigen, Switzerland
[4] Altair Engn GmbH, Edisonstr 3, DE-85716 Unterschleissheim, Munich District, Germany
关键词
Water evaporation; Pore-scale modeling; Gas diffusion layers; Polymer electrolyte fuel cells; Evaporation-induced flows; LIQUID WATER; MANAGEMENT; TRANSPORT; CONDENSATION; WETTABILITY; SATURATION;
D O I
10.1016/j.ijheatmasstransfer.2018.10.042
中图分类号
O414.1 [热力学];
学科分类号
摘要
During the operation of polymer electrolyte fuel cells (PEFC) liquid water clusters generated due to electrochemical reactions in the gas diffusion layers (GDL) create a resistance against gas transport towards the catalyst layers (CL), and hence must be efficiently removed to maintain the cell performance, a process often realized by means of forced evaporation. Water accumulation is of interest not only for the cathode GDL but also for the anode GDL, particularly under thermoneutral cell operation whereby liquid water can be added to either anode or cathode channel flows. Although many works studied water evaporation in air and especially at moderate temperatures, less effort has been devoted in investigating evaporation at elevated temperatures and at the anode side, where hydrogen flows in the gas channels. In this work, direct numerical simulation is used to characterize evaporation at pore level for both anode and cathode sides and at different temperatures (up to 80 degrees C), for which experimental data are rare and micro-scale transport is often difficult to assess in the laboratory. Realistic water distribution and porous GDL geometry, acquired from X-ray tomography, have been used while regularized distributions of liquid water are further considered in order to investigate evaporation at various saturation levels. Key results indicate that (a) the water evaporation rate in hydrogen flows can be up to 4 times larger than the corresponding one in air flows at the same gas stream velocity and temperature, (b) the predicted vertical evaporation-induced velocities under hydrogen are an order of magnitude bigger than the corresponding ones under air and they can grow large enough at elevated temperatures to potentially hamper hydrogen transport towards the CLs. (C) 2018 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1250 / 1262
页数:13
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