摘要
Reliable cold start of large-area proton exchange membrane fuel cells (PEMFCs) remains a key bottleneck for fuel cell vehicles, because most mechanistic studies have focused on small laboratory cells whose behavior cannot be directly extrapolated to large-scale devices. This study develops a transient three-dimensional non-isothermal multi-physics model of a 79.5 cm2 PEMFC with an eleven-channel serpentine flow field to elucidate coupled heat, water and ice processes during self-cold start at −30 °C. On this basis, three start strategies are examined. The global responses reveal three characteristic stages: reaction-limited, self-heating dominated, and icing/transport-limited. These stages develop in a strongly non-uniform manner: downstream regions heat up faster than inlet zones, and the multi-channel serpentine geometry induces pronounced variations of temperature and current density. Higher ramps increase cathode catalyst layer (CL) heating rates from 0.88 to 1.86 K min−1, but also amplify temperature and current-density non-uniformity. Ice forms preferentially in the cathode CL, where limited gas-phase transport and low saturation vapor pressure hinder water removal, and then propagates into the gas diffusion layer (GDL). In-plane distribution and a quantitative uniformity index reveal that aggressive ramps promote early nucleation of ice clusters near channel bends and downstream regions, followed by rapid coalescence into extended ice-rich bands. Through-plane analysis shows that high ramps drive deep ice penetration into the GDL, whereas moderate ramps keep most ice confined near the CL. These results clarify how large-area effects and current-ramp design jointly control cold-start failure, and provide mechanistic guidance to improve cold-start strategies for automotive PEMFCs.
| 源语言 | 英语 |
|---|---|
| 期刊论文编号 | 127988 |
| 期刊 | Applied Energy |
| 卷 | 416 |
| DOI | |
| 出版状态 | 已出版 - 1 8月 2026 |
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此成果有助于实现下列可持续发展目标:
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