<p>For turbine-manufacturing single-crystal superalloys, widely accepted multiple creep strengthening mechanism has been established, but arousing an undesired theoretical operating temperature limit of approximately 1140&#xa0;°C. Although exploratory studies have demonstrated the potential for achieving 1200&#xa0;°C capability, the underlying strengthening mechanisms for ultrahigh-temperature service remain insufficiently understood. We reveal that the creep at 1200&#xa0;°C originates from the well-recognized mechanism of dislocations interacting with precipitates. By quantitatively mapping rupture life at 1200&#xa0;°C against γ′ volume fraction and γ/γ′ lattice misfit, however, we show that effective strengthening occurs only when γ′ precipitates are sufficiently sustained. The dominant role of precipitation strengthening at 1200&#xa0;°C explains why classical theory fails here, as it does not account for the activated thermal instability of γ′ precipitates.</p>

错误:搜索内容不能为空,请输入英文关键词
错误:关键词超出字数限制,请精简
高级检索

Design route for single-crystal superalloys against 1200 °C: extending classical multiple creep strengthening mechanisms to ultrahigh-temperature service

  • Wan-Xin Yu,
  • Yuan-Hang Gao,
  • Shuang-Qi Zhang,
  • Yi-Feng Xing,
  • Bo-Xuan Du,
  • Bin Gan,
  • Shan Li,
  • Shu-Suo Li,
  • Yi Ru,
  • Sheng-Kai Gong,
  • Hui-Bin Xu

摘要

For turbine-manufacturing single-crystal superalloys, widely accepted multiple creep strengthening mechanism has been established, but arousing an undesired theoretical operating temperature limit of approximately 1140 °C. Although exploratory studies have demonstrated the potential for achieving 1200 °C capability, the underlying strengthening mechanisms for ultrahigh-temperature service remain insufficiently understood. We reveal that the creep at 1200 °C originates from the well-recognized mechanism of dislocations interacting with precipitates. By quantitatively mapping rupture life at 1200 °C against γ′ volume fraction and γ/γ′ lattice misfit, however, we show that effective strengthening occurs only when γ′ precipitates are sufficiently sustained. The dominant role of precipitation strengthening at 1200 °C explains why classical theory fails here, as it does not account for the activated thermal instability of γ′ precipitates.