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Earth and Space Sciences · 术语表

什么是 Rate factor (ice)?

Definition 24.2 University Earth and Space Sciences — Year 3 · 第 24 章 — Glaciology

The rate factor A(T)A(T) of Glen’s law, also called the softness of the ice, is written A=A0exp⁡(−Q/RT)A = A_0\exp(-Q/RT), with an activation energy QQ. A widely used fit (Paterson and Budd) takes A0=3.61×10−13 s−1 Pa−3A_0 = 3.61 \times 10^{-13}\,\mathrm{s}^{-1}\,\mathrm{Pa}^{-3} and Q=60 kJ/molQ = 60\,\mathrm{kJ}/\mathrm{mol} below −10 ∘C-10\,{}^{\circ}\mathrm{C}, and A0=1.73×103 s−1 Pa−3A_0 = 1.73 \times 10^{3}\,\mathrm{s}^{-1}\,\mathrm{Pa}^{-3} and Q=139 kJ/molQ = 139\,\mathrm{kJ}/\mathrm{mol} above it, closer to the melting point, where the ice softens faster with temperature.

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