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arXiv 2110.08528cond-mat.mtrl-sci
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考虑组分中相变的可动性时0 ~ 1300 ℃氧化皮热膨胀的广义估计

Generalized estimates for thermal expansion of oxide scale in the range from 0C to 1300C with account for movability of phase transitions in its components

Emmanuil Beygelzimer, Yan Beygelzimer

摘要:

氧化膜的热物理性质一般受相变温度的影响(磁性的或多晶型的)。在这种情况下,由于相变通常伴随着性质的急剧变化,即使这种临界温度的小偏移也会导致其附近的性质的大变化。为了解释这种影响,从各种来源已知的数据上的真实线性热膨胀系数(CLTE)的方铁矿,磁铁矿,赤铁矿,和金属铁概括的近似函数,包括临界温度作为可变参数。结果表明,在相同的额定温度下,磁铁矿的真实CLTE可以相差高达30%,这取决于居里点的位置在其可能的“可动性”的限制。所提出的方法允许考虑的临界温度作为适应参数的氧化皮的热膨胀的工程计算。对于临界温度的固定(基本)值,也以特定的形式给出了每个标度分量的通用公式。提出了氧化膜整体真实CLTE(αsc)与各组分体积分数的关系。模型计算表明,在某些温度下,αsc几乎与结垢成分无关,在某些不稳定区域,αsc主要取决于结垢成分的百分比。建议在对表面存在氧化皮的钢铁产品的生产和加工进行数学建模时使用该工作的结果。

英文摘要:

The thermophysical properties of oxide scale, in the general case, are affected by the variation of the temperature of phase transitions (either magnetic or polymorphic) in its components due to impurities, lattice defects, grain sizes, etc. In this case, since the phase transition is usually accompanied by a sharp change in properties, even a small shift of such a critical temperature can lead to large changes in properties in its vicinity. In order to account for this effect, data known from various sources on the true coefficient of linear thermal expansion (CLTE) of wüstite , magnetite , hematite , and metallic iron are generalized by approximating functions that include critical temperatures as variable parameters. It is shown that the true CLTE of magnetite at the same rated temperature can differ by up to 30% depending on the position of the Curie point within the limits of its possible "movability". The proposed methods allow to take into account the critical temperatures as adaptation parameters in engineering calculations of thermal expansion of oxide scale. Generalized formulas for each scale component are also given in a particular form for fixed (basic) values of critical temperatures. The dependence of the true CLTE of oxide scale as a whole (αsc) on the volume fraction of each component is proposed. It is shown by model computations that there are temperatures at which αsc is almost independent of the scale composition, as well as areas of instability, where αsc depends significantly on the percentage of components. The results of the work are recommended to be used when mathematical modeling of production and processing of steel products in the presence of oxide scale on their surface.

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