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热力学史:缺失的手册。

A History of Thermodynamics: The Missing Manual.

作者信息

Saslow Wayne M

机构信息

Department of Physics, Texas A&M University, College Station, TX 77843-4242, USA.

出版信息

Entropy (Basel). 2020 Jan 7;22(1):77. doi: 10.3390/e22010077.

Abstract

We present a history of thermodynamics. Part 1 discusses definitions, a pre-history of heat and temperature, and steam engine efficiency, which motivated thermodynamics. Part 2 considers in detail three heat conservation-based foundational papers by Carnot, Clapeyron, and Thomson. For a reversible Carnot cycle operating between thermal reservoirs with Celsius temperatures and t + d t , heat from the hot reservoir, and net work , Clapeyron derived W / Q = d t / C ( t ) , with C ( t ) material-independent. Thomson used μ = 1 / C ( t ) to define an absolute temperature but, unaware that an additional criterion was needed, he first proposed a logarithmic function of the ideal gas temperature T g . Part 3, following a discussion of conservation of energy, considers in detail a number of energy conservation-based papers by Clausius and Thomson. As noted by Gibbs, in 1850, Clausius established the first modern form of thermodynamics, followed by Thomson's 1851 rephrasing of what he called the Second Law. In 1854, Clausius theoretically established for a simple Carnot cycle the condition Q 1 / T 1 + Q 2 / T 2 = 0 . He generalized it to ∑ i Q i / T g , i = 0 , and then ∮ d Q / T g = 0 . This both implied a new thermodynamic state function and, with appropriate integration factor 1 / T , the thermodynamic temperature. In 1865, Clausius named this new state function the entropy .

摘要

我们呈现一部热力学史。第1部分讨论了定义、热和温度的史前史以及推动热力学发展的蒸汽机效率。第2部分详细考虑了卡诺、克拉佩龙和汤姆森基于热守恒的三篇奠基性论文。对于在摄氏温度为(t)和(t + dt)的热库之间运行的可逆卡诺循环,从热库吸收的热量(Q)以及净功(W),克拉佩龙推导出(W/Q = dt/C(t)),其中(C(t))与物质无关。汤姆森用(\mu = 1/C(t))定义了绝对温度,但由于未意识到还需要一个额外的标准,他最初提出了理想气体温度(T_g)的对数函数。第3部分在讨论能量守恒之后,详细考虑了克劳修斯和汤姆森基于能量守恒的一些论文。正如吉布斯所指出的,1850年克劳修斯建立了热力学的第一种现代形式,随后汤姆森在1851年对他所谓的第二定律进行了重新表述。1854年,克劳修斯从理论上为简单卡诺循环建立了条件(Q_1/T_1 + Q_2/T_2 = 0)。他将其推广到(\sum_i Q_i/T_{g,i} = 0),然后是(\oint dQ/T_g = 0)。这既暗示了一个新的热力学状态函数,又通过适当的积分因子(1/T)得到了热力学温度。1865年,克劳修斯将这个新的状态函数命名为熵。

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