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High-temperature heat capacity and thermodynamic properties for end-member titanite (CaTiSiO_5)

机译:端部钛矿(CaTiSiO_5)的高温热容和热力学性质

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The heat capacity of end-member titanite and (CaTiSiO_5) glass has been measured in the range 328-938 K using differential scanning calorimetry. The data show a weak λ-shaped anomaly at 483 ± 5 K, presumably associated with the well-known low-pressure P2_1/a <-> A2/a transition, in good agreement with previous studies. A value of 0.196 ± 0.007 kJ mol~(-1) for the enthalpy of the P2_1/a <-> A2/a transition was determined by integration of the area under the curve for a temperature interval of 438-528 K, bracketing the anomaly. The heat capacity data for end-member titanite and (CaTiSiO_5) glass can be reproduced within <1% using the derived empirical equations (temperature in K, pressure in bars): C_p~(glass) = (114.7155 * 10~6)/(T~3) + (-908.3 * 10~(-3))/(T~2) + (0.3170 * 10~5)/T + (-0.8484 * 10~4)/(T~(1/2)) +0.5796 * 10~3 + (-21.75) * 10~(-2) T + 7.8731 * 10~(-5) T~2 (1) C_p~(solid) = (-2.3952 * 10~6)/(T~3) + (-5.8601 * 10~(-3))/(T~2) + (0.2239 * 10~5)/T + (-0.5913 * 10~4)/(T~(1/2)) + 0.4277 * 10~3 + (-7.772) * 10~(-2) T + 1.3751 * 10~(-5) T~2 + 3.0877 ∑ from 1 to k = 2 of (τ~(3·(2k-1)))/(2k - 1) for τ = T/(T_(transition)) ≤ 1 or 2.3034 ∑ from 1 to k = 2 of (τ~(-5·(2k-1)))/(2k - 1) for τ = T/(T_(transition)) ≥ 1 (2) The available enthalpy of vitrification (80.78 ± 3.59 kJ mol~(-1)), and the new heat capacity equations for solid and glass can be used to estimate (1) the enthalpy of fusion of end-member titanite (122.24 ± 0.2 kJ mol~(-1)), (2) the entropy of fusion of end-member titanite (73.85 ± 0.1 J/mol K~(-1), and (3) a theoretical glass transition temperature of 1130 ± 55 K. The latter is in considerable disagreement with the experimentally determined glass transition temperature of 1013 ± 3 K. This discrepancy vanishes when either the adopted enthalpy of vitrification or the liquid heat content, or both, are adjusted. Calculations using Eq. (2), new P-V-T data for titanite, different but also internally consistent thermodynamic data for anorthite, rutile, and kyanite, and experimental data for the reaction: anorthite + rutile = titanite + kyanite strongly suggest: (1) the practice to adjust the enthalpy of formation of titanite to fit phase equilibrium data may be erroneous, and (2) it is probably the currently accepted entropy of 129.2 ± 0.8 J/mol K~(-1) that may need revision to a smaller value.
机译:使用差示扫描量热法在328-938 K范围内测量了端部钛矿和(CaTiSiO_5)玻璃的热容量。数据显示在483±5 K处有一个弱的λ形异常,大概与众所周知的低压P2_1 / a-A2 / a跃迁有关,这与以前的研究非常吻合。 P2_1 / a <-> A2 / a跃迁的焓的值为0.196±0.007 kJ mol〜(-1),是通过对438-528 K的温度区间内的曲线下面积进行积分确定的。异常。使用导出的经验方程式(以K为单位的温度,以bar为单位的压力),可以将端部钛矿和(CaTiSiO_5)玻璃的热容量数据复制到<1%以内:C_p〜(玻璃)=(114.7155 * 10〜6)/ (T〜3)+(-908.3 * 10〜(-3))/(T〜2)+(0.3170 * 10〜5)/ T +(-0.8484 * 10〜4)/(T〜(1/2 ))+0.5796 * 10〜3 +(-21.75)* 10〜(-2)T + 7.8731 * 10〜(-5)T〜2(1)C_p〜(solid)=(-2.3952 * 10〜6) /(T〜3)+(-5.8601 * 10〜(-3))/(T〜2)+(0.2239 * 10〜5)/ T +(-0.5913 * 10〜4)/(T〜(1 / 2))+ 0.4277 * 10〜3 +(-7.772)* 10〜(-2)T + 1.3751 * 10〜(-5)T〜2 + 3.0877Σ从1到k = 2(τ〜(3· (2k-1)))/(2k-1)对于τ= T /(T_(transition))≤1或2.3034 ∑从(τ〜(-5·(2k-1)))的1到k = 2 /(2k-1)对于τ= T /(T_(transition))≥1(2)可用的玻璃化焓(80.78±3.59 kJ mol〜(-1))以及新的固体和玻璃热容方程可用于估计(1)端成员钛矿的熔化焓(122.24±0.2 kJ mol〜(-1)),(2)端成员钛矿的熔化熵(73.85±0.1 J / mol K 〜(-1)和(3)的理论玻璃化转变温度为1130±55K。后者与实验确定的1013±3 K的玻璃化转变温度有很大不同。当采用任何一种玻璃化焓时,这种差异就会消失。或调整液体热量,或同时调整两者。使用公式计算(2),新的钛铁矿的PVT数据,钙长石,金红石和蓝晶石的热力学数据不同但内部一致的,以及反应的实验数据:钙长石+金红石=钛矿+蓝晶石强烈建议:(1)调整钛矿形成的焓与相平衡数据相符可能是错误的,并且(2)可能需要将当前的熵129.2±0.8 J / mol K〜(-1)修正为一个较小的值。

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