首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >GIBBS FREE ENERGY OF FORMATION AND HEAT CAPACITY OF PDO - A NEW CALIBRATION OF THE PD-PDO BUFFER TO HIGH TEMPERATURES AND PRESSURES
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GIBBS FREE ENERGY OF FORMATION AND HEAT CAPACITY OF PDO - A NEW CALIBRATION OF THE PD-PDO BUFFER TO HIGH TEMPERATURES AND PRESSURES

机译:PDO的吉布斯自由能和热容量-PD-PDO缓冲液在高温和高压下的新标定

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The oxygen potential defined by the reaction 2Pd + O-2 = 2PdO has been measured from 730 K to 1200 K using the electrochemical cell: Pt, Pd + PdO CSZ YDT (air), Pt. Measurements were taken while going up and down in temperature. Two rigorous tests of the reversibility of the data were also conducted by perturbing the composition of the gas phase in the cell. The Gibbs free energy of formation (in terms of 1 mol of O-2) relative to a reference pressure of 1 bar is given by Delta fG(PdO)(O) = -238842 + 316.129T - 15.192T ln T(J mol(-1), temperature in K). The uncertainty is estimated to be +/-40 J . mol(-1) above 800 K and +/-200 J . mol(-1) at lower temperatures. This is in good agreement with several other studies conducted with a variety of different techniques. C-p of PdO was measured between 370 K and 1065 K using a differential scanning calorimeter operated in step heating mode. The data were fitted to a two-term expression, C-p = 71.08 - 531.6 T-(0.5) (J . mol(-1) . K-1). The uncertainty in the data is estimated to be +/-1 J . mol(-1) . K-1. The heat capacity results are significantly different from the measurements of the only previous study, but a third-law analysis proved the Gibbs free energy of formation and heat capacity data to be internally consistent. From the third-law analysis we obtained values of 33.74 J . mol(-1) . K-1 for S-298.15(0) (PdO) and -117.42KJ . mol(-1) for Delta(f)H(298.15)(0) (PdO). The new thermodynamic data for PdO was used to revise the temperature and pressure dependence of the oxygen fugacity of the Pd-PdO buffer. Including corrections for the thermal expansivity and compressibility of Pd and PdO we obtain log(10) f(O2) = 16.510 - 12473.4T(-1) - 1.826 log(10) T + P {0.0627 T-1 - 5.22 X 10(-7) (1 - 298 T-1) + 10(-8) PT-1} (T in Kelvin and P in bar) referenced to a standard state of 1 bar. It is also now possible to quantify the unexpected decrease in the activity coefficient of PdO in silicate melt with increasing temperature (in a diopside-anorthite eutectic melt gamma(PdO) = 130 at 1350 degrees C, decreasing to 50 at 1480 degrees C). [References: 29]
机译:由反应2Pd + O-2 = 2PdO定义的氧势已使用电化学电池在730 K至1200 K范围内测量:Pt,Pd + PdO CSZ YDT(空气),Pt。在温度升高和降低的同时进行测量。还通过扰乱电解池中气相的组成对数据的可逆性进行了两次严格测试。相对于1 bar参考压力的吉布斯自由形成能(以1 mol O-2表示)由Delta fG(PdO)(O)= -238842 + 316.129T-15.192T ln T(J mol)给出(-1),温度以K为单位)。不确定性估计为+/- 40J。 mol(-1)在800 K和+/- 200 J以上。在较低温度下为mol(-1)。这与使用多种不同技术进行的其他几项研究非常吻合。使用在步进加热模式下运行的差示扫描量热计,在370 K和1065 K之间测量了PdO的C-p。将数据拟合为两项表达式,C-p = 71.08-531.6 T-(0.5)(J。mol(-1)。K-1)。数据中的不确定性估计为+/- 1J。 mol(-1)。 K-1。热容结果与先前的唯一一项研究的测量结果显着不同,但是第三定律分析证明了吉布斯自由能和热容数据在内部是一致的。从第三定律分析,我们获得了33.74 J的值。 mol(-1)。 S-1298.15(0)(PdO)和-117.42KJ的K-1。 Delta(f)H(298.15)(0)(PdO)的mol(-1)。 PdO的新热力学数据用于修正Pd-PdO缓冲液中氧气逸度的温度和压力依赖性。包括对Pd和PdO的热膨胀性和可压缩性的校正,我们得到log(10)f(O2)= 16.510-12473.4T(-1)-1.826 log(10)T + P {0.0627 T-1-5.22 X 10( -7)(1-298 T-1)+ 10(-8)PT-1}(T以开尔文表示,P以巴为单位)参考1 bar的标准状态。现在还可以量化硅酸盐熔体中PdO的活性系数的意外降低,其随温度升高而变化(在透辉石-无长石共晶熔体中,γ(PdO)在13050摄氏度时为130,在1480摄氏度时降至50)。 [参考:29]

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