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Prediction of thermodynamic properties of inorganic solids by the method of group contributions.

机译:用基团贡献法预测无机固体的热力学性质。

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摘要

Heats of formation, Gibbs free energies of formation, and heat capacities as a function of temperature are thermodynamic properties of solids often needed in process calculations. Literature data for these properties of many inorganic salts, minerals, clays, and related substances are not available. As greater effort is being directed towards problems such as environmental cleanup, these thermodynamic properties are needed to perform the required process calculations. Two different additive group contribution techniques are developed to provide the additivity constants for the prediction of these properties. The first technique provides values for group additivity constants of anions and cations which combine to form solid inorganic salts where ionic bonds predominate. The second considers oxide and hydroxide groups which combine to form minerals, clays, and related substances with primarily covalent bonds. Multiple linear regression is used to estimate the contributions for each of the required additivity constants. For solid inorganic salts, data from 938, 687, and 664 compounds are used, respectively, to obtain 136 cation and 22 anion additivity constants for heats of formation, 126 cation and 21 anion constants for free energies of formation, and 129 cation and 17 anion sets of constants for heat capacity temperature function coefficients. For minerals, clays, and related solids, data from 190 compounds are used to obtain 44 additivity constants for heats and free energies of formation and from 157 compounds to obtain 42 sets of additivity constants for heat capacities. The average errors in the predictions for solid inorganic salts are 2.57% for heats of formation, 2.60% for free energies of formation, and 3.14% for heat capacities at 298 K. For minerals, clays, and related substances the average errors are 1.00% for heats of formation, 1.01% for free energies of formation, and 1.75%, increasing to 2.95% for heat capacities from 298 K to 800 K, respectively.
机译:地层热,地层吉布斯自由能以及热容量随温度的变化是过程计算中经常需要的固体热力学性质。没有许多无机盐,矿物,粘土和相关物质的这些特性的文献数据。随着对诸如环境净化之类的问题的更多努力,需要这些热力学性质来执行所需的过程计算。开发了两种不同的添加剂组贡献技术,以提供用于预测这些性质的可加常数。第一种技术提供阴离子和阳离子的基团加和常数的值,这些阴离子和阳离子结合形成固体无机盐,其中离子键占主导地位。第二个考虑的氧化物和氢氧化物基团结合形成具有主要共价键的矿物,粘土和相关物质。多元线性回归用于估计每个所需加性常数的贡献。对于固体无机盐,分别使用来自938、687和664化合物的数据来获得136阳离子和22阴离子对形成热的加和常数,126阳离子和21阴离子对形成自由能的常数,129阳离子和17阴离子。负离子组的热容温度函数系数。对于矿物,粘土和相关固体,使用190种化合物的数据来获得44个热量和地层自由能的加和常数,使用157个化合物的数据来获得42个热容量的加和常数。固体无机盐预测的平均误差为:地层热为2.57%,地层自由能为2.60%,热容为298 K时为3.14%。矿物,粘土和相关物质的平均误差为1.00%对于地层热,热能从298 K升至800 K分别为1.01%和1.75%,增至2.95%。

著录项

  • 作者

    Mostafa, A. T. M. Golam.;

  • 作者单位

    New Mexico State University.;

  • 授予单位 New Mexico State University.;
  • 学科 Chemical engineering.;Inorganic chemistry.
  • 学位 Ph.D.
  • 年度 1995
  • 页码 239 p.
  • 总页数 239
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

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