评估线性密度模型在预测超临界水中解离-结合平衡方面的有效性和局限性

IF 4.5 1区 地球科学 Q1 GEOCHEMISTRY & GEOPHYSICS Geochimica et Cosmochimica Acta Pub Date : 2024-10-16 DOI:10.1016/j.gca.2024.10.008
Maximilian Schulze, Thomas Driesner, Sandro Jahn
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Yet, neither a theoretical foundation nor an assessment of the ranges of validity have been presented. Here, we use classical molecular dynamics (MD) simulations as a complementary tool to assess the validity of this linear relationship for the example of NaCl and reveal its limits at water densities below ca. 0.3<ce:hsp sp=\"0.16667\"></ce:hsp>g<ce:hsp sp=\"0.16667\"></ce:hsp>cm<ce:sup loc=\"post\">−3</ce:sup>. The derivative <mml:math altimg=\"si4.svg\" display=\"inline\"><mml:mrow><mml:mi>∂</mml:mi><mml:mo>log</mml:mo><mml:mrow><mml:mo>(</mml:mo><mml:mi>K</mml:mi><mml:mo>)</mml:mo></mml:mrow><mml:mo>/</mml:mo><mml:mi>∂</mml:mi><mml:mo>log</mml:mo><mml:mrow><mml:mo>(</mml:mo><mml:msub><mml:mrow><mml:mi>ρ</mml:mi></mml:mrow><mml:mrow><mml:msub><mml:mrow><mml:mi mathvariant=\"normal\">H</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub><mml:mi mathvariant=\"normal\">O</mml:mi></mml:mrow></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:mrow></mml:math> is calculated based on the volume of reaction and water compressibility derived from the simulations performed in the isothermal–isobaric ensemble at 673<ce:hsp sp=\"0.16667\"></ce:hsp>K. Our results corroborate the linear dependence of <mml:math altimg=\"si1.svg\" display=\"inline\"><mml:mrow><mml:mo>log</mml:mo><mml:mrow><mml:mo>(</mml:mo><mml:mi>K</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:mrow></mml:math> vs. <mml:math altimg=\"si6.svg\" display=\"inline\"><mml:mrow><mml:mo>log</mml:mo><mml:mrow><mml:mo>(</mml:mo><mml:msub><mml:mrow><mml:mi>ρ</mml:mi></mml:mrow><mml:mrow><mml:msub><mml:mrow><mml:mi mathvariant=\"normal\">H</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub><mml:mi mathvariant=\"normal\">O</mml:mi></mml:mrow></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:mrow></mml:math> in the experimentally studied density range and suggest that the linear dependence also extends to higher densities. However, towards lower densities, <mml:math altimg=\"si1.svg\" display=\"inline\"><mml:mrow><mml:mo>log</mml:mo><mml:mrow><mml:mo>(</mml:mo><mml:mi>K</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:mrow></mml:math> decreases and takes on values that are lower than would be expected by simply extrapolating the linear behavior. This decrease is consistent with earlier theoretical predictions for the behavior of <mml:math altimg=\"si1.svg\" display=\"inline\"><mml:mrow><mml:mo>log</mml:mo><mml:mrow><mml:mo>(</mml:mo><mml:mi>K</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:mrow></mml:math> at vapor-like densities but questions the relevance of some indirect experimental evidence obtained at low temperatures. Although the function described by <mml:math altimg=\"si1.svg\" display=\"inline\"><mml:mrow><mml:mo>log</mml:mo><mml:mrow><mml:mo>(</mml:mo><mml:mi>K</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:mrow></mml:math> vs <mml:math altimg=\"si6.svg\" display=\"inline\"><mml:mrow><mml:mo>log</mml:mo><mml:mrow><mml:mo>(</mml:mo><mml:msub><mml:mrow><mml:mi>ρ</mml:mi></mml:mrow><mml:mrow><mml:msub><mml:mrow><mml:mi mathvariant=\"normal\">H</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub><mml:mi mathvariant=\"normal\">O</mml:mi></mml:mrow></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:mrow></mml:math> is non-linear in the low density range, it can be considered well-behaved even at near critical conditions.","PeriodicalId":327,"journal":{"name":"Geochimica et Cosmochimica Acta","volume":"15 1","pages":""},"PeriodicalIF":4.5000,"publicationDate":"2024-10-16","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Assessing the validity and limits of linear density models for predicting dissociation–association equilibria in supercritical water\",\"authors\":\"Maximilian Schulze, Thomas Driesner, Sandro Jahn\",\"doi\":\"10.1016/j.gca.2024.10.008\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"A linear relationship between the logarithms of solute dissociation constants, <mml:math altimg=\\\"si1.svg\\\" display=\\\"inline\\\"><mml:mrow><mml:mo>log</mml:mo><mml:mrow><mml:mo>(</mml:mo><mml:mi>K</mml:mi><mml:mo>)</mml:mo></mml:mrow></mml:mrow></mml:math>, and the density of water, <mml:math altimg=\\\"si2.svg\\\" display=\\\"inline\\\"><mml:mo>log</mml:mo></mml:math> (<mml:math altimg=\\\"si274.svg\\\" display=\\\"inline\\\"><mml:msub><mml:mrow><mml:mi>ρ</mml:mi></mml:mrow><mml:mrow><mml:msub><mml:mrow><mml:mi mathvariant=\\\"normal\\\">H</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub><mml:mi mathvariant=\\\"normal\\\">O</mml:mi></mml:mrow></mml:msub></mml:math>), has empirically been demonstrated for decades and raised hope for an universal formalism to describe solute thermodynamic properties over wide ranges of temperature and density at supercritical conditions. Yet, neither a theoretical foundation nor an assessment of the ranges of validity have been presented. Here, we use classical molecular dynamics (MD) simulations as a complementary tool to assess the validity of this linear relationship for the example of NaCl and reveal its limits at water densities below ca. 0.3<ce:hsp sp=\\\"0.16667\\\"></ce:hsp>g<ce:hsp sp=\\\"0.16667\\\"></ce:hsp>cm<ce:sup loc=\\\"post\\\">−3</ce:sup>. The derivative <mml:math altimg=\\\"si4.svg\\\" display=\\\"inline\\\"><mml:mrow><mml:mi>∂</mml:mi><mml:mo>log</mml:mo><mml:mrow><mml:mo>(</mml:mo><mml:mi>K</mml:mi><mml:mo>)</mml:mo></mml:mrow><mml:mo>/</mml:mo><mml:mi>∂</mml:mi><mml:mo>log</mml:mo><mml:mrow><mml:mo>(</mml:mo><mml:msub><mml:mrow><mml:mi>ρ</mml:mi></mml:mrow><mml:mrow><mml:msub><mml:mrow><mml:mi mathvariant=\\\"normal\\\">H</mml:mi></mml:mrow><mml:mrow><mml:mn>2</mml:mn></mml:mrow></mml:msub><mml:mi mathvariant=\\\"normal\\\">O</mml:mi></mml:mrow></mml:msub><mml:mo>)</mml:mo></mml:mrow></mml:mrow></mml:math> is calculated based on the volume of reaction and water compressibility derived from the simulations performed in the isothermal–isobaric ensemble at 673<ce:hsp sp=\\\"0.16667\\\"></ce:hsp>K. 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引用次数: 0

摘要

几十年来,溶质解离常数 log(K) 的对数与水的密度 log (ρH2O) 之间的线性关系已通过经验得到证实,并使人们希望有一种通用的形式来描述超临界条件下温度和密度范围很宽的溶质热力学性质。然而,无论是理论基础还是对有效范围的评估都尚未提出。在此,我们使用经典分子动力学(MD)模拟作为补充工具,以 NaCl 为例,评估这种线性关系的有效性,并揭示其在水密度低于约 0.3gcm-3 时的极限。导数∂log(K)/∂log(ρH2O)是根据在 673K 等温等压模拟中得出的反应体积和水的可压缩性计算得出的。我们的结果证实了在实验研究的密度范围内 log(K) 与 log(ρH2O) 的线性关系,并表明这种线性关系也延伸到了更高的密度。然而,在密度较低时,log(K) 会下降,其值低于简单推断线性行为的预期值。这种下降与早先关于 log(K) 在类似蒸汽密度下的行为的理论预测一致,但对在低温下获得的一些间接实验证据的相关性提出了质疑。虽然 log(K) vs log(ρH2O) 所描述的函数在低密度范围内是非线性的,但即使在接近临界的条件下,它也可以被认为是乖巧的。
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Assessing the validity and limits of linear density models for predicting dissociation–association equilibria in supercritical water
A linear relationship between the logarithms of solute dissociation constants, log(K), and the density of water, log (ρH2O), has empirically been demonstrated for decades and raised hope for an universal formalism to describe solute thermodynamic properties over wide ranges of temperature and density at supercritical conditions. Yet, neither a theoretical foundation nor an assessment of the ranges of validity have been presented. Here, we use classical molecular dynamics (MD) simulations as a complementary tool to assess the validity of this linear relationship for the example of NaCl and reveal its limits at water densities below ca. 0.3gcm−3. The derivative log(K)/log(ρH2O) is calculated based on the volume of reaction and water compressibility derived from the simulations performed in the isothermal–isobaric ensemble at 673K. Our results corroborate the linear dependence of log(K) vs. log(ρH2O) in the experimentally studied density range and suggest that the linear dependence also extends to higher densities. However, towards lower densities, log(K) decreases and takes on values that are lower than would be expected by simply extrapolating the linear behavior. This decrease is consistent with earlier theoretical predictions for the behavior of log(K) at vapor-like densities but questions the relevance of some indirect experimental evidence obtained at low temperatures. Although the function described by log(K) vs log(ρH2O) is non-linear in the low density range, it can be considered well-behaved even at near critical conditions.
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来源期刊
Geochimica et Cosmochimica Acta
Geochimica et Cosmochimica Acta 地学-地球化学与地球物理
CiteScore
9.60
自引率
14.00%
发文量
437
审稿时长
6 months
期刊介绍: Geochimica et Cosmochimica Acta publishes research papers in a wide range of subjects in terrestrial geochemistry, meteoritics, and planetary geochemistry. The scope of the journal includes: 1). Physical chemistry of gases, aqueous solutions, glasses, and crystalline solids 2). Igneous and metamorphic petrology 3). Chemical processes in the atmosphere, hydrosphere, biosphere, and lithosphere of the Earth 4). Organic geochemistry 5). Isotope geochemistry 6). Meteoritics and meteorite impacts 7). Lunar science; and 8). Planetary geochemistry.
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