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関連する概念動画

Theories of Dissolution: The Danckwerts' Model and Interfacial Barrier Model01:09

Theories of Dissolution: The Danckwerts' Model and Interfacial Barrier Model

Various dissolution theories provide insight into the factors that influence the dissolution rate. Danckwerts' Model suggests that turbulence, rather than a stagnant layer, characterizes the dissolution medium at the solid-liquid interface. In this model, the agitated solvent contains macroscopic packets that move to the interface via eddy currents, facilitating the absorption and delivery of the drug to the bulk solution. The regular replenishment of solvent packets maintains the concentration...
Theories of Dissolution: Diffusion Layer Model01:15

Theories of Dissolution: Diffusion Layer Model

Dissolution, the process by which drug particles dissolve in a solvent, is explained by the diffusion layer model, a theoretical framework that simulates the absorption of oral drugs and allows us to analyze experimental data.
This process starts with a thin layer, saturated with the drug, forming at the interface between the solid and liquid. The solute then diffuses from this layer into the main solution. The Noyes-Whitney equation suggests that the rate of dissolution relies on the diffusion...
The Debye–Hückel Theory of Electrolyte Solutions01:27

The Debye–Hückel Theory of Electrolyte Solutions

The Debye–Hückel theory, established by Peter Debye and Erich Hückel in 1923, is a fundamental concept in physical chemistry. It provides an understanding of the behavior of strong electrolytes in solution, particularly explaining their deviations from ideal behavior.The theory is based on Coulombic interactions (the attraction or repulsion between charged particles) between ions in solution. In an ionic solution, oppositely charged ions tend to attract each other. This means that cations...
Thermodynamics: Activity Coefficient01:24

Thermodynamics: Activity Coefficient

Activity is the measure of the effective concentration of the species in solution. It can be expressed as the product of the molar concentration of the species and its activity coefficient. The activity coefficient is a dimensionless quantity and depends on the total ionic strength of the solution.
The activity coefficient is a measure of the deviation from ideal behavior. When the ionic strength of the solution is minimal, the activity coefficient of an ionic species is close to unity, making...
Factors Affecting Activity Coefficient01:17

Factors Affecting Activity Coefficient

The extended Debye-Hückel equation indicates that the activity coefficient of an ion in an aqueous solution at 25°C depends on three partially interdependent properties: the ionic strength of the solution, the charge of the ion, and the ion size. 
The activity coefficient value for an ion is close to one when the solution has almost zero ionic strength, i.e., when the solution shows close to ideal behavior. As the ionic strength of the solution increases from 0 to 0.1 mol/L, a decrease in the...
Debye–Huckel–Onsager Conductance Equation01:28

Debye–Huckel–Onsager Conductance Equation

The Debye-Hückel-Onsager equation is a cornerstone of physical chemistry, providing a method to determine the molar conductance (Λm) and molar conductance at infinite dilution (Λ°m) for uni-univalent electrolytes.Uni-univalent electrolytes are electrolytes that dissociate in solution to produce one cation with a +1 charge and one anion with a –1 charge per formula unit.This equation addresses two crucial phenomena: the asymmetry effect and the electrophoretic effect. According to this equation,...

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関連する実験動画

Updated: Jul 12, 2026

Analyzing Melts and Fluids from Ab Initio Molecular Dynamics Simulations with the UMD Package
06:37

Analyzing Melts and Fluids from Ab Initio Molecular Dynamics Simulations with the UMD Package

Published on: September 17, 2021

シリケート鉱物の拡散係数を予測するための経験的モデル.

S M Fortier, B J Giletti

    Science (New York, N.Y.)
    |September 29, 1989
    PubMed
    まとめ

    経験的モデルは,水熱条件下でシリケート鉱物における酸素拡散を予測する. このモデルは,地質学的プロセスを理解するために不可欠な拡散係数を正確に推定します.

    科学分野:

    • 地質化学 地質化学
    • ミネラル物理学 ミネラル物理学

    背景:

    • 拡散運動学は,地質系における鉱物変異と元素輸送を理解するために重要である.
    • 以前のモデルには,特定の熱水条件下での経験的検証が欠けていたことが多い.

    研究 の 目的:

    • シリケート鉱物における酸素拡散運動の実証モデルを確立する.
    • 水熱条件下でのモデルの予測能力を検証する.

    主な方法:

    • 実験データに基づく経験的方程式の開発.
    • モデルを773〜1073Kの温度範囲と100MPaの水圧でテストする.

    主要な成果:

    • 確立されたモデル: log D = アルファ + (ベータ/T) + (ガンマ + (デルタ/T)) Z.
    • このモデルは,酸素拡散の再生可能性の2の因数内で拡散係数を予測します.
    • 予備的なデータは,シリケート中のアルゴン拡散に適用できると示唆しています.

    結論:

    • 開発された経験的モデルは,シリケートにおける酸素拡散を予測するための信頼できるツールを提供します.
    • モデルの精度は実験的な限界内にあり,その実用的な有用性を高めています.

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    Analyzing Melts and Fluids from Ab Initio Molecular Dynamics Simulations with the UMD Package
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    Fluid-cell Raman Spectroscopy for operando Studies of Reaction and Transport Phenomena during Silicate Glass Corrosion

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    In Situ Monitoring of Diffusion of Guest Molecules in Porous Media Using Electron Paramagnetic Resonance Imaging
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    In Situ Monitoring of Diffusion of Guest Molecules in Porous Media Using Electron Paramagnetic Resonance Imaging

    Published on: September 2, 2016

  • アルゴンなどの他の拡散種へのモデルの潜在的な拡張が示されています.