相关实验视频
Updated: May 20, 2025

08:01
The Diffusion of Passive Tracers in Laminar Shear Flow
Published on: May 1, 2018
8.4K
通过在不和多孔介质中的排水 - 嵌合周期来增强溶液的扩散
Ali Saeibehrouzi1, Petr Denissenko2, Ran Holtzman3
1School of Engineering, University of Warwick, Coventry, CV4 7AL, UK; Centre for Fluid and Complex Systems, Coventry University, Coventry, CV1 2NL, UK.
Water research
|May 17, 2025
概括
在不和的多孔介质中,连续的排水-沉积循环改变了溶液运输路径. 这些循环通过改变流体路径来非单调地影响溶液的传播,在几次循环后,影响变得可以忽略不计.
科学领域:
- 环境科学 环境科学
- 地质科学 地质科学
- 流体动力学 流体动力学
背景情况:
- 在不和多孔介质中的溶液运输对于环境和工程应用至关重要.
- 了解循环流体变化对溶液运输的影响仍然是一个挑战.
研究的目的:
- 为了研究连续的排水-沉浸循环对不和多孔介质中溶液运输的影响.
- 阐明这些循环改变溶液扩散和混合的机制.
主要方法:
- 集成微流体实验以确定流体分布.
- 高准确度的直接数值模拟用于模拟溶液运输.
- 分析移动和不移动路径以评估混合.
主要成果:
- 排水-阻塞循环通过改变通路体积和曲度来非单调地增加溶液的传播.
- 循环减少载体流体和,并增加由于hysteresis的路径长度.
- 循环对溶液混合的影响在1-2个循环后变得可以忽略不计.
结论:
- 流体相的周期变化显著影响不和多孔介质中的溶液运输动力学.
- 这项研究提供了关键的见解,污染物和营养物质的运输在波动的土壤含水量下.
- 这些发现有助于我们更好地了解地表下环境中的多相流和运输.
相关概念视频
Osmosis and Osmotic Pressure of Solutions
38.8K
A number of natural and synthetic materials exhibit selective permeation, meaning that only molecules or ions of a certain size, shape, polarity, charge, and so forth, are capable of passing through (permeating) the material. Biological cell membranes provide elegant examples of selective permeation in nature, while dialysis tubing used to remove metabolic wastes from blood is a more simplistic technological example. Regardless of how they may be fabricated, these materials are generally...
38.8K
Theories of Dissolution: Diffusion Layer Model
653
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...
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...
653
Solution Equilibrium and Saturation
18.3K
Imagine adding a small amount of sugar to a glass of water, stirring until all the sugar has dissolved, and then adding a bit more. You can repeat this process until the sugar concentration of the solution reaches its natural limit, a limit determined primarily by the relative strengths of the solute-solute, solute-solvent, and solvent-solvent attractive forces. You can be certain that you have reached this limit because, no matter how long you stir the solution, undissolved sugar remains. The...
18.3K
Precipitation Processes
350
The experimental conditions in a gravimetric analysis should be optimized to maximize the particle size and purity of the obtained precipitate. Ideally, the concentration of the precipitating reagent should be low with effective stirring to maintain low relative supersaturation for the growth of large crystals. In homogeneous precipitation, the precipitant is slowly generated by a chemical reaction in the solution to avoid local reagent excesses. For example, urea decomposes gradually to...
350
Theories of Dissolution: The Danckwerts' Model and Interfacial Barrier Model
256
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...
256
Solubility Equilibria: Overview
570
When a substance such as sodium chloride is added to water, it dissolves, forming an aqueous solution. The extent of dissolution is called solubility. The process of dissolution can exist in equilibrium, just like other chemical processes. Solubility equilibria are also called precipitation equilibria because the process of solubility can be reversible. The reverse of the solubility process is called precipitation.
Solubility is important in biological and environmental processes. A notable...
Solubility is important in biological and environmental processes. A notable...
570

