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Boundary Layer Characteristics01:18

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When a fluid encounters a solid surface, a boundary layer forms due to the interaction between the fluid's motion and the stationary surface. This phenomenon is characterized by a thin region adjacent to the surface where viscous forces dominate, influencing the fluid's velocity profile. The development of the boundary layer begins at the leading edge of the surface and evolves as the fluid moves downstream.As the fluid flows over the surface, friction between the fluid and the wall slows down...
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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...
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Phase Transitions: Vaporization and Condensation02:39

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The physical form of a substance changes on changing its temperature. For example, raising the temperature of a liquid causes the liquid to vaporize (convert into vapor). The process is called vaporization—a surface phenomenon. Vaporization occurs when the thermal motion of the molecules overcome the intermolecular forces, and the molecules (at the surface) escape into the gaseous state. When a liquid vaporizes in a closed container, gas molecules cannot escape. As these gas phase...
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Capillarity in Fluid01:19

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Capillarity describes the movement of liquid in small spaces without external forces acting on it. The capillarity is driven by surface tension and adhesive interactions between the liquid and surrounding solid surfaces. This effect is often seen in narrow tubes, porous materials, and fine particles.
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Growth of solid conical structures during multistage drying of sessile poly(ethylene oxide) droplets.

Physical chemistry chemical physics : PCCP·2010
See all related articles
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Related Experiment Video

Updated: Apr 18, 2026

Film Control to Study Contributions of Waves to Droplet Impact Dynamics on Thin Flowing Liquid Films
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Classifying dynamic contact line modes in drying drops.

Kyle Anthony Baldwin1, David John Fairhurst

  • 1School of Physics and Astronomy, University of Nottingham, Nottingham NG7 2RD, UK. kyle.baldwin@nottingham.ac.uk.

Soft Matter
|January 20, 2015
PubMed
Summary
This summary is machine-generated.

This study reveals new droplet evaporation modes beyond constant contact radius (CCR) and constant contact angle (CCA). Droplet receding speed is inversely proportional to contact radius, enabling continuous alteration of evaporation pathways.

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Area of Science:

  • Fluid dynamics
  • Surface science
  • Materials science

Background:

  • Sessile droplet evaporation is typically classified as constant contact radius (CCR) or constant contact angle (CCA).
  • Existing models may not fully capture the diverse range of droplet evaporation behaviors observed in various systems.

Purpose of the Study:

  • To investigate alternative evaporation modes for sessile droplets.
  • To characterize new evaporative pathways and their underlying physics.

Main Methods:

  • Experimental analysis of poly(ethylene oxide) (PEO) solutions and blood.
  • Utilizing novel "clock-drop" imaging and dimensionless height-radius plots.
  • Applying scaling arguments to analyze droplet evolution.

Main Results:

  • Identified two new evaporation modes: "slowly receding" and "rapidly receding".
  • Demonstrated that receding speed is inversely proportional to the three-phase contact radius (R).
  • Showed that evaporation mode can be continuously tuned by varying a proportionality constant (A).

Conclusions:

  • Droplet evaporation is more complex than previously characterized by CCR and CCA modes alone.
  • The inverse relationship between receding speed and contact radius offers a new framework for understanding droplet evaporation.
  • New modes lead to distinct deposit morphologies, such as "doughnut" and "pillar" structures.