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Precipitation Processes01:12

Precipitation Processes

3.8K
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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States of Water01:23

States of Water

55.6K
Water exists in any one of the three classical states: solid (ice), liquid (water), and gas (steam or water vapor). The state of water depends on i) the intermolecular forces that draw molecules together and ii) the kinetic energy that leads to movements that pull them apart.
Water freezes when the intermolecular forces are greater than the kinetic energy. Unlike most other substances, water is less dense in its solid state than in its liquid state. This is because each water molecule can form...
55.6K
Design Example: Designing Water Slide01:18

Design Example: Designing Water Slide

532
When designing a water slide, controlling the speed of water flow is crucial for rider safety while maintaining an exciting experience. As water flows down the slide, gravity causes it to accelerate, with its speed at the bottom depending on the height from which it starts. The higher the slide, the more potential energy the water has at the top, which is converted into kinetic energy as it descends, increasing its speed.
Bernoulli's principle determines the water's velocity along the slide....
532
Precipitation and Co-precipitation01:17

Precipitation and Co-precipitation

3.7K
Precipitation and coprecipitation methods can be used to separate a mixture of ions in a solution. In qualitative inorganic analysis, ions that form sparingly soluble precipitates with the same reagent are separated based on the differences in solubility products. For example, consider the separation of Cu(II) and Fe(II) ions by precipitation as insoluble sulfides. First, copper(II) sulfide is precipitated by the addition of acidic H2S, where the dissociation of H2S is suppressed. Adding H2S...
3.7K
Dry Friction01:30

Dry Friction

773
Dry friction occurs between two solid surfaces in contact as they attempt to move relative to one another. In daily life, dry friction is encountered in various forms, such as when walking on the ground, sliding an object across a table, or rubbing hands together. Despite its ubiquity, the underlying mechanisms behind dry friction are not readily visible.
To illustrate this concept, imagine a wooden crate resting on a rough, non-uniform horizontal surface. When an external force is applied to...
773
Types of Coprecipitation01:10

Types of Coprecipitation

4.1K
Coprecipitation is the contamination of a precipitate by otherwise soluble species and occurs via different processes. In colloidal precipitates, coprecipitation occurs via surface adsorption. For instance, barium sulfate has a primary layer of adsorbed barium ions and a secondary layer of nitrate counterions. This results in contamination of the precipitate by barium nitrate.
Sometimes, ions in a crystal lattice can undergo isomorphous replacement by inclusions of similar charge and size. For...
4.1K

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Four Temporary Waterslide Designs Adapted to Different Slope Conditions to Encourage Child Socialization in Playgrounds
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Rain and Sun Create Slippery Layers in Eastern Pacific Fresh Pool.

Andrey Y Shcherbina1, Eric A D'Asaro1, Ramsey R Harcourt1

  • 1Applied Physics Laboratory, University of Washington, Seattle, WA, USA.

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|July 25, 2020
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Summary
This summary is machine-generated.

Ocean surface layers rapidly stratify due to warming and rainfall, creating a "slippery layer" that distorts wind-driven currents. Autonomous floats captured this dynamic upper-ocean behavior.

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Area of Science:

  • Oceanography
  • Physical Oceanography
  • Fluid Dynamics

Background:

  • Upper-ocean stratification significantly influences heat and momentum transfer.
  • Diurnal and daily weather events create complex vertical structures in the ocean surface boundary layer.
  • Understanding these processes is crucial for climate modeling and predicting ocean dynamics.

Purpose of the Study:

  • To observe and analyze the evolution of upper-ocean stratification and velocity.
  • To investigate the impact of diurnal warming and rainfall on near-surface ocean structure.
  • To document the formation and effects of the "slippery layer" phenomenon.

Main Methods:

  • Deployment of an autonomous Lagrangian float equipped with a high-resolution acoustic Doppler current profiler.
  • Continuous observation for over 100 days in the Eastern Pacific Fresh Pool (August-November 2016).
  • Measurement of temperature, salinity, velocity, turbulence, and internal wave components.

Main Results:

  • Convective mixing homogenized the water column nightly, but diurnal warming and rainfall created strong stratification in the upper 10 m daily.
  • This stratification was rapidly mixed into the bulk layer within hours.
  • Strong stratification decoupled near-surface waters, leading to accelerated flow (slippery layer) and distorted Ekman profiles.

Conclusions:

  • Autonomous Lagrangian floats provide valuable data on rapidly evolving ocean surface boundary layer processes.
  • The "slippery layer" effect significantly alters wind-driven current profiles.
  • High-resolution numerical modeling is needed for quantitative interpretation of these complex ocean dynamics.