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  2. Brine rejection - Wikipedia

    en.wikipedia.org/wiki/Brine_rejection

    Once the ice reaches a critical thickness, roughly 15 cm, the concentration of salt ions in the liquid around the ice begins to increase, as leftover brine is rejected from the cells. [1] This increase is associated with the appearance of strong convective plumes, which flow from channels and within the ice and carry a significant salt flux.

  3. Why salt melts ice — and how to use it on your sidewalk - AOL

    www.aol.com/lifestyle/chemists-told-us-why-salt...

    A chemistry professor explains the science that makes salt a cheap and efficient way to lower freezing temperature. Skip to main content. 24/7 Help. For premium support please call: ...

  4. Cooling bath - Wikipedia

    en.wikipedia.org/wiki/Cooling_bath

    Cooling baths are generally one of two types: (a) a cold fluid (particularly liquid nitrogen, water, or even air) — but most commonly the term refers to (b) a mixture of 3 components: (1) a cooling agent (such as dry ice or ice); (2) a liquid "carrier" (such as liquid water, ethylene glycol, acetone, etc.), which transfers heat between the ...

  5. Freezing-point depression - Wikipedia

    en.wikipedia.org/wiki/Freezing-point_depression

    Workers spreading salt from a salt truck for deicing the road Freezing point depression is responsible for keeping ice cream soft below 0°C. [1]Freezing-point depression is a drop in the maximum temperature at which a substance freezes, caused when a smaller amount of another, non-volatile substance is added.

  6. Brinicle - Wikipedia

    en.wikipedia.org/wiki/Brinicle

    A brinicle (brine icicle, also known as an ice stalactite) is a downward-growing hollow tube of ice enclosing a plume of descending brine that is formed beneath developing sea ice. As seawater freezes in the polar ocean, salt brine concentrates are expelled from the sea ice, creating a downward flow of dense, extremely cold, saline water , with ...

  7. Ice–albedo feedback - Wikipedia

    en.wikipedia.org/wiki/Ice–albedo_feedback

    Thus, climate change models do not include them in their projections of 21st century climate change: experiments where they model their disappearance indicate that the total loss of the Greenland Ice Sheet adds 0.13 °C (0.23 °F) to global warming (with a range of 0.04–0.06 °C), while the loss of the West Antarctic Ice Sheet adds 0.05 °C ...

  8. Common-ion effect - Wikipedia

    en.wikipedia.org/wiki/Common-ion_effect

    The effect is commonly seen as an effect on the solubility of salts and other weak electrolytes. Adding an additional amount of one of the ions of the salt generally leads to increased precipitation of the salt, which reduces the concentration of both ions of the salt until the solubility equilibrium is reached. The effect is based on the fact ...

  9. Salt and ice challenge - Wikipedia

    en.wikipedia.org/wiki/Salt_and_ice_challenge

    The ions in sodium chloride (table salt) are heavily influenced by the molecular polarizability of the ice. [7] The difference between the spacing of the electrons in the table salt and ice causes this reaction. The melting point of ice is decreased due to the incorporation of table salt and this then causes a binding of the two substances. The ...