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  2. Phases of ice - Wikipedia

    en.wikipedia.org/wiki/Phases_of_ice

    Amorphous ice is produced either by rapid cooling of liquid water to its glass transition temperature (about 136 K or −137 °C) in milliseconds (so the molecules do not have enough time to form a crystal lattice), or by compressing ordinary ice at low temperatures.

  3. Frigorific mixture - Wikipedia

    en.wikipedia.org/wiki/Frigorific_mixture

    A frigorific mixture may be used to obtain a liquid medium that has a reproducible temperature below ambient temperature. Such mixtures were used to calibrate thermometers. In chemistry a cooling bath may be used to control the temperature of a strongly exothermic reaction. A frigorific mixture may be used as an alternative to mechanical ...

  4. Ice - Wikipedia

    en.wikipedia.org/wiki/Ice

    The ice within permafrost is divided into four categories: pore ice, vein ice (also known as ice wedges), buried surface ice and intrasedimental ice (from the freezing of underground waters). [60] One example of ice formation in permafrost areas is aufeis - layered ice that forms in Arctic and subarctic stream valleys.

  5. Stefan problem - Wikipedia

    en.wikipedia.org/wiki/Stefan_problem

    Consider a semi-infinite one-dimensional block of ice initially at melting temperature = for [; +). The most well-known form of Stefan problem involves melting via an imposed constant temperature at the left hand boundary, leaving a region [ 0 ; s ( t ) ] {\displaystyle [0;s(t)]} occupied by water.

  6. Phase diagram - Wikipedia

    en.wikipedia.org/wiki/Phase_diagram

    A phase diagram in physical chemistry, engineering, mineralogy, and materials science is a type of chart used to show conditions (pressure, temperature, etc.) at which thermodynamically distinct phases (such as solid, liquid or gaseous states) occur and coexist at equilibrium.

  7. Frost heaving - Wikipedia

    en.wikipedia.org/wiki/Frost_heaving

    Photograph taken 21 March 2010 in Norwich, Vermont. Frost heaving (or a frost heave) is an upwards swelling of soil during freezing conditions caused by an increasing presence of ice as it grows towards the surface, upwards from the depth in the soil where freezing temperatures have penetrated into the soil (the freezing front or freezing boundary).

  8. How to Fix Your Frozen Pipes, According to Experts - AOL

    www.aol.com/lifestyle/keep-pipes-freezing-winter...

    When temperatures drop below 55 degrees, there's a risk of freezing. And if the water does freeze, your pipes could crack, warp, or even burst as the water stretches and then ultimately thaws ...

  9. 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.