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  2. Frost diagram - Wikipedia

    en.wikipedia.org/wiki/Frost_diagram

    Example of Frost diagram for the manganese species. A Frost diagram or Frost–Ebsworth diagram is a type of graph used by inorganic chemists in electrochemistry to illustrate the relative stability of a number of different oxidation states of a particular substance.

  3. Frost - Wikipedia

    en.wikipedia.org/wiki/Frost

    Frost is a thin layer of ice on a solid surface, which forms from water vapor that deposits onto a freezing surface. Frost forms when the air contains more water vapor than it can normally hold at a specific temperature.

  4. Frost weathering - Wikipedia

    en.wikipedia.org/wiki/Frost_weathering

    Frost weathering is a collective term for several mechanical weathering processes induced by stresses created by the freezing of water into ice. The term serves as an umbrella term for a variety of processes, such as frost shattering, frost wedging, and cryofracturing.

  5. Water - Wikipedia

    en.wikipedia.org/wiki/Water

    Water is an inorganic compound with the chemical ... frost is deposited on cold surfaces while snowflakes form by deposition on an aerosol ... Phase diagram of water.

  6. Phases of ice - Wikipedia

    en.wikipedia.org/wiki/Phases_of_ice

    An alternative formulation of the phase diagram for certain ices and other phases of water [13] Ice, water, and water vapour can coexist at the triple point , which is exactly 273.16 K (0.01 °C) at a pressure of 611.657 Pa .

  7. Weathering - Wikipedia

    en.wikipedia.org/wiki/Weathering

    This makes frost wedging, in which pore water freezes and its volumetric expansion fractures the enclosing rock, appear to be a plausible mechanism for frost weathering. Ice will simply expand out of a straight open fracture before it can generate significant pressure. Thus, frost wedging can only take place in small tortuous fractures. [5]

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  9. 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).