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  2. Regelation - Wikipedia

    en.wikipedia.org/wiki/Regelation

    Regelation is the phenomenon of ice melting under pressure and refreezing when the pressure is reduced. This can be demonstrated by looping a fine wire around a block of ice, with a heavy weight attached to it. The pressure exerted on the ice slowly melts it locally, permitting the wire to pass through the entire block.

  3. Pressure melting point - Wikipedia

    en.wikipedia.org/wiki/Pressure_melting_point

    The pressure melting point of ice is the temperature at which ice melts at a given pressure. The pressure melting point is nearly a constant 0 °C at pressures above the triple point at 611.7 Pa, where water can exist in only the solid or liquid phases, through atmospheric pressure (100 kPa) until about 10 MPa. With increasing pressure above 10 ...

  4. Simon–Glatzel equation - Wikipedia

    en.wikipedia.org/wiki/Simon–Glatzel_equation

    However, at very high pressures higher melting temperatures are generally observed as the liquid usually occupies a larger volume than the solid making melting more thermodynamically unfavorable at elevated pressure. If the liquid has a smaller volume than the solid (as for ice and liquid water) a higher pressure leads to a lower melting point.

  5. Phases of ice - Wikipedia

    en.wikipedia.org/wiki/Phases_of_ice

    The resulting form is metastable at room pressure while under 120 K (−153 °C; −244 °F), but collapses into ice I h (ordinary ice) when brought above 130 K (−143 °C; −226 °F). [79] The crystal structure is hexagonal in nature, and the pores are helical channels with a diameter of about 6.10 Å (6.10 × 10 −10 m; 2.40 × 10 −8 in).

  6. Phase diagram - Wikipedia

    en.wikipedia.org/wiki/Phase_diagram

    The pressure on a pressure-temperature diagram (such as the water phase diagram shown above) is the partial pressure of the substance in question. 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 ...

  7. Ice - Wikipedia

    en.wikipedia.org/wiki/Ice

    Different stages of ice melt in a pond The melting of floating ice. Ablation of ice refers to both its melting and its dissolution. [103] The melting of ice entails the breaking of hydrogen bonds between the water molecules. The ordering of the molecules in the solid breaks down to a less ordered state and the solid melts to become a liquid.

  8. Tetens equation - Wikipedia

    en.wikipedia.org/wiki/Tetens_equation

    where temperature T is in degrees Celsius (°C) and saturation vapor pressure P is in kilopascals (kPa). According to Monteith and Unsworth, "Values of saturation vapour pressure from Tetens' formula are within 1 Pa of exact values up to 35 °C." Murray (1967) provides Tetens' equation for temperatures below 0 °C: [3]

  9. Enthalpy–entropy chart - Wikipedia

    en.wikipedia.org/wiki/Enthalpy–entropy_chart

    An enthalpy–entropy chart, also known as the H–S chart or Mollier diagram, plots the total heat against entropy, [1] describing the enthalpy of a thermodynamic system. [2] A typical chart covers a pressure range of 0.01–1000 bar , and temperatures up to 800 degrees Celsius . [ 3 ]