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  2. Phases of ice - Wikipedia

    en.wikipedia.org/wiki/Phases_of_ice

    Ice from a theorized superionic water may possess two crystalline structures. At pressures in excess of 50 GPa (7,300,000 psi) such superionic ice would take on a body-centered cubic structure. However, at pressures in excess of 100 GPa (15,000,000 psi) the structure may shift to a more stable face-centered cubic lattice.

  3. Ice drilling - Wikipedia

    en.wikipedia.org/wiki/Ice_drilling

    If the fluid is only used in the lower part of the hole, permeability is not an issue. Alternatively the hole can be cased down past the point where the firn turns to ice. If water is used as a drilling fluid, in cold enough temperatures, it will turn to ice in the surrounding snow and firn and seal the hole. [44]

  4. Capillary pressure - Wikipedia

    en.wikipedia.org/wiki/Capillary_pressure

    In fluid statics, capillary pressure is the pressure between two immiscible fluids in a thin tube (see capillary action), resulting from the interactions of forces between the fluids and solid walls of the tube. Capillary pressure can serve as both an opposing or driving force for fluid transport and is a significant property for research and ...

  5. Ice - Wikipedia

    en.wikipedia.org/wiki/Ice

    Ice is still used to cool and preserve food in portable coolers. [112] Ice cubes or crushed ice can be used to cool drinks. As the ice melts, it absorbs heat and keeps the drink near 0 °C (32 °F). [141] Ice can be used as part of an air conditioning system, using battery- or solar-powered fans to blow hot air over the

  6. Pumpable ice technology - Wikipedia

    en.wikipedia.org/wiki/Pumpable_ice_technology

    Pumpable ice can be produced in one of two ways: either by mixing crushed ice with a liquid or by freezing water within a liquid. The primary way is to manufacture commonly used forms of crystal solid ice, such as plate, tube, shell or flake ice, by crushing and mixing it with water. This mixture of different ice concentrations and particle

  7. Glacier - Wikipedia

    en.wikipedia.org/wiki/Glacier

    Ice flows around these obstacles by melting under the high pressure on their stoss side; the resultant meltwater is then forced into the cavity arising in their lee side, where it re-freezes. [40] As well as affecting the sediment stress, fluid pressure (p w) can affect the friction between the glacier and the bed. High fluid pressure provides ...

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    The search engine that helps you find exactly what you're looking for. Find the most relevant information, video, images, and answers from all across the Web.

  9. Properties of water - Wikipedia

    en.wikipedia.org/wiki/Properties_of_water

    The melting point of ice is 0 °C (32 °F; 273 K) at standard pressure; however, pure liquid water can be supercooled well below that temperature without freezing if the liquid is not mechanically disturbed. It can remain in a fluid state down to its homogeneous nucleation point of about 231 K (−42 °C; −44 °F). [52]