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  2. Brinicle - Wikipedia

    en.wikipedia.org/wiki/Brinicle

    When water freezes, most impurities are excluded from the water crystals; even ice from seawater is relatively fresh compared to the seawater from which it is formed. As a result of forcing the impurities out (such as salt and other ions) sea ice is very porous and spongelike, quite different from the solid ice produced when fresh water freezes.

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

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

    Ice has a semi-liquid surface layer; When you mix salt onto that layer, it slowly lowers its melting point.. The more surface area salt can cover, the better the chances for melting ice.. Ice ...

  4. List of fictional elements, materials, isotopes and subatomic ...

    en.wikipedia.org/wiki/List_of_fictional_elements...

    A more stable polymorph of water than common ice (Ice I h), which instead of melting when above 0°C (32°F), only melts at 45.8°C (114.4°F). When ice-nine comes in contact with liquid water below 45.8°C, it acts as a seed crystal, and causes the solidification of the entire body of water, which quickly crystallizes as more ice-nine ...

  5. Brine rejection - Wikipedia

    en.wikipedia.org/wiki/Brine_rejection

    The salts do not fit in the crystal structure of water ice, so the salt is expelled. Since the oceans are salty, this process is important in nature. Salt rejected by the forming sea ice drains into the surrounding seawater, creating saltier, denser brine. The denser brine sinks, influencing ocean circulation.

  6. Halite - Wikipedia

    en.wikipedia.org/wiki/Halite

    Halite is also often used both residentially and municipally for managing ice. Because brine (a solution of water and salt) has a lower freezing point than pure water, putting salt or saltwater on ice that is below 0 °C (32 °F) will cause it to melt—this effect is called freezing-point depression.

  7. Fog - Wikipedia

    en.wikipedia.org/wiki/Fog

    Fog is a visible aerosol consisting of tiny water droplets or ice crystals suspended in the air at or near the Earth's surface. [1] [2] Fog can be considered a type of low-lying cloud usually resembling stratus and is heavily influenced by nearby bodies of water, topography, and wind conditions.

  8. Salt deformation - Wikipedia

    en.wikipedia.org/wiki/Salt_deformation

    When comparing the tensional and compressional strength of wet salt and dry salt with other typical rocks at a strain rate of 10 −14 s −1, such as shale and quartzite, both wet and dry salt shows lower strength than the other rocks. [10] Wet salt is even weaker than dry salt: when the water content of rock salt exceeds 0.01%, the rock salt ...

  9. Road salt - Wikipedia

    en.wikipedia.org/wiki/Road_salt

    Road salt (also known as de-icing salt, rock salt, or snow salt) is a salt used mainly as an anti-slip agent in winter road conditions, but also to prevent dust and snow build-up on roads. [1] Various kinds of salts are used as road salt, but calcium chloride and sodium chloride (rock salt) are among the most common.