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  2. Phases of ice - Wikipedia

    en.wikipedia.org/wiki/Phases_of_ice

    Virtually all ice in the biosphere is ice I h (pronounced: ice one h, also known as ice-phase-one). Ice I h exhibits many peculiar properties that are relevant to the existence of life and regulation of global climate. [138] For instance, its density is lower than that of liquid water.

  3. Thermochemical equation - Wikipedia

    en.wikipedia.org/wiki/Thermochemical_equation

    In thermochemistry, a thermochemical equation is a balanced chemical equation that represents the energy changes from a system to its surroundings.One such equation involves the enthalpy change, which is denoted with In variable form, a thermochemical equation would appear similar to the following:

  4. Enthalpy change of solution - Wikipedia

    en.wikipedia.org/wiki/Enthalpy_change_of_solution

    Dissolution by most gases is exothermic. That is, when a gas dissolves in a liquid solvent, energy is released as heat, warming both the system (i.e. the solution) and the surroundings. The temperature of the solution eventually decreases to match that of the surroundings.

  5. Differential scanning calorimetry - Wikipedia

    en.wikipedia.org/wiki/Differential_scanning...

    This transition from amorphous solid to crystalline solid is an exothermic process, and results in a peak in the DSC signal. As the temperature increases the sample eventually reaches its melting temperature (T m). The melting process results in an endothermic peak in the DSC curve.

  6. Thermochemistry - Wikipedia

    en.wikipedia.org/wiki/Thermochemistry

    The temperature of the chamber is monitored either using a thermometer or thermocouple, and the temperature plotted against time to give a graph from which fundamental quantities can be calculated. Modern calorimeters are frequently supplied with automatic devices to provide a quick read-out of information, one example being the differential ...

  7. Reaction calorimeter - Wikipedia

    en.wikipedia.org/wiki/Reaction_calorimeter

    This method allows for precise temperature control, even during strongly exothermic or endothermic events, as additional cooling can be achieved by increasing the area over which heat is exchanged. This system is generally more accurate than heat balance calorimetry, as changes in the delta temperature (T out - T in ) are magnified by keeping ...

  8. Ice core may hold answers to mysteries of Earth’s past

    www.aol.com/ice-core-may-hold-answers-172341016.html

    Air bubbles and particles trapped inside the ice could also reveal why the planet’s ice ages suddenly became longer and more intense about 1 million years ago, which may have caused ancient ...

  9. Cooling curve - Wikipedia

    en.wikipedia.org/wiki/Cooling_curve

    A cooling curve is a line graph that represents the change of phase of matter, typically from a gas to a solid or a liquid to a solid. The independent variable (X-axis) is time and the dependent variable (Y-axis) is temperature. [1] Below is an example of a cooling curve used in castings.