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  2. Soil thermal properties - Wikipedia

    en.wikipedia.org/wiki/Soil_thermal_properties

    Apart from the basic soil composition, which is constant at one location, soil thermal properties are strongly influenced by the soil volumetric water content, volume fraction of solids and volume fraction of air. Air is a poor thermal conductor and reduces the effectiveness of the solid and liquid phases to conduct heat.

  3. Spring (hydrology) - Wikipedia

    en.wikipedia.org/wiki/Spring_(hydrology)

    Geysers are a type of hot spring where steam is created underground by trapped superheated groundwater resulting in recurring eruptions of hot water and steam. [6] Carbonated springs, such as Soda Springs Geyser, are springs that emit naturally occurring carbonated water, due to dissolved carbon dioxide in the water content. They are sometimes ...

  4. Under-soil heating - Wikipedia

    en.wikipedia.org/wiki/Under-soil_heating

    The system consists of a network of corrosion-resistant metal pipes laid beneath the soil or turf. These pipes are connected to a central heating unit that contains energy-efficient heating elements. [8] When the system is activated, the heating unit circulates warm water or air through the pipes, effectively raising the soil temperature ...

  5. Hot spring - Wikipedia

    en.wikipedia.org/wiki/Hot_spring

    The related term "warm spring" is defined as a spring with water temperature less than a hot spring by many sources, although Pentecost et al. (2003) suggest that the phrase "warm spring" is not useful and should be avoided. [9] The US NOAA Geophysical Data Center defines a "warm spring" as a spring with water between 20 and 50 °C (68 and 122 ...

  6. Frost heaving - Wikipedia

    en.wikipedia.org/wiki/Frost_heaving

    The dominant cause of soil displacement in frost heaving is the development of ice lenses. During frost heave, one or more soil-free ice lenses grow, and their growth displaces the soil above them. These lenses grow by the continual addition of water from a groundwater source that is lower in the soil and below the freezing line in the soil.

  7. Soil moisture - Wikipedia

    en.wikipedia.org/wiki/Soil_moisture

    The amount of water already in the soil; Soil temperature. Warm soils take in water faster while frozen soils such as permafrost may not be able to absorb depending on the type of freezing. [37] Water infiltration rates range from 0.25 cm per hour for high clay soils to 2.5 cm per hour for sand and well stabilized and aggregated soil structures ...

  8. Hot Water Bottles and Other Old-Fashioned Ways to Keep Warm ...

    www.aol.com/news/2011-02-02-hot-water-bottles...

    How it works: boil water, pour into a hot water bottle and slip it in between the sheets of your bed (perhaps down by the feet) a few minutes prior to bedtime. Instead of bracing for those first ...

  9. Ground-coupled heat exchanger - Wikipedia

    en.wikipedia.org/wiki/Ground-coupled_heat_exchanger

    Generally, dry-and-low-density soil with little or no ground shade will yield the least benefit, while dense damp soil with considerable shade should perform well. A slow drip watering system may improve thermal performance. Damp soil in contact with the cooling tube conducts heat more efficiently than dry soil.