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  2. Interstitial condensation - Wikipedia

    en.wikipedia.org/wiki/Interstitial_condensation

    Interstitial condensation is a type of condensation that may occur within an enclosed wall, roof or floor cavity structure, which can create dampening.. When moisture-laden air at dew point temperature penetrates inside a cavity of the structure, it condenses into liquid water on that surface.

  3. Damp (structural) - Wikipedia

    en.wikipedia.org/wiki/Damp_(structural)

    Condensation comes from water vapour within the building. Common sources may include cooking, bathing, dishwashers, etc. The moisture in the air condenses on cold surfaces, sometimes inside the walls called interstitial condensation. Buildings with poorly insulated walls are very prone to this problem.

  4. Condensation - Wikipedia

    en.wikipedia.org/wiki/Condensation

    Condensation on a window during a rain shower. Condensation in building construction is an unwanted phenomenon as it may cause dampness, mold health issues, wood rot, corrosion, weakening of mortar and masonry walls, and energy penalties due to increased heat transfer. To alleviate these issues, the indoor air humidity needs to be lowered, or ...

  5. Air well (condenser) - Wikipedia

    en.wikipedia.org/wiki/Air_well_(condenser)

    An air well or aerial well is a structure or device that collects water by promoting the condensation of moisture from air. [1] Designs for air wells are many and varied, but the simplest designs are completely passive, require no external energy source and have few, if any, moving parts.

  6. Can You Keep Mums Indoors? Here's How to Overwinter Them - AOL

    www.aol.com/keep-mums-indoors-heres-overwinter...

    If you have a cold weather snap coming and expect the weather to warm up again after that, bring your potted fall mums indoors for the freezing temps and put them back out on display when the ...

  7. Lifting condensation level - Wikipedia

    en.wikipedia.org/wiki/Lifting_condensation_level

    If the air parcel is lifting further beyond the LCL, water vapor in the air parcel will begin condensing, forming cloud droplets. (In the real atmosphere, it is usually necessary for air to be slightly supersaturated, normally by around 0.5%, before condensation occurs; this translates into about 10 meters or so of additional lifting above the ...

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