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  2. Damp (structural) - Wikipedia

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

    It often causes damage similar to damp in a building and often appears in similar places. This is because it occurs in the "dead air" pockets that accumulate in both horizontal and vertical corners (i.e. out of circulating air patterns). Mould growth caused by condensation in dead air pocket behind books

  3. Dust bunny - Wikipedia

    en.wikipedia.org/wiki/Dust_bunny

    Dust bunnies (or dustbunnies) are small clumps of dust that form under furniture and in corners that are not cleaned regularly. [ 1 ] [ 2 ] They are made of hair, lint , flakes of dead skin, spider webs , dust, and sometimes light rubbish and debris and are held together by static electricity and felt -like entanglement. [ 3 ]

  4. 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. The moisture laden air can penetrate into hidden ...

  5. A Ranked List of the COOLEST Influencer Bedrooms on the Internet

    www.aol.com/lifestyle/ranked-list-coolest...

    The Internet is saturated with home influencer content, so we've narrowed down the top 9 influencer bedrooms you should look to for inspiration.

  6. Ventilation (architecture) - Wikipedia

    en.wikipedia.org/wiki/Ventilation_(architecture)

    Poor ventilation in rooms is identified to significantly increase the localized moldy smell in specific places of the room including room corners. [11] There are three types of natural ventilation occurring in buildings: wind-driven ventilation , pressure-driven flows, and stack ventilation . [ 15 ]

  7. Lifting condensation level - Wikipedia

    en.wikipedia.org/wiki/Lifting_condensation_level

    The convective condensation level (CCL) results when strong surface heating causes buoyant lifting of surface air and subsequent mixing of the planetary boundary layer, so that the layer near the surface ends up with a dry adiabatic lapse rate. As the mixing becomes deeper, it will get to the point where the LCL of an air parcel starting at the ...