Glossary
Air flow/infiltration: The movement that carries moist air into
and through materials. Air flow depends on the difference between indoor
and outdoor pressures, wind speed and direction as well as the permeability
of materials.
Bulk water: The large quantity of moisture from roof and ground run-off
that can enter into a building either above grade or below grade.
Capillary action: The force that moves moisture through the pore
structure of materials. Generally referred to as rising damp, moisture
at or below the foundation level will rise vertically in a wall to a height
at which the rate of evaporation balances the rate at which it can be drawn
up by capillary forces.
Condensation: The physical process by which water vapor is transformed
into a liquid when the relative humidity of the air reaches 100% and the
excess water vapor forms, generally as droplets, on the colder adjacent
surface.
Convection: Heat transfer through the atmosphere by a difference
in force or air pressure is one type of air transport. Sometimes referred
to as the "stack effect," hotter less dense air will rise, colder
dense air will fall creating movement of air within a building.
Dewpoint: The temperature at which water vapor condenses when the
air is cooled at a constant pressure and constant moisture content.
Diffusion: The movement of water vapor through a material. Diffusion
depends on vapor pressure, temperature, relative humidity, and the permeability
of a material.
Evaporation: The transformation of liquid into a vapor, generally
as a result of rise of temperature, is the opposite of condensation. Moisture
in damp soil, such as in a crawl space, can evaporate into the air, raise
the relative humidity in that space, and enter the building as a vapor.
Ground moisture: The saturated moisture in the ground as a result
of surface run-off and naturally occuring water tables. Ground moisture
can penetrate through cracks and holes in foundation walls or can migrate
up from moisture under the foundation base.
Monitoring instrumentation: These devices are generally used for
long term diagnostic analysis of a problem, or to measure the performance
of a treatment, or to measure changes of conditions or environment. In-wall
probes or sensors are often attached to data-loggers which can be down-loaded
into computers.
Permeability: A characteristic of porosity of a material generally
listed as the rate of diffusion of a pressurized gas through a material.
The pore structure of some materials allows them to absorb or adsorb more
moisture than other materials. Limestones are generally more permeable
than granites.
Relative humidity (RH): Dampness in the air is measured as the percent
of water vapor in the air at a specific temperature relative to the amount
of water vapor that can be held in a vapor form at that specific temperature.
Survey instrumentation: technical instrumentation that is used on-site
to provide quick readings of specific physical conditions. Generally these
are hand-held survey instruments, such as moisture, temperature and relative
humidity readers, dewpoint sensors, and fiber optic boroscopes.