Some well types and water sources are more susceptible
to contamination than others.
Two major types of aquifers exist. "Confined" aquifers are protected
from surface contamination by a layer of low permeability material
(silt, clay or till). "Unconfined" aquifers do not have an impermeable layer overlying and protecting the aquifer and therefore are more vulnerable to surface contamination (the contaminants can
infiltrate into the ground and reach the aquifer). In the
Comox Valley eight of the fifteen know aquifers
are classified as vulnerable to contamination.
Water is "cleaned" naturally (through filtration and biological
processes) as it flows through the soil. However the amount of
contaminants removed by this process depends on the type of soil,
the type of contaminant, and the distance the water travels before
reaching the water table. Water moves quickly through coarse soils
(such as sand and gravel) and therefore these soils remove fewer
contaminants. Water moves more slowly through fine-textured soil
(such as peat, clay and silt) and therefore these soils are more
effective at removing contaminants before they reach the groundwater