=230. Introduction of Water to Intermittent Filters.=—Where
intermittent filters are used it is of the greatest importance to
conduct the water to them so as not to disturb the sand on their
surfaces. This can readily be done in a number of ways. If the shape
of the filter is not oblong, it will be advisable to form a number of
main drains or passages in the sand from which smaller depressions or
passages near together may lead the water to all parts of the surface.
The flowing of the first water through these depressions will permit
the entire surface to be covered so gradually as not to disturb the
sand grains, and it is essential that such means or their equivalent
be employed. If the filter is long and narrow in shape, the main
ditch along one of the longer sides, with depressions at right angles
to it or across the filter and near together, will be sufficient
to accomplish the desired purpose. Obviously when filters are not
intermittently used such precautions are not needed.
=231. Effect of Low Temperature.=—In the early days of the use of
sand filters in this country it was frequently supposed that the low
temperature of the winter caused decreased bacterial purification and a
decrease in power to reduce organic material. It now appears that such
is not the case. The effects of low temperature, such as is experienced
in winters of this climate, may be overcome by temporarily covering the
filters so that heavy ice cannot form and produce disturbances in one
way or another prejudicial to efficiency of operation. The agencies
which operate to reduce efficiency in cold weather are no longer
believed to be those due to low temperature. They are rather indirect
and mechanical, and may be readily overcome by the prevention of the
formation of ice.
=232. Choice of Intermittent or Continuous Filtration.=—The process of
slow sand filtration when continuous has been shown by experience to
be entirely effective for ordinary potable waters, but in those cases
where the amount of dissolved oxygen may be low and where the amount
of organic matter is relatively high it may be advisable to resort to
intermittent filtration. Neither method, however, can be depended upon
to render potable a water which has been robbed of its free oxygen
by an excessive amount of contaminated organic matter. Nor can these
processes be expected to remove coloring matter produced by peaty
soils or other conditions in which large amounts of vegetable matter
have been absorbed by the water. The methods, therefore, have their
limitations, although their field of application is sufficiently wide
to cover nearly all classes of potable water.
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