The filtration of public water-supplies: Third edition, revised and enlarged.Hazen, Allen
Science
The filtration of public water-supplies: Third edition, revised and enlarged.
Hazen, Allen
Filters and filtration; Water-supply
The depth of gravel likely to be adopted as a result of this
calculation, when the drains are not too far apart, will be much less
than that actually used in most European works, but as the two feet or
more there employed are, I believe, simply the result of speculation,
there is no reason for following the precedent where calculations show
that a smaller quantity is adequate.
The reason for recommending a thin lower layer of coarse gravel, which
alone is assumed to provide for the lateral movement of the water,
is that if more than about six inches of gravel is required to give a
satisfactory resistance, it will almost always be cheaper to use more
drains instead of more gravel; and the reason for recommending thinner
upper layers for preventing the sand from settling into the coarse
gravel is that no failures of this portion of filters are on record,
and in the few instances where really thin layers have been used the
results have been entirely satisfactory. In Königsberg filters were
built by Frühling,[7] in which the sand was supported by five layers
of gravel of increasing sizes, respectively 1.2, 1.2, 1.6, 2.0, 3.2,
or, together, 9.2 inches thick, below which there were an average of
five inches of coarse gravel. These were examined after eight years of
operation and found to be in perfect order.
At the Lawrence Experiment Station filters have been repeatedly
constructed with a total depth of supporting gravel layers not
exceeding six inches, and among the scores of such filters there has
not been a single failure, and so far as they have been dug up there
has never been found to have been any movement whatever of the sand
into the gravel. The Lawrence city filter, built with corresponding
layers, has shown no signs of being inadequately supported. In
arranging the Lawrence gravel layers care has always been taken that no
material should rest on another material more than three or four times
as coarse as itself, and that each layer should be complete at every
point, so that by no possibility could two layers of greater difference
in size come together. And it is believed that if this is carefully
attended to, no trouble need be anticipated, however thin the single
layers may be.
UNDERDRAINS.
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