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
=Amsterdam.=—The water is derived from open canals in the dunes. These
canals have an aggregate length of about 15 miles, and drain about 6200
acres. The water, as it enters the canals from the fine dune-sand,
contains iron, but this is oxidized and deposited in the canals. The
water after collection is filtered. It has been suggested that by using
covered drains instead of open canals for collecting the water, the
filtration would be unnecessary; but, on the other hand, the cost of
building and maintaining covered drains in the very fine sand would be
much greater than that of the canals, and it is believed, also, that
the water so collected would contain iron, the removal of which might
prove as expensive as the present filtration. In 1887 filters were
built to take water from the river Vecht, but the city has refused to
allow the English company which owns the water-works to sell this water
for domestic purposes, and it is only used for public and manufacturing
purposes, only a fraction of the available supply being required.
Leyden, the Hague, and some other Dutch cities have supplies like the
dune supply of Amsterdam, and they are invariably filtered.
=Antwerp= is also supplied by an English company. The raw water is
drawn from a small tidal river, which at times is polluted by the
sewage of Brussels. It is treated by metallic iron in Anderson revolver
purifiers, and is afterward filtered at a rather low average rate. The
hygienic results are closely watched by the city authorities, and are
said to be satisfactory.
=Rotterdam.=—The raw water is drawn from the Maas, as the Dutch
call the main stream of the Rhine after it crosses their border. The
population upon the river and its tributaries in Switzerland, Germany,
Holland, France, and Belgium is very great; but the flow is also great,
and the low water flow is exceptionally large in proportion to the
average flow, on account of the melting snow in summer in Switzerland,
where it has its origin.
The original filters had wooden under-drains, and there was constant
trouble with crenothrix until the filters were reconstructed without
wood, since which time there has been no farther trouble. The present
filters are large and well managed. There is ample preliminary
sedimentation.
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