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
January | | 129 | 206 | 166 | 91 | 39
February | | 244 | 283 | 315 | 79 | 45
March | | 455 | 405 | 133 | 67 | 34
April | | 281 | 84 | 40 | 47 | 21
| | | | | |
May | | 134 | 68 | 56 | 35 | 48
June | | 110 | 68 | 22 | 56 | 50
July | | 25 | 50 | 39 | 106 | 22
August | | 36 | 38 | 146 | 72 | 28
| | | | | |
September | 6,850 | 42 | 40 | 37 | 98 | 67
October | 1,216 | 116 | 60 | 30 | 33 | 28
November | 161 | 175 | 64 | 37 | 27 | 122
December | 111 | 364 | 84 | 67 | 24 |
+--------+--------+--------+--------+--------+--------
Average | 2,084 | 176 | 121 | 91 | 61 | 46
| | | | | |
Average | | | | | |
efficiency | 91.55 | 98.31 | 98.91 | 98.72 | 99.41 | 98.95
CHEMNITZ WATER-WORKS.
The only other place which I have found where anything approaching
intermittent filtration of water is systematically employed is
Chemnitz, Germany. The method there used bears the same relation to
intermittent filtration as does broad irrigation of sewage to the
corresponding method of sewage treatment; that is, the principles
involved are mainly the same, but a much larger filtering area is used,
and the processes take place at a lower rate and under less close
control.
[Illustration: FIG. 17.—PLAN OF AREA USED FOR INTERMITTENT FILTRATION
AT CHEMNITZ.]
The water-works were built about twenty years ago by placing
thirty-nine wells along the Zwönitz River, connected by siphon pipes,
with a pumping-station which forced the water to an elevated reservoir
near the city (Fig. 17). The wells are built of masonry, 5 or 6 feet in
diameter and 10 or 12 feet deep, and are on the rather low bank of the
river. The material, with the exception of the surface soil, and loam
about 3 feet deep, is a somewhat mixed gravel with an effective size of
probably from 0.25 to 0.50 mm., so that water is able to pass through
it freely. The wells are, on an average, about 120 feet apart, and the
line is seven eighths of a mile long.
It was found that in dry times the ground-water level in the entire
neighborhood was lowered some feet below the level of the river without
either furnishing water enough or stopping the flow of the river below.
The channel of the river was so silted that, notwithstanding the porous
material, the water could not penetrate it to go toward the wells.
Public-domain text, read in full here on John Shaqi.
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