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
--------------+-----------------------------------------------
| Suspended Matters: Parts in 100,000.
Turbidity, +-----------------------------------------------
Platinum-wire | | River | River | River
Standard. | Settled | Waters, | Waters, | Waters,
| Waters. | Finest | Average | Coarsest
| | Sediment. | Sediment. | Sediment.
--------------+-----------+-----------+-----------+-----------
0.01 | 0.16 | | |
0.05 | 0.80 | 0.85 | 1.30 | 2.40
0.10 | 1.60 | 1.75 | 2.60 | 4.90
0.20 | 3.20 | 3.60 | 5.50 | 10.00
0.30 | 4.80 | 5.70 | 8.50 | 15.00
0.40 | 6.40 | 7.80 | 11.60 | 21.00
0.50 | 8.00 | 10.00 | 15.00 | 26.00
1.00 | 16.00 | 23.00 | 36.00 | 59.00
1.50 | 24.00 | 40.00 | 62.00 | 97.00
2.00 | 32.00 | 61.00 | 94.00 | 140.00
3.00 | 48.00 | 110.00 | 175.00 | 250.00
--------------+-----------+-----------+-----------+-----------
SOURCE OF TURBIDITY.
Much turbidity originates in plowed fields of clayey soil, or in
fields upon which crops are growing. If it has not rained for some
days, and the surface-soil is comparatively dry, the first rain that
falls upon such land is absorbed by the pores of the soil until they
are filled. If the rain is not heavy, but little runs off over the
surface. If, however, the rain continues rapidly after the surface-soil
is saturated, the excess runs off over the surface to the nearest
watercourse. The impact of the rain-drops upon the soil loosens
the particles, and the water flowing off carries some of them in
suspension, and the water is said to be muddy.
The particles carried off in this way are extremely small. Mr. George
W. Fuller, in his report upon water purification at Louisville,
estimates that many of them are not more than a hundred thousandth of
an inch in diameter, and not more than a tenth as large as common water
bacteria.
The turbidity of the water flowing from a field of loose soil may be
2.00 or more; that is to say, the wire is hidden by a depth of half an
inch of water or less. When the water reaches the nearest watercourse
it meets with water from other kinds of land, such as woodlands and
grassed fields, and these waters are less turbid. The water in the
first little watercourse is thus a mixture and has a turbidity of
perhaps 1.00.
Public-domain text, read in full here on John Shaqi.
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