The filtration of public water-supplies: Third edition, revised and enlarged. — John Shaqi
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
As even a very small percentage of fine material is capable of
getting in the narrow places and reducing the carrying power of the
gravel, it is important that all such matters should be carefully
removed by washing before putting the gravel in place. In England and
Germany gravel is commonly screened for use in revolving cylinders of
wire-cloth of the desired sizes, on which water is freely played from
numerous jets, thus securing perfectly clean gravel. In getting gravel
for the Lawrence filter, an apparatus was used, in which advantage was
taken of the natural slope of the gravel bank to do the work, and the
use of power was avoided. The respective grades of gravel obtained were
even in size, and reasonably free from fine material, but it was deemed
best to wash them with a hose before putting them in the filter.
To calculate the frictional resistance of water in passing gravel, we
may assume that for the very low velocities which are actually found in
filters the quantity of water passing varies directly with the head,
which for these velocities is substantially correct, although it would
not be true for higher rates, especially with the coarser gravels.[6]
In the case of parallel underdrains the friction from the middle point
between drains to the drains may be calculated by the formula:
Total head = (1/2)[(Rate of filtration × (1/2 distance between
drains)^2)/(Average depth of gravel × discharge coefficient)].
The discharge coefficient for any gravel is 1000 times the quantity
of water which will pass when _h_/_l_ is 1/1000 expressed in million
gallons per acre daily. The approximate values of this coefficient for
different-sized gravels are as follows:
VALUES OF DISCHARGE COEFFICIENT.
For gravel with effective size 5 mm _c_ = 23,000
For gravel with effective size10 mm _c_ = 65,000
For gravel with effective size15 mm _c_ = 110,000
For gravel with effective size20 mm _c_ = 160,000
For gravel with effective size25 mm _c_ = 230,000
For gravel with effective size30 mm _c_ = 300,000
For gravel with effective size35 mm _c_ = 390,000
For gravel with effective size40 mm _c_ = 480,000
Example: What is the loss of head in the gravel at a rate of filtration
of 2 million gallons per acre daily, with underdrains 20 feet apart,
where the supporting gravel has an effective size of 35 millimeters,
and is uniformly 1 ft. deep?
Total head = (1/2)[(2 × 10^2)/(1 × 390,000)] = .000256 ft.
The total friction would be the same with the same average depth of
gravel whether it was uniformly 1 foot deep, or decreasing from 1.5 at
the drains to 0.5 in the middle, or from 2.0 to 0. The reverse case
with the gravel layer thicker in the middle than at the drains does not
occur and need not be discussed.
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