The Nation's River: A report on the Potomac: From the U.S. Department of the InteriorUnited States. Department of the Interior
History
The Nation's River: A report on the Potomac: From the U.S. Department of the Interior
United States. Department of the Interior
Potomac River
In terms of dissolved oxygen, dilution of such a body of water for
quality improvement appears to decrease in unit effectiveness as the
volume of dilution is stepped up, which means that past a certain
minimal point of improvement it gets expensive and requires
unreasonable amounts of storage. In terms of nutrients, one authority
has calculated that about 20,000 cubic feet per second would be required
to reduce the nutrient level in the upper estuary to a point where it
would be only twice that of a normal and healthily "rich" section of the
upper Chesapeake Bay. Some augmentation below the point of diminishing
returns will undoubtedly be needed, not only for the estuary but to keep
the river alive in its gorge above Washington during periods of low
flow. But as a main tool for the metropolitan river, it will not
substitute for achievement of the best possible standard treatment
followed by advanced treatment and other techniques.
Obviously, just as in water supply, an ultimate cure for water quality
ills is going to consist of a "mix" of solutions, different techniques
being applied to the situations they are best suited to deal with, and
combinations of them being worked out where combinations are what is
indicated. Already the same kind of sophisticated mathematical models of
given bodies of water--including the Potomac--that are being used to
study solutions for water supply problems are being put to use on water
quality as well, weighing the benefits and drawbacks of various
combinations of means. And, just as in water supply, ultimate "hard"
technology is undoubtedly going to make better solutions possible, while
a strong and meaningful start is possible with the technology that is on
hand.
* * * * *
Silt is a truly Basinwide problem. The individual tiny grains of soil
that mass to sully and choke the estuary may have originated anywhere
in the thousands of square miles of drainage above. They constitute an
economic loss at their points of origin as well as a trouble all along
their downstream course of migration.
The basic-physical ways of preventing silt are twofold and easily
defined: first, the maintenance of proper land cover--vegetation or
humus or mulch which blankets and anchors the soil particles and
prevents falling or flowing water from dislodging them--and second,
structural approaches that control the flow of water and can also serve
to trap eroded material. These latter can be anything from good contour
plowing practices to a major reservoir with a certain silt capacity
built into it.
[Illustration]
Public-domain text, read in full here on John Shaqi.
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