SUMMARY OF MAJOR FINDINGS
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The Allegheny and Monongahela River Basins drain
19,145 square miles of Pennsylvania, West Virginia, New York, and
Maryland. About 64 percent of the study area is forested; the remainder
is a patchwork of land uses. Agriculture (30 percent) is commonly
low intensity pasture, dairy, and hay. Urban areas account for about
4 percent of the area, but they include many forested ridges. Coal-mining
activities influence water quality in most of the study area but are
not visible on this surface land-use map. (Land-use coverage is based
on 1991, 1992, and 1993 land-use data.) |
Stream and River Highlights
Streams and rivers in the Allegheny and
Monongahela River Basins range from those of high quality that support
diverse aquatic life to those that are seriously degraded and support
few aquatic species and few human uses of the water. Higher quality stream
reaches are generally in the northern one-third of the study area and
in mountainous areas in eastern sections. These areas are dominated by
forest, low-intensity agriculture, and rural communities. Urban development
and coal-mining activities through much of the basins have had a significant
influence on water quality and aquatic life. Industrial activity in small
and large towns has resulted in contaminated streambed sediments and contaminated
fish. Acid- and(or) mineral-laden mine drainage from abandoned coal mines
is one of the most serious and persistent water-quality problems in the
basins, limiting water use and aquatic resources. Sulfate concentrations
were 5 times greater in streams draining mined areas than in streams draining
unmined areas.
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Sulfate concentration is closely related
to coal production in the sampled basins but not as clearly related
to pH or dissolved metal concentration. (See
page 6.)
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Since 1980, treatment of drainage from
active and abandoned mines has generally resulted in improved water
quality, with increased pH and lower metal and sulfate concentrations,
but diversity and abundance of aquatic organisms remain reduced in
comparison to unmined areas. (See pages 7, 20, and 21.)
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Zinc in bed sediment exceeded aquatic-life
guidelines at 15 of 50 sites. (See
page 9.)
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Arsenic concentrations most often
exceeded aquatic-life guidelines in bed sediment in streams draining
northern, once glaciated areas, and high concentrations appear to
be unrelated to human activity. (See
page 10.)
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Streams in forested settings are among
the most diverse nationally with respect to aquatic insects among
NAWQA sites sampled between 1996 and 1998. (See
page 8.)
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A group of now-banned industrial chemicals,
polychlorinated biphenyls (PCBs), was detected in 43 percent of sediment
and fish-tissue samples. Consumption advisories are in place for several
fish species because of PCB and chlordane contamination in some large
river reaches. (See pages 11 and 12.)
- Some of the most degraded stream reaches have, since
the early 1900s, supported few aquatic organisms. Yet, the quality of
many reaches is now improving, and abundant fish and invertebrate populations
include sensitive species not seen here in decades. (See page 11.)
- In sampled streams in basins dominated by urban or
agricultural land, pesticides and volatile organic compounds (VOCs)
were commonly detected, although generally at concentrations meeting
drinking-water and aquatic-life standards and guidelines. (See pages
12–13
and 15–17.)
- Pesticide concentrations in stream water exceeded
drinking-water guidelines in single samples from each of two basins,
one dominated by agriculture and the other dominated by urban land use.
(See pages 12 and 13.)
Major Influences on Streams and Rivers
- Surface, underground, reclaimed, and abandoned
coal mines
- Impoundments and maintenance of navigation
channels
- Increased urban development
- Reductions in agriculture, industrial activity,
and coal production
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Ground-Water Highlights
Although not regulated, the quality of water from domestic
wells—the predominant water source for residents of rural areas—meets
Federal standards for drinking water for most substances analyzed in this
study. Ground-water supply generally meets or exceeds expectations from
wells in the highly permeable glaciofluvial deposits of the valley-fill
aquifers in the northwest. Ground-water supply often meets needs but can
be meager from wells tapping the water-filled fractures of the fractured-rock
aquifers present throughout much of the rest of the study area.
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- Compared to ground water in unmined areas of the
coal-bearing rocks, water in shallow private domestic wells near reclaimed
surface coal mines had higher concentrations of sulfate, iron, and manganese,
even after all mining and reclamation had been completed. (See
pages 9 and 21.)
- Pesticides were detected more frequently in the valley-fill
aquifers of the glacial sediments than in fractured-rock aquifers. (See
pages 13-15.)
- Overall, VOCs were detected at very low levels in
the 95 ground-water samples analyzed. Gasoline-related compounds were
detected slightly more frequently and at slightly higher concentrations
in ground water near reclaimed surface coal mines than near unmined
areas. (See pages 16 and 17.)
- Nitrate was detected in 62 percent of sampled wells,
although only one domestic-well sample exceeded the drinking-water standard
for nitrate. (See pages 17 and
18.)
- Radon was detected at levels exceeding the proposed
Federal drinking-water standard of 300 pCi/L (picocuries per liter)
in 56 percent of the ground-water samples. The proposed alternative
standard (4,000 pCi/L) was exceeded in 2 percent of the samples. (See
page 19.)
Major Influences on Ground
Water
- Coal mining
- Pesticide and fertilizer application
- Widespread use of gasoline and oxygenates
- Naturally occurring concentrations of radon
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Glossary
U.S. Geological Survey Circular
1202
Suggested citation:
Anderson, R.M., Beer, K.M., Buckwalter,
T.F., Clark, M.E., McAuley, S.D., Sams, J.I. III, and
Williams, D.R., 2000, Water Quality in the Allegheny and Monongahela
River Basins Pennsylvania, West Virginia, New York, and Maryland,
1996-98: U.S. Geological Survey Circular 1202, 32p., on-line
at http://+++1202url+++
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