Water quality of North Carolina
streams--Water-quality characteristics for selected sites on the Cape
Fear River, North Carolina, 1955-80--Variability, loads, and trends of
selected constituents
Water-Supply Paper
2185-F
By J.K. Crawford
Abstract
Historical water-quality data collected by the U.S. Geological
Survey from the Cape Fear River at Lock 1, near Kelly, North
Carolina, show increasing concentrations of total-dissolved
solids, specific conductance, sulfate, chloride, nitrite plus
nitrate nitrogen, magnesium, sodium, and potassium during the
past 25 years. Silica and pH show decreasing trends during the
same 1957-80 period. These long-term changes in water quality
are statistically related to increasing population in the basin
and especially to manufacturing employment. Comparisons of
water-quality data for present conditions with estimated natural
conditions indicate that over 50 percent of the loads of most
major dissolved substances in the river at Lock 1 are the result
of development impacts in the basin. Over 80 percent of the
nutrients plus nitrate nitrogen, ammonia nitrogen, and total
phosphorus presently in the streams originate from development.
At four sampling stations on the Cape Fear River and its
tributaries, recent water-quality data show that most
constituents are always within North Carolina water-quality
standards and Environmental Protection Agency water-quality
criteria. However, iron, manganese and mercury concentrations
usually exceed standards. Although no algal problems have been
identified in the Cape Fear River, nitrogen and phosphorus are
present in concentrations that have produced nuisance algal
growths in lakes.
Citation:
Crawford, J.K., 1985, Water-quality characteristics for selected sites on the Cape Fear River, North Carolina, 1955-80-Variability, loads, and trends of selected constituents in Water quality of North Carolina streams: U.S. Geological Survey Water-Supply Paper 2185-F, 44 p.
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