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T.M. Mastrilli

Publications and source records attributed to T.M. Mastrilli.

3 recordsLinked to original sources

Effects of surface mining on the hydrology and biology in the Stony Fork basin, Fayette County, Pennsylvania, 1978-85

The effects of surface coal mining on the water quality, sediment discharge, and aquatic biology of streams in the Stony Fork Basin in southwestern Pennsylvania were studied from 1978 through 1985. Data were collected at five stream sites and one mine discharge site. Field data included streamflow, temperature, specific conductance, pH, acidity, and alkalinity. Laboratory analyses included sulfate, aluminum, iron, manganese, zinc, and selected trace elements. Annual streamflow at gaged sites was not substantially different, suggesting that mining did not affect the total volume of streamflow significantly. Comparisons of sediment yields of the upstream control site (site 5) to the downstream site (site 1) indicated that the sediment yield at site 5 was greatest in 1978, 1981-83, and 1985. The sediment yields at both sites in 1979-80 were about the same. Differences in the drainage area sizes and effective control of sediment in the mined areas may explain the lack of increased sediment yield at the downstream site. As mining became more extensive throughout the basin in 1979-80 and later, several water-quality effects were observed downstream. Generally, specific conductance, sulfate, manganese, aluminum, and zinc increased; pH and alkalinity decreased. Acidity and iron typically increased immediately downstream of mined areas. No trace-element concentrations exceeded maximum contaminant levels established by the U.S. Environmental Protection Agency. Surface mining in the Stony Fork Basin severely affected the stream invertebrate and fish populations. During 1977-84, the number of taxonomic groups of invertebrates at sites affected by mine drainage decreased by 45 to 71 percent; the number of fish species decreased by 81 to 88 percent.

Pennsylvania↗

Effects of surface coal mining on suspended-sediment discharge in a small mountain watershed, Fayette County, Pennsylvania

Data collected in the upper Stony Fork basin from July 1980 to November 1981 indicate that logging operations associated with block-cut surface mining temporarily increased suspended-sediment discharge of Stony Fork. However, the strip-mining operation did not increase the suspended sediment discharges of Stony Fork because of effective sediment-control measures. These controls included diversion control terraces and a large sediment-control pond. The 50-acre mine site yielded an average of 6.9 tons of sediment per acre, whereas, the sediment yield of the 2.5-square-mile study area was 0.13 tons per acre. During most storms, sharp rises in streamflow were accompanied by corresponding rises in suspended sediment concentrations. At the end of a storm, suspended sediment concentrations quickly returned to base-flow levels. Instantaneous stream discharge ranged from 0.02 to 146 cubic feet per second. Suspended sediment concentration ranged from less than 10 to 905 milligrams per liter. The highest daily mean suspended sediment concentration was 176 milligrams per liter. (USGS)

Water-Resources Investigations Report↗

Effects of surface mining on streamflow, suspended-sediment, and water quality in the Stony Fork drainage basin, Fayette County, Pennsylvania

A study of the Stony Fork basin in southern Fayette County, Pennsylvania, from 1977 through 1980 determined the impacts of surface coal mining on surface-water quality. Stony Fork was sampled at six sites, during which time the area of surface mines increased from 0.5 to 5.5 percent of the study area. Streamflow, suspended-sediment, and water quality data were collected at gaging stations upstream and downstream of mining. The total runoff between the upstream and downstream stations differed by one percent; this small difference could not be attributed to the effects of mining. The suspended-sediment yield increased during storms due to erosion from the mining sites. The suspended-sediment yield doubled at the downstream site following mining. Specific conductance was highly variable during storm runoff but generally varied inversely with flow and increased slightly during the study period. The pH ranged between 4.8 and 7.9 with values below 6.0 usually occurring during storm runoff. Concentrations of dissolved zinc and sulfate increased between the upstream and downstream sampling sites. Laboratory analysis of a precipitation sample indicates that acid precipitation may be partly responsible for pH depressions during storm runoff periods. (USGS)

Water-Resources Investigations Report↗