Heavy Metal Patterns in Stream Waters, Stream Sediments, and Selected Aquatic Life, Northern New Lead Belt, Southeast Missouri (518b4dd9-0c6f-459c-ae51-f92bb334ec63)

- Organization:
- The American Institute of Mining, Metallurgical, and Petroleum Engineers
- Pages:
- 6
- File Size:
- 471 KB
- Publication Date:
- Jan 1, 1980
Abstract
Heavy metal contents in stream waters, sediments, and selected aquatic algae were determined for the upper Meramec River basin, Missouri, of 3905 km2 (1508 sq mi) area and site of the proposed and controversial Meramec dam and reservoir. Six distinct drainage areas within the basin are: (1) a lightly industrialized and farm area, (2) a primitive forested- ranch area, (3) an area which includes the Northern New Lead Belt, (4) the westward drainage of an old and extensive barite mining area, (5) the main trunk of the Meramec River, and (6) short north-divide tributaries of the Meramec River. Lower Paleozoic sediments rest nonconformably upon eroded and hilly Precambrian igneous basement. This locally rises as major inliers and also makes up the St. Francois Mountains to the east. Major lead, and lesser zinc, copper, cobalt, and nickel mineralization occurs in the buried Cambrian Bonneterre dolomite. Residual barite is present along the eastern fringe of the basin and is derived from the Potosi formation. Some 62 water samples, active stream sediments (AS), bank samples (BS), and 11 selected aquatic algae samples were collected in the various drainage areas and analyzed for copper, lead, zinc, cadmium, nickel, arsenic, and mercury contents. Heavy metals in water have a maximum range of 1-120 ppb (parts per billion), and this for zinc. The AS and BS sediments have orders of magnitude greater acid leachable metal contents in the -80 mesh fraction, with lead hawing the greatest range of 11-1028 ppm. Heavy metal content of stream-algae approaches that of the sediments in which they grow. Most anomalous heavy metal accumulations occur near mining and milling activities and in the streams draining such areas. Significant distortions of the primary dispersion pattern militate against geochemical exploration for hidden ore zones, but do demonstrate the mining, milling, and smelting activities of man, and sporadic mineral occurrences in younger horizons.
Citation
APA:
(1980) Heavy Metal Patterns in Stream Waters, Stream Sediments, and Selected Aquatic Life, Northern New Lead Belt, Southeast Missouri (518b4dd9-0c6f-459c-ae51-f92bb334ec63)MLA: Heavy Metal Patterns in Stream Waters, Stream Sediments, and Selected Aquatic Life, Northern New Lead Belt, Southeast Missouri (518b4dd9-0c6f-459c-ae51-f92bb334ec63). The American Institute of Mining, Metallurgical, and Petroleum Engineers, 1980.