A. L. Young,The history,use, disposition and environmental fate of Agent Orange

Environmental Science and Pollution Research -     

Discriminating between Copper and Silver Mill Tailings in Silver Bow Creek Overbank Deposits,Butte, Montana,U.S.A.

Mining of the Butte deposit evolved over 100 years from placer mining starting in 1864 through silver mining to copper mining in the 1900s. Tailings resulting from milling during the period 1876-1924 were typically sluiced into the adjacent Silver Bow Creek (SBC) where they were washed downstream. The most significant flood event in 1908, among others, resulted in emplacement of approximately 2.9 m tons of sediment intermixed with tailings as overbank deposits along SBC between Butte and the Warm Springs Ponds. Apportioning the associated costs was contingent in part on discriminating between ownership of liability for the silver and copper tailings, which together formed the most significant portion of the overbank deposits. Samples were collected of tailings end-members and SBC deposits and their characteristic mineralogy (e.g. galena for silver tailings, and enargite for copper tailings) used to ascertain mixing of the tailings along SBC. This analysis identified Pb as a signature element for silver tailings and Cu for copper tailings. Two-hundred and twenty-four Cu and Pb chemical analyses representing 43 transects through the overbank deposits along SBC allowed calculation of the proportional contribution of the end members for each integrated transect. Accumulating the volumes from each transect resulted in an apportionment of 53% copper and 47% silver tailings in the overbank deposits.     

Discriminating between Copper and Silver Mill Tailings in Silver Bow Creek Overbank Deposits,Butte, Montana,U.S.A.

Mining of the Butte deposit evolved over 100 years from placer mining starting in 1864 through silver mining to copper mining in the 1900s. Tailings resulting from milling during the period 1876–1924 were typically sluiced into the adjacent Silver Bow Creek (SBC) where they were washed downstream. The most significant flood event in 1908, among others, resulted in emplacement of approximately 2.9 m tons of sediment intermixed with tailings as overbank deposits along SBC between Butte and the Warm Springs Ponds. Apportioning the associated costs was contingent in part on discriminating between ownership of liability for the silver and copper tailings, which together formed the most significant portion of the overbank deposits. Samples were collected of tailings end-members and SBC deposits and their characteristic mineralogy (e.g. galena for silver tailings, and enargite for copper tailings) used to ascertain mixing of the tailings along SBC. This analysis identified Pb as a signature element for silver tailings and Cu for copper tailings. Two-hundred and twenty-four Cu and Pb chemical analyses representing 43 transects through the overbank deposits along SBC allowed calculation of the proportional contribution of the end members for each integrated transect. Accumulating the volumes from each transect resulted in an apportionment of 53% copper and 47% silver tailings in the overbank deposits.     

Arsenic Background Concentrations in Florida,U.S.A. Surface Soils: Determination and Interpretation

Background concentrations of soil arsenic have been used as an alternative soil cleanup criterion in many states in the U.S. This research addresses issues related to the interpretation of background concentrations of arsenic in near pristine soils in Florida. Total arsenic was measured in 448 taxonomic and geographic representative surface soil samples using USEPA Method 3052 (HCl-HNO 3 -HF, microwave digestion) and graphite furnace atomic absorption spectrophotometry analysis procedure. Values were log-normally distributed, with geometric mean and baseline concentration (defined as 95% of the expected range of background concentrations) providing the most satisfactory statistical results. An upper baseline concentration of 6.21 mg As/kg was estimated for undisturbed soils (n=267) compared to 7.63 mg As/kg for disturbed soils (n=181). Temporal trend of total soil arsenic concentrations from 1967 to 1989 paralleled decreased usage of arsenic in U.S. agriculture. Soil arsenic background concentrations were generally higher in south Florida than in north and central Florida, and associated with wet soils. Individual high arsenic sites were scattered throughout the state, but the most highly concentrated of these occurred in the Leon-Lee belt along the Ocala uplift district extending to the southwestern flatwoods district. Extrapolation of the data using a single arsenic value regardless of the taxonomic and geographical differences in soil arsenic distribution would underestimate potential arsenic contamination in upland soils.     

Arsenic Background Concentrations in Florida,U.S.A. Surface Soils: Determination and Interpretation

Background concentrations of soil arsenic have been used as an alternative soil cleanup criterion in many states in the U.S. This research addresses issues related to the interpretation of background concentrations of arsenic in near pristine soils in Florida. Total arsenic was measured in 448 taxonomic and geographic representative surface soil samples using USEPA Method 3052 (HCl-HNO₃-HF, microwave digestion) and graphite furnace atomic absorption spectrophotometry analysis procedure. Values were log-normally distributed, with geometric mean and baseline concentration (defined as 95% of the expected range of background concentrations) providing the most satisfactory statistical results. An upper baseline concentration of 6.21 mg As/kg was estimated for undisturbed soils (n = 267) compared to 7.63 mg As/kg for disturbed soils (n = 181). Temporal trend of total soil arsenic concentrations from 1967 to 1989 paralleled decreased usage of arsenic in U.S. agriculture. Soil arsenic background concentrations were generally higher in south Florida than in north and central Florida, and associated with wet soils. Individual high arsenic sites were scattered throughout the state, but the most highly concentrated of these occurred in the Leon-Lee belt along the Ocala uplift district extending to the southwestern flatwoods district. Extrapolation of the data using a single arsenic value regardless of the taxonomic and geographical differences in soil arsenic distribution would underestimate potential arsenic contamination in upland soils.     

Arsenic accumulation by the aquatic fern Azolla: comparison of arsenate uptake, speciation and efflux by A. caroliniana and A. filiculoides

This study investigates As accumulation and tolerance of the aquatic fern Azolla. Fifty strains of Azolla showed a large variation in As accumulation. The highest- and lowest-accumulating ferns among the 50 strains were chosen for further investigations. Azolla caroliniana accumulated two times more As than Azolla filiculoides owing to a higher influx velocity for arsenate. A. filiculoides was more resistant to external arsenate due to a lower uptake. Both strains showed a similar degree of tolerance to internal As. Arsenate and arsenite were the dominant As species in both Azolla strains, with methlyated As species accounting for <5% of the total As. A. filiculoides had a higher proportion of arsenite than A. caroliniana. Both strains effluxed more arsenate than arsenite, and the amount of As efflux was proportional to the amount of As accumulation. The potential of growing Azolla in paddy fields to reduce As transfer from soil and water to rice should be further evaluated.     

Quantifying Metal Contributions from Multiple Sources to the Clark Fork River,Montana, U.S.A.

Identifying and quantifying the contributions of multiple sources of trace elements to stream sediments in a basin containing several possible inputs presents a unique problem related to the investigation of rivers impacted by industrial activity. A multi-source dilution-mixing model was developed and applied to determine the relative contributions to As, Cu and Pb burdens in the Clark Fork River, Montana, a recipient of historical mine wastes as a result of over a century of mining and milling operations. The results identified the Flint Creek drainage as a major source of anthropogenic As (47%) and Pb (35%) to sediments of the Clark Fork River and the Milltown Reservoir, in addition to the major sources associated with mining operations in Butte, MT. The Little Blackfoot River also contributes anthropogenic As (3%) and Pb (4%) to the Clark Fork River, while minor inputs of Cu (1%) and Pb (2%) emanate from the Blackfoot River. The model allows source quantification, and an understanding of the fate and transport of mine wastes in a basin, allowing identification and eventual prioritization of sites destined for remediation.