Biofiltration of trimethylamine, dimethylamine, and methylamine by immobilized Paracoccus sp. CP2 and Arthrobacter sp. CP1

A biofilter using granular activated carbon with immobilized Paracoccus sp. CP2 was applied to the elimination of 10–250 ppm of trimethylamine (TMA), dimethylamine (DMA), and methylamine (MA). The results indicated that the system effectively treated MA (>93%), DMA (>90%), and TMA (>85%) under high loading conditions, and the maximum degradation rates were 1.4, 1.2, and 0.9 g-N kg⁻¹ GAC d⁻¹. Among the three different amines treated, TMA was the most difficult to degrade and resulted in ammonia accumulation. Further study on TMA removal showed that the optimal pH was near neutral (6.0–8.0). The supply of high glucose (>0.1%) inhibited TMA removal, maybe due to substrate competition. However, complete TMA degradation was achieved under the co-immobilization of Paracoccus sp. CP2 and Arthrobacter sp. CP1 (96%). Metabolite analysis results demonstrated that the metabolite concentrations decreased by a relatively small 27% while the metabolite apparently increased by heterotrophic nitrification of Arthrobacter sp. CP1 in the co-immobilization biofilter.     

Groundwater munition residues and nitrate near Grand Island,Nebraska, U.S.A.

Munition residues from waste disposal on ordnance property have resulted in a defined plume of RDX contaminated groundwater stretching 6.5 km and underlying an area of 6.5 km². A smaller plume of TNT was detected near the plant's boundary. The relative positions of the plumes combined with an historical review of total plant output of RDX and TNT indicates that RDX is much more persistent than TNT. The estimated RDX transport velocity of 0.5 m day⁻¹ closely approximates the calculated Darcian velocity. The RDX plume sinks with recharge at a rate of about 0.5 m yr⁻¹.Nitrate is associated primarily with adjacent upgradient landuse and is not related to plant manufacture of ammonium nitrate. The average δ¹⁵N of the Nitrate was about + 10% and strongly suggests that animal wastes are the predominant source.     

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

Environmental Science and Pollution Research -     

Electro-Fenton degradation of the antibiotic sulfanilamide with Pt/carbon-felt and BDD/carbon-felt cells. Kinetics,reaction intermediates,and toxicity assessment

The degradation of 230 mL of a 0.6-mM sulfanilamide solution in 0.05 M Na₂SO₄ of pH 3.0 has been studied by electro-Fenton process. The electrolytic cell contained either a Pt or boron-doped diamond (BDD) anode and a carbon-felt cathode. Under these conditions, organics are oxidized by hydroxyl radicals formed at the anode surface from water oxidation and in the bulk from Fenton’s reaction between initially added (and then electrochemically regenerated) Fe²⁺ and cathodically generated H₂O₂. From the decay of sulfanilamide concentration determined by reversed-phase liquid chromatography, an optimum Fe²⁺ concentration of 0.20 mM in both cells was found. The drug disappeared more rapidly using BDD than Pt, and, in both cases, it was more quickly removed with raising applied current. Almost total mineralization was achieved using the BDD/carbon-felt cell, whereas the alternative use of Pt anode led to a slightly lower mineralization degree. In both cells, the degradation rate was accelerated at higher current but with the concomitant fall of mineralization current efficiency due to the greater increase in rate of the parasitic reactions of hydroxyl radicals. Reversed-phase liquid chromatography allowed the identification of catechol, resorcinol, hydroquinone, p-benzoquinone, and 1,2,4-trihydroxybenzene as aromatic intermediates, whereas ion exclusion chromatography revealed the formation of malic, maleic, fumaric, acetic, oxalic, formic, and oxamic acids. NH₄ ⁺, NO₃ ^?, and SO₄ ^2? ions were released during the electro-Fenton process. A plausible reaction sequence for sulfanilamide mineralization involving all detected intermediates has been proposed. The toxicity of the solution was assessed from the Vibrio fischeri bacteria luminescence inhibition. Although it acquired its maximum value at short electrolysis time, the solution was completely detoxified at the end of the electro-Fenton treatment, regardless of the anode used.     

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.