Membrane-based wet electrostatic precipitation

Emissions of fine particulate matter, PM2.5, in both primary and secondary form, are difficult to capture in typical dry electrostatic precipitators (ESPs). Wet (or water-based) ESPs are well suited for collection of acid aerosols and fine particulates because of greater corona power and virtually no re-entrainment. However, field disruptions because of spraying (misting) of water, formation of dry spots (channeling), and collector surface corrosion limit the applicability of current wet ESPs in the control of secondary PM2.5. Researchers at Ohio University have patented novel membrane collection surfaces to address these problems. Water-based cleaning in membrane collectors made of corrosion-resistant fibers is facilitated by capillary action between the fibers, maintaining an even distribution of water. This paper presents collection efficiency results of lab-scale and pilot-scale testing at FirstEnergy's Bruce Mansfield Plant for the membrane-based wet ESP. The data indicate that a membrane wet ESP was more effective at collecting fine particulates, acid aerosols, and oxidized mercury than the metal-plate wet ESP, even with approximately 15% less collecting area.     

Chemical composition and physiological properties of fucoids under conditions of reduced salinity

Thallus segments of Fucus serratus L. and F. vesiculosus L. (Phaeophyceae, Fucales) were transferred into seawater media with a salinity range from 32.65 to 2.25 and maintained for at least 2 weeks. Several parameters of chemical composition as well as rates of photosynthetic and respiratory oxygen exchange, ¹⁴C-assimilate patterns, and release of ¹⁴C-assimilates into the culture medium have been investigated. Compared to controls, in both species dry weight, ash, chloride, and mannitol contents distinctly decline proportionally to reduction of salinity in the incubation media, whereas content of total N (in terms of protein content) remarkably increase. Respiratory O₂-consumption is markedly increased at lower salinities, whereas rate of photosynthetic O₂-evolution shows some depression. Relatively little effects of salinity changes are observed in distribution of photosynthetically assimilated ¹⁴C among the major groups of photosynthates. Release of ¹⁴C-assimilates into the incubation medium never exceeds 2% of total ¹⁴C-uptake, but is stimulated in media of reduced salt content. The results are discussed with emphasis on phenomena of long-term adaptation and osmoregulation in the marine fucoid species.     

Mikrobiologische Volatilisierung von anorganischem Selen aus Deponiesickerwässern bei umweltrelevanten Konzentrationen

Background, aim, and scope Determination of the rates of microbial alkylation are of interest with respect to natural attenuation of harmful selenium concentrations or selenium charges in contaminated ecosystems. Materials and methods Landfill gas and the headspace of microbial microcosm incubation vessels were sampled in Tedlar^® bags. On-line hyphenation of an efficient enrichment method (cryotrapping-cryofocusing), a gaschromatographic separation technique, and the sensitive ICP-MS detection system was used for speciation of volatile organoselenium compounds. A detection limit at the ultra trace level (pg Se) was achieved with this CT-CF-GC-ICP-MS technique. Results Incubation of landfill leachate with Alternata alternata as an active methylating organism showed a production of volatile selenium compounds (DMSe, DMDSe, EMDSe, DEDSe) over the whole range of applied inorganic selenium concentrations (10?µg?L^–1 to 10?mg?L^–1), with volatilization rates of up to 10?mg m^–3?d^–1. For selenium concentrations of 1?mg?L^–1 in the nutrient broth, up to 7?% of the inorganic selenium was volatilized after one week. The same volatile selenium compounds were observed in landfill gas. Discussion The amount of volatilized selenium was comparable to that found in other studies with microbial pure cultures as well as isolates from waters or soils, but at much lower initial concentrations used in the incubations. Conclusions The alkylation of selenium in the enriched mixed culture from landfill leachate at environmentally relevant concentrations indicates that the organoselenium compounds of same species composition and distribution determined in landfill gas are produced by microorganisms. Recommendations and perspectives The microbial alkylation of toxic inorganic selenium species to less toxic or non-toxic, volatile compounds is an efficient method for bioremediation of contaminated sites even at relatively low Se concentrations.     

Characterization and growth response of bacteria in soil following application of carbofuran.

Enhanced biodegradation of carbofuran (2, 3-dihydro-2, 2 dimethyl-7-benzofuranyl methyl carbamate) is an economically significant, but poorly understood, microbial phenomenon in soil. A series of experiments was conducted to examine short term changes in soil bacterial populations stimulated by carbofuran application at field rates. In the field experiment, commercially formulated carbofuran and butylate (S-ethyl diisobutyl carbamothioate) were applied at 5.6 kg ai ha-1 and 8.4 kg ai ha-1, respectively, on a soil (Putnam silt loam) exhibiting enhanced degradation of carbofuran. In laboratory studies, technical grade carbofuran (20 mg kg-1 soil) was applied to samples of the field soil. Bacterial populations were estimated using non-selective (tryptic soy agar) and selective media containing carbofuran or butylate. Largest population increases in pesticide-treated soil were observed between 7 and 15 days after treatment (DAT) compared to populations in non-treated soil. Significant increases (P less than 0.05) in total bacterial populations and presumed carbofuran-degraders due to carbofuran application were associated with increased populations of Pseudomonas spp. and Flavobacterium spp. Application of carbofuran appeared to provide a competitive advantage to these species over actinomycetes persisting beyond 20 DAT. Growth responses of bacteria to carbofuran in the Putnam soil were compared to those in a native prairie soil (Mexico silt loam), which exhibited a much slower rate of carbofuran degradation. Bacterial population response to carbofuran was measurable, but small and short-lived. Perpetuation of the enhanced degradation phenomenon may lie in a persistent pesticide-induced competitive advantage given to a very small segment of the microbial population. This advantage may not be detectable after 20 days using conventional plating techniques.     

Untersuchungen zur Physiologie von Volemit in der marinen Braunalge Pelvetia canaliculata

The heptitol volemitol, formerly only known in some fungi, lichens, and roots of Primula species, has recently been shown to occur also in the marine brown alga Pelvetia canaficulata (L.) Decne, et Thur. in considerable amounts. Photosynthesis experiments in H¹⁴CO _- ³ provided evidence that, among other substances, ¹⁴C-volemitol is formed almost 30 sec after beginning of ¹⁴C-assimilation. ¹⁴C-volemitol was not detectable after dark fixation. Percentage labelling of this polyol rose from 4.5% after 30 sec to 12% after 10 min. These data show that, in P. canaliculata, volemitol is accumulated during photosynthesis beside mannitol, the major constituent of the soluble fraction. Biosynthesis of volemitol proceeds in the alga only, not in its systemic fungal endosymbiont Mycosphaerella pelvetiae, since the brown alga Ascophyllum nodosum, infected with the same fungus, doess not synthesize a heptitol. Having regard to these metabolic characteristics, we conclude that there is no lichenoid interrelationship between Pelvetia/Ascophyllum and their systemic fungus Mycosphaerella.     

Frequency-domain sensitivity analyses of an estuarine ecosystem simulation model

A mathematical simulation model of the Narragansett Bay (RI) ecosystem which simulates realistic daily values of phytoplankton, several life stages of zooplankton, and three inorganic nutrients, was modified by removing all seasonally-changing environmental forcing functions. This unforced version of the model generated time-series values for the state variables which resulted only from internal mechanistic formulations, not from environmental inputs. Steady state time-series data for biotic responses were analyzed using variance spectral analysis, which partitions the variance of data among frequencies of oscillation. Periodicities at 0.035 and 0.068 cycles d^?1 dominated the response spectra for phytoplankton, and juvenile and adult zooplankton. The dominance of these oscillations generally prevailed in experimental runs using constant 1 January and 30 June environmental conditions, and in runs which perturbed the ecosystem with a random temperature component (±1.5 or ±3.0°C) about 1 January (3°C) or 30 June (18°C) temperatures. Biomass decayed to near-zero levels in a temperature perturbation of a version of the model from which nutrient regeneration by the benthos had been eliminated. This result was compared with the responses of microcosms from which a benthic component had been omitted. The dominance of periodicities at 0.035 and 0.068 cycles d^?1 cannot be attributed to any single mechanism within the phytoplankton or zooplankton formulations of the model. The lack of sensitivity of model components to temperature perturbations over a wide band of frequencies, and their insensitivity to gross changes in steady-state temperature values, suggest that further analyses should displace rate coefficients of internal mechanisms in order to identify the stability properties of major material cycles of the system.     

Respiration and excretion by the ctenophore Mnepiopsis leidyi

Respiration (dissolved oxygen and carbon dioxide) and excretion (dissolved organic carbon, inorganic and organic nitrogen and phosphorus) rates were measured for a variety of sizes of Mnemiopsis leidyi over a temperature range of 10.3° to 24.5°C. Both respiration and excretion rates were a direct linear function of animal weight and very temperature sensitive (Q₁₀4). Oxygen uptake ranged from 155 to 489 g at O/(g dry weight) day^-1 and carbon dioxide release from 43 to 166 M. Organic carbon made up about 38% of the total carbon released. Inorganic nitrogen excretion, exclusively in the form of ammonium, comprised 54% of the total nitrogen release and ranged from 10 to 36 M NH₄/(g dry weight) day^-1. Average release of dissolved primary amines (expressed as glycine equivalents) equaled 43% of the organic nitrogen fraction. Inorganic phosphorus release ranged from 2.0 to 4.9 M/(g dry weight) day^-1 and made up about 72% of the total phosphorus loss. The turnover of elements in the body was calculated as 5 to 19% per day for carbon and nitrogen, depending on the temperature, and an even higher 20 to 48% per day for phosphorus. These values are comparable to rates observed for small, active zooplankton.