Dynamic behaviour of Cd2+ adsorption in equilibrium batch studies by CaCO3 −-rich Corbicula fluminea shell

This work presents the structural and adsorption properties of the CaCO₃ ^?-rich Corbicula fluminea shell as a natural and economic adsorbent to remove Cd ions from aqueous solutions under batch studies. Experiments were conducted with different contact times, various initial concentrations, initial solution pH and serial biosorbent dosage to examine the dynamic characterization of the adsorption and its influence on Cd uptake capacity. The characterization of the C. fluminea shell using SEM/EDX revealed that the adsorbent surface is mostly impregnated by small particles of potentially calcium salts. The dominant Cd adsorption mechanism is strongly pH and concentration dependent. A maximum Cd removal efficiency of 96.20 % was obtained at pH 7 while the optimum adsorbent dosage was observed as 5 g/L. The Langmuir isotherm was discovered to be more suitable to represent the experimental equilibrium isotherm results with higher correlation coefficients (R ²?>?0.98) than Freundlich (R ²?<?0.97).The correlation coefficient values (p?<?0.01) indicated the superiority of the Langmuir isotherm over the Freundlich isotherm.     

Experimental study on the stability of the ClHgSO3 − in desulfurization wastewater

Environmental Science and Pollution Research - Wet flue gas desulfurization technologies have received much concern for their superior performance on co-controlling the acid gases and mercury....     

Measurements of aerosol particles in the Škocjan Caves,Slovenia

For the first time, continuous aerosol measurements were performed in the ?kocjan Caves, one of the most important cave systems in the world, and listed by UNESCO as a natural and cultural world heritage site since 1986. Measurements of PM₁₀ were performed during three different periods: (1) in December 2011, the average background concentration was found to be about 4 μg m^?3; (2) in June 2012, a higher concentration was measured (8 μg m^?3); and (3) from 8 to 20 August 2012, the highest concentration of 15.3 μg m^?3 was measured. Based on the PM₁₀ measurement results, and as compared to similar measurements outside the cave, it can be hypothesized that the increase in the cave's aerosol concentration during the summer was connected to both the higher number of visitors and the polluted atmospheric air entering the cave upon entering of the cave system. Additional measurement of nanoparticles with scanning mobility particle sizer spectrometer (size between 14.1 and 710.5 nm) confirmed these findings; during the summer period, a severe raise in the total aerosol concentration of 30–50 times was found when groups of visitors entered the cave. Our results on nanoparticles demonstrated that we were able to detect very small changes and variations in aerosol concentration inside the cave. To our knowledge, these are the first results on nanoaerosol measurements in a cave, and we believe that such measurements may lead to the implementation of better protection of delicate cave systems.     

Snow-to-air exchanges of mercury in an Arctic seasonal snow pack in Ny-Ålesund,Svalbard

The study of mercury (Hg) cycle in Arctic regions is a major subject of concern due to the dramatic increases of Hg concentrations in ecosystem in the last few decades. The causes of such increases are still in debate, and an important way to improve our knowledge on the subject is to study the exchanges of Hg between atmosphere and snow during springtime. We organized an international study from 10 April to 10 May 2003 in Ny-Ålesund, Svalbard, in order to assess these fluxes through measurements and derived calculations.Snow-to-air emission fluxes of Hg were measured using the flux chamber technique between ∼0 and 50 ng m⁻² h⁻¹. A peak in Gaseous Elemental Mercury (GEM) emission flux from the snow to the atmosphere has been measured just few hours after an Atmospheric Mercury Depletion Event (AMDE) recorded on 22 April 2004. Surprisingly, this peak in GEM emitted after this AMDE did not correspond to any increase in Hg concentration in snow surface. A peak in GEM flux after an AMDE was observed only for this single event but not for the four other AMDEs recorded during this spring period.In the snow pack which is seasonal and about 40 cm depth above permafrost, Hg is involved in both production and incorporation processes. The incorporation was evaluated to ∼5–40 pg m² h. Outside of AMDE periods, Hg flux from the snow surface to the atmosphere was the consequence of GEM production in the air of snow and was about ∼15–50 ng m⁻² h⁻¹, with a contribution of deeper snow layers evaluated to ∼0.3–6.5 ng m⁻² h⁻¹. The major part of GEM production is then mainly a surface phenomenon. The internal production of GEM was largely increasing when snow temperatures were close to melting, indicating a chemical process occurring in the quasi-liquid layer at the surface of snow grains.     

On the difference between SO2−4 and NO−3 in wintertime precipitation

Winter rains have lower NO⁻₃ levels but higher SO²⁻₄ levels than snows in the NE United States. In this study, four years of winter precipitation data from SE Michigan were examined to help understand these differences. Although NO⁻₃ levels were indeed higher in snow than winter rain, the higher concentrations could be attributed to the generally lower precipitation depths associated with snow events than with rain events. The NO⁻₃ concentrations are inversely correlated with precipitation depth. There was no evidence that snow scavenged HNO₃ in the air more efficiently than rain.Conversely, SO²⁻₄ was far higher in winter rain than in snow. This could not be explained in terms of ground-level ambient S concentrations or the wind direction from which the storm originated. However, the cloud temperatures were high enough in the case of rain to suggest that the cloud hydrometeors could have been present as liquid droplets rather than ice crystals. The SO²⁻₄ concentrations of the precipitation were highly correlated with the temperatures of the cloud layers. The data suggest that SO₂ is incorporated and oxidized to SO²⁻₄ in clouds most efficiently when the hydrometeors are present as liquid droplets. The fact that NO⁻₃does not show the same relationship suggests that incorporation of N species into cloud water followed by oxidation is not as important a process for N as for S.     

Measurements of air–surface exchange rates of volatile organic compounds

Vertical gradients of volatile organic compounds (VOCs) were measured over a maize field and a soybean field in 1995 and 1996, respectively, in the Lower Coastal Plains of North Carolina. The measurements over the maize field were conducted in its early growth period, during May 1995, and the measurements over the soybean field were conducted in its middle and later growth periods during July through August 1996 at the same location. These measurements were combined with micrometeorological flux measurements to determine emission flux measurements for various VOCs. This measurement programme was part of project NOVA (Natural emissions of Oxidant precursors: Validation of techniques and Assessment) to estimate the flux of VOCs. Methanol was identified as the major biogenic compound for both years with the average flux of 3450 ± 1456 µg/m²/hr over maize and 3079 ± 2766 µg/m²/hr over soybean. Acetone is another compound that was identified as a biogenic compound for both years with the average flux of 425 ± 223 µg/m²/hr over maize and 2701 ± 1710 µg/m²/hr over soybean. In addition to biogenic compounds, a large number of aromatic compounds, including styrene and 1,2,4-trimethylbenzene, were also identified as emissions from the ground over the soybean field.     

The use of conversion factors in air pollution studies: Sulphur dioxide ppm—μg m−3

Some recently developed and now widely used continuous sulphur analysers express SO₂ sampling in ppm. which must be converted to μg m⁻³ where comparability arises of gaseous with particulate and aerosol sampling, or with other types of continuous SO₂ analysers recording directly in μg m⁻³.The percentage deviations from the conversion factor now generally used (related to NTP values) that arise with the substitution of the actual climatic variables under which sampling takes place, are discussed. A method for the graphical calculations of these deviations is suggested, for application where there is need for closer precision in the conversion of ppm to μg m⁻³ than the factor presently used (2858) can provide.     

NH4+, NO3−, and SO42− in roadside and rural size-resolved particles and transformation of NO2/SO2 to nanoparticle-bound NO3−/SO42−

This study investigates ammonium, nitrate, and sulfate (NH₄⁺, NO₃^?, and SO₄^2?) in size-resolved particles (particularly nano (PM_0.01–0.056)/ultrafine (PM_0.01–0.1)) and NO_x/SO₂ collected near a busy road and at a rural site. The average (mass) cumulative fraction of secondary inorganic aerosols (SO₄^2?+NO₃^?+NH₄⁺) in nano or ultrafine particles at the roadside was found to be three to four times that at the rural site. The above three secondary inorganic aerosol species were present in similar cumulative fractions in particles of size 1–18 μm at both sites; however, dissimilar fractions were observed for Cl^?, Na⁺, and K⁺. The nitrogen ratios (NRs: NR = NO₃^??N/(NO₃^??N + NO₂–N)), sulfur ratios (SRs: SR = SO₄^2??S/(SO₄^2??S + SO₂–S)), dNR/D_P (derivative of NR with respect to D_P (particle diameter)), and dSR/D_P (derivative of SR with respect to D_P) at the roadside were higher than those at the rural site for nano/ultrafine particles. At both sites (particularly the roadside), the nanoparticles had significantly higher dNR/D_P and dSR/D_P values than differently sized particles, implying that NO₃^?/SO₄^2? (from NO₂/SO₂ transformation or NO₃^?/SO₄^2? deposition) were present on these particles.     

An ambient experimental study of phase equilibrium in the atmospheric system: Aerosol H+, NH4+, SO2−4, NO3−-NH3(g), HNO3(g)

A major simplification in the quantitative modeling of the atmospheric impact of the major aerosol and gaseous sulfur and nitrogen compounds would result from demonstration of phase equilibrium between the gases NH₃, HNO₃ and the appropriate aerosol-phase ionic or molecular species in the ambient atmosphere. The phase diagram of the (NH₄)₂SO₄-H₂SO₄-H₂O and NH₄NO₃-H₂O systems have been recently refined by experimental measurements and preliminary calculations of the mixed nitrate-sulfate system have also been made. Experiments to test the applicability of existing phase equilibria considerations to the ambient atmosphere have been designed and conducted based on newly devised techniques for continuous determination of gaseous NH₃ with time resolution < 5 min and unambiguous speciation of nitric acid and aerosol nitrate with time resolution of ~ 15 min. Preliminary results suggest that during a daytime period with aerosol composition approximating a letovicite-NH₄NO₃ mixture, observed products of NH₃ (g) and HNO₃(g) concentrations agreed very well with the equilibrium constant calculated for the ammonium nitrate-NH₃(g), HNO₃(g) equilibrium. During a night-time period, the predicted ammonia concentrations, based on bulk aerosol composition data, were much lower and nitric acid concentrations much higher, respectively, than the observed values. The error sources in the measured and calculated values do not appear to account for the apparent deviations from gas-phase concentrations based on the droplet-pH controlling bisulfate-sulfate equilibrium.     

Measurements of CCl3F and CCl4 at harwell over the period January 1975–June 1981 and the atmospheric lifetime of CCl3F

Measurements of CCl₃F and CCl₄ in the ambient air have been made at Harwell since October 1974. The background CCl₃F concentration at Harwell has increased with time throughout the period up to June 1981 when it had reached a value of 191 ppt. The increase was about 1.1 ppt month⁻¹ at the start of our study but it has now slowed down following the levelling off in global CCl₃F emissions. This data set represents one of the longest maintained attempts to determine the growth in CCl₃F in which careful attention has been paid to details of absolute calibration. Over the period that the measurements have been made the CCl₃F concentration has increased by over a half its original value, which provides a solid basis for comparison with release estimates.Two dimensional modelling is employed to obtain the atmospheric lifetime of CCl₃F from the observed Harwell 1975–1981 times series and the published CCl₃F historical release. The “best estimate” of the CCl₃F atmospheric lifetime is 75 y with 5–95 % confidence limits of 65–90 y. The limits are much tighter than those obtained from the first 3 y of data which would in principle have allowed a lifetime as short as 18 y (Penkett et al., 1979). This latest estimate of 75 y is wholly consistent with current theoretical estimates of the atmospheric lifetime due to stratospheric photolysis alone.Since 1979 the precision and resolution of the CCl₄ measurements at Harwell has been significantly improved. The background CCl₄ concentration found at Harwell for 1980–1981 is found to be 99–102 ppt. Whilst these values are in excellent agreement with model calculations assuming CCl₄ is wholly man-made in origin they are somewhat lower than some other published observations. Simultaneous observations of elevated concentrations of CCl₃ F and CCl₄ support the contention that CCl₄ is largely of man-made origins.     

Decomposition of NO in automobile exhaust by plasma–photocatalysis synergy

The combination of plasma discharge and TiO₂ photocatalysis exhibits high performances in the removal of nitrogen monoxide (NO). This article is aimed at elucidating the relationships between NO decomposition efficiency and various experimental parameters, including voltages, humidity and temperature. The experimental results indicate that the efficiency of NO removal by synergic plasma-catalyst coupling is significantly higher than plasma only or photocatalyst only systems. Moreover, the NO removal efficiency improves with the increase of applied voltage. Meanwhile, a higher humidity results in a reduced number of electron–hole pairs at the surface of TiO₂ photocatalyst, leading to lower synergic purification efficiencies. Finally, the efficiency of NO removal is raised with the increase of temperature due to the fact that the adsorption of NO and water by nano-TiO₂ is affected by environmental temperature.     

Determination of picogram quantities of chlortoluron in soil samples by luminol–chitosan chemiluminescence system

Based on the enhancing effect of chitosan (CS) on luminol-dissolved oxygen chemiluminescence (CL) reaction, a flow injection (FI) luminol–CS CL system was established. It was found that the increase of CL intensity was proportional to the concentrations of CS ranging from 0.7 to 10.0 μmol l^?1. In the presence of chlortoluron (CTU), the CL intensity of luminol–CS system could be obviously inhibited and the decrements of CL intensity were linearly proportional to the logarithm of CTU concentrations ranging from 0.01 to 70.0 ng ml^?1, giving the limit of detection 3.0 pg ml^?1 (3σ). At a flow rate of 2.0 ml min^?1, the whole process including sampling and washing could be accomplished within 36 s, offering a sample throughput of 100 h^?1. The proposed FI–CL method was successfully applied to the determination of CTU in soil samples with recoveries ranging from 95.0 % to 105.3 % and the relative standard deviations (RSDs) of less than 4.0 %.     

Modeling redistribution of α-HCH in Chinese soil induced by environment factors

This study explores long-term environmental fate of α-HCH in China from 1952 to 2007 using ChnGPERM (Chinese Gridded Pesticide Emission and Residue Model). The model captures well the temporal and spatial variations of α-HCH concentration in Chinese soils by comparing with a number of measured data across China in different periods. The results demonstrate α-HCH grasshopping effect in Eastern China and reveal several important features of the chemical in Northeast and Southeast China. It is found that Northeast China is a prominent sink region of α-HCH emitted from Chinese sources and α-HCH contamination in Southwest China is largely attributed to foreign sources. Southeast China is shown to be a major source contributing to α-HCH contamination in Northeast China, incurred by several environmental factors including temperature, soil organic carbon content, wind field and precipitation.     

Long-term measurements of iron-containing aerosols by Mössbauer spectroscopy in Poland

Mössbauer spectroscopy was applied to analyze the iron compounds present in atmospheric aerosol. As a significant part of air pollution, especially in winter months, iron appeared in the form of iron sulfides (FeS₂, FeS and Fe_1−xS), which were products of coal combustion. Also, iron oxyhydroxides and iron oxides, mostly α-Fe₂O₃ (bulk) and in the form of ultra fine particles in superparamagnetic state were observed. The concentration of iron in atmospheric air was calculated from the experimental spectra. Seasonal variations of iron concentration in atmospheric air measured over twenty years in the mountain region of Poland are discussed.     

Biodegradation of α and β Endosulfan in Soil as Influenced by Application of Different Organic Materials

Abstract

A laboratory pot experiment was conducted to study the effect of amending soil with four different sources of organic matter on the degradation rate of α and β endosulfan isomers. Poultry by-product meal, poultry manure, dairy manure, and municipal solid waste compost were cured, dried, ground (<1 mm) and thoroughly mixed with a calcareous soil at a rate of 2% and placed in plastic pots. Endosulfan was added at the rate of 20 mg kg^?1. The moisture level was kept near field capacity and the pots were kept at room temperature. Soil sub-samples, 100 g each, were collected from every pot at days 1, 8, 15, 22, 29, 43, and 57 for the measurement of endosulfan isomers. Endosulfan residues were extracted from the soil samples with acetone. The supernatant was filtered through anhydrous sodium sulphate, 5 mL aliquot was diluted to 25 mL with hexane, mixed well, and then two sub-samples from the filtrates were analyzed for α and β endosulfan isomers by gas chromatography. The results indicated that the half-life (T _½) of α-endosulfan in the poultry by-product meal treatment was 15 days compared to about 22 days in the other treatments. The T _½ of β-endosulfan was 22 days in the poultry by-product meal treatment and followed a bi-phasic pattern, 57 days in the municipal solid waste compost treatment and the extrapolated T _½ was about 115 days for the other three treatments.     

Determination of neonicotinoids in Estonian honey by liquid chromatography–electrospray mass spectrometry

The aim of the study was to provide a comprehensive overview of neonicotinoid pesticide residues in honey samples for a single country and compare the results with the import data for neonicotinoid pesticides. The levels of four neonicotinoid pesticides, namely thiamethoxam, imidacloprid, acetamiprid, and thiacloprid, were determined in 294 honey samples harvested from 2005 to 2013 from more than 200 locations in Estonia. For the analyzed honey samples, 27% contained thiacloprid, and its levels in all cases were below the maximum residue level set by the European Union. The other neonicotinoids were not detected. The proportion of thiacloprid-positive samples for different years correlates well with the data on thiacloprid imports into Estonia, indicating that honey contamination with neonicotinoids can be estimated based on the import data.     

The electro-oxidation of tetracycline hydrochloride in commercial DSA® modified by electrodeposited platinum

Environmental Science and Pollution Research - Tetracycline hydrochloride (TCH) electro-oxidation by commercial DSA® and commercial DSA® modified by platinum electrodeposition was...     

Sorption and desorption of lindane by wood charcoal in fixed‐bed reactor

Abstract

Sorption and desorption of lindane (y‐HCH) by wood charcoal (WC) and wood charcoal treated by 1N HNO₃ (WCT) in fixed‐bed reactor (FBR) were investigated in this study. WCT revealed a better performance than WC, in removing lindane in FBR. The breakthrough of lindane was significantly affected by the size of WCT, flow rate to the FBR, and depth of WCT bed. The removal of lindane in the presence of mixture of other pesticides was considerably reduced. The design parameters for FBR were calculated based on the bed‐depth service time (BDST) approach. Many parameters Viz. depth of sorption zone, velocity of sorption, sorbent use rate, critical bed‐depth, bed efficiency, and service time, were determined for design of the fixed‐bed. Using the material balance principle, the characteristics of the wave‐front were evaluated and found that the wave‐front velocity is approximately equal to the sorption velocity determined from the BDST approach. Desorption studies were performed in dilute organic solvent media and they gave an excellent performance in regeneration process.     

Induction of glutathione reductase enzyme activity by β‐aminobutyric acid in plant leaves

Abstract

Treatment of pea and tobacco leaf discs with the resistance inducer DL‐β‐amino‐n‐butyric acid (BABA) led to a substantial induction of glutathione reductase (GR, E.C. 1.6.4.2.) enzyme activity. After exposure to 1 mM BABA for 96 hrs, the GR activities were 3.2‐fold and 2.9‐fold higher in pea and tobacco leaf discs, respectively, than GR activities in untreated controls. Elevated GR levels may contribute to the antioxidative protection of plants during pathogen attack.