Neuropsychological dysfunction related to earlier occupational exposure to mercury vapor

We assessed the neuropsychological test performances of 26 patients (mean age = 41.5 ± 6.1 years; mean years of education = 9.8 ± 1.8; 20 males) diagnosed with chronic occupational mercurialism who were former workers at a fluorescent lamp factory. They had been exposed to elemental mercury for an average of 10.2 ± 3.8 years and had been away from this work for 6 ± 4.7 years. Mean urinary mercury concentrations 1 year after cessation of work were 1.8 ± 0.9 µg/g creatinine. Twenty control subjects matched for age, gender, and education (18 males) were used for comparison. Neuropsychological assessment included attention, inhibitory control, verbal and visual memory, verbal fluency, manual dexterity, visual-spatial function, executive function, and semantic knowledge tests. The Beck Depression Inventory and the State and Trait Inventory were used to assess depression and anxiety symptoms, respectively. The raw score for the group exposed to mercury indicated slower information processing speed, inferior performance in psychomotor speed, verbal spontaneous recall memory, and manual dexterity of the dominant hand and non-dominant hand (P < 0.05). In addition, the patients showed increased depression and anxiety symptoms (P < 0.001). A statistically significant correlation (Pearson) was demonstrable between mean urinary mercury and anxiety trait (r = 0.75, P = 0.03). The neuropsychological performances of the former workers suggest that occupational exposure to elemental mercury has long-term effects on information processing and psychomotor function, with increased depression and anxiety also possibly reflecting the psychosocial context.

The role of organic matter on the adsorption of mercury in sediments from Amazon lakes, Brazil

Gold has been exploited intensively in the Brazilian Amazon during the past 20 years, and the elemental mercury (Hg) used in amalgamating the gold has caused abnormal Hg concentrations in waterways. Since 1986 particular attention has been given to the Madeira River because it is the largest tributary of the Amazon River and gold mining was officially allowed on a 350-km sector of the river. In this paper, samples of sediments from nine lakes located in the Madeira River basin, Rondonia State, Brazil, were analysed for mercury and organic matter. The average Hg content ranged between 33 and 157 ppb, which is about 8-40 times higher than the average value corresponding to 4.4 ppb for rocks occurring in the area (regional background). Significant correlation was found between the Hg content and organic matter in the sediments, indicating its importance on the retention of this heavy metal.

IMPACT OF 2000-2050 CLIMATE CHANGE ON GLOBAL ATMOSPHERIC TRANSPORT AND DEPOSITION OF MERCURY

Since it is very toxic and accumulates in organisms, particularly in fish, mercury is a very important pollutant and one of the most studies. And this concern over the toxicity and human health risks of mercury has prompted efforts to regulate anthropogenic emissions. As mercury pollution problem is getting increasingly serious, we are curious about how serious this problem will be in the future. What is more, how the climate change in the future will affect the mercury concentration in the atmosphere. So we investigate the impact of climate change on mercury concentration in the atmosphere. We focus on the comparison between the mercury data for year 2000 and for year 2050. The GEOS-Chem model shows that the mercury concentrations for all tracers (1 to 3), elemental mercury (Hg(0)), divalent mercury (Hg(II)) and primary particulate mercury (Hg(P)) have differences between 2000 and 2050 in most regions over the world. From the model results, we can see the climate change from 2000 to 2050 would decrease Hg(0) surface concentration in most of the world. The driving factors of Hg(0) surface concentration changes are natural emissions(ocean and vegetation) and the transformation reactions between Hg(0) and Hg(II). The climate change from 2000 to 2050 would increase Hg(II) surface concentration in most of mid-latitude continental parts of the world while decreasing Hg(II) surface concentration in most of high-latitude part of the world. The driving factors of Hg(II) surface concentration changes is deposition amount change (majorly wet deposition) from 2000 to 2050 and the transformation reactions between Hg(0) and Hg(II). Climate change would increase Hg(P) concentration in most of mid-latitude area of the world and meanwhile decrease Hg(P) concentration in most of high-latitude regions of the world. For the Hg(P) concentration changes, the major driving factor is the deposition amount change (mainly wet deposition) from 2000 to 2050.

Interaction entre le mercure élémentaire et les sédiments lacustres

Mémoire numérisé par la Division de la gestion de documents et des archives de l'Université de Montréal

Avaliação do risco de exposição ao mercúrio elementar em uma Unidade de Terapia Intensiva

O metal mercúrio é conhecido pela sua grande toxidade apesar de seu emprego difundido. Desde a Antigüidade, se reconhece sua ação tóxica na exposição ocupacional. Em alguns ambientes laborais, os riscos são maiores, como é o caso de hospitais, que utilizam o mercúrio elementar em vários equipamentos, especialmente em termômetros de verificação da temperatura corporal, largamente empregados. Como na instituição objeto deste estudo foram quebrados 148 termômetros em uma Unidade de Terapia Intensiva no período de um ano, esta pesquisa objetivou a realização de uma avaliação de alguns indicadores ambientais neste espaço de trabalho e de alguns indicadores biológicos e psicológicos em uma amostra de trabalhadores desta unidade, que se dispuseram a participar da pesquisa. A avaliação de tais indicadores são recomendados como pertinentes pela literatura (ATSDR, 1989). Não se detectou em nenhuma das avaliações realizadas, índices acima das normas estabelecidas. Interpreta-se que a temperatura da unidade (20ºC) reduz a possibilidade do mercúrio se volatizar e intoxicar os trabalhadores. As regras de higiene, típicas do contexto hospitalar, e a rotina de rápido recolhimento dos resíduos dos termômetros quebrados e seu acondicionamento em recipientes com tampa são os principais fatores explicativos para os índices encontrados.

Konzeptionelle Entwicklung von Mikrokosmos-Experimenten zur Untersuchung der speziesspezifischen Transformationsprozesse des Quecksilbers mittels Isotopenverhältnisbestimmungen

Zur Untersuchung der speziesspezifischen Transformationsprozesse des Quecksilbers in der Umwelt wurden erstmalig Mikrokosmosexperimente unter Verwendung von isotopenangereicherten Verbindungen durchgeführt. Es wurden naturrelevante Bedingungen simuliert, um eine spätere Übertragbarkeit der Ergebnisse auf den biogeochemischen Kreislauf des Quecksilbers zu gewährleisten. Die aufgebauten Mikrokosmen bestanden aus Boden/Pflanzen/Luft-Kompartimenten. Der Boden der Mikrokosmen wurde mit isotopenangereicherten Quecksilberspezies dotiert. Durch die Verwendung von isotopenangereicherten Verbindungen, verbunden mit gleichzeitiger ICP/MS-Detektion, konnten auftretende Transformationsprozesse beobachtet werden. Die Messung der Quecksilberspezies erfolgte mittels GC-ICP/MS nach vorheriger Derivatisierung mit Natriumtetraethylborat und Anreicherung per 'purge and trap'.Die Massenspuren der einzelnen Quecksilberisotope wurden für alle Quecksilberspezies gemessen und daraus dann für jede Spezies die Isotopenverhältnisse gebildet. Bei einer Änderung des Isotopenverhältnisses kann von einer Speziestransformation ausgegangen werden.Aus den Mikrokosmosexperimenten, denen Methylquecksilber als angereicherte Isotopenverbindung zugegeben wurde, konnte gefolgert werden, dass Methylquecksilber im Boden zunächst zu anorganischem Quecksilber demethyliert wurde. Im Anschluss daran erfolgte eine Reduktion zu elementarem Quecksilber. Dieses gebildete elementare Quecksilber verflüchtigte sich nahezu vollständig (ca. 90-100%) vom Boden in die Atmosphäre.Bei der Zugabe von anorganischem Quecksilber als angereicherte Isotopenverbindung in den Boden wurde vorwiegend eine Reduktion zu elementarem Quecksilber beobachtet, das dann in die Atmosphäre emittiert. Es konnte aber auch eine geringe Methylierung (ca. 5%) zu Methylquecksilber beobachtet werden. Daraus kann gefolgert werden, dass die methylierten Quecksilberverbindungen eine wesentliche Rolle im natürlichen Kreislauf des Quecksilbers spielen.Parallel zu den Mikrokosmosexperimenten wurden Feldversuche in einem flussnahen Feuchtgebiet, aus dem auch der Boden für die Mikrokosmosexperimente entnommen worden war, durchgeführt. In den Feldversuchen wurden Quecksilberkonzentrationen und der Quecksilberfluss zwischen dem Boden und der Atmosphäre mit Hilfe von Flusskammerexperimenten bestimmt. Es konnten mit Hilfe von Mikrokosmen, die natürliche Verhältnisse simulieren sollten, und mit Hilfe verschieden angereicherter Isotopenspikes erstmals Speziestransformationen des Quecksilbers direkt beobachtet werden. Die GC-ICP/MS-Methode ermöglichte eine eindeutige Identifikation von Edukt und Produkt der jeweiligen Umwandlung. Allerdings wurde die Untersuchung eingeschränkt durch die irreversiblen biologischen Veränderungen in den eingesetzten Mikrokosmen nach über einer Woche und durch die Notwendigkeit, vergleichsweise hohe Konzentrationen der Spikes einzusetzen, um eine statistisch signifikante Auswertung der Veränderung der Isotopenverhältnisse zu erreichen. Somit sind Mikrokosmosexperimente nur eingeschränkt für Untersuchungen des Quecksilberverhaltens geeignet.Im Rahmen dieser Arbeit ist es aber gelungen, die Mikrokosmenexperimente unter Verwendung von isotopenangereicherten Verbindungen und der GC-ICP/MS-Methode als leistungsstarkes Verfahren zur Beobachtung von Speziestransformationsprozessen des Quecksilbers zu etablieren.

Au@Hg nanoalloy formation through direct amalgamation: Structural, spectroscopic, and computational evidence for slow nanoscale diffusion

Dynamic core-shell nanoparticles have received increasing attention in recent years. This paper presents a detailed study of Au-Hg nanoalloys, whose composing elements show a large difference in cohesive energy. A simple method to prepare Au@Hg particles with precise control over the composition up to 15 atom% mercury is introduced, based on reacting a citrate stabilized gold sol with elemental mercury. Transmission electron microscopy shows an increase of particle size with increasing mercury content and, together with X-ray powder diffraction, points towards the presence of a core-shell structure with a gold core surrounded by an Au-Hg solid solution layer. The amalgamation process is described by pseudo-zero-order reaction kinetics, which indicates slow dissolution of mercury in water as the rate determining step, followed by fast scavenging by nanoparticles in solution. Once adsorbed at the surface, slow diffusion of Hg into the particle lattice occurs, to a depth of ca. 3 nm, independent of Hg concentration. Discrete dipole approximation calculations relate the UV-vis spectra to the microscopic details of the nanoalloy structure. Segregation energies and metal distribution in the nanoalloys were modeled by density functional theory calculations. The results indicate slow metal interdiffusion at the nanoscale, which has important implications for synthetic methods aimed at core-shell particles.

Determination of total and inorganic mercury in whole blood by cold vapor inductively coupled plasma mass spectrometry (CV ICP-MS) with alkaline sample preparation

A simple method with a fast sample preparation procedure for total and inorganic mercury determinations in blood samples is proposed based on flow injection cold vapor inductively coupled plasma mass spectrometry (FI-CVICP-MS). Aliquots of whole blood (500 mL) are diluted 1 + 1 v/v with 10.0% v/v tetramethylammonium hydroxide (TMAH) solution, incubated for 3 h at room temperature and then further diluted 1 + 4 v/v with 2.0% v/v HCl. The inorganic Hg was released by online addition of L-cysteine and then reduced to elemental Hg by SnCl(2). On the other hand, total mercury was determined by on-line addition of KMnO(4) and then reduced to elemental Hg by NaBH(4). Samples were calibrated against matrix-matching. The method detection limit was found to be 0.80 mu g L(-1) and 0.08 mu g L(-1) for inorganic and total mercury, respectively. Sample throughput is 20 samples h(-1). The method accuracy is traceable to Standard Reference Material (SRM) 966 Toxic Metals in Bovine Blood from the National Institute of Standards and Technology (NIST). For additional validation purposes, human whole blood samples were analyzed by the proposed method and by an established CV AAS method, with no statistical difference between the two techniques at 95% confidence level on applying the t-test.

Sulfur isotope analysis of cinnabar from Roman wall paintings by elemental analysis/isotope ratio mass spectrometry - tracking the origin of archaeological red pigments and their authenticity

The most valuable pigment of the Roman wall paintings was the red color obtained from powdered cinnabar (Minium Cinnabaris pigment), the red mercury sulfide (HgS), which was brought from mercury (Hg) deposits in the Roman Empire. To address the question of whether sulfur isotope signatures can serve as a rapid method to establish the provenance of the red pigment in Roman frescoes, we have measured the sulfur isotope composition (delta(34) S value in parts per thousand VCDT) in samples of wall painting from the Roman city Aventicum (Avenches, Vaud, Switzerland) and compared them with values from cinnabar from European mercury deposits (Almaden in Spain, Idria in Slovenia, Monte Amiata in Italy, Moschellandsberg in Germany, and Genepy in France). Our study shows that the delta(34) S values of cinnabar from the studied Roman wall paintings fall within or near to the composition of Almaden cinnabar; thus, the provenance of the raw material may be deduced. This approach may provide information on provenance and authenticity in archaeological, restoration and forensic studies of Roman and Greek frescoes. Copyright (c) 2010 John Wiley & Sons, Ltd.

A thermal analysis study of dithizone and dithizonates of mercury, silver and bismuth

Solid dithizonates of Hg(I), Ag(I) and Bi(III) have been prepared. Thermogravimetry (TG), derivative thermogravimetry (DTG), differential scanning calorimetry (DSC), X ray diffraction powder patterns and elemental analysis have been used to characterize and to study the thermal stability and thermal decomposition of the dithizone and of these dithizonates.

Mercury Redox Chemistry in the Negro River Basin, Amazon: The Role of Organic Matter and Solar Light

Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

Determination of sulfur compounds in gasoline using mercury film electrode by square wave voltammetry

A sensitive method based on square wave voltammetry is described for the quantitative determination of elemental sulfur, disulfide and mercaptan in gasoline using a mercury film electrode. These sulfur compounds can be quantified by direct dissolution of gasoline in a supporting electrolyte followed by subsequent voltammetric measurement. The supporting electrolyte is 1.4 mol L-1 sodium acetate and No acetic acid in methanol. Chemical and optimum operational conditions for the formation of the mercury film were analyzed in this study. The values obtained were a 4.3 mu m thickness for the mercury film, a 1000 rpm rotation frequency, -0.9 V applied potential and 600 s depositing time. Voltammetric measurements were obtained using square wave voltammetry with detection limits of the 3.0 x 10(-9), 1.6 x 10(-7) and 4.9 x 10(-7) mol L-1 for elemental sulfur, disulfide and mercaptan, respectively. (C) 2007 Elsevier Ltd. All rights reserved.

A thermal analysis study of dithizone and dithizonates of mercury, silver and bismuth

Foram preparados os ditizonatos de Hg (I), Ag (I) e Bi (III). Termogravimetria (TG), termogravimetria derivada (DTG), calorimetria exploratória diferencial (DSC), difratometria de raios X pelo método do pó e análise elementar foram usados para caracterizar e para estudar a estabilidade térmica e a decomposição térmica da ditizona e destes ditizonatos.

Reduction of mercury(II) by tropical river humic substances (Rio Negro) - Part II. Influence of structural features (molecular size, aromaticity, phenolic groups, organically bound sulfur)

The influence of structural features of tropical river humic substances (HS) on their capability to reduce mercury(II) in aqueous solutions was studied. The HS investigated were conventionally isolated from Rio Negro water-Amazonas State/Brazil by means of the collector XAD 8. In addition, the isolated HS were on-line fractionated by tangential-flow multistage ultrafiltration (nominal molecular-weight cut-offs: 100, 50, 30, 10, 5 kDa) and characterized by potentiometry and UV/VIS spectroscopy. The reduction of Hg(II) ions to elemental Hg by size-fractions of Rio Negro HS was assessed by cold-vapor AAS (CVAAS). UV/VIS spectrometry revealed that the fractions of high molecular-size (F-1 > 100 kDa and F-2: 50-100 kDa) have a higher aromaticity compared to the fractions of small molecular-size (F-5: 5-10 kDa, F-6: < 5 kDa). In contrast, the potentiometric study showed different concentration of functional groups in the studied HS fractions. The reduction of Hg(II) by aquatic HS fractions at pH 5 proceeded in two steps (I, II) of slow first order kinetics (t(1/2) of I: 160 min, t(1/2) of II: 300 min) weakly influenced by the molecular-size, in contrast to the differing degree of Hg(II) reduction (F-5 > F-2 > > F-1 > F-3 > F-4 > > F-6). Accordingly, Hg(II) ions were preferably reduced by HS molecules having a relatively high ratio of phenolic/carboxylic groups and a small concentration of sulfur. From these results a complex 'competition' between reduction and complexation of mercury(II) by aquatic HS occurring in tropical rivers such as the Rio Negro can be suggested. (C) 2003 Elsevier B.V. All rights reserved.