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  • 1
    Online Resource
    Online Resource
    Newark :John Wiley & Sons, Incorporated,
    Keywords: Trace elements--Analysis. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (443 pages)
    Edition: 1st ed.
    ISBN: 9781118274583
    Language: English
    Note: Cover -- Title page -- Copyright page -- Contents -- Preface -- About the companion website -- CHAPTER 1: Introduction -- 1.1 A historical background to metal aquatic chemistry -- 1.2 Historical problems with metal measurements in environmental media -- 1.3 Recent advances in aquatic metal analysis -- References -- Problems -- CHAPTER 2: An introduction to the cycling of metals in the biosphere -- 2.1 The hydrologic cycle -- 2.2 An introduction to the global cycling of trace metal(loid)s -- 2.2.1 The sources and cycling of metal(loid)s in the biosphere -- 2.2.2 Metal(loid) partitioning and solubility in natural waters -- 2.2.3 Human influence over metal(loid) fate and transport -- 2.2.4 Trace metal(loid) inputs to the atmosphere -- 2.2.5 Metal(loid)s in the terrestrial environment and freshwater ecosystems -- 2.2.6 The transport of metal(loid)s to the ocean -- 2.2.7 Trace metal(loid)s in ocean waters -- 2.2.8 Trace metal(loid) inputs from hydrothermal vents -- 2.3 Global cycles of some important trace metals -- 2.3.1 The global cycles of cadmium, copper, and zinc -- 2.3.2 The global cycle of mercury and lead -- 2.4 Chapter summary -- References -- Problems -- CHAPTER 3: Chemical thermodynamics and metal(loid) complexation in natural waters -- 3.1 Thermodynamic background for understanding trace metal(loid) complexation -- 3.1.1 The relationship between free energy and the equilibrium constant -- 3.1.2 Ionic strength effects -- 3.1.3 Thermodynamic equilibrium, kinetics and steady state -- 3.2 Bonding, electronic configuration, and complex formation -- 3.2.1 Ligand Field Theory -- 3.2.2 Thermodynamic effects of orbital splitting -- 3.2.3 Inorganic chemistry and complexation of transition metals -- 3.2.4 Inorganic chemistry and complexation of non-transition metals and metalloids -- 3.3 Complexation of metals in solution. , 3.3.1 Inorganic complexation -- 3.3.2 An approach to determining metal(loid) speciation in solution -- 3.3.3 The chemistry and speciation of metal-binding ligands -- 3.3.4 The complexation of the major ions in solution -- 3.3.5 Metal complexation with low molecular weight organic ligands -- 3.3.6 Complexation to large molecular weight organic matter -- 3.4 Trace metal interactions with the solid phase -- 3.4.1 Precipitation and dissolution -- 3.4.2 Adsorption of metals to aqueous solids -- 3.4.3 Dissolved-particulate partition coefficients -- 3.4.4 Adsorption isotherms -- 3.4.5 A complexation-based model for adsorption -- 3.5 Redox transformations and thermodynamic calculations -- 3.5.1 Electrochemistry and the equilibrium constant -- 3.5.2 The range in electrode potential and the stability of water -- 3.5.3 Equilibrium calculations involving redox reactions -- 3.5.4 Environmental considerations and controlling reactions -- 3.6 Chapter summary -- References -- Problems -- CHAPTER 4: Modeling approaches to estimating speciation and interactions in aqueous systems -- 4.1 Introduction -- 4.2 The underlying basis and application of chemical equilibrium models -- 4.3 Adsorption modeling -- 4.4 Modeling interactions between cations and organic matter, and inorganic surfaces -- 4.4.1 The WHAM modeling approach -- 4.4.2 The NICA-Donnan modeling framework -- 4.4.3 Modeling the adsorption of humic acids to surfaces and the interaction with metal(loid)s -- 4.5 Modeling redox transformations -- 4.6 Modeling the kinetics of reactions -- 4.6.1 Reactions in solution -- 4.6.2 Adsorption/desorption kinetics -- 4.6.3 Uptake kinetics for microorganisms -- 4.7 Incorporating kinetics and thermodynamics into fate and transport modeling -- 4.8 Chapter summary -- Appendix 4.1 -- Appendix 4.1a -- Appendix 4.1b -- References -- Problems. , CHAPTER 5: Metal(loid)s in the atmosphere and their inputs to surface waters -- 5.1 Introduction -- 5.2 Atmospheric transport and deposition -- 5.2.1 Dry deposition -- 5.2.2 Aerosol distributions and metal(loid) concentrations -- 5.2.3 Wet deposition -- 5.2.4 Atmospheric deposition fluxes -- 5.2.5 Source apportionment of atmospheric metal(loid)s -- 5.2.6 Gaseous volatilization and gas exchange of metal(loid) compounds -- 5.3 Atmospheric chemistry and surface water photochemistry of metals -- 5.4 Solubilization of aerosol metal(loid)s in natural waters -- 5.5 Focus topics -- 5.5.1 Focus topic: Atmospheric inputs and atmospheric chemistry of iron -- 5.5.2 Atmospheric chemistry and air-water exchange of mercury -- 5.6 Inputs of atmospheric metals to the biosphere -- 5.7 Chapter summary -- References -- Problems -- CHAPTER 6: Trace metal(loid)s in marine waters -- 6.1 Introduction -- 6.2 Metal(loid) partitioning in coastal and open ocean waters -- 6.2.1 The mechanisms of partitioning -- 6.2.2 Examination of metal speciation in the particulate phase -- 6.2.3 Examination of the complexation of metals with natural ligands in the filtered fraction -- 6.2.4 Metal concentrations in coastal waters -- 6.3 Metals in coastal and offshore sediments -- 6.3.1 Metals in the bulk phase -- 6.3.2 Metals in sediment porewater -- 6.3.3 Modeling metal cycling in sediments -- 6.3.4 Modeling of metal speciation in marine sediment porewaters -- 6.3.5 The importance of sediment resuspension and extreme events in coastal metal dynamics -- 6.3.6 Deep ocean sediments and manganese nodules and accretions -- 6.3.7 The biogeochemistry of metals in hydrothermal systems -- 6.4 Metal distributions in open ocean waters -- 6.4.1 Vertical distribution of metal(loid)s and controlling factors -- 6.4.2 Coordinated ocean studies: GEOTRACERS and prior and related programs. , 6.4.3 Iron, manganese, and aluminum cycling in open ocean waters -- 6.4.4 The biogeochemical cycling of zinc and cadmium in the ocean -- 6.4.5 Copper, cobalt, and other nutrient transition metals in the oceans -- 6.4.6 Anthropogenic metals - lead, silver, and mercury -- 6.4.7 Metalloids and other oxyanion cycling in seawater -- 6.4.8 Other transition metals, the lanthanides, and actinides -- 6.4.9 Particulate metal fluxes to the deep ocean -- 6.5 Chapter summary -- References -- Problems -- CHAPTER 7: Trace metals in freshwaters -- 7.1 Overview of metal cycling in freshwaters -- 7.2 Trace element cycling in lakes -- 7.2.1 Processes influencing metal(loid) fate and dissolved speciation in lakes -- 7.2.2 Modeling the speciation and association of trace elements in stratified systems -- 7.2.3 Focus topic: Mercury cycling in lakes -- 7.3 Trace elements in rivers and groundwater -- 7.3.1 Trace elements in rivers -- 7.3.2 Trace elements in groundwater -- 7.3.3 Focus topic: Mining impacts and acid mine drainage -- 7.3.4 Arsenic in surface water and groundwater -- 7.3.5 Metal inputs from groundwater and margin exchange processes -- 7.4 Human activities and their impact on trace metal(loid) concentrations in drinking water and receiving waters -- 7.4.1 Lead in drinking water -- 7.4.2 Metal inputs from waste water treatment facilities and other industrial discharges -- 7.5 Metal stable isotopes and their use -- 7.6 Chapter summary -- References -- Problems -- CHAPTER 8: Trace metals and organisms: Essential and toxic metals, organometallics, microbial processes, and metal bioaccumulation -- 8.1 Introduction -- 8.2 Mechanisms of metal accumulation by microorganisms -- 8.2.1 The transport of metals across membranes -- 8.2.2 Passive transport (diffusion) -- 8.2.3 Facilitated transport (accelerated diffusion) -- 8.2.4 Active uptake -- 8.3 Essential trace metals. , 8.3.1 An overview of essential trace metals -- 8.3.2 Focus topic: Iron uptake by microbes in marine waters -- 8.3.3 Focus topic: Transition metals and carbon fixation by microbes -- 8.3.4 The biochemistry of metals and their presence in the early biosphere -- 8.4 Organometallic compounds and microbial transformations of metals -- 8.4.1 Mechanisms of metal methylation -- 8.4.2 Less common organometallic compounds -- 8.4.3 Alkylated mercury compounds -- 8.4.4 Lead and tin compounds -- 8.4.5 Organometallics of arsenic, antimony, and bismuth -- 8.5 Bioavailability and bioaccumulation -- 8.5.1 Introduction -- 8.5.2 Trophic transfer of metals -- 8.5.3 Exposure and bioaccumulation models -- 8.6 Chapter Summary -- References -- Problems -- Index.
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  • 2
    Online Resource
    Online Resource
    [s.l.] : Wiley-Blackwell
    Keywords: Water chemistry ; Water Analysis ; Trace elements Analysis ; Electronic books
    Description / Table of Contents: "The textbooks that currently exist do not deal with this particular subject in a comprehensive fashion, and therefore this book is being proposed to full this gap"--
    Type of Medium: Online Resource
    Pages: Online Ressource (23825 KB, 448 S.)
    Edition: 1. Aufl.
    ISBN: 1405160489 , 1299241557 , 1118274598 , 9781299241558 , 9781118274590
    Language: English
    Note: Includes bibliographical references and index , 2.2.3 Human influence over metal(loid) fate and transport2.2.4 Trace metal(loid) inputs to the atmosphere; 2.2.5 Metal(loid)s in the terrestrial environment and freshwater ecosystems; 2.2.6 The transport of metal(loid)s to the ocean; 2.2.7 Trace metal(loid)s in ocean waters; 2.2.8 Trace metal(loid) inputs from hydrothermal vents; 2.3 Global cycles of some important trace metals; 2.3.1 The global cycles of cadmium, copper, and zinc; 2.3.2 The global cycle of mercury and lead; 2.4 Chapter summary; References; Problems. , 3.2.4 Inorganic chemistry and complexation of non-transition metals and metalloids3.3 Complexation of metals in solution; 3.3.1 Inorganic complexation; 3.3.2 An approach to determining metal(loid) speciation in solution; 3.3.3 The chemistry and speciation of metal-binding ligands; 3.3.4 The complexation of the major ions in solution; 3.3.5 Metal complexation with low molecular weight organic ligands; 3.3.6 Complexation to large molecular weight organic matter; 3.4 Trace metal interactions with the solid phase; 3.4.1 Precipitation and dissolution; 3.4.2 Adsorption of metals to aqueous solids. , 3.4.3 Dissolved-particulate partition coefficients3.4.4 Adsorption isotherms; 3.4.5 A complexation-based model for adsorption; 3.5 Redox transformations and thermodynamic calculations; 3.5.1 Electrochemistry and the equilibrium constant; 3.5.2 The range in electrode potential and the stability of water; 3.5.3 Equilibrium calculations involving redox reactions; 3.5.4 Environmental considerations and controlling reactions; 3.6 Chapter summary; References; Problems; CHAPTER 4: Modeling approaches to estimating speciation and interactions in aqueous systems; 4.1 Introduction. , CHAPTER 3: Chemical thermodynamics and metal(loid) complexation in natural waters3.1 Thermodynamic background for understanding trace metal(loid) complexation; 3.1.1 The relationship between free energy and the equilibrium constant; 3.1.2 Ionic strength effects; 3.1.3 Thermodynamic equilibrium, kinetics and steady state; 3.2 Bonding, electronic configuration, and complex formation; 3.2.1 Ligand Field Theory; 3.2.2 Thermodynamic effects of orbital splitting; 3.2.3 Inorganic chemistry and complexation of transition metals. , Cover; Title page; Copyright page; Contents; Preface; About the companion website; CHAPTER 1: Introduction; 1.1 A historical background to metal aquatic chemistry; 1.2 Historical problems with metal measurements in environmental media; 1.3 Recent advances in aquatic metal analysis; References; Problems; CHAPTER 2: An introduction to the cycling of metals in the biosphere; 2.1 The hydrologic cycle; 2.2 An introduction to the global cycling of trace metal(loid)s; 2.2.1 The sources and cycling of metal(loid)s in the biosphere; 2.2.2 Metal(loid) partitioning and solubility in natural waters.
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  • 3
    Publication Date: 2022-05-26
    Description: Author Posting. © Association for the Sciences of Limnology and Oceanography, 2012. This article is posted here by permission of Association for the Sciences of Limnology and Oceanography for personal use, not for redistribution. The definitive version was published in Limnology and Oceanography: Methods 10 (2012): 90-100, doi:10.4319/lom.2012.10.90.
    Description: We conducted a laboratory intercomparison of total mercury (Hg) determination in seawater collected during U.S. GEOTRACES Intercalibration cruises in 2008 and 2009 to the NW Atlantic and NE Pacific Oceans. Results indicated substantial disagreement between the participating laboratories, which appeared to be affected most strongly by bottle cleanliness and preservation procedures. In addition, we examined the effectiveness of various collection and sample preparation procedures that may be used on future GEOTRACES cruises. The type of sampling system and filtration medium appeared to make little difference to results. Finally, and in light of results from experiments that considered sample bottle material effect and the development of new methods for CH3Hg+ extraction from seawater, we propose a recommended procedure for determining all four of the major Hg species in seawater (elemental, dimethyl-, monomethyl-, and total Hg).
    Description: This work was supported by the National Science Foundation program in Chemical Oceanography under grants OCE–0825157, –0825108, –0825583 and –0825068.
    Repository Name: Woods Hole Open Access Server
    Type: Article
    Format: application/pdf
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  • 4
    Publication Date: 2022-10-31
    Description: Dataset: LIS plankton
    Description: Concentrations of mercury forms and ancillary parameters were investigated in size fractionated plankton samples and in water from Long Island Sound and the adjacent shelf. Samples were collected in three separate seasons (Spring, Summer, Fall) during 2014 to research the temporal trophic transfer dynamics of mercury and methylmercury into zooplankton and phytoplankton. For a complete list of measurements, refer to the full dataset description in the supplemental file 'Dataset_description.pdf'. The most current version of this dataset is available at: https://www.bco-dmo.org/dataset/840875
    Description: NSF Division of Ocean Sciences (NSF OCE) OCE-1634048
    Keywords: Methylmercury ; Phytoplankton ; Zooplankton ; Estuary ; Mercury
    Repository Name: Woods Hole Open Access Server
    Type: Dataset
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  • 5
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Environmental science & technology 28 (1994), S. 577-585 
    ISSN: 1520-5851
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Energy, Environment Protection, Nuclear Power Engineering
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    s.l. : American Chemical Society
    Environmental science & technology 29 (1995), S. 2157-2161 
    ISSN: 1520-5851
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology , Energy, Environment Protection, Nuclear Power Engineering
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    Springer
    Water, air & soil pollution 56 (1991), S. 791-803 
    ISSN: 1573-2932
    Source: Springer Online Journal Archives 1860-2000
    Topics: Energy, Environment Protection, Nuclear Power Engineering
    Notes: Abstract The cycling of dissolved gaseous Hg (DGM) has been examined in our studies of the troposphericHg cycle, air-water exchange and their importance to the biogeochemical behavior and fate of Hg in temperate lakes. Five seepage lakes in northcentral Wisconsin, ranging in pH from 4.7 to 7.2, have been studied under a variety of limnological conditions which included the following seasonal periods: summer (peak stratification), fall (following turnover) and late winter (under ice). Analytically, DGM was determined after purging lake water with argon and collecting the volatile Hg fraction on gold coated sand. The Hg collections were analysed by pyrolysis in a two-stage Au amalgamation gas train with detection by atomic fluorescence spectroscopy (AFS). In addition, chemical speciation of the volatile fraction has been achieved by trapping on a nondestructive substrate followed by gas chromatographic separation and AFS detection. The DGM consists principally of elemental Hg (Hgo) under all sampling conditions, with no significant contribution from volatile organic Hg species (detection limit of 3 femtomolar). Atmospheric gaseous Hg, which also consists principally of Hgo, was measured and the air-water partitioning determined. In general, the lake waters have been supersaturated with Hgo relative to the atmosphere. Supersaturation was greater in the summer, ranging from ca. 1.4 to 12 times (x) the saturation concentration. During the other sampling periods, Hgo ranged from saturation to ca. 7x the equilibrium concentration. The flux of Hg from the lakes due to gas evasion is significant and is estimated at approximately 10% of the annual atmospheric input of Hg to the lakes. An apparent relationship between Hgo and pH has been observed with lakes of lower pH having smaller Hgo concentrations.
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Springer
    Biogeochemistry 40 (1998), S. 235-247 
    ISSN: 1573-515X
    Keywords: fish ; invertebrates ; ligands ; mercury ; methylmercury ; phytoplankton
    Source: Springer Online Journal Archives 1860-2000
    Topics: Chemistry and Pharmacology , Geosciences
    Notes: Abstract To understand the accumulation of inorganic mercury and methylmercury at the base of the estuarine food chain, phytoplankton (Thalassiosira weissflogii) uptake and mercury speciation experiments were conducted. Complexation of methylmercury as methylmercury-bisulfide decreased the phytoplankton uptake rate while the uptake rate of the methylmercury-cysteine and -thiourea complexes increased with increasing complexation by these ligands. Furthermore, our results indicated that while different ligands influenced inorganic mercury/methylmercury uptake by phytoplankton cells, the ligand complex had no major influence on either where the mercury was sequestered within the phytoplankton cell nor the assimilation efficiency of the mercury by copepods. The assimilation efficiency of inorganic mercury/methylmercury by copepods and amphipods feeding on algal cells was compared and both organisms assimilated methylmercury much more efficiently; the relative assimilation efficiency of methylmercury to inorganic mercury was 2.0 for copepods and 2.8 for amphipods. The relative assimilation is somewhat concentration dependent as experiments showed that as exposure concentration increased, a greater percentage of methylmercury was found in the cytoplasm of phytoplankton cells, resulting in a higher concentration in the copepods feeding on these cells. Additionally, food quality influenced assimilation by invertebrates. During decay of a T. weissflogii culture, which served as food for the invertebrates, copepods were increasingly less able to assimilate the methylmercury from the food, while even at advanced stages of decay, amphipods were able to assimilate mercury from their food to a high degree. Finally, fish feeding on copepods assimilated methylmercury more efficiently than inorganic mercury owing to the larger fraction of methylmercury found in the soft tissues of the copepods.
    Type of Medium: Electronic Resource
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  • 9
    Publication Date: 2024-02-07
    Description: Highlights: • Copepods more efficiently assimilated methylmercury than inorganic mercury. • Algal size can consequentially influence uptake for different mercury species. • The fraction of methylmercury transferred to zooplankton varies with algae species. • Uptake of mercury species into algae is active. • Demonstrated the usefulness of stable isotopes approaches. Mercury (Hg) and methylmercury (CH3Hg) are found at trace levels in most marine waters. These species, particularly CH3Hg, then ominously bioaccumulate through marine food chains eventually reaching potentially harmful levels in top oceanic wildlife. Accordingly, it is important to measure and evaluate uptake at environmentally relevant concentrations where trophic transfer initiates; during uptake in primary producers, and consumption by plankton grazers. Experiments using cultured copepods (Acartia tonsa) and field zooplankton assemblages were performed with two different sized diatom species labeled with stable isotopes of inorganic Hg (Hg-200) and CH3Hg ((CH3Hg)-Hg-199) at different concentrations. We observed size-specific effects on algal uptake and transfer to copepods, in addition to effects of Hg species concentration. Prey size effects were likewise observed on copepod assimilation efficiencies (AE). Average AE of Hg-200 for copepods feeding on smaller diatoms was 50%, and 39% for larger diatoms. The AEs were much greater for (CH3Hg)-Hg-199, yielding 71% for the smaller and 88% for the larger diatoms. These experiments add evidence demonstrating a significant relationship between Hg and CH3Hg exposure concentration and subsequent algal uptake and transfer to zooplankton. Furthermore, results imply that facilitated uptake of CH3Hg into algae occurs at low (similar to pM) concentrations, which has been suggested but not confirmed in previous research.
    Type: Article , PeerReviewed
    Format: text
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  • 10
    Publication Date: 2024-05-13
    Description: Highlights • Mercury methylation in sediment rapidly transported into water and diatoms. • CH3Hg flux was highest for sediments with higher sulfide and organic content. • Mineral and compressed sediment released minor Hg and CH3Hg. • Higher sediment Hg species flux does not correlate with high sediment content. • Stable isotope incubations provide substantial insight to environmental Hg cycling. Abstract Mercury (Hg) is a conspicuous and persistent global pollutant. Ionic Hg can be methylated into noxious methylmercury (CH3Hg), which biomagnifies in marine tropic webs and poses a health risk to humans and organisms. Sediment Hg methylation rates are variable, and the output flux of created CH3Hg are dependent on sediment characteristics and environmental factors. Thus, uncertainties remain about the formation and flux of CH3Hg from sediment, and how this could contribute to the bioaccumulative burden for coastal organisms in shallow ecosystems. Cores were collected from 3 estuarine locations along the Eastern USA to examine how sediments characteristics influence the introduction of Hg and CH3Hg into the base of the food chain. Stable isotopes of inorganic 200Hg and CH3199Hg were injected into sediments of individual cores, with cultured diatoms constrained to overlying waters. Five different treatments were done on duplicate cores, spiked with: (1) no Hg isotopes (control); (2) inorganic 200Hg; (3) CH3199Hg; (4) both 200Hg and CH3199Hg isotopes, (5) both 200Hg and CH3199Hg into overlying waters (not sediment). Experimental cores were incubated for 3 days under temperature and light controlled conditions. These results demonstrate that upper sediments characteristics lead to high variability in Hg cycling. Notably, sediments which contained abundant and peaty organic material (∼28 %LOI), had the highest pore water DOC (3206 μM) and displayed bands of sulfur reducing bacteria yielded the greatest methylation rate (1.97 % day−1) and subsequent diatom uptake of CH3200Hg (cell quota 0.18 amol/cell) in the overlying water.
    Type: Article , PeerReviewed
    Format: text
    Format: text
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