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Complexation reactions in aquatic systems : an analytical approach / J. Buffle, translators S.P. Kounaves, A. Kounaves and R.S. Altman

J. Buffle
- Vol. 1990, Iss: 1990, pp 1-99
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The article was published on 1990-01-01 and is currently open access. It has received 812 citations till now.

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WHAM—a chemical equilibrium model and computer code for waters, sediments, and soils incorporating a discrete site/electrostatic model of ion-binding by humic substances

E. Tipping
TL;DR: The WHAM (Windermere Humic Aqueous Model) as mentioned in this paper is a simple inorganic speciation code for aqueous solutions that combines Humic Ion-Binding Model V with a simple, inorganic inorganic specciation code.
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Ion binding to natural organic matter : competition, heterogeneity, stoichiometry and thermodynamic consistency

TL;DR: The NICCA-Donnan model as mentioned in this paper is a semi-empirical model that is similar to the NICA-donnan model except that it introduces an additional degree of scaling that ensures thermodynamic consistency and allows for variable stoichiometry of binding, which implicitly accounts for the large degree of chemical heterogeneity of humic particles.
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A unifying model of cation binding by humic substances

TL;DR: Model V describes the binding of ions by humic substances in terms of complexation at discrete sites, modified by electrostatic attraction and/or repulsion, and also takes account of nonspecific binding due to counterion accumulation.
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A Generalized Description of Aquatic Colloidal Interactions: The Three-colloidal Component Approach

TL;DR: In this article, the physicochemical properties of the different groups of colloids are described, and the role of each colloid class is discussed with respect to homoaggregation (aggregation within a given colloid) and hetero-aggregation among different colloid types.
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The effect of humic acid adsorption on pH-dependent surface charging and aggregation of magnetite nanoparticles

TL;DR: The pH-dependent adsorption of humic acid (HA) on magnetite and its effect on the surface charging and the aggregation of oxide particles were investigated and nanoparticles are stabilized in a way of combined steric and electrostatic effects.
References
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The role of geochemistry in environmental and epidemiological studies in developing countries: a review

TL;DR: The role of geochemistry in the preparation of high resolution baseline data to identify potential hazards, understanding the pathways of chemical elements from rocks and soils to man and animals, and developing amelioration strategies to reduce the impacts of inappropriate land use, power generation and mining is discussed in this paper.
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A nickel availability study in serpentinised areas of Portugal

TL;DR: In this paper, the factors that control Ni availability and adsorption in serpentine soils from the northeast of Portugal, which developed under temperate climacteric conditions, were investigated following characterisation of the soils' selected physicochemical properties.
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Complexation of Cd(II) and Pb(II) with humic acids studied by anodic stripping voltammetry using differential equilibrium functions and discrete site models

TL;DR: In this paper, the binding of CdII and Pb(II) to two humic acids was studied by differential pulse anodic stripping voltammetry using continuous differential equilibrium functions and linear Scatchard plots.
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Labile/inert metal species in aquatic humic substances: an ion-exchange study

TL;DR: An ion exchange procedure has been developed for the analytical fractionation of metals (e.g., Al, Co, Cu, Fe, Mn, Ni, Pb, Zn) forming labile/inert complexes with aquatic humic substances (HS) isolated from bog, forest, ground and lake water as discussed by the authors.
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The effect of pH and atmospheric deposition on concentrations of trace elements in acidified freshwaters: A statistical approach

TL;DR: In this article, a statistical evaluation of freshwaters from little polluted stream basins in the Czech Republic indicated a relationship between the Pb, Cu, Zn, Cd, Be, As, Mn, Sr, F− and Fe concentrations and the pH, over a range of pH 3.6 to 9.6.