Detailed studies have been made on the ion exchange and sorptive properties of aqueous dispersions of single crystals of beta-iron oxide hydroxide and monoclinic zirconia. These microcrystals were prepared in the laboratory and characterised by transmission electron micrographs and electron diffraction patterns. The crystals are typically 1000-2000A in size and have amphoteric ion exchange properties. In this work, a multiion selective electrode titration system working with a highly developed computational and graphic system was developed to determine the ion exchange and sorption properties of these crystals. Ion sieving characteristics of betaFeOOH have been proven and extended to include a separation of chloride from solutions containin...
Inner surface potential, one of the most important variables affecting the interfacial equilibrium o...
Ion exchange and surface complexation are the main models used to quantify the sorption processes. T...
The partitioning of solutes between the solid mineral and aqueous phase frequently controls the fate...
Detailed studies have been made on the ion exchange and sorptive properties of aqueous dispersions o...
The amphoteric ion exchange and sorptive properties of monoclinic zirconia are studied here in detai...
Research has been performed on the ion exchange and sorption processes which occur on the surfaces a...
One model system for the investigation of selectivity in inorganic ion exchangers is a group of syn...
The work described in this thesis consists of investigations into the sorptive behaviour of magnetit...
Hydrated oxides such as HAO,\u27HFO, goethite, and BA40 are prevalent in soils and sediments as disc...
Iron (oxyhydr)oxide (FeOOH) minerals play important roles in various natural, technological and soci...
349-350Distribution coefficients of a large number of metal ions on zirconium(IV) iodomolybdate have...
The specific surface area (SSA) of metal oxides is pivotal for scaling of surface phenomena. For fer...
Three iron oxide materials have been studied for uptake of three anions (arsenate, phosphate and flu...
The formation of Fe oxides is influenced by pedogenic factors including ionic environments However,...
Typescript (photocopy).The adsorption of HSO4-, Cl- and I- from aqueous solutions was examined using...
Inner surface potential, one of the most important variables affecting the interfacial equilibrium o...
Ion exchange and surface complexation are the main models used to quantify the sorption processes. T...
The partitioning of solutes between the solid mineral and aqueous phase frequently controls the fate...
Detailed studies have been made on the ion exchange and sorptive properties of aqueous dispersions o...
The amphoteric ion exchange and sorptive properties of monoclinic zirconia are studied here in detai...
Research has been performed on the ion exchange and sorption processes which occur on the surfaces a...
One model system for the investigation of selectivity in inorganic ion exchangers is a group of syn...
The work described in this thesis consists of investigations into the sorptive behaviour of magnetit...
Hydrated oxides such as HAO,\u27HFO, goethite, and BA40 are prevalent in soils and sediments as disc...
Iron (oxyhydr)oxide (FeOOH) minerals play important roles in various natural, technological and soci...
349-350Distribution coefficients of a large number of metal ions on zirconium(IV) iodomolybdate have...
The specific surface area (SSA) of metal oxides is pivotal for scaling of surface phenomena. For fer...
Three iron oxide materials have been studied for uptake of three anions (arsenate, phosphate and flu...
The formation of Fe oxides is influenced by pedogenic factors including ionic environments However,...
Typescript (photocopy).The adsorption of HSO4-, Cl- and I- from aqueous solutions was examined using...
Inner surface potential, one of the most important variables affecting the interfacial equilibrium o...
Ion exchange and surface complexation are the main models used to quantify the sorption processes. T...
The partitioning of solutes between the solid mineral and aqueous phase frequently controls the fate...