Optimisation of the anaerobic digestion of agricultural resources.

Minerals and organic matter (OM) may form intricate associations via myriad interactions. In soils, the associations of OM with mineral surfaces are mainly investigated because of their role in determining the long-term retention of OM. OM “must decay in order to release the energy and nutrients that drive live processes all over the planet” ( Janzen, 2006 ). Thus, the processes and mechanisms that retain OM in soil are a central concern to very different branches of environmental research. An agronomist may want to synchronize periods of high nutrient and energy release with the growth stages of a crop. An environmental chemist may wish to either immobilize an organic soil contaminant or enhance its decomposition into less harmful metabolites, while climate scientists need to understand the processes that mediate the production of potent greenhouse gases from decomposing OM. Associations of OM with pedogenic minerals (henceforth termed mineral–organic associations (MOAs)) are known to be key controls in these and many other processes. Here we strive to present an overview of the current knowledge on MOAs and identify key questions and future research needs.

Chapter One – Mineral–Organic Associations: Formation, Properties, and Relevance in Soil Environments

Common to liquids, solids and substances in between the former two is that if a stress is applied to them, they will strain. Stress may be visualized by placing a small amount of fluid between two parallel plates. When one plate slides over the other, forces act on the fluid dependent upon the rate of the plate movement. This causes a shear stress on the liquid. Recall laminar flow of fluids through a tubular vessel. Strain is the response to the stress. If solids are elastic, they deform and return to their original shape. Since fluids are not elastic and, hence, viscous, their deformation is irreversible.

Introduction to rheology

The experimental conditions were optimized for the synthesis of amorphous SiO2 particles by the reaction of neutralization of sodium silicate solution with H2SO4 solution Amorphous SiO2 particles were characterized by XRD, FT-IR, FE-SEM, EDS and microelectrophoresis The amorphous peak was located at 2θ = 218o in the XRD pattern Primary SiO2 particles were ~ 15 to ~ 30 nm in size and they aggregated into bigger particles Amorphous SiO2 particles showed a specific surface area up to 130 m2g-1, dependent on the parameters of the precipitation process The EDS spectrum of amorphous SiO2 particles did not show contamination with sulfate or other ions, which cannot be excluded in traces pHzpc =17 was obtained by microelectrophoresis

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Precipitation of amorphous SiO2 particles and their properties

The technology of extracting vanadium from stone coal in China: History, current status and future prospects

An environmentally-friendly technology of vanadium extraction from stone coal

The effect of sodium alginate on the flotation separation of scheelite from calcite and fluorite

Investigations on the extraction of molybdenum and vanadium from ammonia leaching residue of spent catalyst

http://www.ysxbcn.com/down/upfile/soft/20110531/29-p1149.pdf

Guofan Zhang

Papers

An environmentally-friendly technology of vanadium extraction from stone coal

The effect of sodium alginate on the flotation separation of scheelite from calcite and fluorite

Investigations on the extraction of molybdenum and vanadium from ammonia leaching residue of spent catalyst

Effect of surface dissolution on flotation separation of fine ilmenite from titanaugite

Kinetics of saprolitic laterite leaching by sulphuric acid at atmospheric pressure