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Oxidants, water-soluble organic matter

Chemical oxidation reactions and radical-induced hydrophobic-to-hydrophilic aging processes tend to increase the water solubility of OAs and, therefore, are thought to enhance the activity of atmospheric OAs as cloud condensation nuclei (CCN). As discussed by Gysel et al. (2004), at 75-90% of relative humidity (RH) the inorganic fraction dominates the water uptake (59-80%). Nevertheless, under the same conditions of RH, between 20% and 40% of total particulate water is associated with water-soluble organic matter. More data concerning the multiphase aerosol and cloud processes, as well as the chemical reactivity of carbonaceous aerosol components, have been compiled in the reviews of Jacobson et al. (2000), Kanakidou et al. (2005), and Poschl (2005) (and references therein). [Pg.462]

In contrast to NH4, NOi—the thermodynamically favoured species in oxygenated waters—is anionic, soluble and not retained in soils. Therefore, NOf from rainwater or fertilizers, or derived from the oxidation of soil organic matter... [Pg.167]

In the field of water analysis the interest is in differentiation between soluble and particulate chromium as well as between the two main oxidation states. The system Cr(III)/Cr(VI) is subject to redox reactions, especially in the presence of oxygen and/or organic materials. As soon as possible after its collection, water samples should be filtered if metal speciation is to be studied in order to avoid any remobilization of metals bound or sorbed to particulate matter. While pressure filtration offers advantages in terms of speed of filtration it may contribute to enhanced soluble organic matter by rupture of phytoplankton cells. [Pg.687]

The major raw materials used at present for the production of alumina are bauxites, which are found in the following mineral forms gibbsite (Al(OH)3), boehmite (AlO OH), and diaspore (AlO OH). The major impurities are the oxides of iron, silicon, and titanium, and organic compounds, all of which must be removed before alumina is suitable for aluminum production. The process objectives are, therefore, separation of impurities and compound production in the present case. Bauxite is first dried to facilitate grinding, destroy organic matter, and oxidize the associated ferrous minerals to the ferric state. The temperature of drying is not allowed to exceed 150 °C, because at higher temperature a part of the combined water is expelled and the solubility is affected adversely. [Pg.484]

As it was not known what kind of organic matter acts as the major ligand for chromium in seawater, Nakayama et al. [38] used ethylene diaminetetra-acetic acid (EDTA) and 8-quinolinol-4-sulfuric acid to examine the collection and decomposition of organic chromium species, because these ligands form quite stable water-soluble complexes with chromium (III), although they are not actually present in seawater. Both of these chromium (III) chelates are stable in seawater at pH 8.1 and are hardly collected with either of the hydrated oxides. The organic chromium species were then decomposed to inorganic... [Pg.69]

Total metal Water-soluble and exchangeable Organic matter Hydrated iron oxides Mineral soil matter... [Pg.159]

The pE-range 2 is representative of many ground and soil waters where 02 has been consumed (by degradation of organic matter), but SO is not yet reduced. In this range soluble Fe(II) and Mn(II) are present their concentration is redox-buffered because of the presence of solid Fe(III) and Mn(IIUV) oxides. [Pg.331]

Phosphate is remineralized during the oxidation of organic matter and dissolution of hard parts, such as bones and teeth, that are composed of the minerals hydroxyapatite and fluoroapatite. Unlike the other products of remineralization, pore-water phosphate concentrations are regulated only by mineral solubility, such as through vivianite (iron phosphate) and francolite (carbonate fluoroapatite). Redox reactions are not significant because phosphorus exists nearly entirely in the h-5 oxidation state. [Pg.319]

D. The acid-soluble inorganic matter and the organic material can probably be dissolved (and oxidized) together by wet ashing with HNOa + H2S04 in a Teflon-lined bomb in a microwave oven. The insoluble residue should be washed well with water and the washings combined with the acid solution. After the residue has been dried, it can be fused with one of the fluxes in Table 28-6, dissolved in dilute acid, and combined with the previous solution. [Pg.770]


See other pages where Oxidants, water-soluble organic matter is mentioned: [Pg.361]    [Pg.401]    [Pg.3]    [Pg.142]    [Pg.249]    [Pg.64]    [Pg.39]    [Pg.199]    [Pg.273]    [Pg.479]    [Pg.102]    [Pg.436]    [Pg.215]    [Pg.312]    [Pg.145]    [Pg.404]    [Pg.538]    [Pg.739]    [Pg.157]    [Pg.138]    [Pg.141]    [Pg.402]    [Pg.152]    [Pg.286]    [Pg.363]    [Pg.81]    [Pg.362]    [Pg.117]    [Pg.62]    [Pg.93]    [Pg.81]    [Pg.130]    [Pg.44]    [Pg.357]    [Pg.380]    [Pg.802]    [Pg.490]    [Pg.733]    [Pg.159]    [Pg.494]   


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Organic oxidant

Organic oxidation

Organic soluble

Oxidant water

Oxidation organic matter

Solubility organic

Soluble Organic Matter

Soluble matter

Water organic matter

Water oxidation

Water-soluble organic matter

Water-soluble organics

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