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Mineral component

Location AI2O3 SiOj TiO Loss on ignition (LOI), % Mineral components... [Pg.132]

In ceramics, plasticity is usually evaluated by means of the water of plasticity. Values for the common clay minerals are given in Table 1. Each clay mineral can be expected to show a range of values because particle size, exchangeable ion composition, and crystallinity of the clay mineral also exert an influence. Nonclay mineral components, soluble salts, organic compounds, and texture can also affect the water of plasticity. [Pg.204]

Variety of biochemical composition and physical features of milk, as well as compound forms of mineral components foreordain necessity to develop the analytical procedures, in which initial sample state suffers minimum change. Absence of dried milk reference standai ds (RSMs) is an obstacle to use nondestructive XRF for solving the given analytical task. In this communication results of nondestmctive x-ray fluorescence determination of Na, Mg, Al, Si, P, S, Cl, K, Ca, Cr, Mn, Fe, Ni, Cu, Zn, Rb, Sr, Zr in dried milk powders of limited mass (less than 2 g), obtained with using plant RSMs to calibrate, ai e discussed. [Pg.224]

NOTE For any boiler, the maximum recommended tolerance for deposit thickness can be related to a weight of deposit per unit area clearly, the weight will vary dependent on the density of the deposit. Typically, deposit densities vary between 2.3 and 5.7 g/cm3. The densities of calcite and magnetite (which are two common mineral components of deposits) are 2.71 and 5.17 g/cm3, respectively. Table 4.2 assumes an average deposit density of 3.5 g/cm3. [Pg.164]

TPN is used to prevent nitrogen and weight loss or to treat negative nitrogen (mineral component in protein and amino acids) balance (a situation in which more nitrogen is used by the body than is taken in) in the following situations ... [Pg.645]

Xenobiotics exist not only in the free state but also in association with organic and mineral components of particles in the water mass, and the soil and sediment phases. This association is a central determinant of the persistence of xenobiotics in the environment, since the extent to which the reactions are reversible is generally unknown. Such residues may therefore be inaccessible to microbial attack and apparently persistent. This is a critical factor in determining the effectiveness of bioremediation (Harkness et al. 1993). Although the most persuasive evidence for the significance of reduced bioavailability comes from data on the persistence of agrochemicals in terrestrial systems (Calderbank 1989), the principles can be translated with modification to aquatic and sediment phases that contain organic matter that resembles structurally that of soils. [Pg.205]

V. G. Fil, L. A. Ezlova, V. D. Kovalenko, D. A. Kostenko, B. I. Navrot-skij, V. V. Koptenko, and S. P. Dombrovskaya. Plugging solution for oil and gas wells—comprises Portland cement, asbestos reinforcing component, mixture of sodium chloride and sulphate mineral component, fly ash and water, (rus). Patent RU 2013525-C, 1994. [Pg.386]

The main mineral components of baghouse dust are silica, clay, some resin evaporation residue, and metal fines. Its composition is related to the way it is collected. Shake-out dust mainly contains silica and clay. Metal fines may be present in the dust collected from areas used for cleaning, grinding, and melting processes. [Pg.167]

In practice, evaluating the wettability of a soil is far more uncertain, because soil is a mixture of gravel, sand, silt, and clay particles, as well as other chemical precipitates. The mineral components of soil particles include quartz, feldspar, carbonates, and clay. These components have different wettability by water and oil. Therefore, the retention of oil or water in a soil matrix is heterogeneous and variable. The general wettability of soil or liquid retention in a soil is reported on a statistical basis. [Pg.697]

Thiel G, Danzer K (1997) Direct analysis of mineral components in wine by inductively coupled plasma optical emission spectrometry (ICP-OES). Fresenius J Anal Chem 357 553... [Pg.241]

Figure 3. Positive TOF-SIMS spectra of various mineral components silylated with CH3Si(OC2H5)3. Figure 3. Positive TOF-SIMS spectra of various mineral components silylated with CH3Si(OC2H5)3.
Strusinska D, Mierzejewska J and Skok A (2004), Concentration of mineral components, beta-carotene, vitamins A and E in cow colostrum and milk when using mineral-vitamin supplements , Medycyna Weterynaryjna, 60, 202-206. [Pg.115]

Mineral components are distributed among the mass of actual mineral in the system and the amount required to make up the dissolved species. In a system containing a mole of quartz, for example, there is (in the absence of other silica-bearing components) somewhat more than a mole of component quartz. The additional component mass is required to make up species such as Si02(aq) and IhSiO. Since vy moles of mineral component k go into making up each mole of secondary species j, mass balance is expressed as,... [Pg.43]

Here, we arbitrarily specify the amounts of the minerals that coexist with the fluid. The amount chosen (in this case, 1 cm3), of course, has no effect on the predicted fluid composition. We set free constraints because we wish to specify amounts of actual minerals (w ), rather than mineral components (M ). [Pg.96]

The model then swaps aqueous species Aj into the basis locations Ak held by the mineral components. The technique for swapping the basis is explained in Chapter 5, and a method for selecting an appropriate species Aj to include in the basis is described in Chapter 4. When the procedure is complete, the equilibrium system contains only the original fluid. [Pg.199]

In the flow-through model, any mineral mass present at the end of a reaction step is sequestered from the equilibrium system to avoid back-reaction. At the end of each step, the model eliminates the mineral mass (including any sorbed species) from the equilibrium system, keeping track of the total amount removed. To do so, it applies Equation 13.11 for each mineral component and sets each nk to a vanishingly small number. It is best to avoid setting nk to exactly zero in order to maintain the mineral entries Ak in the basis. The model then updates the system composition according to Equations 13.5-13.7 and takes another reaction step. [Pg.199]


See other pages where Mineral component is mentioned: [Pg.402]    [Pg.182]    [Pg.199]    [Pg.205]    [Pg.272]    [Pg.1787]    [Pg.1834]    [Pg.233]    [Pg.50]    [Pg.277]    [Pg.141]    [Pg.287]    [Pg.28]    [Pg.51]    [Pg.549]    [Pg.642]    [Pg.454]    [Pg.97]    [Pg.144]    [Pg.598]    [Pg.173]    [Pg.59]    [Pg.124]    [Pg.238]    [Pg.411]    [Pg.466]    [Pg.489]    [Pg.325]    [Pg.327]    [Pg.40]    [Pg.26]    [Pg.124]    [Pg.42]    [Pg.194]    [Pg.207]   
See also in sourсe #XX -- [ Pg.394 ]




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