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Mass balance analysis

Step 2 Mass Balance Analysis and Mechanistic Studies... [Pg.151]

Scheme 2, vide infra for characterization of these structures) [15]. At an intermediate temperature of 500 °C, a 65/35 mixture of these two complexes is obtained [16]. The proposed structure is further confirmed by the mass balance analysis since hydrolysis or ethanolysis of the resulting solid yields the complementary amounts of neopentane, these are 2 and 3 equiv. of neopentane/Ta for [(=SiO)2Ta(= CHlBu)(CH2fBu)] and [(=SiO)Ta(= CH(Bu)(CH2fBu)2], respectively. Moreover, elemental analysis provides further information indeed, 4.2 wt % of Ta grafted onto sihca partially dehydroxylated at 700 °C corresponds to 0.22 mmol of Ta/g of sofid [ 17,18]. This is comparable to the amount of silanol present on this support (0.26 mmol OH/g), which shows that most of them have reacted during grafting (as observed by IR spectroscopy). [Pg.155]

Yet, mass balance analysis should be checked thoroughly since there can be some deviations/exceptions depending on the support and the metal. For instance, while the reaction of [Zr(CH2fBu)4] with Si02-(5oo) generates a monosiloxy species, its reaction with a MCM-41 material partially dehydroxylated at 500 °C yields a bissiloxy surface complex [21], and the reaction... [Pg.155]

Heat and Mass Balance Analysis of the Process Flow Sheet..141... [Pg.127]

Heat/mass balance analysis of the process flow sheet... [Pg.139]

Small hospital in a small urban catchment area a local mass balance analysis of micro- and macropoUutant loads can provide useful information about the contribution of the different users. Environmental risk assessment of the expected final effluent and analysis of the characteristics of the local receiving water body will guide selection of the advanced treatment sequence (MBR, ozone, UV). [Pg.164]

Similarly, [(Bu CH2)2Mo(=NAr)(=CHCMe2R)] reacts with the silanols group of a silica or a molecular silanol to yield [(=SiO)Mo(=NAr)(=CHCMe2R)(CH2Bu )] via direct electrophilic cleavage of the Mo-C bond, according to mass balance analysis, NMR and calculations (Scheme 2.27) [72, 73]. [Pg.49]

The rhenium perhydrocarbyl complex Re(=CBu )(= CHBu )(CH2Bu )2 reacts with the surface hydroxyl groups of a silica(7oo) (Scheme 2.29) to form a well-defined surface species, monografted on silica and containing one alkyl, one alkylidene and one alkylidyne ligands according to mass balance analysis IR, NMR, EXAFS [79-82] and calculations [83, 84]. [Pg.52]

Reverse osmosis for concentrating trace organic contaminants in aqueous systems by using cellulose acetate and Film Tec FT-30 commercial membrane systems was evaluated for the recovery of 19 trace organics representing 10 chemical classes. Mass balance analysis required determination of solute rejection, adsorption within the system, and leachates. The rejections with the cellulose acetate membrane ranged from a negative value to 97%, whereas the FT-30 membrane exhibited 46-99% rejection. Adsorption was a major problem some model solutes showed up to 70% losses. These losses can be minimized by the mode of operation in the field. Leachables were not a major problem. [Pg.426]

Recovery levels for individual organic compounds were, as expected, less than the values predicted by using the membrane solute rejections. Differences in the actual recovery and the theoretical recovery were partially due to adsorption losses. Mass balance analysis still indicated a deficiency in some cases. Rectification of the inconsistencies in these data was complicated by the limited water solubility of compounds chosen for study, the necessity of using a cosolvent in spiking, and, in particular, the limitations of the analytical procedures at these extremely low concentrations. [Pg.452]

System Energy Flow/Mass/Balance Analysis... [Pg.296]

Wania, R A global mass balance analysis of the source of perfluorocarboxy lie acids in the Arctic Ocean. Environ. Sci. TechnoL, 41 4529 535 (2007). [Pg.66]

From an environmental viewpoint, the mass balance analysis is aided by the calculation of two parameters (1,35) ... [Pg.206]

On a time series of Quaternary marine terraces in northern California, Brimhall et al. (1992) conducted the first mass balance analysis of soil formation over geologic time spans. This analysis provided quantitative data on well-known qualitative observations of soil formation (i) the earliest stages of soil formation (on timescales of 10 -10 yr) are visually characterized by loss of sedimentary/rock structure, the accumulation of roots and organic matter, and the reduction of bulk density and (ii) the later stages of soil development (>10 yr) are characterized by the accumulation of weathering products (iron oxides, silicate clays, and carbonates) and the loss of many products of weathering. [Pg.2267]

Jersak J., Amundson R., and BrimhaU G. (1995) A mass balance analysis of podzolization examples from the northeastern United States. Geoderma 66, 15-42. [Pg.2291]


See other pages where Mass balance analysis is mentioned: [Pg.153]    [Pg.156]    [Pg.166]    [Pg.81]    [Pg.220]    [Pg.564]    [Pg.583]    [Pg.587]    [Pg.212]    [Pg.57]    [Pg.315]    [Pg.151]    [Pg.187]    [Pg.187]    [Pg.146]    [Pg.81]    [Pg.84]    [Pg.94]    [Pg.1479]    [Pg.1481]    [Pg.2105]    [Pg.2269]    [Pg.2272]    [Pg.2381]   
See also in sourсe #XX -- [ Pg.154 , Pg.155 , Pg.156 , Pg.157 , Pg.158 , Pg.159 , Pg.160 ]

See also in sourсe #XX -- [ Pg.212 , Pg.285 ]

See also in sourсe #XX -- [ Pg.154 , Pg.155 , Pg.156 , Pg.157 , Pg.158 , Pg.159 , Pg.160 ]

See also in sourсe #XX -- [ Pg.15 ]




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