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Analysis Iron content

Industrial Analysis UV/Vis molecular absorption is used for the analysis of a diverse array of industrial samples, including pharmaceuticals, food, paint, glass, and metals. In many cases the methods are similar to those described in Tables 10.6 and 10.7. For example, the iron content of food can be determined by bringing the iron into solution and analyzing using the o-phenanthroline method listed in Table 10.6. [Pg.397]

The molecular absoi ption spectra, registered at a lower temperature (e.g. 700 °C for iodide or chloride of potassium or sodium), enable one to find the absorbance ratio for any pair of wavelengths in the measurement range. These ratios can be used as a correction factor for analytical signal in atomic absoi ption analysis (at atomization temperatures above 2000 °C). The proposed method was tested by determination of beforehand known silicon and iron content in potassium chloride and sodium iodide respectively. The results ai e subject to random error only. [Pg.78]

Irrespectively of the iron content, the applied synthesis procedure yielded highly crystalline microporous products i.e. the Fe-ZSM-22 zeolite. No contamination with other microporous phases or unreacted amorphous material was detected. The SEM analysis revealed that size and morphology of the crystals depended on the Si/Fe ratio. The ZSM-22 samples poor in Fe (Si/Fe=150) consisted of rice-like isolated crystals up to 5 p. On the other hand the preparation with a high iron content (Fe=27, 36) consisted of agglomerates of very small (<0.5 p) poorly defined crystals. The incorporation of Fe3+ into the framework positions was confirmed by XRD - an increase of the unit cell parameters with the increase in the number of the Fe atoms introduced into the framework was observed, and by IR - the Si-OH-Fe band at 3620 cm 1 appeared in the spectra of activated Fe-TON samples. [Pg.114]

Fig. 6.3. Saturation indices of Amazon River water with respect to various minerals (left) calculated directly from a chemical analysis, and (right) computed assuming that equilibrium with kaolinite and hematite controls the fluid s aluminum and iron content. Fig. 6.3. Saturation indices of Amazon River water with respect to various minerals (left) calculated directly from a chemical analysis, and (right) computed assuming that equilibrium with kaolinite and hematite controls the fluid s aluminum and iron content.
On the basis of extensive past analysis the iron content of an homogeneous ore sample is accepted to be 19.85%. An analysis of seven samples gave an average of 20.06% Fe. Within what probability levels is a determinate error indicated in the analysis if the absolute standard deviation of the results is 0.14% ... [Pg.24]

If the analysis of a sample for iron content yields a mean result of 35.40% with a standard deviation of 0.30%, the size of the confidence interval will vary inversely with the number of measurements made. For two measurements, the confidence interval (90%) is... [Pg.630]

After analysis for iron content, a water sample was found to have a concentration of 4.62 ppm iron. How many milligrams of iron are contained in 100.0 mL of the water ... [Pg.177]

An iron content in some of the lithotype ashes was indicated by their brownish-red to dark earth brown colors. An x-ray fluorescence analysis (Table X) of the ash substantiated the presupposed presence of iron. Iron was generally found in all of the lithotypes. Detectable amounts of calcium were found in all the vitrains. [Pg.370]

These complexes are usually named as follows I, NADH-ubiquinone oxidoreductase II, succinate-ubiquinone oxidoreductase III, ubiquinol-cytochrome c oxidoreductase IV, cytochrome c oxidase. The designation complex V is sometimes applied to ATP synthase (Fig. 18-14). Chemical analysis of the electron transport complexes verified the probable location of some components in the intact chain. For example, a high iron content was found in both complexes I and II and copper in complex IV. [Pg.1021]

I.R. characterisation of the samples is carried out using the KBr technique. U.V. spectroscopy was used for the semi-quantitative determination of the amount of intracrystalline phthallocyanines, after dissolution of the zeolite in concentrated sulfuric acid (0.1 g of catalyst in 10 ml of concentrated H2SO4 for 4 h). The iron content of the samples is determined by chemical analysis. X-ray powder diffraction is used to ensure good crystallinity of the zeolite after the synthesis and purification procedures. [Pg.396]

Carpenter, C.E. and Clark, E. 1995. Evaluation of methods used in meat iron analysis and iron content of raw and cooked meats. J. Agric. Food Chem. 43 1824-1827. [Pg.906]

Lines of best fit for D2 of calculated vs. measured iron content computed from regression analysis at the... [Pg.414]

CQ—0,9 mm/s and 5 =0,32 mm/s) which corresponds to MgFe204 and is responsible for the rests of the initial catalyst. It takes in a spectrum approximately 7% from the common area. This essential reduction of a doublet area in comparison with a spectrum of the initial catalyst allows to conclude that during the synthesis MgFe204 undergoes complex structural and chemical transformations leading to Fe3C, and carbon nanotube and nanofibres formation. Also in examined spectrum there are two doublet subspectra which spectral parameters analysis allows to attribute them to two Fe2+ nonequivalent positions in formed Mgi xFxO solid solution. The intensities ratio of these two doublets in Mossbauer spectrum allows to find the amount of the iron content in solid solution as x=0.15 [4]. Central singlet (with 5 = 0,07 mm/s) corresponds to y-Fe (C) with concentration of carbon in a sample about 1,5 % [5]. [Pg.513]

Table 8. Iron content in adrenodoxin determined by EPR and chemical analysis (68)... Table 8. Iron content in adrenodoxin determined by EPR and chemical analysis (68)...
Analysis of numerous data on the iron content of volcanogenic waters in the Kurile Islands (Markhinin, 1967a) permits drawing the following conclusion within limits of acidity of the waters from 0 to 2.5, the Fe content ranges from a few units to 250 mg/1, and Fe " " from traces to 200 mg/1. However, waters are encountered which contain 500-700 mg/1 Fe (Upper... [Pg.147]


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See also in sourсe #XX -- [ Pg.354 ]




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Iron content

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