253 research outputs found
Possible Correction of Preferential Orientation of Crystallites in Quantitative X-ray Determination by Means of Basal Reflections
In a previously published work1 we have described a method by which the
intensity of an X-ray reflection that has been strengthened by preferential crystallite orientation can be corrected by measuring its ratio to the intensity of a reflection that is weakened by the same effect. In this way the intensity can be corrected to that given by a sample with a selected define degree of preferential orientation and then applied in quantitative analysis
The Crystal and Molecular Structure of Phthalyl-Urea
Using the methods of X-ray analysis we have shown that phthalyl-urea has the structure given by the formula (I). Thus we have confirmed the result previously obtained by V. Hah
Correction of Preferential Crystallite Orientation in X-ray Quantitative Analysis. Quantitative X:ray Determination of Ca (OH)2
The work deals with the problem of preferential orientation
of crystallites in quantitafrwe X-ray analysis. A n ew method has
been worked out theoretically. and practically for the correction
of reflection intensities from \u27polycrystalline samples w ith preferentially
oriented crystallites. Equations are included for the
determination of correction parameters. Practical a pplication of
the new method is demonstrated on quantitative X-ray analysis of
calcium hydroxide. The work includes a calibration graph for the
determination of coefficient a, comparing corrected and uncorrecte
d values of analytical intensities of Ca(OH)2
X-Ray-Quantitative Analysis of Multiphase Systems
The equation by which the X-ray diffra cted intensity of one
component is related to the concentrations of all Ā· components is
unsuitable for studying multiphase systems without an internal
standard. It is shown that even in such a case the concentration of
one component can be expressed as a function of the characteristic
X-ray diffracted intensities of all components of a multiphase
system. One of them is chosen , at will, as the standard
An X-ray and Proton Magnetic Resonance Study of the Dehydration and Deuteration of Borax, Na2[B40s(OH)4] Ā· 8 H20
A quantitative powder-x-ray analysis was developed for
this case by which it was shown that carefully prepared borax
dehydrates directly into an unhydrous amorphous phase. Eight
molecul es of water are quantitatively lost on complete dehydration
(below 50Ā°C) as required by the structural formula.. The proton
m agnetic resonance results agree with these findings showing also
that the spectrum due to OH-groups changes considerably on
dehydration. This was used ~n following deuteration (solid/gas)
of dehydrated borax. The p.m.r. spectra, the x-ray di agrams,
and the measured regain indicate Ā·a reconshltution of the borax-
lattice towards the formula Na2,[B 40 5(0H) 4] ā¢ 8D 20
The Quantitative X-Ray Analysis of Bauxite. I. The System Hydrargillite-Boehmite-Goehtite-Haematite
A photographic X-Ray method for quantitative analysis of
the main four- component system in bauxites is described. The
required standard straigp.t lines are given. The use of the overl apping
haematite- goehtite line (d = 2.69 A a nd d = 2.67 A resp.) is
shown theoretically to be possible and is experimentally verified
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