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		<title>The Way PRDX4 Made Me Rich And Famous - Історія редагувань</title>
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		<updated>2026-05-24T04:37:26Z</updated>
		<subtitle>Історія редагувань цієї сторінки в вікі</subtitle>
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		<id>http://istoriya.soippo.edu.ua/index.php?title=The_Way_PRDX4_Made_Me_Rich_And_Famous&amp;diff=115656&amp;oldid=prev</id>
		<title>Cell0linda: Створена сторінка: 6 ?): (a) the average Si��O distance in the silicate tetrahedra plotted ... Fig. 7 ?(b) shows that for the Ca��O polyhedra that are present in the 35 ph...</title>
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				<updated>2016-11-21T19:15:22Z</updated>
		
		<summary type="html">&lt;p&gt;Створена сторінка: 6 ?): (a) the average Si��O distance in the silicate tetrahedra plotted ... Fig. 7 ?(b) shows that for the Ca��O polyhedra that are present in the 35 ph...&lt;/p&gt;
&lt;p&gt;&lt;b&gt;Нова сторінка&lt;/b&gt;&lt;/p&gt;&lt;div&gt;6 ?): (a) the average Si��O distance in the silicate tetrahedra plotted ... Fig. 7 ?(b) shows that for the Ca��O polyhedra that are present in the 35 phases, there is a good linear correlation between the average Ca��O distance and the average Ca��O coordination; the linear regression equation is given in equation (18) (r 2 = 0.88), which should provide a useful guide for modelling studies, as indeed should the maximum and minimum values. A good linear correlation also exists between the volume of the Ca��O polyhedra and the average Ca��O coordination number [Fig. 7 ? c, equation (19); r 2 = 0.90]. 5.2. Structural models for C-S-H(I) derived using crystal-chemical and geometrical reasoning ? It is noted in ��2 that refinements that involve even quite small changes in lattice parameters can lead to crystal-chemically implausible distances and coordinations if [http://www.selleckchem.com/products/ipi-145-ink1197.html Duvelisib cost] atomic coordinates are not included in the refinement, which has so far proved to be impossible because of the lack of information in the diffraction data. The problem with a change in the c parameter resulting in expansion or compression of the central Ca��O core of the structure is resolved in this work by recalculation of the z/c coordinate of the atoms in the asymmetric unit so that the relative z positions of the atoms in the central Ca��O core are unaffected by the change. The details of the 16 model structures that [http://en.wikipedia.org/wiki/PRDX4 PRDX4] are developed in this section are deposited2 in a CIF file. The name of the datablock for each structure starts with ��T�� to denote ��tobermorite-based structure��; a number or ���ޡ� that denotes the mean length of the silicate chains; and an underscore. The rest of the datablock name can be understood after reading ��5 and using the following key: 11 or 14 = any infinite-chain part of the model structure has a layer spacing of approximately 11 or 14??; s = staggered; a = adjacent; o = ortho; c = clino; noCa = there are no interlayer Ca2+ ions; LS1 = the first of two alternative layer spacings; LS2 = the second of two alternative layer spacings. Datablock names from the CIF are referred to throughout the text and figure captions. 5.2.1. Dimeric structures that are based on ortho?tobermorite ? The end-members of the dotted line on Fig. 5 ? [i.e. equation (16)] are a structure with infinite silicate chains and no interlayer Ca at Ca/Si = , and an entirely [http://www.selleckchem.com/products/Bleomycin-sulfate.html Bleomycin] dimeric structure at Ca/Si = , which will be referred to respectively as T�� and T2 (after Richardson &amp;amp; Groves, 1992a ?). It is therefore necessary to first develop models for these two end-member structures. All previous studies, including those discussed in ��2, have concerned orthotobermorite structures, which as a consequence were used as a starting point in this work. Fig. 8 ? shows two hypothetical structures for a dimer that were established as having interlayer Ca atoms in the most plausible positions.&lt;/div&gt;</summary>
		<author><name>Cell0linda</name></author>	</entry>

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