Superplasticizer to layered calcium aluminate hydrate interface characterized using model organic molecules

2018 ◽  
Vol 110 ◽  
pp. 52-69 ◽  
Author(s):  
Qirong Wang ◽  
Christine Taviot-Gueho ◽  
Fabrice Leroux ◽  
Karine Ballerat-Busserolles ◽  
Clémence Bigot ◽  
...  
2018 ◽  
Vol 47 (12) ◽  
pp. 4209-4218 ◽  
Author(s):  
H. Rojo ◽  
A. C. Scheinost ◽  
B. Lothenbach ◽  
A. Laube ◽  
E. Wieland ◽  
...  

Strong Se(-ii) sorption mainly in the interlayer of hemicarbonate (AFm-HC). Weak Se(-ii) sorption restricted to sorption sites on the surface of monocarbonate (AFm-MC).


2019 ◽  
Vol 188 ◽  
pp. 248-255 ◽  
Author(s):  
Guo-zhi Lu ◽  
Ting-an Zhang ◽  
Li-nan Ma ◽  
Yan-xiu Wang ◽  
Wei-guang Zhang ◽  
...  

1988 ◽  
Vol 136 ◽  
Author(s):  
G. J. McCarthy ◽  
P. J. Tikalsky ◽  
R. L. Carrasquillo ◽  
O. E. Manz ◽  
A. Thedchanamoorthy

ABSTRACTThe objective of this summary is to report on work in progress that is examining parameters, measurable through chemical and XRD analyses, that could indicate whether a fly ash will enhance, degrade or have no effect on the sulfate resistance of fly ash concrete.Mehta [1–4] has discussed the factors that contribute to attack of sulfates on fly ash concrete. As noted in his review paper on this subject in the preceding volume in this series [1], the agents responsible for concrete expansion and cracking are alumina-bearing hydrates, such as calcium monosulfoaluminate and calcium aluminate hydrate, that are attacked by the sulfate ion to form ettringite, calcium trisulfoaluminate. Acidic type interactions between sulfate ions and calcium hydroxide also lead to strength and mass loss.


2011 ◽  
Vol 41 (6) ◽  
pp. 571-578 ◽  
Author(s):  
Ju-hyuk Moon ◽  
Jae Eun Oh ◽  
Magdalena Balonis ◽  
Fredrik P. Glasser ◽  
Simon M. Clark ◽  
...  

Author(s):  
W. W. Barker ◽  
W. E. Rigsby ◽  
V. J. Hurst ◽  
W. J. Humphreys

Experimental clay mineral-organic molecule complexes long have been known and some of them have been extensively studied by X-ray diffraction methods. The organic molecules are adsorbed onto the surfaces of the clay minerals, or intercalated between the silicate layers. Natural organo-clays also are widely recognized but generally have not been well characterized. Widely used techniques for clay mineral identification involve treatment of the sample with H2 O2 or other oxidant to destroy any associated organics. This generally simplifies and intensifies the XRD pattern of the clay residue, but helps little with the characterization of the original organoclay. Adequate techniques for the direct observation of synthetic and naturally occurring organoclays are yet to be developed.


Author(s):  
Douglas L. Dorset

The quantitative use of electron diffraction intensity data for the determination of crystal structures represents the pioneering achievement in the electron crystallography of organic molecules, an effort largely begun by B. K. Vainshtein and his co-workers. However, despite numerous representative structure analyses yielding results consistent with X-ray determination, this entire effort was viewed with considerable mistrust by many crystallographers. This was no doubt due to the rather high crystallographic R-factors reported for some structures and, more importantly, the failure to convince many skeptics that the measured intensity data were adequate for ab initio structure determinations.We have recently demonstrated the utility of these data sets for structure analyses by direct phase determination based on the probabilistic estimate of three- and four-phase structure invariant sums. Examples include the structure of diketopiperazine using Vainshtein's 3D data, a similar 3D analysis of the room temperature structure of thiourea, and a zonal determination of the urea structure, the latter also based on data collected by the Moscow group.


Author(s):  
Y.G. Wang ◽  
H.Q. Ye ◽  
K.H. Kuo

A synthetic compound Ca4Al6SO16 (usually abbreviated as C4A3S) obtained by mixing CaO, A12O3 and CaSO4 powders and finally sintered at 1380°C is a cement with excellent hydraulicity and greatly expanding in application. It is hydralysed rapidly by water to form predominatly calcium aluminate hydrates and therefore unlikly to occur naturally, although structurally it may be regarded as an end member of the sodalite-hauynite series of naturally occuring minerals. C4A3S has a cubic structure with ao=9.19Å and space group . Fig.1 is the projection viewed down axis, in which there are two sets of 8C position in , namely CaI and CaII, occupied by the calcium atoms, respectively, and the ratio of occupations in these two sets of positions is about 3:1. This suggests that the calcium atoms can freely occupy these sites in various degrees and usually they almost locates on the CaI positions. A through-focus series of the lattice images were found in good agreement with the simulated ones. Each bright spot in the image taken at Scherzer defocus correspounds to a colunm of sulphur atom in the structural model (Fig.1).


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