Characterization of Liquid-Solid Reactions. Hydrochloric Acid-Calcium Carbonate Reaction

1970 ◽  
Vol 9 (4) ◽  
pp. 589-596 ◽  
Author(s):  
B. B. Williams ◽  
J. L. Gidley ◽  
J. A. Guin ◽  
R. S. Schechter
2010 ◽  
Vol 198 (1) ◽  
pp. 131-134 ◽  
Author(s):  
Chengyu Wang ◽  
Cheng Piao ◽  
Xianglin Zhai ◽  
F. Neal Hickman ◽  
Jian Li

2010 ◽  
Vol 119 (6) ◽  
pp. 3560-3565 ◽  
Author(s):  
Jun Zhang ◽  
Bing Han ◽  
Ning-Lin Zhou ◽  
Jue Fang ◽  
Juan Wu ◽  
...  

2014 ◽  
Vol 602-603 ◽  
pp. 142-145
Author(s):  
Su Li ◽  
Jun Shou Li ◽  
Fang Zhao ◽  
Ming Yuan Wang ◽  
Xiao Juan Wu

On the basis of magnesiothermy, with Mg powder, TiO2 powder and B2O3 powder as mixed reactants, relatively pure TiB2 powder was prepared by self-propagating high temperature synthesis (SHS) after leached in diluted hydrochloric acid with the suitable concentration. The product after leached was examined by XRD for qualitative and quantitative analysis, SEM for morphology analysis and infrared spectroscopy for transmittance analysis. It was found that diluted hydrochloric acid could decrease most of the impurities, and the proportion of TiB2 phase in the product is more than 99%, which was hexagonal shape crystal with the grain size of 200-300 nm. Compare with the infrared spectrogram of the middle infrared spectral region of the product of before and after acid pickling, it was found that the transmittance of TiB2 is extremely low in the range of 2000-4000 cm-1, which can be excellent infrared absorption material in the corresponding wave band.


2012 ◽  
Vol 27 (4) ◽  
pp. 708-714 ◽  
Author(s):  
Xianyong Chen ◽  
Qin Tang ◽  
Daijun Liu ◽  
Weibing Hu ◽  
Youmeng Dan

2019 ◽  
Vol 9 (1) ◽  
Author(s):  
Michael B. Toffolo ◽  
Giulia Ricci ◽  
Luisa Caneve ◽  
Ifat Kaplan-Ashiri

Abstract In nature, calcium carbonate (CaCO3) in the form of calcite and aragonite nucleates through different pathways including geogenic and biogenic processes. It may also occur as pyrogenic lime plaster and laboratory-precipitated crystals. All of these formation processes are conducive to different degrees of local structural order in CaCO3 crystals, with the pyrogenic and precipitated forms being the least ordered. These variations affect the manner in which crystals interact with electromagnetic radiation, and thus formation processes may be tracked using methods such as X-ray diffraction and infrared spectroscopy. Here we show that defects in the crystal structure of CaCO3 may be detected by looking at the luminescence of crystals. Using cathodoluminescence by scanning electron microscopy (SEM-CL) and laser-induced fluorescence (LIF), it is possible to discern different polymorphs and their mechanism of formation. We were thus able to determine that pyrogenic calcite and aragonite exhibit blue luminescence due to the incorporation of distortions in the crystal lattice caused by heat and rapid precipitation, in agreement with infrared spectroscopy assessments of local structural order. These results provide the first detailed reference database of SEM-CL and LIF spectra of CaCO3 standards, and find application in the characterization of optical, archaeological and construction materials.


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